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Yin S, Liu Y, Wei C, Zhu D. Comparing molecular signatures of dissolved organic matter (DOM) in four large freshwater lakes differing in hydrological connectivity to the Changjiang River. THE SCIENCE OF THE TOTAL ENVIRONMENT 2024; 946:174401. [PMID: 38964414 DOI: 10.1016/j.scitotenv.2024.174401] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 05/17/2024] [Revised: 06/28/2024] [Accepted: 06/29/2024] [Indexed: 07/06/2024]
Abstract
Freshwater lakes serve as active conduits for processing terrestrial dissolved organic matter (DOM), playing a crucial role in global carbon cycle. Little attention has been paid to how hydrological connectivity to a large river would affect the molecular signatures of DOM in lakes. Here, we systematically characterized and compared the molecular signatures of DOM in surface waters of four large freshwater lakes in the middle and lower Changjiang River basin that are directly connected to the river (Lake Dongting and Lake Poyang, referred to as Lakeconnected) or indirectly connected to the river (Lake Chao and Lake Tai, referred to as Lakenonconnected). The DOM in Lakeconnected was found to have similar total organic carbon (TOC)-normalized contents and characteristics of lignin phenols to the DOM in surface waters from the upstream Changjiang river, indicating allochthonous/terrestrial sources from riverine inputs. As indicated by the UV-vis and fluorescence analyses, the DOM in Lakeconnected overall had higher aromaticity and larger average molecular weight as well as stronger allochthonous feature compared to the DOM in Lakenonconnected. Consistently, the FT-ICR MS analysis revealed that the DOM in Lakeconnected had higher molecular diversity, higher unsaturation degree, and larger proportions of highly aromatic compounds. In contrast, the DOM in Lakenonconnected had larger proportions of lipids and peptide-like structures, but lower proportions of aromatic compounds, which could be ascribed to the enhanced autochthonous production and photodegradation due to pollution and eutrophication as well as longer water residence time. The results highlight the strong impacts of the hydrological connectivity to a large river on the molecular signatures of lake DOM. CAPSULE: The hydrological connectivity of the lakes to the Changjiang River has strong impacts on the molecular signatures of lake DOM.
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Affiliation(s)
- Shujun Yin
- School of Urban and Environmental Sciences, Key Laboratory of the Ministry of Education for Earth Surface Processes, Peking University, Beijing 100871, China
| | - Yafang Liu
- School of Urban and Environmental Sciences, Key Laboratory of the Ministry of Education for Earth Surface Processes, Peking University, Beijing 100871, China
| | - Chenhui Wei
- School of Urban and Environmental Sciences, Key Laboratory of the Ministry of Education for Earth Surface Processes, Peking University, Beijing 100871, China
| | - Dongqiang Zhu
- School of Urban and Environmental Sciences, Key Laboratory of the Ministry of Education for Earth Surface Processes, Peking University, Beijing 100871, China.
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2
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Rodrigues Matos R, Jennings EK, Kaesler J, Reemtsma T, Koch BP, Lechtenfeld OJ. Post column infusion of an internal standard into LC-FT-ICR MS enables semi-quantitative comparison of dissolved organic matter in original samples. Analyst 2024; 149:3468-3478. [PMID: 38742449 DOI: 10.1039/d4an00119b] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 05/16/2024]
Abstract
Ultrahigh resolution mass spectrometry hyphenated with liquid chromatography (LC) is an emerging tool to explore the isomeric composition of dissolved organic matter (DOM). However, matrix effects limit the potential for semi-quantitative comparison of DOM molecule abundances across samples. We introduce a post-column infused internal standard (PCI-IS) for reversed-phase LC-FT-ICR MS measurements of DOM and systematically evaluate matrix effects, detector linearity and the precision of mass peak intensities. Matrix effects for model compounds spiked into freshwater DOM samples ranging from a headwater stream to a major river were reduced by 5-10% for PCI-IS corrected mass peak intensities as compared to raw (i.e., untransformed) intensities. A linear regression of PCI-IS corrected DOM mass peak intensities across a typical DOM concentration range (2-15 mg dissolved organic carbon L-1) in original, non-extracted freshwater samples demonstrates excellent linearity of the detector response (r2 > 0.9 for 98% of detected molecular formulas across retention times). Importantly, PCI-IS could compensate for 80% of matrix effects across an environmental gradient of DOM composition from groundwater to surface water. This enabled studying the ionization efficiency of DOM isomers and linking the observed differences to the biogeochemical sources. With PCI-IS original, non-extracted DOM samples can be analysed by LC-FT-ICR MS without carbon load adjustment, and mass peak intensities can be reliably used to semi-quantitatively compare isomer abundances between compositionally similar DOM samples.
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Affiliation(s)
- Rebecca Rodrigues Matos
- Department of Environmental Analytical Chemistry, Helmholtz Centre for Environmental Research - UFZ, Permoserstr. 15, 04318 Leipzig, Germany.
| | - Elaine K Jennings
- Department of Environmental Analytical Chemistry, Helmholtz Centre for Environmental Research - UFZ, Permoserstr. 15, 04318 Leipzig, Germany.
| | - Jan Kaesler
- Department of Environmental Analytical Chemistry, Helmholtz Centre for Environmental Research - UFZ, Permoserstr. 15, 04318 Leipzig, Germany.
| | - Thorsten Reemtsma
- Department of Environmental Analytical Chemistry, Helmholtz Centre for Environmental Research - UFZ, Permoserstr. 15, 04318 Leipzig, Germany.
- Institute of Analytical Chemistry, University of Leipzig, 04103 Leipzig, Germany
| | - Boris P Koch
- Alfred-Wegener-Institute Helmholtz Centre for Polar and Marine Research, Ecological Chemistry, Am Handelshafen 12, 27570 Bremerhaven, Germany
- Hochschule Bremerhaven, University of Applied Sciences, An der Karlstadt 8, 27568 Bremerhaven, Germany
| | - Oliver J Lechtenfeld
- Department of Environmental Analytical Chemistry, Helmholtz Centre for Environmental Research - UFZ, Permoserstr. 15, 04318 Leipzig, Germany.
- ProVIS-Centre for Chemical Microscopy, Helmholtz Centre for Environmental Research - UFZ, Permoserstr. 15, 04318 Leipzig, Germany
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3
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Zhou X, Ma A, Chen X, Zhang Q, Guo X, Zhuang G. Climate Warming-Driven Changes in the Molecular Composition of Soil Dissolved Organic Matter Across Depth: A Case Study on the Tibetan Plateau. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2023; 57:16884-16894. [PMID: 37857299 DOI: 10.1021/acs.est.3c04899] [Citation(s) in RCA: 1] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 10/21/2023]
Abstract
Dissolved organic matter (DOM) is critical for soil carbon sequestration in terrestrial ecosystems. DOM molecular composition varies with soil depth. However, the spatial heterogeneity of depth-dependent DOM in response to climate warming remains unclear, especially in alpine ecosystems. In this study, the DOM of alpine meadow soil samples was characterized comprehensively by using spectroscopy and mass spectrometry, and open-top chambers (OTCs) were employed to simulate warming. It was found that climate warming had the greatest impact on the upper layer (0-30 cm), followed by the lower layer (60-80 cm), while the middle layer (30-60 cm) was the most stable among the three soil layers. The reasons for the obvious changes in DOM in the upper and lower layers of soil were further explained based on biotic and abiotic factors. Specifically, soil nutrients (NH4+-N, NO3--N, TC, and TP) affected the molecular composition of DOM in layer L1 (0-15 cm), while pH affected layer L5 (60-80 cm). Gemmatimonadetes, Proteobacteria, and Actinobacteria played important roles in the composition of DOM in the L5 layer (60-80 cm), while the dominant fungal groups affecting the DOM composition increased in the L1 layer (0-15 cm) under warming. In summary, this research has contributed to a deeper understanding of depth-dependent changes in DOM molecular composition in alpine ecosystems.
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Affiliation(s)
- Xiaorong Zhou
- Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
- College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China
| | - Anzhou Ma
- Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
- College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China
| | - Xianke Chen
- Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
- College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China
- Sino-Danish College of University of Chinese Academy of Sciences, Beijing 101400, China
- Sino-Danish Center for Education and Research, Beijing 101400, China
| | - Qinwei Zhang
- Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
- College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China
| | - Xiaowei Guo
- Key Laboratory of Adaptation and Evolution of Plateau Biota, Northwest Institute of Plateau Biology, Chinese Academy of Sciences, Xining 810008, China
| | - Guoqiang Zhuang
- Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
- College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China
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4
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Song X, Zhao Y, Xie L, Zhang G, Wei Z, Gao W, Dong G, Li J. Origin, distribution and spatial characteristics of dissolved organic matter in the Heilongjiang River. JOURNAL OF ENVIRONMENTAL MANAGEMENT 2023; 345:118881. [PMID: 37659372 DOI: 10.1016/j.jenvman.2023.118881] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 05/18/2023] [Revised: 08/13/2023] [Accepted: 08/26/2023] [Indexed: 09/04/2023]
Abstract
The Heilongjiang River Basin is a vast area with significant DOM sources and composition differences. The mechanism of DOM degradation under spatial variation remains unclear. This research investigated the degradation characteristics of DOM in different watersheds of the Heilongjiang River. DOM levels were higher in midstream waters, while DOM degradation rates were higher in midstream and downstream waters. The parallel factor analysis (PARAFAC) results showed that the upstream amino acid fraction was significantly depleted, the midstream was dominated by the degradation of DOM of terrestrial origin, and the downstream humic acid fraction was decreased considerably. Gene sequencing results indicated that the upstream, middle, and downstream water bodies' microbial community composition and structure differed significantly. The network analysis results revealed microorganisms in upstream water bodies mainly utilized amino acid-like substances and small molecule humic acids. Microorganisms in the middle and lower reaches of the water column were characterized by the utilization of humic acid-like fractions. In this study, we further screened the key driving microorganisms (e.g., Flavobacterium and Lacibacter) responsible for the difference in the DOM utilization function of upstream-to-midstream and midstream-to-downstream microorganisms in the Heilongjiang River. These findings will help identify the cycling process of DOM under spatial variation and predict the succession pattern of microbial communities.
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Affiliation(s)
- Xinyu Song
- Tianjin Key Laboratory of Animal and Plant Resistance, College of Life Sciences, Tianjin Normal University, Tianjin, 300387, China; Engineering Research Center of Agricultural Microbiology Technology, Ministry of Education & Heilongjiang Provincial Key Laboratory of Ecological Restoration and Resource Utilization for Cold Region & Key Laboratory of Molecular Biology, College of Heilongjiang Province & School of Life Sciences, Heilongjiang University, Harbin, 150080, China; College of Life Sciences, Northeast Agricultural University, Harbin, 150030, China
| | - Yue Zhao
- College of Life Sciences, Northeast Agricultural University, Harbin, 150030, China.
| | - Lina Xie
- Tianjin Key Laboratory of Animal and Plant Resistance, College of Life Sciences, Tianjin Normal University, Tianjin, 300387, China
| | - Guogang Zhang
- Tianjin Key Laboratory of Animal and Plant Resistance, College of Life Sciences, Tianjin Normal University, Tianjin, 300387, China
| | - Zimin Wei
- Tianjin Key Laboratory of Animal and Plant Resistance, College of Life Sciences, Tianjin Normal University, Tianjin, 300387, China.
| | - Wenfang Gao
- Tianjin Key Laboratory of Animal and Plant Resistance, College of Life Sciences, Tianjin Normal University, Tianjin, 300387, China
| | - Guanhong Dong
- Mudanjiang Natural Resources Comprehensive Survey Center, China Geological Survey, Mudanjiang, 157000, China
| | - Jinxuan Li
- Mudanjiang Natural Resources Comprehensive Survey Center, China Geological Survey, Mudanjiang, 157000, China
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5
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Wang S, Heal KV, Zhang Q, Yu Y, Tigabu M, Huang S, Zhou C. Soil microbial community, dissolved organic matter and nutrient cycling interactions change along an elevation gradient in subtropical China. JOURNAL OF ENVIRONMENTAL MANAGEMENT 2023; 345:118793. [PMID: 37619380 DOI: 10.1016/j.jenvman.2023.118793] [Citation(s) in RCA: 3] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 02/10/2023] [Revised: 07/27/2023] [Accepted: 08/09/2023] [Indexed: 08/26/2023]
Abstract
To identify possible dominating processes involved in soil microbial community assembly, dissolved organic matter (DOM) and multi-nutrient cycling (MNC) interactions and contribute to understanding of climate change effects on these important cycles, we investigated the interaction of soil chemistry, DOM components and microbial communities in five vegetation zones - ranging from evergreen broad-leaved forest to alpine meadow - along an elevation gradient of 290-1960 m in the Wuyi Mountains, Fujian Province, China. Soil DOM composition and microbial community assembly were characterized using Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS) and Illumina MiSeq high-throughput sequencing, respectively. Sloan's neutral model and the modified stochasticity ratio were used to infer community assembly processes. Key microbial drivers of the soil MNC index were identified from partial least squares path models. Our results showed that soil DOM composition is closely related to the vegetation types along an elevation gradient, the structure and composition of the microbial community, and soil nutrient status. Overall, values of the double bond equivalent (DBE), modified aromaticity index (AImod) increased, and H/C ratio and molecular lability boundary (MLBL) percentage decreased with elevation. Lignins/CRAM-like structures compounds dominated soil DOM in each vegetation type and its relative abundance decreased with elevation. Aliphatic/protein and lipids components also decreased, but the relative abundance of aromatic structures and tannin increased with elevation. The alpha diversity index of soil bacteria gradually decreased with elevation, with deterministic processes dominating the microbial community assembly in the highest elevation zone. Bacterial communities were conducive to the decomposition of labile degradable DOM compounds (H/C ≥ 1.5) at low elevation. In the cooler and wetter conditions at higher-elevation sites the relative abundance of potentially resistant soil DOM components (H/C < 1.5) gradually increased. Microbial community diversity and composition were important predictors of potential soil nutrient cycling. Although higher elevation sites have higher nutrient cycling potential, soil DOM was assessed to be a more stable carbon store, with apparent lower lability and bioavailability than at lower elevation sites. Overall, this study increases understanding of the potential linkage between soil microbial community, multiple nutrient cycling and DOM fate in subtropical mountain ecosystems that can help predict the effect of climate change on soil carbon sequestration and thus inform ecosystem management.
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Affiliation(s)
- Shuzhen Wang
- Co-Innovation Center for Sustainable Forestry in Southern China of Jiangsu Province, Key Laboratory of Soil and Water Conservation and Ecological Restoration of Jiangsu Province, Nanjing Forestry University, Nanjing, 210037, China; Forestry College, Fujian Agriculture and Forestry University, Fuzhou, 350002, Fujian Province, China
| | - Kate V Heal
- School of GeoSciences, The University of Edinburgh, Crew Building, Alexander Crum Brown Road, Edinburgh, EH9 3FF, UK
| | - Qin Zhang
- Forestry College, Fujian Agriculture and Forestry University, Fuzhou, 350002, Fujian Province, China
| | - Yuanchun Yu
- Co-Innovation Center for Sustainable Forestry in Southern China of Jiangsu Province, Key Laboratory of Soil and Water Conservation and Ecological Restoration of Jiangsu Province, Nanjing Forestry University, Nanjing, 210037, China
| | - Mulualem Tigabu
- Swedish University of Agricultural Sciences, Faculty of Forest Science, Southern Swedish Forest Research Centre, P.O. Box 190, SE-234 22, Lomma, Sweden
| | - Shide Huang
- National Observation and Research Station of Fujian Wuyishan Forest Ecosystem, Wuyishan, 354315, Fujian Province, China
| | - Chuifan Zhou
- Co-Innovation Center for Sustainable Forestry in Southern China of Jiangsu Province, Key Laboratory of Soil and Water Conservation and Ecological Restoration of Jiangsu Province, Nanjing Forestry University, Nanjing, 210037, China; Forestry College, Fujian Agriculture and Forestry University, Fuzhou, 350002, Fujian Province, China.
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6
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Glöckler D, Harir M, Schmitt-Kopplin P, Elsner M, Bakkour R. Selectivity of β-Cyclodextrin Polymer toward Aquatic Contaminants: Insights from Ultrahigh-Resolution Mass Spectrometry of Dissolved Organic Matter. Anal Chem 2023; 95:15505-15513. [PMID: 37831967 DOI: 10.1021/acs.analchem.3c01394] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 10/15/2023]
Abstract
Selectivity in solid-phase extraction (SPE) materials has become increasingly important for analyte enrichment in sensitive analytical workflows to alleviate detrimental matrix effects. Molecular-level investigation of matrix constituents, which are preferentially extracted or excluded, can provide the analytical chemist with valuable information to learn about their control on sorbent selectivity. In this work, we employ nontargeted Fourier transform ion cyclotron resonance mass spectrometry (FTICR MS) to elucidate the molecular chemodiversity of freshwater-derived dissolved organic matter (DOM) extracted by the selective model sorbent β-cyclodextrin polymer (β-CDP) in comparison to conventional, universal SPE sorbents (i.e., Oasis HLB, Supel-Select HLB, and LiChrolut EN). Statistical analysis of MS data corroborated the highly selective nature of β-CDP by revealing the extracted DOM spectra that are most dissimilar to original compositions. We found that its selectivity was characterized by pronounced discrimination against highly oxygenated and unsaturated DOM compounds, which were associated with the classes of lignin-like, tannin-like, and carboxylic-rich alicyclic molecules. In contrast, conventional sorbents excluded less highly oxygenated compounds and showed a more universal extraction behavior for a wide range of DOM compositional space. We lay these findings in a larger context that aids the analyst in obtaining an a priori estimate of sorbent selectivity toward any target analyte of interest serving thereby an optimization of sample preparation. This study highlights the great value of nontargeted ultrahigh-resolution MS for better understanding of targeted analytics and provides new insights into the selective sorption behavior of novel sorbents.
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Affiliation(s)
- David Glöckler
- TUM School of Natural Sciences, Chair of Analytical Chemistry and Water Chemistry, Technical University of Munich, Garching 85748 , Germany
| | - Mourad Harir
- Research Unit Analytical BioGeoChemistry, Helmholtz Munich, Neuherberg 85764, Germany
- TUM School of Life Sciences, Chair of Analytical Food Chemistry, Technical University of Munich, Freising 85354, Germany
| | - Philippe Schmitt-Kopplin
- Research Unit Analytical BioGeoChemistry, Helmholtz Munich, Neuherberg 85764, Germany
- TUM School of Life Sciences, Chair of Analytical Food Chemistry, Technical University of Munich, Freising 85354, Germany
| | - Martin Elsner
- TUM School of Natural Sciences, Chair of Analytical Chemistry and Water Chemistry, Technical University of Munich, Garching 85748 , Germany
| | - Rani Bakkour
- TUM School of Natural Sciences, Chair of Analytical Chemistry and Water Chemistry, Technical University of Munich, Garching 85748 , Germany
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7
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Zhao C, Hou Y, Wang Y, Li P, He C, Shi Q, Yi Y, He D. Unraveling the photochemical reactivity of dissolved organic matter in the Yangtze river estuary: Integrating incubations with field observations. WATER RESEARCH 2023; 245:120638. [PMID: 37742401 DOI: 10.1016/j.watres.2023.120638] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/16/2023] [Revised: 09/13/2023] [Accepted: 09/15/2023] [Indexed: 09/26/2023]
Abstract
Dissolved organic matter (DOM) sustains a substantial part of the organic matter transported seaward in large estuaries, where photochemical reactions significantly influence its transformation and fate. Irradiation experiments can provide valuable information on the photochemical reactivity (photo-labile, photo-resistant, and photo-product) of molecules. However, previous research paid less attention to exploring the controls of the initial DOM chemistry to irradiation experiments and examining the applicability of their further integration with field research. Here, we conducted irradiation experiments for samples from the freshwater and seawater endmember of the Yangtze River Estuary (YRE), which receives organic matter transport from the largest river in China, the Yangtze River. Molecules that occurred before and after irradiation experiments were characterized by the Fourier transform ion cyclotron resonance mass spectrometry. Results show that both post-irradiation samples have the lower aromaticity degree and reduced oxidation state, while the freshwater endmember sample exhibits more dramatic changes, indicating the controls of parent molecules to the effect of irradiation experiments. Integrating with the "molecular matching" approach, we compared the molecules occurring in field samples with the classified molecules (photo-resistant, photo-labile, and photo-product) acquired from performed irradiation experiments and correlated the relative intensity of photochemical reactivity types with salinity. When applying results from different experiments to conduct "molecular matching", the photo-resistant and photo-labile relative intensity possess consistently positive and negative trends with increasing salinity, respectively. This suggests their reliability for molecular matching applications, while the inconsistent trends for the photo-product relative intensity with salinity suggest its uncertainty in assessing the photo-induced effects. Moreover, the molecular composition within the photochemical reactivity types in field samples also evolved along the salinity gradient and showed similar trends with the DOM changes after experimental irradiation. Despite various factors influencing estimations, it is revealed that a fraction of aromatic molecules and majority of carboxyl-rich alicyclic molecules considered with biologically persistent nature in the YRE freshwater zone are simultaneously not susceptible to photochemical transformation to potentially constitute a long-term marine carbon sink. This study emphasizes the importance and limitations of the combination of field research and laboratory-controlled experiments to provide a better understanding of the crucial role of photochemical reactions in affecting carbon cycling in large estuaries.
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Affiliation(s)
- Chen Zhao
- Department of Ocean Science and Center for Ocean Research in Hong Kong and Macau, The Hong Kong University of Science and Technology, Hong Kong, China
| | - Yifu Hou
- Department of Ocean Science and Center for Ocean Research in Hong Kong and Macau, The Hong Kong University of Science and Technology, Hong Kong, China
| | - Yuntao Wang
- State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China
| | - Penghui Li
- School of Marine Sciences, Sun Yat-sen University, Zhuhai 519082, China; Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519082, China; Guangdong Provincial Key Laboratory of Marine Resources and Coastal Engineering, Zhuhai 519082, China
| | - Chen He
- State Key Laboratory of Heavy Oil Processing, China University of Petroleum, Changping District, Beijing 102249, China
| | - Quan Shi
- State Key Laboratory of Heavy Oil Processing, China University of Petroleum, Changping District, Beijing 102249, China
| | - Yuanbi Yi
- Department of Ocean Science and Center for Ocean Research in Hong Kong and Macau, The Hong Kong University of Science and Technology, Hong Kong, China.
| | - Ding He
- Department of Ocean Science and Center for Ocean Research in Hong Kong and Macau, The Hong Kong University of Science and Technology, Hong Kong, China; State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China; State Key Laboratory of Marine Pollution, City University of Hong Kong, Tat Chee Avenue, Kowloon, Hong Kong, China.
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8
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Li S, Harir M, Schmitt-Kopplin P, Machado-Silva F, Gonsior M, Bastviken D, Enrich-Prast A, Valle J, Hertkorn N. Distinct Non-conservative Behavior of Dissolved Organic Matter after Mixing Solimões/Negro and Amazon/Tapajós River Waters. ACS ES&T WATER 2023; 3:2083-2095. [PMID: 37588807 PMCID: PMC10425957 DOI: 10.1021/acsestwater.2c00621] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 12/07/2022] [Revised: 05/04/2023] [Accepted: 05/04/2023] [Indexed: 08/18/2023]
Abstract
Positive and negative electrospray ionization Fourier transform ion cyclotron resonance mass spectrometry and 1H NMR revealed major compositional and structural changes of dissolved organic matter (DOM) after mixing two sets of river waters in Amazon confluences: the Solimões and Negro Rivers (S + N) and the Amazon and Tapajós Rivers (A + T). We also studied the effects of water mixing ratios and incubation time on the composition and structure of DOM molecules. NMR spectra demonstrated large-scale structural transformations in the case of S + N mixing, with gain of pure and functionalized aliphatic units and loss of all other structures after 1d incubation. A + T mixing resulted in comparatively minor structural alterations, with a major gain of small aliphatic biomolecular binding motifs. Remarkably, structural alterations from mixing to 1d incubation were in essence reversed from 1d to 5d incubation for both S + N and A + T mixing experiments. Heterotrophic bacterial production (HBP) in endmembers S, N, and S + N mixtures remained near 0.03 μgC L-1 h-1, whereas HBP in A, T, and A + T were about five times higher. High rates of dark carbon fixation took place at S + N mixing in particular. In-depth biogeochemical characterization revealed major distinctions between DOM biogeochemical changes and temporal evolution at these key confluence sites within the Amazon basin.
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Affiliation(s)
- Siyu Li
- Research
Unit Analytical Biogeochemistry, Helmholtz
Munich, Ingolstaedter
Landstrasse 1, Neuherberg 85764, Germany
| | - Mourad Harir
- Research
Unit Analytical Biogeochemistry, Helmholtz
Munich, Ingolstaedter
Landstrasse 1, Neuherberg 85764, Germany
- Chair
of Analytical Food Chemistry, Technische
Universität München, Alte Akademie 10, Freising-Weihenstephan 85354, Germany
| | - Philippe Schmitt-Kopplin
- Research
Unit Analytical Biogeochemistry, Helmholtz
Munich, Ingolstaedter
Landstrasse 1, Neuherberg 85764, Germany
- Chair
of Analytical Food Chemistry, Technische
Universität München, Alte Akademie 10, Freising-Weihenstephan 85354, Germany
| | - Fausto Machado-Silva
- Program
in Geosciences—Environmental Geochemistry, Chemistry Institute, Fluminense Federal University, Niteroi 24020-141, Brazil
- Department
of Environmental Sciences, University of
Toledo, Toledo, Ohio 43606, United States
| | - Michael Gonsior
- Chesapeake
Biological Laboratory, University of Maryland
Center for Environmental Science, Solomons, Maryland 20688, United States
| | - David Bastviken
- Department
of Thematic Studies—Environmental Change, Linköping University, Linköping SE-581 83, Sweden
| | - Alex Enrich-Prast
- Department
of Thematic Studies—Environmental Change and Biogas Solutions
Research Center (BSRC), Linköping
University, Linköping SE-581 83, Sweden
- Multiuser
Unit of Environmental Analysis, University
Federal of Rio de Janeiro, Rio
de Janeiro 11070-100, Brazil
| | - Juliana Valle
- Research
Unit Analytical Biogeochemistry, Helmholtz
Munich, Ingolstaedter
Landstrasse 1, Neuherberg 85764, Germany
| | - Norbert Hertkorn
- Research
Unit Analytical Biogeochemistry, Helmholtz
Munich, Ingolstaedter
Landstrasse 1, Neuherberg 85764, Germany
- Department
of Thematic Studies—Environmental Change and Biogas Solutions
Research Center (BSRC), Linköping
University, Linköping SE-581 83, Sweden
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9
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Bai L, Liu X, Wu Y, Cheng H, Wang C, Jiang H, Wang A. Distinct seasonal variations of dissolved organic matter across two large freshwater lakes in China: Lability profiles and predictive modeling. JOURNAL OF ENVIRONMENTAL MANAGEMENT 2023; 339:117880. [PMID: 37080098 DOI: 10.1016/j.jenvman.2023.117880] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 01/07/2023] [Revised: 03/28/2023] [Accepted: 04/03/2023] [Indexed: 05/03/2023]
Abstract
Biological lability of dissolved organic matter (DOM) is a crucial indicator of carbon cycle and contaminant attenuation in freshwater lakes. In this study, we employed a multi-stage plug-flow bioreactor and spectrofluorometric indices to characterize the seasonal variations in DOM composition and lability across Poyang Lake (PY) and Lake Taihu (TH), two large freshwater lakes in China with distinct hydrological seasonality. Our findings showed that the export of floodplain-derived organics and river-lake interaction led to a remarkable increase in terrestrial aromatic and humic-like DOM with high molecular weights and long turnover times in PY. Consequently, the labile fraction was extremely low (average LDOC% of 3%) during the rising-to-flood season (spring and summer). Conversely, autochthonous production in TH considerably enriched semi-labile (average SDOC% of 26%) and biodegradable DOM (average BDOC% of 34%) during the phytoplankton bloom to post-bloom season (summer and autumn). This was reflected by the accumulation of low-light-absorbing and protein-like components with high biological and fluorescence indices. In the dry and non-bloom season (winter), the better preservation of humic substances maintained the high molecular weight and humic degree of DOM in PY, while the decay of aquatic plants strengthened autochthonous production, resulting in a similar BDOC% of PY samples (23%-34%) to TH samples (18%-33%). We further applied partial least squares regression using DOM optical indices as predictive proxies, which generated a greater prediction strength for BDOC% (R2 = 0.80) compared to SDOC% (R2 = 0.57) and LDOC% (R2 = 0.28). The regression model identified aromaticity (SUVA254) as the most effective and negative predictor and low molecular weight (A250/A365) as the highly and positively influential factor. Our study provides new evidence that the seasonality of DOM lability profiles is regulated by the trade-off between flow-related variation and phytoplankton production, and presents an approach to describe and predict DOM lability across freshwater lakes.
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Affiliation(s)
- Leilei Bai
- State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing, 210008, China
| | - Xin Liu
- College of Biology and Environment, Nanjing Forestry University, Nanjing, 210037, China
| | - Yuanqiang Wu
- College of Biology and Environment, Nanjing Forestry University, Nanjing, 210037, China
| | - Hongyu Cheng
- Zhengzhou Architectural Design Institute, Zhengzhou, 450001, China
| | - Changhui Wang
- State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing, 210008, China
| | - Helong Jiang
- State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing, 210008, China.
| | - Aijie Wang
- CAS Key Laboratory of Environmental Biotechnology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing, 100085, China.
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10
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Rožman M, Lekunberri I, Grgić I, Borrego CM, Petrović M. Effects of combining flow intermittency and exposure to emerging contaminants on the composition and metabolic response of streambed biofilm bacterial communities. THE SCIENCE OF THE TOTAL ENVIRONMENT 2023; 877:162818. [PMID: 36914121 DOI: 10.1016/j.scitotenv.2023.162818] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/05/2022] [Revised: 02/20/2023] [Accepted: 03/08/2023] [Indexed: 05/06/2023]
Abstract
Freshwater ecosystems are characterised by the co-occurrence of stressors that simultaneously affect the biota. Among these, flow intermittency and chemical pollution severely impair the diversity and functioning of streambed bacterial communities. Using an artificial streams mesocosm facility, this study examined how desiccation and pollution caused by emerging contaminants affect the composition of stream biofilm bacterial communities, their metabolic profiles, and interactions with their environment. Through an integrative analysis of the composition of biofilm communities, characterization of their metabolome and composition of the dissolved organic matter, we found strong genotype-to-phenotype interconnections. The strongest correlation was found between the composition and metabolism of the bacterial community, both of which were influenced by incubation time and desiccation. Unexpectedly, no effect of the emerging contaminants was observed, which was due to the low concentration of the emerging contaminants and the dominant impact of desiccation. However, biofilm bacterial communities modified the chemical composition of their environment under the effect of pollution. Considering the tentatively identified classes of metabolites, we hypothesised that the biofilm response to desiccation was mainly intracellular while the response to chemical pollution was extracellular. The present study demonstrates that metabolite and dissolved organic matter profiling may be effectively integrated with compositional analysis of stream biofilm communities to yield a more complete picture of changes in response to stressors.
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Affiliation(s)
- Marko Rožman
- Ruđer Bošković Institute, Bijenička cesta 54, 10000 Zagreb, Croatia; Catalan Institute for Water Research (ICRA), Emili Grahit 101, 17003 Girona, Spain.
| | - Itziar Lekunberri
- Catalan Institute for Water Research (ICRA), Emili Grahit 101, 17003 Girona, Spain
| | - Ivana Grgić
- Ruđer Bošković Institute, Bijenička cesta 54, 10000 Zagreb, Croatia
| | - Carles M Borrego
- Catalan Institute for Water Research (ICRA), Emili Grahit 101, 17003 Girona, Spain; Group of Molecular Microbial Ecology, Institute of Aquatic Ecology, University of Girona, E-17001 Girona, Spain
| | - Mira Petrović
- Catalan Institute for Water Research (ICRA), Emili Grahit 101, 17003 Girona, Spain; Catalan Institution for Research and Advanced Studies (ICREA), Passeig Lluís Companys 23, 08010 Barcelona, Spain
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11
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Kurek MR, Garcia-Tigreros F, Nichols NA, Druschel GK, Wickland KP, Dornblaser MM, Striegl RG, Niles SF, McKenna AM, Aukes PJK, Kyzivat ED, Wang C, Smith LC, Schiff SL, Butman D, Spencer RGM. High Voltage: The Molecular Properties of Redox-Active Dissolved Organic Matter in Northern High-Latitude Lakes. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2023. [PMID: 37235632 DOI: 10.1021/acs.est.3c01782] [Citation(s) in RCA: 2] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/28/2023]
Abstract
Redox-active functional groups in dissolved organic matter (DOM) are crucial for microbial electron transfer and methane emissions. However, the extent of aquatic DOM redox properties across northern high-latitude lakes and their relationships with DOM composition have not been thoroughly described. We quantified electron donating capacity (EDC) and electron accepting capacity (EAC) in lake DOM from Canada to Alaska and assessed their relationships with parameters from absorbance, fluorescence, and ultrahigh resolution mass spectrometry (FT-ICR MS) analyses. EDC and EAC are strongly tied to aromaticity and negatively related to aliphaticity and protein-like content. Redox-active formulae spanned a range of aromaticity, including highly unsaturated phenolic formulae, and correlated negatively with many aliphatic N and S-containing formulae. This distribution illustrates the compositional diversity of redox-sensitive functional groups and their sensitivity to ecosystem properties such as local hydrology and residence time. Finally, we developed a reducing index (RI) to predict EDC in aquatic DOM from FT-ICR MS spectra and assessed its robustness using riverine DOM. As the hydrology of the northern high-latitudes continues to change, we expect differences in the quantity and partitioning of EDC and EAC within these lakes, which have implications for local water quality and methane emissions.
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Affiliation(s)
- Martin R Kurek
- Department of Earth, Ocean and Atmospheric Science, Florida State University, 1011 Academic Way, Tallahassee, Florida 32304, United States
- National High Magnetic Field Laboratory Geochemistry Group, 1800 E Paul Dirac Drive, Tallahassee, Florida 32310, United States
| | - Fenix Garcia-Tigreros
- School of Environmental and Forest Sciences, University of Washington, 3715 W Stevens Way NE, Seattle, Washington 98195, United States
| | - Natalie A Nichols
- Department of Earth Sciences, Indiana University-Purdue University Indianapolis, 723 W Michigan Street, Indianapolis, Indiana 46202, United States
| | - Gregory K Druschel
- Department of Earth Sciences, Indiana University-Purdue University Indianapolis, 723 W Michigan Street, Indianapolis, Indiana 46202, United States
| | - Kimberly P Wickland
- Geosciences and Environmental Change Science Center, United States Geological Survey, Denver Federal Center, Denver, Colorado 80225-0046, United States
| | - Mark M Dornblaser
- Water Resources Mission Area, United States Geological Survey, 3215 Marine Street, Boulder, Colorado 80303, United States
| | - Robert G Striegl
- Water Resources Mission Area, United States Geological Survey, 3215 Marine Street, Boulder, Colorado 80303, United States
| | - Sydney F Niles
- National High Magnetic Field Laboratory Ion Cyclotron Resonance Facility, 1800 E Paul Dirac Drive, Tallahassee, Florida 32310, United States
| | - Amy M McKenna
- National High Magnetic Field Laboratory Ion Cyclotron Resonance Facility, 1800 E Paul Dirac Drive, Tallahassee, Florida 32310, United States
- Department of Soil & Crop Sciences, Colorado State University, 307 University Avenue, Fort Collins, Colorado 80521, United States
| | - Pieter J K Aukes
- Department of Earth & Environmental Studies, University of Waterloo, 200 University Avenue W, Waterloo, Ontario N2L 3G1, Canada
- Geography & Environmental Studies, Wilfrid Laurier University, 75 University Avenue W, Waterloo, Ontario N2L 3C5, Canada
| | - Ethan D Kyzivat
- Department of Earth, Environmental & Planetary Sciences and Institute at Brown for Environment & Society, Brown University, 324 Brook Street, Providence, Rhode Island 02912, United States
| | - Chao Wang
- Department of Earth, Marine and Environmental Sciences, University of North Carolina, 104 South Road, CB#3315, Chapel Hill, North Carolina 27514, United States
| | - Laurence C Smith
- Department of Earth, Environmental & Planetary Sciences and Institute at Brown for Environment & Society, Brown University, 324 Brook Street, Providence, Rhode Island 02912, United States
| | - Sherry L Schiff
- Department of Earth & Environmental Studies, University of Waterloo, 200 University Avenue W, Waterloo, Ontario N2L 3G1, Canada
| | - David Butman
- School of Environmental and Forest Sciences, University of Washington, 3715 W Stevens Way NE, Seattle, Washington 98195, United States
- Department of Civil and Environmental Engineering, University of Washington, 201 More Hall, Seattle, Washington 98195-2700, United States
| | - Robert G M Spencer
- Department of Earth, Ocean and Atmospheric Science, Florida State University, 1011 Academic Way, Tallahassee, Florida 32304, United States
- National High Magnetic Field Laboratory Geochemistry Group, 1800 E Paul Dirac Drive, Tallahassee, Florida 32310, United States
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12
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Li S, Meng L, Zhao C, Gu Y, Spencer RGM, Álvarez-Salgado XA, Kellerman AM, McKenna AM, Huang T, Yang H, Huang C. Spatiotemporal response of dissolved organic matter diversity to natural and anthropogenic forces along the whole mainstream of the Yangtze River. WATER RESEARCH 2023; 234:119812. [PMID: 36881953 DOI: 10.1016/j.watres.2023.119812] [Citation(s) in RCA: 17] [Impact Index Per Article: 17.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 01/21/2023] [Revised: 02/23/2023] [Accepted: 02/24/2023] [Indexed: 06/18/2023]
Abstract
The Yangtze River, the largest river in Asia, plays a crucial role in linking continental and oceanic ecosystems. However, the impact of natural and anthropogenic disturbances on composition and transformation of dissolved organic matter (DOM) during long-distance transport and seasonal cycle is not fully understood. By using a combination of elemental, isotopic and optical techniques, as well as Fourier-transform ion cyclotron resonance mass spectrometry (FT-ICR MS), we investigated DOM abundance and composition along the whole mainstream at highly spatial resolution in the dry and early wet seasons. Our findings showed that the concentration and flux of dissolved organic carbon (DOC) in the Yangtze River was much lower compared with other worldwide larger rivers. The distribution of δ13CDOC and higher abundance of humic-like fluorescent component and highly unsaturated and phenolics (HUPs) compound reflected a prominent contribution of allochthonous DOM. Further optical and molecular analysis revealed humic-like fluorescent components were coupled with CHO molecules and HUPs compound with higher aromatic, unsaturated, molecular weight and stable characteristics between upstream and midstream reaches. With increasing agricultural and urban land downstream, there were more heteroatomic formulae and labile aliphatic and protein-like compounds which were derived from human activities and in situ primary production. Meanwhile, DOM gradually accumulates with slow water flow and additional autochthonous organics. Weaker solar radiation and water dilution during the dry/cold season favours highly aromatic, unsaturated and oxygenated DOM compositions. Conversely, higher discharge during the wet/warm season diluted the terrestrial DOM, but warm temperatures could promote phytoplankton growth that releases labile aliphatic and protein-like DOM. Besides, chemical sulfurization, hydrogenation and oxygenation were found during molecular cycling processes. Our research emphasizes the active response of riverine DOM to natural and anthropogenic controls, and provides a valuable preliminary background to better understand the biogeochemical cycling of DOM in a larger river.
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Affiliation(s)
- Shuaidong Li
- School of Geography, Nanjing Normal University, Nanjing 210023, China; Organic Geochemistry Lab, Instituto de Investigacións Mariñas (IIM), Consejo Superior de Investigaciones Científicas (CSIC), Vigo 36208, Spain
| | - Lize Meng
- School of Geography, Nanjing Normal University, Nanjing 210023, China
| | - Chu Zhao
- School of Geography, Nanjing Normal University, Nanjing 210023, China
| | - Yu Gu
- School of Geography, Nanjing Normal University, Nanjing 210023, China
| | - Robert G M Spencer
- Department of Earth, Ocean and Atmospheric Science, Florida State University, Tallahassee, FL 32306, USA
| | - Xosé Antón Álvarez-Salgado
- Organic Geochemistry Lab, Instituto de Investigacións Mariñas (IIM), Consejo Superior de Investigaciones Científicas (CSIC), Vigo 36208, Spain
| | - Anne M Kellerman
- Department of Earth, Ocean and Atmospheric Science, Florida State University, Tallahassee, FL 32306, USA
| | - Amy M McKenna
- National High Magnetic Field Laboratory, Florida State University, Tallahassee, FL 32310, USA
| | - Tao Huang
- School of Geography, Nanjing Normal University, Nanjing 210023, China; Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application, Nanjing Normal University, Nanjing 210023, China; Key Laboratory of Virtual Geographic Environment (Nanjing Normal University), Ministry of Education, Nanjing 210023, China; State Key Laboratory Cultivation Base of Geographical Environment Evolution (Jiangsu Province), Nanjing 210023, China
| | - Hao Yang
- School of Geography, Nanjing Normal University, Nanjing 210023, China; Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application, Nanjing Normal University, Nanjing 210023, China; Key Laboratory of Virtual Geographic Environment (Nanjing Normal University), Ministry of Education, Nanjing 210023, China; State Key Laboratory Cultivation Base of Geographical Environment Evolution (Jiangsu Province), Nanjing 210023, China
| | - Changchun Huang
- School of Geography, Nanjing Normal University, Nanjing 210023, China; Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application, Nanjing Normal University, Nanjing 210023, China; Key Laboratory of Virtual Geographic Environment (Nanjing Normal University), Ministry of Education, Nanjing 210023, China; State Key Laboratory Cultivation Base of Geographical Environment Evolution (Jiangsu Province), Nanjing 210023, China.
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13
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Herzsprung P, Kamjunke N, Wilske C, Friese K, Boehrer B, Rinke K, Lechtenfeld OJ, von Tümpling W. Data evaluation strategy for identification of key molecular formulas in dissolved organic matter as proxies for biogeochemical reactivity based on abundance differences from ultrahigh resolution mass spectrometry. WATER RESEARCH 2023; 232:119672. [PMID: 36739660 DOI: 10.1016/j.watres.2023.119672] [Citation(s) in RCA: 6] [Impact Index Per Article: 6.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/22/2022] [Accepted: 01/25/2023] [Indexed: 06/18/2023]
Abstract
The molecular composition of dissolved organic matter (DOM) is of relevance for global carbon cycling and important for drinking water processing also. The detection of variation of DOM composition as function of time and space from a methodological viewpoint is essential to observe DOM processing and was addressed so far. High resolution concerning DOM quality was achieved with Fourier-transform ion cyclotron resonance mass spectrometry (FTICR-MS). However almost none of the existing FTICR-MS data sets were evaluated addressing the fate of single mass features / molecular formulas (MFs) abundance during experiments. In contrast to former studies we analyze the function of MF abundance of time and space for such MFs which are present in all samples and which were formerly claimed as recalcitrant in not all but a great number of studies. For the first time the reactivity of MFs was directly compared by their abundance differences using a simple equation, the relative intensity difference (δRI). Search strategies to find out the maximum δRI values are introduced. The corresponding MFs will be regarded as key MFs (KEY-MFs). In order to test this new approach data from a recent photo degradation experiment were combined with monitoring surveys conducted in two drinking water reservoirs. The δRI values varied over one order of magnitude (more than five-fold). MFs like C9H12O6 and C10H14O6 revealed high biogeochemical reactivity as photo products. Some of the KEY-MFs were identical with MFs identified as disinfection byproducts precursors in recent studies. Other KEY-MFs were oxygen-rich and relatively unsaturated (poly-phenol-like) and hence relevant to flocculation procedures.
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Affiliation(s)
- Peter Herzsprung
- UFZ - Helmholtz Centre for Environmental Research, Department Lake Research, Brückstraße 3a, Magdeburg D-39114, Germany.
| | - Norbert Kamjunke
- UFZ - Helmholtz Centre for Environmental Research, Department River Ecology, Brückstraße 3a, Magdeburg D-39114, Germany
| | - Christin Wilske
- UFZ - Helmholtz Centre for Environmental Research, Department River Ecology, Brückstraße 3a, Magdeburg D-39114, Germany
| | - Kurt Friese
- UFZ - Helmholtz Centre for Environmental Research, Department Lake Research, Brückstraße 3a, Magdeburg D-39114, Germany
| | - Bertram Boehrer
- UFZ - Helmholtz Centre for Environmental Research, Department Lake Research, Brückstraße 3a, Magdeburg D-39114, Germany
| | - Karsten Rinke
- UFZ - Helmholtz Centre for Environmental Research, Department Lake Research, Brückstraße 3a, Magdeburg D-39114, Germany
| | - Oliver J Lechtenfeld
- UFZ - Helmholtz Centre for Environmental Research, Department Analytical Chemistry, Permoserstr. 15, Leipzig D-04318, Germany; UFZ - Helmholtz Centre for Environmental Research, ProVIS - Centre for Chemical Microscopy, Permoserstr. 15, Leipzig D-04318, Germany
| | - Wolf von Tümpling
- UFZ - Helmholtz Centre for Environmental Research, Department River Ecology, Brückstraße 3a, Magdeburg D-39114, Germany
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14
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Retter A, Haas JC, Birk S, Stumpp C, Hausmann B, Griebler C, Karwautz C. From the Mountain to the Valley: Drivers of Groundwater Prokaryotic Communities along an Alpine River Corridor. Microorganisms 2023; 11:microorganisms11030779. [PMID: 36985351 PMCID: PMC10055094 DOI: 10.3390/microorganisms11030779] [Citation(s) in RCA: 2] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/27/2023] [Revised: 03/08/2023] [Accepted: 03/11/2023] [Indexed: 03/19/2023] Open
Abstract
Rivers are the “tip of the iceberg”, with the underlying groundwater being the unseen freshwater majority. Microbial community composition and the dynamics of shallow groundwater ecosystems are thus crucial, due to their potential impact on ecosystem processes and functioning. In early summer and late autumn, samples of river water from 14 stations and groundwater from 45 wells were analyzed along a 300 km transect of the Mur River valley, from the Austrian alps to the flats at the Slovenian border. The active and total prokaryotic communities were characterized using high-throughput gene amplicon sequencing. Key physico-chemical parameters and stress indicators were recorded. The dataset was used to challenge ecological concepts and assembly processes in shallow aquifers. The groundwater microbiome is analyzed regarding its composition, change with land use, and difference to the river. Community composition and species turnover differed significantly. At high altitudes, dispersal limitation was the main driver of groundwater community assembly, whereas in the lowland, homogeneous selection explained the larger share. Land use was a key determinant of the groundwater microbiome composition. The alpine region was more diverse and richer in prokaryotic taxa, with some early diverging archaeal lineages being highly abundant. This dataset shows a longitudinal change in prokaryotic communities that is dependent on regional differences affected by geomorphology and land use.
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Affiliation(s)
- Alice Retter
- Department of Functional and Evolutionary Ecology, University of Vienna, 1030 Wien, Austria
| | | | - Steffen Birk
- Institute of Earth Sciences, NAWI Graz Geocenter, University of Graz, 8010 Graz, Austria
| | - Christine Stumpp
- Institute of Soil Physics and Rural Water Management, University of Natural Resources and Life Sciences (BOKU), 1180 Wien, Austria
| | - Bela Hausmann
- Joint Microbiome Facility of the Medical University of Vienna and the University of Vienna, 1030 Wien, Austria
- Department of Laboratory Medicine, Medical University of Vienna, 1090 Wien, Austria
| | - Christian Griebler
- Department of Functional and Evolutionary Ecology, University of Vienna, 1030 Wien, Austria
| | - Clemens Karwautz
- Department of Functional and Evolutionary Ecology, University of Vienna, 1030 Wien, Austria
- Correspondence:
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15
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Humphries GE, Espinosa JI, Ambrosone M, Ayala ZR, Tzortziou M, Goes JI, Greenfield DI. Transitions in nitrogen and organic matter form and concentration correspond to bacterial population dynamics in a hypoxic urban estuary. BIOGEOCHEMISTRY 2023; 163:219-243. [PMID: 36968009 PMCID: PMC9959957 DOI: 10.1007/s10533-023-01021-2] [Citation(s) in RCA: 3] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 09/26/2022] [Accepted: 01/18/2023] [Indexed: 06/18/2023]
Abstract
UNLABELLED Nitrogen (N) inputs to developed coastlines are linked with multiple ecosystem and socio-economic impacts worldwide such as algal blooms, habitat/resource deterioration, and hypoxia. This study investigated the microbial and biogeochemical processes associated with recurrent, seasonal bottom-water hypoxia in an urban estuary, western Long Island Sound (WLIS), that receives high N inputs. A 2-year (2020-2021) field study spanned two hypoxia events and entailed surface and bottom depth water sampling for dissolved nutrients as inorganic N (DIN; ammonia-N and nitrite + nitrate (N + N)), organic N, orthophosphate, organic carbon (DOC), as well as chlorophyll a and bacterial abundances. Physical water quality data were obtained from concurrent conductivity, temperature, and depth casts. Results showed that dissolved organic matter was highest at the most-hypoxic locations, DOC was negatively and significantly correlated with bottom-water dissolved oxygen (Pearson's r = -0.53, p = 0.05), and ammonia-N was the dominant DIN form pre-hypoxia before declining throughout hypoxia. N + N concentrations showed the reverse, being minimal pre-hypoxia then increasing during and following hypoxia, indicating that ammonia oxidation likely contributed to the switch in dominant DIN forms and is a key pathway in WLIS water column nitrification. Similarly, at the most hypoxic sampling site, bottom depth bacteria concentrations ranged ~ 1.8 × 104-1.1 × 105 cells ml-1 pre-hypoxia, declined throughout hypoxia, and were positively and significantly correlated (Pearson's r = 0.57; p = 0.03) with ammonia-N, confirming that hypoxia influences N-cycling within LIS. These findings provide novel insight to feedbacks between major biogeochemical (N and C) cycles and hypoxia in urban estuaries. SUPPLEMENTARY INFORMATION The online version contains supplementary material available at 10.1007/s10533-023-01021-2.
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Affiliation(s)
- Georgie E. Humphries
- School of Earth and Environmental Sciences, Queens College, Queens, NY 11367 USA
- Advanced Science Research Center at the Graduate Center, New York, NY 10031 USA
| | - Jessica I. Espinosa
- Advanced Science Research Center at the Graduate Center, New York, NY 10031 USA
- Department of Ecology and Evolutionary Biology, University of Connecticut, Storrs, CT 06269 USA
| | | | - Zabdiel Roldan Ayala
- School of Earth and Environmental Sciences, Queens College, Queens, NY 11367 USA
- Advanced Science Research Center at the Graduate Center, New York, NY 10031 USA
| | - Maria Tzortziou
- City College Center for Discovery and Innovation, New York, NY 10031 USA
- Department of Earth and Atmospheric Sciences, City College of New York, New York, USA
| | | | - Dianne I. Greenfield
- School of Earth and Environmental Sciences, Queens College, Queens, NY 11367 USA
- Advanced Science Research Center at the Graduate Center, New York, NY 10031 USA
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16
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Vaughn DR, Kellerman AM, Wickland KP, Striegl RG, Podgorski DC, Hawkings JR, Nienhuis JH, Dornblaser MM, Stets EG, Spencer RGM. Bioavailability of dissolved organic matter varies with anthropogenic landcover in the Upper Mississippi River Basin. WATER RESEARCH 2023; 229:119357. [PMID: 36455459 DOI: 10.1016/j.watres.2022.119357] [Citation(s) in RCA: 8] [Impact Index Per Article: 8.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/04/2022] [Revised: 11/05/2022] [Accepted: 11/12/2022] [Indexed: 06/17/2023]
Abstract
Anthropogenic conversion of forests and wetlands to agricultural and urban landcovers impacts dissolved organic matter (DOM) within streams draining these catchments. Research on how landcover conversion impacts DOM molecular level composition and bioavailability, however, is lacking. In the Upper Mississippi River Basin (UMRB), water from low-order streams and rivers draining one of three dominant landcovers (forest, agriculture, urban) was incubated for 28 days to determine bioavailable DOC (BDOC) concentrations and changes in DOM composition. The BDOC concentration averaged 0.49 ± 0.30 mg L-1 across all samples and was significantly higher in streams draining urban catchments (0.72 ± 0.34 mg L-1) compared to streams draining agricultural (0.28 ± 0.15 mg L-1) and forested (0.47 ± 0.17 mg L-1) catchments. Percent BDOC was significantly greater in urban (10% ± 4.4%) streams compared to forested streams (5.6% ± 3.2%), corresponding with greater relative abundances of aliphatic and N-containing aliphatic compounds in urban streams. Aliphatic compound relative abundance decreased across all landcovers during the bioincubation (average -4.1% ± 10%), whereas polyphenolics and condensed aromatics increased in relative abundance across all landcovers (average of +1.4% ± 5.9% and +1.8% ± 10%, respectively). Overall, the conversion of forested to urban landcover had a larger impact on stream DOM bioavailability in the UMRB compared to conversion to agricultural landcover. Future research examining the impacts of anthropogenic landcover conversion on stream DOM composition and bioavailability needs to be expanded to a range of spatial scales and to different ecotones, especially with continued landcover alterations.
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Affiliation(s)
- Derrick R Vaughn
- National High Magnetic Field Laboratory Geochemistry Group and Department of Earth, Ocean, and Atmospheric Science, Florida State University, Tallahassee, FL, USA; School of the Environment, Yale University, New Haven, CT, USA.
| | - Anne M Kellerman
- National High Magnetic Field Laboratory Geochemistry Group and Department of Earth, Ocean, and Atmospheric Science, Florida State University, Tallahassee, FL, USA
| | | | - Robert G Striegl
- U.S. Geological Survey, Water Resources Mission Area, Boulder, CO, USA
| | - David C Podgorski
- Department of Chemistry, Chemical Analysis and Mass Spectrometry Facility, Pontchartrain Institute for Environmental Sciences, University of New Orleans, New Orleans, LA, USA
| | - Jon R Hawkings
- National High Magnetic Field Laboratory Geochemistry Group and Department of Earth, Ocean, and Atmospheric Science, Florida State University, Tallahassee, FL, USA; Department of Earth and Environmental Science, University of Pennsylvania, Philadelphia, PA, USA
| | - Jaap H Nienhuis
- Department of Physical Geography, Utrecht University, Utrecht, the Netherlands
| | - Mark M Dornblaser
- U.S. Geological Survey, Water Resources Mission Area, Boulder, CO, USA
| | - Edward G Stets
- U.S. Geological Survey, Water Resources Mission Area, Mounds View, MN, USA
| | - Robert G M Spencer
- National High Magnetic Field Laboratory Geochemistry Group and Department of Earth, Ocean, and Atmospheric Science, Florida State University, Tallahassee, FL, USA
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17
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Osafo NOA, Jan J, Porcal P, Borovec J. Contrasting catchment soil pH and Fe concentrations influence DOM distribution and nutrient dynamics in freshwater systems. THE SCIENCE OF THE TOTAL ENVIRONMENT 2023; 858:159988. [PMID: 36356733 DOI: 10.1016/j.scitotenv.2022.159988] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/15/2022] [Revised: 11/01/2022] [Accepted: 11/02/2022] [Indexed: 06/16/2023]
Abstract
Organic matter (OM) quantity, quality, and nutrient dynamics within twelve shallow lakes in the Czech Republic were assessed in the context of catchment soil pH and iron (Fe) concentration. The catchments of the lakes were classified into two categories: (i) slightly acidic (soil pH = 5.1-6.3) with Fe-rich soils (H_Fe; Fe = 315-344 mg kg-1 in Mehlich 3 extract); and (ii) neutral (soil pH = 6.8-7.6) with Fe-poor soils (L_Fe; Fe = 126-259 mg kg-1 in Mehlich 3 extract). The quality of OM in the two lake types was characterized using a combination of spectroscopic techniques (UV-Vis, fluorescence, and Fourier Transform Infrared spectroscopy). We show that dissolved nutrient and dissolved organic carbon (DOC) concentrations, as well as the amount of aromatic and protein-like compounds in the water column and sediment porewater were significantly (p < 0.01) lower in the H_Fe lakes compared to the waterbodies located within L_Fe catchments. The FTIR analyses of the H_Fe sediments contained higher relative concentrations of aromatic compounds with hydroxyl-containing functional groups and carbohydrates, while more aliphatic and oxidised OM was found in the L_Fe lake sediments. These results suggest that the pH value of catchment soils and, particularly, their Fe content have profound geochemical effects on the mobility of OM and nutrients in the sediments of recipient waters. Because the OM-Fe association stabilises OM in sediments, waterbodies within L_Fe catchments are likely more vulnerable to increasing eutrophication and oxygen depletion compared to those in H_Fe catchments and this has important implications for water quality management, risk assessment, and predictions of aquatic ecosystem vulnerability under conditions of accelerating climate change.
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Affiliation(s)
- Nana O-A Osafo
- Institute of Soil Biology and Biogeochemistry, Biology Centre CAS, České Budějovice, Czech Republic; Faculty of Science, University of South Bohemia, České Budějovice 370 05. Czech Republic.
| | - Jiří Jan
- Institute of Soil Biology and Biogeochemistry, Biology Centre CAS, České Budějovice, Czech Republic
| | - Petr Porcal
- Faculty of Science, University of South Bohemia, České Budějovice 370 05. Czech Republic; Institute of Hydrobiology, Biology Centre CAS, České Budějovice 370 05, Czech Republic
| | - Jakub Borovec
- Institute of Soil Biology and Biogeochemistry, Biology Centre CAS, České Budějovice, Czech Republic; Faculty of Science, University of South Bohemia, České Budějovice 370 05. Czech Republic
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18
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Hong Z, Ma H, Zhang T, Wang Q, Chang Y, Song Y, Li Z, Cui F. Joint role of land cover types and microbial processing on molecular composition of dissolved organic matter in inland lakes. THE SCIENCE OF THE TOTAL ENVIRONMENT 2023; 857:159522. [PMID: 36270364 DOI: 10.1016/j.scitotenv.2022.159522] [Citation(s) in RCA: 3] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/06/2022] [Revised: 10/10/2022] [Accepted: 10/13/2022] [Indexed: 06/16/2023]
Abstract
Anthropogenic activities have greatly changed the land use and land cover (LULC) and further influenced the chemical properties and amount of DOM transported into aquatic systems, meanwhile, microbial processing is also critical to DOM molecular composition in freshwaters. However, how they jointly shape DOM's chemical composition and chemodiversity in lakes is poorly understood. Here we examined DOM characteristics for seven inland lakes with three different land cover conditions (forest-dominated, cropland-dominated, and urban-dominated). Results indicated that DOM in cropland-dominated and forest-dominated lakes exhibited more characteristics of terrestrial organic matter, while urban-dominated lakes had more allochthonous organic matter driven by relatively high nutrient input. Human activities extended terrestrial DOM input to lakes and intensified the amount of heteroatomic organic molecules containing nitrogen and sulfur in lakes, with cropland contributing more N-containing compounds and urban contributing more S-containing compounds. Differential bacterial community composition appeared in the three types of land cover lakes, while strong co-occurrence/exclusion patterns between specific microbes and molecular formula groups revealed the key DOM metabolism functions of these bacteria. Matrix correlations based on Mantel tests confirmed that watershed landcover status was a dominating factor for DOM sources and molecular composition in mountainous lakes through direct input of terrestrial organic matter, and microbial processing was not the key factor for DOM molecular formula. Our findings help to assess the influence of human activities and microbial processing in the transfer and transformation of DOM in environmental waters.
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Affiliation(s)
- Zhicheng Hong
- Key Laboratory of the Three Gorges Reservoir Region's Eco-Environment, Ministry of Education, Chongqing, China
| | - Hua Ma
- Key Laboratory of the Three Gorges Reservoir Region's Eco-Environment, Ministry of Education, Chongqing, China; College of Environment and Ecology, Chongqing University, Chongqing, China.
| | - Ting Zhang
- Key Laboratory of the Three Gorges Reservoir Region's Eco-Environment, Ministry of Education, Chongqing, China
| | - Qianru Wang
- Key Laboratory of the Three Gorges Reservoir Region's Eco-Environment, Ministry of Education, Chongqing, China
| | - Yilin Chang
- Key Laboratory of the Three Gorges Reservoir Region's Eco-Environment, Ministry of Education, Chongqing, China
| | - Yingyue Song
- Key Laboratory of the Three Gorges Reservoir Region's Eco-Environment, Ministry of Education, Chongqing, China
| | - Zhe Li
- Key Laboratory of the Three Gorges Reservoir Region's Eco-Environment, Ministry of Education, Chongqing, China
| | - Fuyi Cui
- Key Laboratory of the Three Gorges Reservoir Region's Eco-Environment, Ministry of Education, Chongqing, China; College of Environment and Ecology, Chongqing University, Chongqing, China
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19
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Wen L, Yang F, Li X, Liu S, Lin Y, Hu E, Gao L, Li M. Composition of dissolved organic matter (DOM) in wastewater treatment plants influent affects the efficiency of carbon and nitrogen removal. THE SCIENCE OF THE TOTAL ENVIRONMENT 2023; 857:159541. [PMID: 36265625 DOI: 10.1016/j.scitotenv.2022.159541] [Citation(s) in RCA: 9] [Impact Index Per Article: 9.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/21/2022] [Revised: 10/13/2022] [Accepted: 10/13/2022] [Indexed: 06/16/2023]
Abstract
Wastewater treatment plants (WWTPs) play a critical role in receiving, removing, and discharging dissolved organic matter (DOM) in aquatic systems. To date, understanding the composition and fate of DOM in different WWTPs with various environmental and socioeconomic conditions is limited. This study analyzed DOM components in the influent and effluent samples from 49 WWTPs in China using EEM-PARAFAC and ESI-FT-ICR-MS methods. The influencing factors of DOM components in the influent were also analyzed. Geographic location and GDP showed significant (p < 0.05) correlations with DOM components in the influent. The removal efficiency of DOM in WWTPs was closely related to the DOM compositions, where carbohydrates, lipids, and protein-like components (removal efficiencies > 75 %) were more readily decomposed than the humic-like components, lignin, and tannin. The relative fraction of humic-like compound C3 in the influent was correlated negatively with total nitrogen (TN) and chemical oxygen demand (COD) removal in WWTPs (p < 0.05). Besides, the relative fraction of DOM containing the element sulfur also showed significant negative correlations with the humification of DOM (p < 0.05). The results from EEM-PARAFAC and ESI-FT-ICR-MS methods showed no obvious correlation for the DOM characterizations except for humic-like fluorescent fraction C3 and lignin, while significant positive correlations (p < 0.05) between the aromatic index (AI_mod) from the ESI-FT-ICR-MS analysis and the humification index (HIX) from spectrofluorimetry. This supports the use of these spectral indexes as simple surrogates to represent part chemical compositions in further research.
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Affiliation(s)
- Ling Wen
- College of Natural Resources and Environment, Northwest A & F University, Yangling 712100, PR China
| | - Fang Yang
- College of Natural Resources and Environment, Northwest A & F University, Yangling 712100, PR China
| | - Xuan Li
- School of Civil, Mining and Environmental Engineering, University of Wollongong, Australia
| | - Siwan Liu
- College of Natural Resources and Environment, Northwest A & F University, Yangling 712100, PR China
| | - Yuye Lin
- College of Natural Resources and Environment, Northwest A & F University, Yangling 712100, PR China
| | - En Hu
- Shaanxi Provincial Academy of Environmental Science, Xi'an 710061, PR China
| | - Li Gao
- South East Water, 101 Wells Street, Frankston, VIC 3199, Australia
| | - Ming Li
- College of Natural Resources and Environment, Northwest A & F University, Yangling 712100, PR China.
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20
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Harir M, Cawley KM, Hertkorn N, Schmitt-Kopplin P, Jaffé R. Molecular and spectroscopic changes of peat-derived organic matter following photo-exposure: Effects on heteroatom composition of DOM. THE SCIENCE OF THE TOTAL ENVIRONMENT 2022; 838:155790. [PMID: 35550890 DOI: 10.1016/j.scitotenv.2022.155790] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 02/14/2022] [Revised: 05/04/2022] [Accepted: 05/04/2022] [Indexed: 06/15/2023]
Abstract
The temporal evolution of molecular compositions and changes in structural features of Hillsboro Canal (Florida, USA) dissolved organic matter (DOM) was studied with an emphasis on nitrogen and sulfur containing molecules, after a 13 day time-series exposure to simulated sunlight. The Hillsboro Canal drains from the ridge and slough wetland environment underlain by peat soils from the northern extent of the Greater Everglades Ecosystem. The Hillsboro Canal-DOM was characterized by combining ultrahigh-resolution mass spectrometry (FT-ICR-MS), high-field nuclear magnetic resonance spectroscopy (1H NMR), size exclusion chromatography (SEC) with UV detection, and ultraviolet/visible (UV/vis) absorbance and excitation emission matrix (EEM) fluorescence spectroscopy. Size exclusion chromatography (SEC) demonstrated progressive depletion of higher mass molecules and a concomitant decrease of absorbance during photo-irradiation. NMR and FT-ICR-MS revealed nonlinear temporal evolution of DOM. In fact, FT-ICR-MS showed an initial depletion of supposedly chromophoric molecules often carrying major unsaturation accompanied by an uneven evolution of numbers of CHO, CHOS and CHNO compounds. While CHNO compounds continually increased throughout the entire photo-exposure time, CHO and CHOS compounds temporarily increased but declined after further light exposure. Progressive loss of highly unsaturated compounds was accompanied by production of low mass CHO and CHNO compounds with high O/C ratios. Area-normalized 1H NMR spectra of DOM in water and of the water insoluble fraction (~5%) in methanol revealed clear distinctions between irradiated and non-irradiated samples and congruent evolution of DOM structural features during irradiation, with more uniform trends in methanolic-DOM. Photoirradiation caused initial photoproduction of oxygenated aliphatic compounds, continued depletion of phenols and oxygenated aromatics, substantial change from initial natural product derived olefins to photoproduced olefins, and uneven evolution of carboxylated and alkylated benzene derivatives. This study demonstrates longer-term heteroatom-dependent photochemistry of DOM, which will affect the speciation of N and S heteroatoms, their connections to inorganic nutrients, and potentially their bioavailability.
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Affiliation(s)
- Mourad Harir
- Research Unit Analytical Biogeochemistry, Helmholtz Munich, 85764 Neuherberg, Germany; Analytical Food Chemistry, Technische Universität München, Maximus-von-Imhof-Forum 2, 85354 Freising-Weihenstephan, Germany.
| | - Kaelin M Cawley
- Southeast Environmental Research Center and Department of Chemistry and Biochemistry, Florida International University, Miami, FL, USA; Battelle, National Ecological Observatory Network (NEON) Project, Boulder, CO, USA
| | - Norbert Hertkorn
- Research Unit Analytical Biogeochemistry, Helmholtz Munich, 85764 Neuherberg, Germany
| | - Philippe Schmitt-Kopplin
- Research Unit Analytical Biogeochemistry, Helmholtz Munich, 85764 Neuherberg, Germany; Analytical Food Chemistry, Technische Universität München, Maximus-von-Imhof-Forum 2, 85354 Freising-Weihenstephan, Germany
| | - Rudolf Jaffé
- Southeast Environmental Research Center and Department of Chemistry and Biochemistry, Florida International University, Miami, FL, USA.
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21
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Hassanpour B, Blair N, Aristilde L. Metabolomics analysis of unresolved molecular variability in stoichiometry dynamics of a stream dissolved organic matter. WATER RESEARCH 2022; 223:118923. [PMID: 36001905 DOI: 10.1016/j.watres.2022.118923] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 05/04/2022] [Revised: 07/20/2022] [Accepted: 07/28/2022] [Indexed: 06/15/2023]
Abstract
Broad molecular classification based on stoichiometric ratio relationships has been used extensively to characterize the chemical diversity of aquatic dissolved organic matter (DOM). However, variability in the molecular composition within this classification has remained elusive, thus limiting the interpretation of DOM dynamics, especially with respect to transport versus transformation patterns in response to hydrologic or landscape changes. Here, leveraging high-frequency spatiotemporal sampling during rainfall events at a Critical Zone Observatory project site in Clear Creek, Iowa, we apply a metabolomics-based analysis validated with fragmentation using tandem mass spectrometry to uncover patterns in the molecular features of the DOM composition that were not resolved by classification based on stoichiometric ratios in the chemical formulae. From upstream to downstream sites, beyond the increased aromaticity implied by changes in the stoichiometric ratios, we identified an increased abundance of flavonoids and other phenylpropanoids, two important subgroups of aromatic compounds. The stoichiometric analysis also proposed a localized decline in the abundance of lipid-like compounds, which we attributed specifically to medium-chain and short-chain fatty acids; other lipids such as long-chain fatty acids and sterol lipids remained unchanged. We further determined in-stream molecular transitions and specific compound degradation by capturing changes in the molecular masses of terpenoids, phenylpropanoids, fatty acids, and amino acids. In sum, the metabolomics analysis of the chemical formulae resolved molecular variability imprinted on the stoichiometric DOM composition to implicate key molecular subgroups underlying carbon transport and cycling dynamics in the stream.
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Affiliation(s)
- Bahareh Hassanpour
- Department of Civil and Environmental Engineering, McCormick School of Engineering and Applied Science, Northwestern University, Evanston, IL 60208, United States
| | - Neal Blair
- Department of Civil and Environmental Engineering, McCormick School of Engineering and Applied Science, Northwestern University, Evanston, IL 60208, United States; Department of Earth and Planetary Sciences, Weinberg College of Arts and Sciences, Northwestern University, Evanston, IL 60208, United States
| | - Ludmilla Aristilde
- Department of Civil and Environmental Engineering, McCormick School of Engineering and Applied Science, Northwestern University, Evanston, IL 60208, United States.
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22
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Sanchez-Arcos C, Ueberschaar N, Pohnert G. Aquifer system and depth specific chemical patterns in fractured-rock groundwater from the Critical Zone revealed by untargeted LC-MS-based metabolomics. WATER RESEARCH 2022; 219:118566. [PMID: 35580391 DOI: 10.1016/j.watres.2022.118566] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/15/2021] [Revised: 05/04/2022] [Accepted: 05/05/2022] [Indexed: 06/15/2023]
Abstract
In the Earth's Critical Zone, water plays an essential role as a collector and transporter of metabolites and their transformation products. It is generally believed that the chemical profiles of groundwater are strongly impacted by land use. However, predictors for the effects of above-ground natural and anthropogenic activities on below-ground chemistry are rare. We reasoned that comparing groundwater metabolomes from different land-use sites and depths can give insight into this coupling of above and below-ground processes in the Critical Zone. This study used an LC-MS-based untargeted metabolomic approach to identify links between groundwater metabolomes from monitoring wells in fractured carbonate-/siliciclastic alternations along a hillslope of the Hainich Critical Zone Exploratory (CZE) in Thuringia, Germany. Our results identify the land-use type, aquifer system, and sampling depth as critical factors determining the differences among groundwater metabolomes. We established five groundwater metabolic clusters and correlated these to the aquifer systems, hydrogeochemistry, and microbial community composition. Our untargeted metabolomic approach reveals the limited connectivity of groundwater chemical profiles with above-ground activities and illustrates how deep the input signals can travel.
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Affiliation(s)
- Carlos Sanchez-Arcos
- Institute for Inorganic and Analytical Chemistry, Bioorganic Analytics, Friedrich-Schiller-Universität Jena, Lessingstrasse 8, D-07743, Jena, Germany
| | - Nico Ueberschaar
- Institute for Inorganic and Analytical Chemistry, Bioorganic Analytics, Friedrich-Schiller-Universität Jena, Lessingstrasse 8, D-07743, Jena, Germany
| | - Georg Pohnert
- Institute for Inorganic and Analytical Chemistry, Bioorganic Analytics, Friedrich-Schiller-Universität Jena, Lessingstrasse 8, D-07743, Jena, Germany.
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23
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Kamjunke N, Beckers LM, Herzsprung P, von Tümpling W, Lechtenfeld O, Tittel J, Risse-Buhl U, Rode M, Wachholz A, Kallies R, Schulze T, Krauss M, Brack W, Comero S, Gawlik BM, Skejo H, Tavazzi S, Mariani G, Borchardt D, Weitere M. Lagrangian profiles of riverine autotrophy, organic matter transformation, and micropollutants at extreme drought. THE SCIENCE OF THE TOTAL ENVIRONMENT 2022; 828:154243. [PMID: 35245548 DOI: 10.1016/j.scitotenv.2022.154243] [Citation(s) in RCA: 3] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/18/2021] [Revised: 02/23/2022] [Accepted: 02/26/2022] [Indexed: 06/14/2023]
Abstract
On their way from inland to the ocean, flowing water bodies, their constituents and their biotic communities are exposed to complex transport and transformation processes. However, detailed process knowledge as revealed by Lagrangian measurements adjusted to travel time is rare in large rivers, in particular at hydrological extremes. To fill this gap, we investigated autotrophic processes, heterotrophic carbon utilization, and micropollutant concentrations applying a Lagrangian sampling design in a 600 km section of the River Elbe (Germany) at historically low discharge. Under base flow conditions, we expect the maximum intensity of instream processes and of point source impacts. Phytoplankton biomass and photosynthesis increased from upstream to downstream sites but maximum chlorophyll concentration was lower than at mean discharge. Concentrations of dissolved macronutrients decreased to almost complete phosphate depletion and low nitrate values. The longitudinal increase of bacterial abundance and production was less pronounced than in wetter years and bacterial community composition changed downstream. Molecular analyses revealed a longitudinal increase of many DOM components due to microbial production, whereas saturated lipid-like DOM, unsaturated aromatics and polyphenols, and some CHOS surfactants declined. In decomposition experiments, DOM components with high O/C ratios and high masses decreased whereas those with low O/C ratios, low masses, and high nitrogen content increased at all sites. Radiocarbon age analyses showed that DOC was relatively old (890-1870 years B.P.), whereas the mineralized fraction was much younger suggesting predominant oxidation of algal lysis products and exudates particularly at downstream sites. Micropollutants determining toxicity for algae (terbuthylazine, terbutryn, isoproturon and lenacil), hexachlorocyclohexanes and DDTs showed higher concentrations from the middle towards the downstream part but calculated toxicity was not negatively correlated to phytoplankton. Overall, autotrophic and heterotrophic process rates and micropollutant concentrations increased from up- to downstream reaches, but their magnitudes were not distinctly different to conditions at medium discharges.
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Affiliation(s)
- Norbert Kamjunke
- Helmholtz Centre for Environmental Research - UFZ, Department of River Ecology, Brückstraße 3a, D-39114 Magdeburg, Germany.
| | - Liza-Marie Beckers
- Helmholtz Centre for Environmental Research - UFZ, Department of Effect-Directed Analysis, Permoserstr. 15, 04318 Leipzig, Germany
| | - Peter Herzsprung
- Helmholtz Centre for Environmental Research - UFZ, Department Lake Research, Brückstr. 3a, 39114 Magdeburg, Germany
| | - Wolf von Tümpling
- Helmholtz Centre for Environmental Research - UFZ, Department of River Ecology, Brückstraße 3a, D-39114 Magdeburg, Germany
| | - Oliver Lechtenfeld
- Helmholtz Centre for Environmental Research - UFZ, Department of Analytics, Permoserstr. 15, 04318 Leipzig, Germany
| | - Jörg Tittel
- Helmholtz Centre for Environmental Research - UFZ, Department Lake Research, Brückstr. 3a, 39114 Magdeburg, Germany
| | - Ute Risse-Buhl
- Helmholtz Centre for Environmental Research - UFZ, Department of River Ecology, Brückstraße 3a, D-39114 Magdeburg, Germany
| | - Michael Rode
- Helmholtz Centre for Environmental Research - UFZ, Department of Aquatic Ecosystem Analysis, Brückstraße 3a, D-39114 Magdeburg, Germany; Institute of Environmental Science and Geography, University of Potsdam, Karl-Liebknecht-Str. 24-25, 14476 Potsdam, Germany
| | - Alexander Wachholz
- Helmholtz Centre for Environmental Research - UFZ, Department of Aquatic Ecosystem Analysis, Brückstraße 3a, D-39114 Magdeburg, Germany
| | - Rene Kallies
- Helmholtz Centre for Environmental Research - UFZ, Department of Environmental Microbiology, Permoserstr. 15, 04318 Leipzig, Germany
| | - Tobias Schulze
- Helmholtz Centre for Environmental Research - UFZ, Department of Effect-Directed Analysis, Permoserstr. 15, 04318 Leipzig, Germany
| | - Martin Krauss
- Helmholtz Centre for Environmental Research - UFZ, Department of Effect-Directed Analysis, Permoserstr. 15, 04318 Leipzig, Germany
| | - Werner Brack
- Helmholtz Centre for Environmental Research - UFZ, Department of Effect-Directed Analysis, Permoserstr. 15, 04318 Leipzig, Germany; Faculty of Biological Sciences, Goethe University Frankfurt, Max-von-Laue-Strasse, 13 60438 Frankfurt am Main, Germany
| | - Sara Comero
- European Commission, Joint Research Centre, Directorate D - Sustainable Resources, Unit D.02 Water and Marine Resources, Via E. Fermi 2749, T.P. 120, I-21027 Ispra, VA, Italy
| | - Bernd Manfred Gawlik
- European Commission, Joint Research Centre, Directorate D - Sustainable Resources, Unit D.02 Water and Marine Resources, Via E. Fermi 2749, T.P. 120, I-21027 Ispra, VA, Italy
| | - Hello Skejo
- European Commission, Joint Research Centre, Directorate D - Sustainable Resources, Unit D.02 Water and Marine Resources, Via E. Fermi 2749, T.P. 120, I-21027 Ispra, VA, Italy
| | - Simona Tavazzi
- European Commission, Joint Research Centre, Directorate D - Sustainable Resources, Unit D.02 Water and Marine Resources, Via E. Fermi 2749, T.P. 120, I-21027 Ispra, VA, Italy
| | - Giulio Mariani
- European Commission, Joint Research Centre, Directorate D - Sustainable Resources, Unit D.02 Water and Marine Resources, Via E. Fermi 2749, T.P. 120, I-21027 Ispra, VA, Italy
| | - Dietrich Borchardt
- Helmholtz Centre for Environmental Research - UFZ, Department of Aquatic Ecosystem Analysis, Brückstraße 3a, D-39114 Magdeburg, Germany
| | - Markus Weitere
- Helmholtz Centre for Environmental Research - UFZ, Department of River Ecology, Brückstraße 3a, D-39114 Magdeburg, Germany
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24
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Song X, Zhao Y, Zhang L, Xie X, Wu J, Wei Z, Yang H, Zhang S, Song C, Jia L. Photodegradation, bacterial metabolism, and photosynthesis drive the dissolved organic matter cycle in the Heilongjiang River. CHEMOSPHERE 2022; 295:133923. [PMID: 35143859 DOI: 10.1016/j.chemosphere.2022.133923] [Citation(s) in RCA: 2] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/24/2021] [Revised: 10/23/2021] [Accepted: 02/06/2022] [Indexed: 06/14/2023]
Abstract
Dissolved organic matter (DOM) plays a vital role in the biogeochemistry of aquatic ecosystems. However, the mechanisms of DOM cycling in the water column during different seasons have not been fully elucidated to date. The differences in DOM degradation in summer, autumn, and winter water columns were evaluated in this study. The results showed that bacteria played an essential role in the degradation of DOM in the summer water column. Photochemical degradation was the primary degradation pathway of DOM in the autumn and winter water columns. Notably, while DOM is degraded, photosynthetic bacteria produce organic matter through photosynthesis to replenish the water column. EEM-PARAFAC analysis indicated more tryptophan component C1 in summer, but the contents of humic substance component C2 and terrestrial substance C3 were higher in autumn and winter. In summer, more tryptophan-like components were consumed by bacteria, and Cyanobacteria produced more organic matter through photosynthesis to replenish the water column. Moreover, a similar bacterial community structure and a more active tryptophan biosynthesis pathway were found in autumn and winter. Random forest models identified representative bacteria involved in the DOM transformation process in different seasons. The above findings may be helpful to explore the degradation characteristics of DOM in different seasons and predict the fate of DOM in the water column in the future.
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Affiliation(s)
- Xinyu Song
- College of Life Science, Northeast Agricultural University, Harbin, 150030, China
| | - Yue Zhao
- College of Life Science, Northeast Agricultural University, Harbin, 150030, China
| | - Linyuan Zhang
- College of Life Science, Northeast Agricultural University, Harbin, 150030, China
| | - Xinyu Xie
- College of Life Science, Northeast Agricultural University, Harbin, 150030, China
| | - Junqiu Wu
- College of Life Science, Northeast Agricultural University, Harbin, 150030, China
| | - Zimin Wei
- College of Life Science, Northeast Agricultural University, Harbin, 150030, China.
| | - Hongyu Yang
- College of Life Science, Northeast Agricultural University, Harbin, 150030, China
| | - Shubo Zhang
- College of Life Science, Northeast Agricultural University, Harbin, 150030, China
| | - Caihong Song
- College of Life Science, Liaocheng University, Liaocheng, 252000, China
| | - Liming Jia
- Environmental Monitoring Center of Heilongjiang Province, Harbin, 150056, China
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25
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Changes in the Dissolved Organic Matter Characteristics Released from Sediment According to Precipitation in the Namhan River with Weirs: A Laboratory Experiment. INTERNATIONAL JOURNAL OF ENVIRONMENTAL RESEARCH AND PUBLIC HEALTH 2022; 19:ijerph19094958. [PMID: 35564354 PMCID: PMC9101428 DOI: 10.3390/ijerph19094958] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 03/08/2022] [Revised: 04/13/2022] [Accepted: 04/15/2022] [Indexed: 02/04/2023]
Abstract
In this study, changes in the properties of dissolved organic matter (DOM) released from sediments into water layers were investigated. To analyze the spatial and temporal variation in dissolved organic carbon (DOC), sediment and bottom water samples were collected upstream of the Gangcheon, Yeoju, and Ipo weirs of the Namhan River during the rainy and non-rainy seasons. The initial DOC was correlated with precipitation (R2 = 0.295, p = 0.034) and residence time (R2 = 0.275, p = 0.040). The change in the bottom water DOC concentration resulted from the DOC released from the sediments, which may cause water quality issues in the bottom water. The fluorescence analysis revealed that the DOM contained higher levels of hydrophilic and low-molecular-weight (LMW) organic matter in the non-rainy season and higher levels of hydrophobic and high-molecular-weight (HMW) organic matter in the rainy season. Since the Namhan River is the main resource of drinking water for the Seoul metropolitan area, our results can help to optimize the drinking water treatment process by reflecting the DOM characteristics that vary with the seasons. Furthermore, the statistical analysis confirmed that the nutrient content of pore-water and sediment can be used to estimate the DOM release rate from the sediment to the water layer. The results of this study provide a better understanding of DOM movement in aquatic ecosystems and the influences of rainfall on the water quality of the surface waterbody.
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26
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Kalinitchenko VP, Glinushkin AP, Minkina TM, Mandzhieva SS, Sushkova SN, Sukovatov VA, Il'ina LP, Makarenkov DA, Zavalin AA, Dudnikova TS, Barbashev AI, Bren DV, Rajput P, Batukaev AA. Intra-soil waste recycling provides safety of environment. ENVIRONMENTAL GEOCHEMISTRY AND HEALTH 2022; 44:1355-1376. [PMID: 34241721 DOI: 10.1007/s10653-021-01023-9] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 02/27/2021] [Accepted: 06/21/2021] [Indexed: 06/13/2023]
Abstract
Amelioration and remediation technology was developed for phosphogypsum utilization in Haplic Chernozem of South-European facies (Rostov Region). The technology comprises phosphogypsum dispersed application into the soil layer of 20-45 cm during intra-soil milling. In the model experiment, the phosphogypsum doses 0 (control), 10, 20, and 40 t ha-1 were studied. The Cd thermodynamic forms in soil solution were calculated via the developed mathematical chemical-thermodynamic model and program ION-3. The form of ion in soil solution (or water extract) was considered accounting the calcium-carbonate equilibrium (CCE) and association of ion pairs CaCO30; CaSO40, MgCO30, MgSO40, CaHCO3+, MgHCO3+, NaCO3-, NaSO4-, CaOH+, MgOH+. For calculation of the equilibrium of microelements concentration in soil solution ion including heavy metals (HMs), the coefficient of microelement association kas was proposed. According to calculations, Cd2+ ion in soil solution was mostly bounded to associates CdOH+, partly to associates CdCO30 and CdHCO3+. The calculated kas of Cd was 1.24 units in the control option of experiment and decreased to 0.95 units at phosphogypsum dose 40 t ha-1. The ratio of "active [Cd2+] to total Cd" reduced from 33.5% in control option to 28.0% in the option of phosphogypsum dose 40 t ha-1. The biogeochemical barrier for penetration of HMs from soil to plant roots was high after application of phosphogypsum. According to calculation by ION-3, the standard soil environmental limitations overestimate the toxicity of Cd in soil solution. New decision for intra-soil milling and simultaneous application of phosphogypsum was developed to provide the environmentally safe waste recycling.
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Affiliation(s)
- Valery P Kalinitchenko
- Institute of Fertility of Soils of South Russia, 2, Krivoshlykova str., Persianovka, Rostov Region, Russia, 346493.
- All-Russian Phytopathology Research Institute of the Russian Academy of Sciences, 5, Institute St., Big Vyazemy, Moscow Region, Russia, 143050.
| | - Alexey P Glinushkin
- All-Russian Phytopathology Research Institute of the Russian Academy of Sciences, 5, Institute St., Big Vyazemy, Moscow Region, Russia, 143050
| | - Tatiana M Minkina
- Southern Federal University, 194/1, Stachki Prosp., Rostov-on-Don, Russia, 344090
| | - Saglara S Mandzhieva
- Southern Federal University, 194/1, Stachki Prosp., Rostov-on-Don, Russia, 344090
| | - Svetlana N Sushkova
- Southern Federal University, 194/1, Stachki Prosp., Rostov-on-Don, Russia, 344090
| | - Vladimir A Sukovatov
- Institute of Fertility of Soils of South Russia, 2, Krivoshlykova str., Persianovka, Rostov Region, Russia, 346493
| | - Ljudmila P Il'ina
- Southern Scientific Center of the Russian Academy of Sciences, 41, Chekhova prosp, Rostov-on-Don, Russia, 344006
| | - Dmitry A Makarenkov
- Institute of Chemical Reagents and High Purity Chemical Substances of National Research Centre Kurchatov Institute, 3, Bogorodskiy Val st, 107076, Moscow, Russia
| | - Alexey A Zavalin
- All-Russian Research Institute for Agrochemistry Named After D.N. Pryanishnikov of the Russian Academy of Sciences, 31a, Pryanishnikova st, Moscow, Russia, 127434
| | - Tamara S Dudnikova
- Southern Federal University, 194/1, Stachki Prosp., Rostov-on-Don, Russia, 344090
| | - Andrey I Barbashev
- Southern Federal University, 194/1, Stachki Prosp., Rostov-on-Don, Russia, 344090
| | - Dmitry V Bren
- Southern Federal University, 194/1, Stachki Prosp., Rostov-on-Don, Russia, 344090
| | - Priyadarshani Rajput
- Southern Federal University, 194/1, Stachki Prosp., Rostov-on-Don, Russia, 344090
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Benthic Biofilm Bacterial Communities and Their Linkage with Water-Soluble Organic Matter in Effluent Receivers. INTERNATIONAL JOURNAL OF ENVIRONMENTAL RESEARCH AND PUBLIC HEALTH 2022; 19:ijerph19041994. [PMID: 35206183 PMCID: PMC8872271 DOI: 10.3390/ijerph19041994] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 01/15/2022] [Revised: 02/04/2022] [Accepted: 02/07/2022] [Indexed: 02/04/2023]
Abstract
Benthic biofilms are pioneering microbial aggregates responding to effluent discharge from wastewater treatment plants (WWTPs). However, knowledge of the characteristics and linkage of bacterial communities and water-soluble organic matter (WSOM) of benthic biofilms in effluent-receiving rivers remains unknown. Here, we investigated the quality of WSOM and the evolution of bacterial communities in benthic biofilm to evaluate the ecological impacts of effluent discharge on a representative receiving water. Tryptophan-like proteins showed an increased proportion in biofilms collected from the discharge area and downstream from the WWTP, especially in summer. Biofilm WSOM showed weak humic character and strong autochthonous components, and species turnover was proven to be the main factor governing biofilm bacteria community diversity patterns. The bacterial community alpha diversity, interspecies interaction, biological index, and humification index were signally altered in the biofilms from the discharge area, while the values were more similar in biofilms collected upstream and downstream from the WWTP, indicating that both biofilm bacterial communities and WSOM characters have resilience capacities. Although effluent discharge simplified the network pattern of the biofilm bacterial community, its metabolic functional abundance was basically stable. The functional abundance of carbohydrate metabolism and amino acid metabolism in the discharge area increased, and the key modules in the non-random co-occurrence network also verified the important ecological role of carbon metabolism in the effluent-receiving river. The study sheds light on how benthic biofilms respond to effluent discharge from both ecological and material points of view, providing new insights on the feasibility of utilizing benthic biofilms as robust indicators reflecting river ecological health.
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Coble AA, Wymore AS, Potter JD, McDowell WH. Land Use Overrides Stream Order and Season in Driving Dissolved Organic Matter Dynamics Throughout the Year in a River Network. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2022; 56:2009-2020. [PMID: 35007420 DOI: 10.1021/acs.est.1c06305] [Citation(s) in RCA: 11] [Impact Index Per Article: 5.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/14/2023]
Abstract
Anthropogenic land use has increased nutrient concentrations and altered dissolved organic matter (DOM) character and its bioavailability. Despite widespread recognition that DOM character and its reactivity can vary temporally, the relative influence of land use and stream order on DOM characteristics is poorly understood across seasons and the entire flow regime. We examined DOM character and 28-day bioavailable dissolved organic carbon (BDOC) across a river network to determine the relative roles of land use and stream order in driving variability in DOM character and bioavailability throughout the year. DOM in 1st-order streams was distinct from higher stream orders with lower DOC concentrations, less aromatic (specific ultraviolet absorbance at 254 nm (SUVA254)), more autochthonous (fluorescence index), and more recently produced (β/α) DOM. Across all months, variability in DOM character was primarily explained by land use, rather than stream order or season. Land use and stream order explained the most DOM variation in transitional and winter months and the least during dry months. BDOC was greater in watersheds with less aromatic (SUVA254) and more recent allochthonous DOM (β/α) and more development and impervious surface. With continued development, the bioavailability of DOM in the smallest and most impacted watersheds is expected to increase.
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Affiliation(s)
- Ashley A Coble
- Department of Natural Resources and the Environment, University of New Hampshire, Durham, New Hampshire 03824, United States
| | - Adam S Wymore
- Department of Natural Resources and the Environment, University of New Hampshire, Durham, New Hampshire 03824, United States
| | - Jody D Potter
- Department of Natural Resources and the Environment, University of New Hampshire, Durham, New Hampshire 03824, United States
| | - William H McDowell
- Department of Natural Resources and the Environment, University of New Hampshire, Durham, New Hampshire 03824, United States
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29
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Zhang H, Zheng Y, Wang XC, Wang Y, Dzakpasu M. Characterization and biogeochemical implications of dissolved organic matter in aquatic environments. JOURNAL OF ENVIRONMENTAL MANAGEMENT 2021; 294:113041. [PMID: 34126535 DOI: 10.1016/j.jenvman.2021.113041] [Citation(s) in RCA: 25] [Impact Index Per Article: 8.3] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/09/2020] [Revised: 05/12/2021] [Accepted: 06/06/2021] [Indexed: 06/12/2023]
Abstract
Dissolved organic matter (DOM) is viewed as one of the most chemically active organic substances on earth. It plays vital roles in the fate, bioavailability and toxicity of aquatic exogenous chemical species (e.g., heavy metals, organic pollutants, and nanomaterials). The characteristics of DOM such low concentrations, salt interference and complexity in aquatic environments and limitations of pretreatment for sample preparation and application of characterization techniques severely limit understanding of its nature and environmental roles. This review provides a characterization continuum of aquatic DOM, and demonstrate its biogeochemical implications, enabling in-depth insight into its nature and environmental roles. A synthesis of the effective DOM pretreatment strategies, comprising extraction and fractionation methods, and characterization techniques is presented. Additionally, the biogeochemical dynamics of aquatic DOM and its environmental implications are discussed. The findings indicate the collection of representative DOM samples from water as the first and critical step for characterizing its properties, dynamics, and environmental implications. However, various pretreatment procedures may alter DOM composition and structure, producing highly variable recoveries and even influencing its subsequent characterization. Therefore, complimentary use of various characterization techniques is highly recommended to obtain as much information on DOM as possible, as each characterization technique exhibits various advantages and limitations. Moreover, DOM could markedly change the physical and chemical properties of exogenous chemical species, influencing their transformation and mobility, and finally altering their potential bioavailability and toxicity. Several research gaps to be addressed include the impact of pretreatment on the composition and structure of aquatic DOM, molecular-level structural elucidation for DOM, and assessment of the effects of DOM dynamics on the fate, bioavailability and toxicity of exogenous chemical species.
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Affiliation(s)
- Hengfeng Zhang
- Key Laboratory of Northwest Water Resource, Environment and Ecology, MOE, Xi'an University of Architecture and Technology, Xi'an, 710055, People's Republic of China; Shaanxi Key Laboratory of Environmental Engineering, Xi'an University of Architecture and Technology, Xi'an, 710055, People's Republic of China; International Science & Technology Cooperation Center for Urban Alternative Water Resources Development, Xi'an University of Architecture and Technology, Xi'an, 710055, People's Republic of China
| | - Yucong Zheng
- Key Laboratory of Northwest Water Resource, Environment and Ecology, MOE, Xi'an University of Architecture and Technology, Xi'an, 710055, People's Republic of China; Shaanxi Key Laboratory of Environmental Engineering, Xi'an University of Architecture and Technology, Xi'an, 710055, People's Republic of China; International Science & Technology Cooperation Center for Urban Alternative Water Resources Development, Xi'an University of Architecture and Technology, Xi'an, 710055, People's Republic of China
| | - Xiaochang C Wang
- Key Laboratory of Northwest Water Resource, Environment and Ecology, MOE, Xi'an University of Architecture and Technology, Xi'an, 710055, People's Republic of China; Shaanxi Key Laboratory of Environmental Engineering, Xi'an University of Architecture and Technology, Xi'an, 710055, People's Republic of China; International Science & Technology Cooperation Center for Urban Alternative Water Resources Development, Xi'an University of Architecture and Technology, Xi'an, 710055, People's Republic of China
| | - Yongkun Wang
- Key Laboratory of Northwest Water Resource, Environment and Ecology, MOE, Xi'an University of Architecture and Technology, Xi'an, 710055, People's Republic of China; Shaanxi Key Laboratory of Environmental Engineering, Xi'an University of Architecture and Technology, Xi'an, 710055, People's Republic of China; International Science & Technology Cooperation Center for Urban Alternative Water Resources Development, Xi'an University of Architecture and Technology, Xi'an, 710055, People's Republic of China
| | - Mawuli Dzakpasu
- Key Laboratory of Northwest Water Resource, Environment and Ecology, MOE, Xi'an University of Architecture and Technology, Xi'an, 710055, People's Republic of China; International Science & Technology Cooperation Center for Urban Alternative Water Resources Development, Xi'an University of Architecture and Technology, Xi'an, 710055, People's Republic of China.
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30
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Weitere M, Altenburger R, Anlanger C, Baborowski M, Bärlund I, Beckers LM, Borchardt D, Brack W, Brase L, Busch W, Chatzinotas A, Deutschmann B, Eligehausen J, Frank K, Graeber D, Griebler C, Hagemann J, Herzsprung P, Hollert H, Inostroza PA, Jäger CG, Kallies R, Kamjunke N, Karrasch B, Kaschuba S, Kaus A, Klauer B, Knöller K, Koschorreck M, Krauss M, Kunz JV, Kurz MJ, Liess M, Mages M, Müller C, Muschket M, Musolff A, Norf H, Pöhlein F, Reiber L, Risse-Buhl U, Schramm KW, Schmitt-Jansen M, Schmitz M, Strachauer U, von Tümpling W, Weber N, Wild R, Wolf C, Brauns M. Disentangling multiple chemical and non-chemical stressors in a lotic ecosystem using a longitudinal approach. THE SCIENCE OF THE TOTAL ENVIRONMENT 2021; 769:144324. [PMID: 33482551 DOI: 10.1016/j.scitotenv.2020.144324] [Citation(s) in RCA: 6] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/30/2020] [Revised: 12/03/2020] [Accepted: 12/05/2020] [Indexed: 06/12/2023]
Abstract
Meeting ecological and water quality standards in lotic ecosystems is often failed due to multiple stressors. However, disentangling stressor effects and identifying relevant stressor-effect-relationships in complex environmental settings remain major challenges. By combining state-of-the-art methods from ecotoxicology and aquatic ecosystem analysis, we aimed here to disentangle the effects of multiple chemical and non-chemical stressors along a longitudinal land use gradient in a third-order river in Germany. We distinguished and evaluated four dominant stressor categories along this gradient: (1) Hydromorphological alterations: Flow diversity and substrate diversity correlated with the EU-Water Framework Directive based indicators for the quality element macroinvertebrates, which deteriorated at the transition from near-natural reference sites to urban sites. (2) Elevated nutrient levels and eutrophication: Low to moderate nutrient concentrations together with complete canopy cover at the reference sites correlated with low densities of benthic algae (biofilms). We found no more systematic relation of algal density with nutrient concentrations at the downstream sites, suggesting that limiting concentrations are exceeded already at moderate nutrient concentrations and reduced shading by riparian vegetation. (3) Elevated organic matter levels: Wastewater treatment plants (WWTP) and stormwater drainage systems were the primary sources of bioavailable dissolved organic carbon. Consequently, planktonic bacterial production and especially extracellular enzyme activity increased downstream of those effluents showing local peaks. (4) Micropollutants and toxicity-related stress: WWTPs were the predominant source of toxic stress, resulting in a rapid increase of the toxicity for invertebrates and algae with only one order of magnitude below the acute toxic levels. This toxicity correlates negatively with the contribution of invertebrate species being sensitive towards pesticides (SPEARpesticides index), probably contributing to the loss of biodiversity recorded in response to WWTP effluents. Our longitudinal approach highlights the potential of coordinated community efforts in supplementing established monitoring methods to tackle the complex phenomenon of multiple stress.
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Affiliation(s)
- Markus Weitere
- Helmholtz Centre for Environmental Research - UFZ, Department River Ecology, Brückstr. 3a, 39114 Magdeburg, Germany.
| | - Rolf Altenburger
- Helmholtz Centre for Environmental Research - UFZ, Department of Bioanalytical Ecotoxicology, Permoserstr. 15, 04318 Leipzig, Germany; RWTH Aachen University, Institute for Environmental Research, Worringer Weg 1, 52074 Aachen, Germany
| | - Christine Anlanger
- Helmholtz Centre for Environmental Research - UFZ, Department River Ecology, Brückstr. 3a, 39114 Magdeburg, Germany
| | - Martina Baborowski
- Helmholtz Centre for Environmental Research - UFZ, Department River Ecology, Brückstr. 3a, 39114 Magdeburg, Germany
| | - Ilona Bärlund
- Helmholtz Centre for Environmental Research - UFZ, Department of Aquatic Ecosystems Analysis, Brückstr. 3a, 39114 Magdeburg, Germany
| | - Liza-Marie Beckers
- Helmholtz Centre for Environmental Research - UFZ, Department of Effect-Directed Analysis, Permoserstr. 15, 04318 Leipzig, Germany, PAI
| | - Dietrich Borchardt
- Helmholtz Centre for Environmental Research - UFZ, Department of Aquatic Ecosystems Analysis, Brückstr. 3a, 39114 Magdeburg, Germany
| | - Werner Brack
- Helmholtz Centre for Environmental Research - UFZ, Department of Effect-Directed Analysis, Permoserstr. 15, 04318 Leipzig, Germany, PAI; RWTH Aachen University, Institute for Environmental Research, Worringer Weg 1, 52074 Aachen, Germany; Goethe University Frankfurt, Department of Evolutionary Ecology and Environmental Toxicology, Max-von-Laue-Str. 13, 60438 Frankfurt am Main, Germany
| | - Lisa Brase
- Helmholtz Centre Geesthacht - HZG, Department of Aquatic Nutrient Cycles, Max-Planck-Straße 1, 21502 Geesthacht, Germany
| | - Wibke Busch
- Helmholtz Centre for Environmental Research - UFZ, Department of Bioanalytical Ecotoxicology, Permoserstr. 15, 04318 Leipzig, Germany
| | - Antonis Chatzinotas
- Helmholtz Centre for Environmental Research - UFZ, Department of Environmental Microbiology, Permoserstr. 15, 04318 Leipzig, Germany; Leipzig University, Institute of Biology, Talstrasse 33, 04103 Leipzig, Germany
| | - Björn Deutschmann
- RWTH Aachen University, Institute for Environmental Research, Worringer Weg 1, 52074 Aachen, Germany
| | - Jens Eligehausen
- Helmholtz Centre for Environmental Research - UFZ, Department of Aquatic Ecosystems Analysis, Brückstr. 3a, 39114 Magdeburg, Germany; University of Kassel, Department of Landscape Ecology, Gottschalkstr. 26A, 34127 Kassel, Germany
| | - Karin Frank
- Helmholtz Centre for Environmental Research - UFZ, Department of Ecological Modelling, Permoserstr. 15, 04318 Leipzig, Germany
| | - Daniel Graeber
- Helmholtz Centre for Environmental Research - UFZ, Department of Aquatic Ecosystems Analysis, Brückstr. 3a, 39114 Magdeburg, Germany
| | - Christian Griebler
- Helmholtz Zentrum München - German Research Center for Environmental Health (GmbH), Institute of Groundwater Ecology, Ingolstädter Landstrasse 1, 85764 Neuherberg, Germany; University of Vienna, Department for Functional and Evolutionary Ecology, Althanstrasse 14, 1090 Wien, Austria
| | - Jeske Hagemann
- Helmholtz Centre for Environmental Research - UFZ, Department of Aquatic Ecosystems Analysis, Brückstr. 3a, 39114 Magdeburg, Germany
| | - Peter Herzsprung
- Helmholtz Centre for Environmental Research - UFZ, Department Lake Research, Brückstr. 3a, 39114 Magdeburg, Germany
| | - Henner Hollert
- RWTH Aachen University, Institute for Environmental Research, Worringer Weg 1, 52074 Aachen, Germany; Goethe University Frankfurt, Department of Evolutionary Ecology and Environmental Toxicology, Max-von-Laue-Str. 13, 60438 Frankfurt am Main, Germany
| | - Pedro A Inostroza
- Helmholtz Centre for Environmental Research - UFZ, Department of Effect-Directed Analysis, Permoserstr. 15, 04318 Leipzig, Germany, PAI
| | - Christoph G Jäger
- Helmholtz Centre for Environmental Research - UFZ, Department of Aquatic Ecosystems Analysis, Brückstr. 3a, 39114 Magdeburg, Germany; Rosenheim Technical University of Applied Sciences, Centre for Research, Development and Technology Transfer, Hochschulstraße 1, 83024 Rosenheim, Germany
| | - René Kallies
- Helmholtz Centre for Environmental Research - UFZ, Department of Environmental Microbiology, Permoserstr. 15, 04318 Leipzig, Germany
| | - Norbert Kamjunke
- Helmholtz Centre for Environmental Research - UFZ, Department River Ecology, Brückstr. 3a, 39114 Magdeburg, Germany
| | - Bernhard Karrasch
- Helmholtz Centre for Environmental Research - UFZ, Department River Ecology, Brückstr. 3a, 39114 Magdeburg, Germany
| | - Sigrid Kaschuba
- Helmholtz Zentrum München - German Research Center for Environmental Health (GmbH), Institute of Groundwater Ecology, Ingolstädter Landstrasse 1, 85764 Neuherberg, Germany
| | - Andrew Kaus
- Helmholtz Centre for Environmental Research - UFZ, Department of Aquatic Ecosystems Analysis, Brückstr. 3a, 39114 Magdeburg, Germany
| | - Bernd Klauer
- Helmholtz Centre for Environmental Research - UFZ, Department of Economics, Permoserstraße 15, 04318 Leipzig, Germany
| | - Kay Knöller
- Helmholtz Centre for Environmental Research - UFZ, Department Catchment Hydrology, Theodor-Lieser-Str. 4, 06120 Halle, Germany
| | - Matthias Koschorreck
- Helmholtz Centre for Environmental Research - UFZ, Department Lake Research, Brückstr. 3a, 39114 Magdeburg, Germany
| | - Martin Krauss
- Helmholtz Centre for Environmental Research - UFZ, Department of Effect-Directed Analysis, Permoserstr. 15, 04318 Leipzig, Germany, PAI
| | - Julia V Kunz
- Helmholtz Centre for Environmental Research - UFZ, Department of Aquatic Ecosystems Analysis, Brückstr. 3a, 39114 Magdeburg, Germany
| | - Marie J Kurz
- Helmholtz Centre for Environmental Research - UFZ, Department Hydrogeology, Permoserstraße 15, 04318 Leipzig, Germany
| | - Matthias Liess
- Helmholtz Centre for Environmental Research -UFZ, Department of System-Ecotoxicology, Permoserstr. 15, 04318 Leipzig, Germany; RWTH Aachen University, Institute for Environmental Research (Biology V), Aachen, Germany
| | - Margarete Mages
- Helmholtz Centre for Environmental Research - UFZ, Department River Ecology, Brückstr. 3a, 39114 Magdeburg, Germany
| | - Christin Müller
- Helmholtz Centre for Environmental Research - UFZ, Department Catchment Hydrology, Theodor-Lieser-Str. 4, 06120 Halle, Germany
| | - Matthias Muschket
- Helmholtz Centre for Environmental Research - UFZ, Department of Effect-Directed Analysis, Permoserstr. 15, 04318 Leipzig, Germany, PAI
| | - Andreas Musolff
- Helmholtz Centre for Environmental Research - UFZ, Department Hydrogeology, Permoserstraße 15, 04318 Leipzig, Germany
| | - Helge Norf
- Helmholtz Centre for Environmental Research - UFZ, Department River Ecology, Brückstr. 3a, 39114 Magdeburg, Germany; Helmholtz Centre for Environmental Research - UFZ, Department of Aquatic Ecosystems Analysis, Brückstr. 3a, 39114 Magdeburg, Germany
| | - Florian Pöhlein
- Helmholtz Centre for Environmental Research - UFZ, Department Lake Research, Brückstr. 3a, 39114 Magdeburg, Germany
| | - Lena Reiber
- Helmholtz Centre for Environmental Research -UFZ, Department of System-Ecotoxicology, Permoserstr. 15, 04318 Leipzig, Germany; RWTH Aachen University, Institute for Environmental Research (Biology V), Aachen, Germany
| | - Ute Risse-Buhl
- Helmholtz Centre for Environmental Research - UFZ, Department River Ecology, Brückstr. 3a, 39114 Magdeburg, Germany
| | - Karl-Werner Schramm
- Helmholtz Zentrum München-German Research Center for Environmental Health (GmbH), Molecular EXposomics, Ingolstädter Landstr. 1, 85764 Neuherberg, Germany; Technische Universität München, Department für Biowissenschaftliche Grundlagen, Weihenstephaner Steig 23, 85350 Freising, Germany
| | - Mechthild Schmitt-Jansen
- Helmholtz Centre for Environmental Research - UFZ, Department of Bioanalytical Ecotoxicology, Permoserstr. 15, 04318 Leipzig, Germany
| | - Markus Schmitz
- RWTH Aachen University, Institute for Environmental Research, Worringer Weg 1, 52074 Aachen, Germany; Goethe University Frankfurt, Department of Evolutionary Ecology and Environmental Toxicology, Max-von-Laue-Str. 13, 60438 Frankfurt am Main, Germany
| | - Ulrike Strachauer
- Helmholtz Centre for Environmental Research - UFZ, Department of Aquatic Ecosystems Analysis, Brückstr. 3a, 39114 Magdeburg, Germany
| | - Wolf von Tümpling
- Helmholtz Centre for Environmental Research - UFZ, Department River Ecology, Brückstr. 3a, 39114 Magdeburg, Germany
| | - Nina Weber
- Helmholtz Zentrum München - German Research Center for Environmental Health (GmbH), Institute of Groundwater Ecology, Ingolstädter Landstrasse 1, 85764 Neuherberg, Germany
| | - Romy Wild
- Helmholtz Centre for Environmental Research - UFZ, Department River Ecology, Brückstr. 3a, 39114 Magdeburg, Germany
| | - Christine Wolf
- Helmholtz Centre for Environmental Research - UFZ, Department of Economics, Permoserstraße 15, 04318 Leipzig, Germany
| | - Mario Brauns
- Helmholtz Centre for Environmental Research - UFZ, Department River Ecology, Brückstr. 3a, 39114 Magdeburg, Germany
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Kalinitchenko VP, Glinushkin AP, Swidsinski AV, Minkina TM, Andreev AG, Mandzhieva SS, Sushkova SN, Makarenkov DA, Ilyina LP, Chernenko VV, Zamulina IV, Larin GS, Zavalin AA, Gudkov SV. Thermodynamic mathematical model of the Kastanozem complex and new principles of sustainable semiarid protective silviculture management. ENVIRONMENTAL RESEARCH 2021; 194:110605. [PMID: 33316230 DOI: 10.1016/j.envres.2020.110605] [Citation(s) in RCA: 3] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 05/21/2020] [Revised: 10/23/2020] [Accepted: 12/05/2020] [Indexed: 06/12/2023]
Abstract
The Kastanozem complex in the dry steppe of southern Russia underlies an artificially-constructed forest strips. Deep ploughing to a depth of 45 cm was used to process the soil prior to planting. Between 20 and 40 cm depth, soil density was high, 1.57 t m-3. Soil hardness was also high, 440 psi. Soil aggregates greater than 5 cm in size were impermeable to tree roots. The content of such aggregates was high, comprising 35%. The number of tree roots with diameters greater than 0.5 cm that cross the soil profile was as low as 0.15 to 0.3 pcs cm-2. The soil matric potential signifying water availability was low in the vegetation period -0.9 MPa to a depth of 1.0 m. According to modelling experiments, the main salt components in the soil solution drive the transfer of soil organic matter (SOM) and heavy metals (HM). The composition of the soil solution determined by the calcium carbonate equilibrium (CCE) and the association and complexation of ions. ION-3 software was used to calculate the ion equilibrium in the soil solution. Macro-ions Cа2+, Mg2+, SO42-, and CO32- partly bonded as ion pairs. Oversaturation of the soil solution with CaCO3 was calculated according to the analytical content of macro-ion, which was high up to 1000 units, and its value decreased in response to ionic strength, activity, association, complexation, and thermodynamic equilibrium of macro-ions in the soil solution. Oversaturation calculated for Salic Solonetz and Gleyic Solonetz soil solutions was small considering the SOM content. Calculations indicate the profile and lateral loss of C from the soil to the vadose zone. The content of Pb in the soil solution was calculated sirca 75%-80%. The calculated coefficient of Pb2+ association was as high as 52.0. The probability of Pb passivation by SOM in the Kastanozem complex was significant. The probability of uncontrolled transfer and accumulation of HM in the soil and vadose zone was high. Biogeosystem Technique (BGT*) transcendental methodology, an innovative methodology created for stable geomorphological system formation to achieve sustainable agriculture and silviculture, was applied. The BGT* elements were: intra-soil milling of the 30-60 cm soil layer for geophysical conditioning; intra-soil continuously-discrete pulse watering for plants and trees to improve the hydrologic regime. The BGT* methodology reduced HM mobility, controlled biodegradation, enriched nutrient biogeochemical cycling, increased C content, increased soil productivity, and reversible carbon sequester in biological form.
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Affiliation(s)
- Valery P Kalinitchenko
- Institute of Fertility of Soils of South Russia, 346493, Krivoshlykova St., 2, Persianovka, Rostov Region, Russia; All-Russian Research Institute for Phytopathology of the Russian Academy of Sciences, 143050, Institute St., 5, Big Vyazyomy, Moscow Region, Russia.
| | - Alexey P Glinushkin
- All-Russian Research Institute for Phytopathology of the Russian Academy of Sciences, 143050, Institute St., 5, Big Vyazyomy, Moscow Region, Russia
| | | | - Tatiana M Minkina
- Southern Federal University, 344006, Bolshaya Sadovaya str., 105/42, Rostov-on-Don, Russia
| | - Andrey G Andreev
- Institute of Fertility of Soils of South Russia, 346493, Krivoshlykova St., 2, Persianovka, Rostov Region, Russia
| | - Saglara S Mandzhieva
- Southern Federal University, 344006, Bolshaya Sadovaya str., 105/42, Rostov-on-Don, Russia
| | - Svetlana N Sushkova
- Southern Federal University, 344006, Bolshaya Sadovaya str., 105/42, Rostov-on-Don, Russia
| | - Dmitry A Makarenkov
- Institute of Chemical Reagents and High Purity Chemical Substances of the National Research Centre "Kurchatov Institute", 107076, Bogorodsky Val St., 3, Moscow, Russia
| | - Lyudmila P Ilyina
- Southern Scientific Center of the Russian Academy of Sciences, 344006, Chekhova Ave., 41, Rostov-on-Don, Russia
| | - Vladimir V Chernenko
- Institute of Fertility of Soils of South Russia, 346493, Krivoshlykova St., 2, Persianovka, Rostov Region, Russia
| | - Inna V Zamulina
- Southern Federal University, 344006, Bolshaya Sadovaya str., 105/42, Rostov-on-Don, Russia
| | - George S Larin
- Institute of Fertility of Soils of South Russia, 346493, Krivoshlykova St., 2, Persianovka, Rostov Region, Russia
| | - Alexey A Zavalin
- All-Russian Institute for Agrochemistry named after D.N. Pryanishnikov of the Russian Academy of Sciences, 127434, Pryanishnikova St., 31a, Moscow, Russia
| | - Sergey V Gudkov
- Prokhrov General Physics Institute of the Russian Academy of Sciences, 119991, Vavilova St., 38, Moscow, Russia
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32
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Aguilar-Alarcón P, Gonzalez SV, Simonsen MA, Borrero-Santiago AR, Sanchís J, Meriac A, Kolarevic J, Asimakopoulos AG, Mikkelsen Ø. Characterizing changes of dissolved organic matter composition with the use of distinct feeds in recirculating aquaculture systems via high-resolution mass spectrometry. THE SCIENCE OF THE TOTAL ENVIRONMENT 2020; 749:142326. [PMID: 33370913 DOI: 10.1016/j.scitotenv.2020.142326] [Citation(s) in RCA: 12] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/19/2020] [Revised: 09/07/2020] [Accepted: 09/08/2020] [Indexed: 06/12/2023]
Abstract
Recirculating aquaculture systems (RAS) are a new alternative to traditional aquaculture approaches, allowing full control over the fish production conditions, while reducing the water demand. The reduction of water exchange leads to an accumulation of dissolved organic matter (DOM) that can have potential effects on water quality, fish welfare and system performance. Despite the growing awareness of DOM in aquaculture, scarce scientific information exists for understanding the composition and transformation of DOM in RAS. In this study, a non-targeted approach using ultra-performance liquid chromatography coupled to a hybrid quadrupole-time of flight mass spectrometer (UPLC-QTOF-MS) was used to characterize compositional changes of low molecular weight (LMW) DOM in RAS, when operated under two different feed types. A total of 1823 chemicals were identified and the majority of those contained a CHON chemical group in their structure. Changes in the composition of LMW-DOM in RAS waters were observed when the standard feed was switched to RAS feed. The DOM with the use of standard feed, consisted mainly of lignin/CRAM-like, CHO and CHOS chemical groups, while the DOM that used RAS feed, was mainly composed by unsaturated hydrocarbon, CHNO and CHNOS chemical groups. The Bray-Curtis dissimilarity cluster demonstrated differences in the composition of DOM from RAS and was associated to the type of feed used. When the RAS feed was used, the Kendrick mass defect plots of -CH2- homologous units in the pump-sump (after the water treatment) showed a high removal capacity for CHNO, CHNOS and halogenated chemicals with high Kendrick mass defect, KMD > 0.7. To our knowledge, this is the first report of LMW-DOM characterization of RAS by high-resolution mass spectrometry (HRMS).
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Affiliation(s)
- Patricia Aguilar-Alarcón
- Department of Chemistry, Norwegian University of Science and Technology, Høgskoleringen 1, 7491 Trondheim, Norway.
| | - Susana V Gonzalez
- Department of Chemistry, Norwegian University of Science and Technology, Høgskoleringen 1, 7491 Trondheim, Norway
| | - Mads A Simonsen
- Department of Mathematical Sciences, Norwegian University of Science and Technology, Høgskoleringen 1, 7491 Trondheim, Norway
| | - Ana R Borrero-Santiago
- Department of Chemistry, Norwegian University of Science and Technology, Høgskoleringen 1, 7491 Trondheim, Norway
| | - Josep Sanchís
- Catalan Institute for Water Research (ICRA), Scientific and Technological Park of the University of Girona, H(2)O Building, C/Emili Grahit, 101, E17003 Girona, Spain; University of Girona, 17071 Girona, Spain
| | | | | | - Alexandros G Asimakopoulos
- Department of Chemistry, Norwegian University of Science and Technology, Høgskoleringen 1, 7491 Trondheim, Norway.
| | - Øyvind Mikkelsen
- Department of Chemistry, Norwegian University of Science and Technology, Høgskoleringen 1, 7491 Trondheim, Norway
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33
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Kurek MR, Poulin BA, McKenna AM, Spencer RGM. Deciphering Dissolved Organic Matter: Ionization, Dopant, and Fragmentation Insights via Fourier Transform-Ion Cyclotron Resonance Mass Spectrometry. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2020; 54:16249-16259. [PMID: 33211479 DOI: 10.1021/acs.est.0c05206] [Citation(s) in RCA: 13] [Impact Index Per Article: 3.3] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/06/2023]
Abstract
Fourier transform-ion cyclotron resonance mass spectrometry (FT-ICR MS) has been increasingly employed to characterize dissolved organic matter (DOM) across a range of aquatic environments highlighting the role of DOM in global carbon cycling. DOM analysis commonly utilizes electrospray ionization (ESI), while some have implemented other techniques, including dopant-assisted atmospheric pressure photoionization (APPI). We compared various extracted DOM compositions analyzed by negative ESI and positive APPI doped with both toluene and tetrahydrofuran (THF), including a fragmentation study of THF-doped riverine DOM using infrared multiple photon dissociation (IRMPD). DOM compositions followed the same trends in ESI and dopant-assisted APPI with the latter presenting saturated, less oxygenated, and more N-containing compounds than ESI. Between the APPI dopants, THF-doping yielded spectra with more aliphatic-like and N-containing compounds than toluene-doping. We further demonstrate how fragmentation of THF-doped DOM in APPI resolved subtle differences between riverine DOM that was absent from ESI. In both ionization methods, we describe a linear relationship between atomic and formulaic N-compositions from a range of DOM extracts. This study highlights that THF-doped APPI is useful for uncovering low-intensity aliphatic and peptide-like components in autochthonous DOM, which could aid environmental assessments of DOM across biolability gradients.
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Affiliation(s)
- Martin R Kurek
- National High Magnetic Field Laboratory Geochemistry Group and Department of Earth, Ocean, and Atmospheric Science, Florida State University, Tallahassee, Florida 32306, United States
| | - Brett A Poulin
- U.S. Geological Survey, Water Mission Area, Boulder, Colorado 80303, United States
- Department of Environmental Toxicology, University of California Davis, Davis, California 95616, United States
| | - Amy M McKenna
- National High Magnetic Field Laboratory Ion Cyclotron Resonance Facility, Tallahassee, Florida 32310, United States
| | - Robert G M Spencer
- National High Magnetic Field Laboratory Geochemistry Group and Department of Earth, Ocean, and Atmospheric Science, Florida State University, Tallahassee, Florida 32306, United States
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34
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Liao K, Hu H, Ren H. Combined influences of process parameters on microorganism-derived dissolved organic nitrogen (mDON) formation at low temperatures: Multivariable statistical and systematic analysis. THE SCIENCE OF THE TOTAL ENVIRONMENT 2020; 744:140732. [PMID: 32711305 DOI: 10.1016/j.scitotenv.2020.140732] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 05/15/2020] [Revised: 06/29/2020] [Accepted: 07/02/2020] [Indexed: 06/11/2023]
Abstract
Regulation of process parameters is a cost-effective approach to control microorganism-derived dissolved organic nitrogen (mDON) formation in low-temperature biological wastewater conditions. However, the integrated influence of multiple parameters in this process is poorly defined. In this study, mathematical methodology was used to evaluate the combined effects of hydraulic retention time (HRT), solids retention time (SRT), and mixed liquor suspended solids (MLSS) on mDON formation at 8 °C. This study also systematically explored how multiple combinations of those three parameters affected mDON chemodiversity (fluorescent properties and molecular compositions), microbial compositions, and specific relationships between mDON molecules and microbial species in activated sludge systems. Results showed that combined effects significantly controlled the mDON formation at 8 °C (P < .05). The systematic analysis suggested that the multi-parameter effects modulated the distribution of different mDON compositions and shaped the microbial communities. Most bacterial phyla as the generalist and a few as the specialist were displayed in 2487 pairs of strong microbe-mDON connections (|r| ≥ 0.6, P < .05). Moreover, network analysis on microbe-mDON relationships identified the network centers as crucial media in terms of combined effects of process parameters on mDON formation. Our results provide comprehensive insight on the roles of multi-parameter covariation influences in regulating the high complexity of mDON traits and microbe-mDON linkages, thereby highlighting the necessity to focus on the combined effects of process parameters for effective and correct controlling strategies on mDON concentrations.
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Affiliation(s)
- Kewei Liao
- State Key Laboratory of Pollution Control and Resource Reuse, School of the Environment, Nanjing University, Nanjing 210023, Jiangsu, China
| | - Haidong Hu
- State Key Laboratory of Pollution Control and Resource Reuse, School of the Environment, Nanjing University, Nanjing 210023, Jiangsu, China
| | - Hongqiang Ren
- State Key Laboratory of Pollution Control and Resource Reuse, School of the Environment, Nanjing University, Nanjing 210023, Jiangsu, China.
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35
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Herzsprung P, Wentzky V, Kamjunke N, von Tümpling W, Wilske C, Friese K, Boehrer B, Reemtsma T, Rinke K, Lechtenfeld OJ. Improved Understanding of Dissolved Organic Matter Processing in Freshwater Using Complementary Experimental and Machine Learning Approaches. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2020; 54:13556-13565. [PMID: 32966053 DOI: 10.1021/acs.est.0c02383] [Citation(s) in RCA: 24] [Impact Index Per Article: 6.0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/11/2023]
Abstract
Dissolved organic matter plays an important role in aquatic ecosystems and poses a major problem for drinking water production. However, our understanding of DOM reactivity in natural systems is hampered by its complex molecular composition. Here, we used Fourier-transform ion cyclotron resonance mass spectrometry (FT-ICR-MS) and data from two independent studies to disentangle DOM reactivity based on photochemical and microbial-induced transformations. Robust correlations of FT-ICR-MS peak intensities with chlorophyll a and solar irradiation were used to define 9 reactivity classes for 1277 common molecular formulas. Germany's largest drinking water reservoir was sampled for 1 year, and DOM processing in stratified surface waters could be attributed to photochemical transformations during summer months. Microbial DOM alterations could be distinguished based on correlation coefficients with chlorophyll a and often shared molecular features (elemental ratios and mass) with photoreactive compounds. In particular, many photoproducts and some microbial products were identified as potential precursors of disinfection byproducts. Molecular DOM features were used to further predict molecular reactivity for the remaining compounds in the data set based on a random forest model. Our method offers an expandable classification approach to integrate the reactivity of DOM from specific environments and link it to molecular properties and chemistry.
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Affiliation(s)
- Peter Herzsprung
- Department Lake Research, UFZ - Helmholtz Centre for Environmental Research, Brückstraße 3a, D-39114 Magdeburg, Germany
| | - Valerie Wentzky
- Department Lake Research, UFZ - Helmholtz Centre for Environmental Research, Brückstraße 3a, D-39114 Magdeburg, Germany
| | - Norbert Kamjunke
- Department River Ecology, UFZ - Helmholtz Centre for Environmental Research, Brückstraße 3a, D-39114 Magdeburg, Germany
| | - Wolf von Tümpling
- Department River Ecology, UFZ - Helmholtz Centre for Environmental Research, Brückstraße 3a, D-39114 Magdeburg, Germany
| | - Christin Wilske
- Department River Ecology, UFZ - Helmholtz Centre for Environmental Research, Brückstraße 3a, D-39114 Magdeburg, Germany
| | - Kurt Friese
- Department Lake Research, UFZ - Helmholtz Centre for Environmental Research, Brückstraße 3a, D-39114 Magdeburg, Germany
| | - Bertram Boehrer
- Department Lake Research, UFZ - Helmholtz Centre for Environmental Research, Brückstraße 3a, D-39114 Magdeburg, Germany
| | - Thorsten Reemtsma
- Department Analytical Chemistry, UFZ - Helmholtz Centre for Environmental Research, Permoserstr. 15, D-04318 Leipzig, Germany
- Institute of Analytical Chemistry, University of Leipzig, D-04103, Leipzig, Germany
| | - Karsten Rinke
- Department Lake Research, UFZ - Helmholtz Centre for Environmental Research, Brückstraße 3a, D-39114 Magdeburg, Germany
| | - Oliver J Lechtenfeld
- Department Analytical Chemistry, UFZ - Helmholtz Centre for Environmental Research, Permoserstr. 15, D-04318 Leipzig, Germany
- ProVIS - Centre for Chemical Microscopy, UFZ - Helmholtz Centre for Environmental Research, Permoserstr. 15, D-04318 Leipzig, Germany
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Structural Characterization of Dissolved Organic Matter in Permafrost Peatland Lakes. WATER 2020. [DOI: 10.3390/w12113059] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 12/18/2022]
Abstract
Thermokarst lakes result from the thawing of ice-rich permafrost and are widespread across northern landscapes. These waters are strong emitters of methane, especially in permafrost peatland regions, where they are stained black by high concentrations of dissolved organic matter (DOM). In the present study, we aimed to structurally characterize the DOM from a set of peatland thermokarst lakes that are known to be intense sites of microbial decomposition and methane emission. Samples were collected at different depths from three thermokarst lakes in the Sasapimakwananisikw (SAS) River valley near the eastern Hudson Bay community of Kuujjuarapik–Whapmagoostui (Nunavik, Canada). Samples were analyzed by spectrofluorometry, Fourier-transform infrared spectroscopy (FTIR), nuclear magnetic resonance spectroscopy (NMR), and elemental analysis. Fluorescence analyses indicated considerable amounts of autochthonous DOM in the surface waters of one of SAS 1A, indicating a strong bioavailability of labile DOM, and consequently a greater methanogenic potential. The three lakes differed in their chemical composition and diversity, suggesting various DOM transformations phenomena. The usefulness of complementary analytical approaches to characterize the complex mixture of DOM in permafrost peatland waters cannot be overlooked, representing a first step towards greater comprehension of the organic geochemical properties of these permafrost-derived systems.
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Kalinitchenko VP, Glinushkin AP, Minkina TM, Mandzhieva SS, Sushkova SN, Sukovatov VA, Il’ina LP, Makarenkov DA. Chemical Soil-Biological Engineering Theoretical Foundations, Technical Means, and Technology for Safe Intrasoil Waste Recycling and Long-Term Higher Soil Productivity. ACS OMEGA 2020; 5:17553-17564. [PMID: 32715240 PMCID: PMC7377223 DOI: 10.1021/acsomega.0c02014] [Citation(s) in RCA: 8] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Received: 05/01/2020] [Accepted: 06/22/2020] [Indexed: 05/21/2023]
Abstract
The amelioration and remediation technology was developed on the basis of research of phosphogypsum and utilization in the Haplic Chernozem of South-European facies (Rostov Region). Phosphogypsum was utilized via dispersed application into a soil layer of 20-45 cm with intrasoil milling of this layer. The phosphogypsum utilization doses were 0, 10, 20, and 40 t ha-1. The Pb analytical content in soil solution was studied in the model experiment. The soil solution Pb thermodynamic forms were calculated. The mathematical chemical-thermodynamic model ION-2 was developed to calculate the real soil solution (water extract) calcium-carbonate equilibrium (CCE) ion forms, considering the ion pair association. The associated ion pairs CaCO3 0, CaSO4 0, MgCO3 0, MgSO4 0, CaHCO3 +, MgHCO3 +, NaCO3 -, NaSO4 -, CaOH+, and MgOH+ were accounted for in soil solution equilibrium macroion form calculation. The procedure for the microelement ion [including heavy metals (HMs)] equilibrium concentration in the soil solution coefficient k as calculation was proposed to account for the real soil solution CCE, macroions, and HM (including Pb) association. The Pb2+ ion in soil solution was mostly bound to associates PbOH+, Pb(OH)2 0, PbCO3 0, Pb(CO3)2 2-, and PbHCO3 +. The calculation of CCE and ion association in soil solution revealed 14.5-21.5 times HM passivation compared to HM water-soluble values. The calculated HM activity in the soil solution in the example of the Pb2+ ion was less than 4% after phosphogypsum application in the target amelioration layer of 20-45 cm. The studied phosphogypsum doses were substantiated as environmentally safe. This was because the real soil solution CCE provided HM ion form association and consequent passivation. The dry steppe soil remediation after phosphogypsum application was justified as highly probable. The intrasoil milling chemical soil-biological engineering technology was developed for simultaneous soil amelioration and remediation on the basis of the biogeosystem technique (BGT*) transcendental methodology. The BGT*-based technology was tested in the long-term field experiments and is capable of ensuring the priority geophysical micro- and macroaggregate structure via intrasoil milling and mixing of soil illuvial and transitional horizons. This helps synthesize soil multilevel architecture, providing intrasoil-dispersed environmentally safe recycling of wastes of different origin. Addressing the environment safety concerns, a new decision of the intrasoil milling device was proposed for phosphogypsum and other substance application to soil.
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Affiliation(s)
- Valery P. Kalinitchenko
- Institute
of Fertility of Soils of South Russia, Krivoshlykova Street, 2, Persianovka, Oktyabr’skii district, Rostov Region 346493, Russia
- All-Russian
Phytopathology Research Institute RAS, Institute Street, 5, Big Vyazemy, Moscow Region 143050, Russia
| | - Alexey P. Glinushkin
- All-Russian
Phytopathology Research Institute RAS, Institute Street, 5, Big Vyazemy, Moscow Region 143050, Russia
| | - Tatiana M. Minkina
- Southern
Federal University, Prosp. Stachki, 194/1, Rostov-on-Don 344090, Russia
| | | | - Svetlana N. Sushkova
- Southern
Federal University, Prosp. Stachki, 194/1, Rostov-on-Don 344090, Russia
| | - Vladimir A. Sukovatov
- Institute
of Fertility of Soils of South Russia, Krivoshlykova Street, 2, Persianovka, Oktyabr’skii district, Rostov Region 346493, Russia
| | - Ljudmila P. Il’ina
- Southern
Scientific Center RAS, Prosp. Chekhova, 41, Rostov-on-Don 344006, Russia
| | - Dmitry A. Makarenkov
- Institute
of Chemical Reagents and High Purity Chemical Substances of National
Research Centre Kurchatov Institute, Bogorodsky Rampart, 3, Moscow 107076, Russia
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38
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Quality of Dissolved Organic Matter Driven by Autotrophic and Heterotrophic Microbial Processes in a Large River. WATER 2020. [DOI: 10.3390/w12061577] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 11/16/2022]
Abstract
Rivers are regarded as important sites for processing of dissolved organic matter (DOM) from terrestrial sources on its way to the ocean. However, little is known about the longitudinal change of DOM molecular composition in large rivers. Here we performed a Lagrangian sampling in the lower part of the Middle Elbe at low discharge conditions to test how DOM composition changes along the river stretch and how this is related to microbial processes. The concentration of dissolved organic carbon and fluorescence indices showed only subtle longitudinal differences. In contrast, ultra-high-resolution mass spectrometry analysis of riverine DOM detected pronounced changes in molecular composition. Also, chlorophyll a concentration, bacterial abundance, and bacterial production all increased downstream. The three microbial parameters were positively related to intensities of CHO and CHNO molecular formulas with high hydrogen/carbon and low oxygen/carbon ratios but negatively to several CHOS surfactants. To disentangle the role of autotrophic and heterotrophic processes, we developed a new approach and compared slopes from linear regression of DOM compound intensities versus chlorophyll a concentration and bacteria abundance. As a result, most of the positive related DOM compounds were produced by bacteria. In conclusion, longitudinal changes of river DOM seemed to be largely driven by microbial processes.
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