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Kang H, Kim S, Song K, Kwon MJ, Lee J. Intermediate Disturbances Enhance Microbial Enzyme Activities in Soil Ecosystems. Microorganisms 2024; 12:1401. [PMID: 39065169 PMCID: PMC11278743 DOI: 10.3390/microorganisms12071401] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/06/2024] [Revised: 07/08/2024] [Accepted: 07/10/2024] [Indexed: 07/28/2024] Open
Abstract
The Intermediate Disturbance Hypothesis (IDH) posits that maximal plant biodiversity is attained in environments characterized by moderate ecological disturbances. Although the applicability of the IDH to microbial diversity has been explored in a limited number of studies, there is a notable absence of experimental reports on whether soil microbial 'activity' demonstrates a similar response to the frequency or intensity of environmental disturbances. In this investigation, we conducted five distinct experiments employing soils or wetland sediments exposed to varying intensities or frequencies of disturbances, with a specific emphasis on disturbances associated with human activity, such as chemical contamination, hydrologic changes, and forest thinning. Specifically, we examined the effects of bactericide and heavy metal contamination, long-term drainage, tidal flow, and thinning management on microbial enzyme activities in soils. Our findings revealed that microbial enzyme activities were highest at intermediate disturbance levels. Despite the diversity in experiment conditions, each trial consistently demonstrated analogous patterns, suggesting the robustness of the IDH in elucidating microbial activities alongside diversity in soils. These outcomes bear significant implications for ecological restoration and management, as intermediate disturbance may expedite organic matter decomposition and nutrient cycles, crucial for sustaining ecosystem services in soils.
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Affiliation(s)
- Hojeong Kang
- School of Civil and Environmental Engineering, Yonsei University, Seoul 03722, Republic of Korea;
| | - Sunghyun Kim
- Smithsonian Environmental Research Center, Edgewater, MD 21037, USA;
| | - Keunyea Song
- Department of Ecology, State of Washington, Lacey, WA 98504, USA;
| | - Min-Jung Kwon
- Institute of Soil Science, Universität Hamburg, 20146 Hamburg, Germany;
| | - Jaehyun Lee
- School of Civil and Environmental Engineering, Yonsei University, Seoul 03722, Republic of Korea;
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Huang R, Li Z, Xiao Y, Liu J, Jiang T, Deng O, Tang X, Wu Y, Tao Q, Li Q, Luo Y, Gao X, Wang C, Li B. Composition of DOM along the depth gradients in the paddy field treated with crop straw for 10 years. JOURNAL OF ENVIRONMENTAL MANAGEMENT 2024; 353:120084. [PMID: 38281421 DOI: 10.1016/j.jenvman.2024.120084] [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: 08/14/2023] [Revised: 01/06/2024] [Accepted: 01/07/2024] [Indexed: 01/30/2024]
Abstract
Crop straw return is a widely used agricultural management practice. The addition of crop straw significantly alters the pool of dissolved organic matter (DOM) in agricultural soils and plays a pivotal role in the global carbon (C) cycle, which is sensitive to climate change. The DOM concentration and composition at different soil depths could regulate the turnover and further storage of organic C in terrestrial systems. However, it is still unclear how crop straw return influences the change in DOM composition in rice paddy soils. Therefore, a field experiment was conducted in which paddy soil was amended with crop straw for 10 years. Two crop straw-addition treatments [NPK with 50% crop straw (NPK+1/2S) and NPK with 100% crop straw (NPK + S)], a conventional mineral fertilization control (NPK) and a non-fertilized control were included. Topsoil (0-20 cm) and subsoil (20-40 cm) samples were collected to investigate the soil DOM concentration and compositional structure of the profile. Soil nutrients, iron (Fe) fraction, microbial biomass carbon (MBC), and concentration and optical properties (UV-Vis and fluorescence spectra) of soil DOM were determined. Here, we found that the DOM in the topsoil was more humified than that in the subsoil. The addition of crop straw further decreased the humidification degree of DOM in the subsoil. In crop straw-amended topsoil, microbial decomposition controlled the composition of DOM and induced the formation of aromatic DOM. In the straw-treated subsoil, selective adsorption by poorly crystalline Fe(oxyhydr)oxides and microbial decomposition controlled the composition of DOM. In particular, the formation of protein-like compounds could have played a significant role in the microbial degradation of DOM in the subsoil. Overall, this work conducted a case study within long-term agricultural management to understand the changes in DOM composition along the soil profile, which would be further helpful for evaluating C cycling in agricultural ecosystems.
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Affiliation(s)
- Rong Huang
- College of Resources, Sichuan Agricultural University, Chengdu, 611130, China; Interdisciplinary Research Centre for Agriculture Green Development in Yangtze River Basin, Department of Environmental Sciences and Engineering, College of Resources and Environment, Southwest University, Chongqing, 400716, China; Key Laboratory of Investigation and Monitoring, Protection and Utilization for Cultivated Land Resources, Ministry of Natural Resources, Chengdu, 611130, China
| | - Zheng Li
- College of Resources, Sichuan Agricultural University, Chengdu, 611130, China
| | - Yi Xiao
- College of Resources, Sichuan Agricultural University, Chengdu, 611130, China
| | - Jiang Liu
- College of Resources, Sichuan Agricultural University, Chengdu, 611130, China; State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, 550081, China; Interdisciplinary Research Centre for Agriculture Green Development in Yangtze River Basin, Department of Environmental Sciences and Engineering, College of Resources and Environment, Southwest University, Chongqing, 400716, China
| | - Tao Jiang
- Interdisciplinary Research Centre for Agriculture Green Development in Yangtze River Basin, Department of Environmental Sciences and Engineering, College of Resources and Environment, Southwest University, Chongqing, 400716, China.
| | - Ouping Deng
- College of Resources, Sichuan Agricultural University, Chengdu, 611130, China
| | - Xiaoyang Tang
- College of Resources, Sichuan Agricultural University, Chengdu, 611130, China
| | - Yingjie Wu
- College of Resources, Sichuan Agricultural University, Chengdu, 611130, China
| | - Qi Tao
- College of Resources, Sichuan Agricultural University, Chengdu, 611130, China
| | - Qiquan Li
- College of Resources, Sichuan Agricultural University, Chengdu, 611130, China
| | - Youlin Luo
- College of Resources, Sichuan Agricultural University, Chengdu, 611130, China
| | - Xuesong Gao
- College of Resources, Sichuan Agricultural University, Chengdu, 611130, China; Key Laboratory of Investigation and Monitoring, Protection and Utilization for Cultivated Land Resources, Ministry of Natural Resources, Chengdu, 611130, China
| | - Changquan Wang
- College of Resources, Sichuan Agricultural University, Chengdu, 611130, China
| | - Bing Li
- College of Resources, Sichuan Agricultural University, Chengdu, 611130, China.
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3
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Yu J, Wang X, Yang S, Guo Y, Liu M, Xi M. Divergent response of blue carbon components to wetland types and hydrological effects in typical estuarine wetlands of Jiaozhou Bay, China. JOURNAL OF ENVIRONMENTAL MANAGEMENT 2023; 347:119233. [PMID: 37812903 DOI: 10.1016/j.jenvman.2023.119233] [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] [Received: 06/16/2023] [Revised: 09/10/2023] [Accepted: 10/02/2023] [Indexed: 10/11/2023]
Abstract
As ecosystems subject to periodic tides, estuarine wetlands have a significant capacity to sequester carbon over time. Understanding the distribution patterns of soil carbon components and identifying the key factors influencing these patterns are key to gaining insight into the function of "blue carbon" in coastal wetlands. To clarify the response of soil carbon components to wetland types and hydrological effects in estuarine wetlands, the typical estuarine wetlands in Jiaozhou Bay, China were selected as the study area, and the soil organic carbon (SOC), dissolved organic carbon (DOC), microbial biomass carbon (MBC), soil inorganic carbon (SIC) and dissolved inorganic carbon (DIC) under different wetland types and hydrological effects were investigated. The results showed that the SOC, SIC, and MBC contents were significantly influenced by the wetland types. The SOC and MBC contents were as follows: mudflat (GT) > Phragmites australis wetland (PA) > Suaeda salsa wetland (SS). The overall content of SIC was highest in PA, followed by GT and SS. Hydrological effects had significant influence on the soil MBC, DOC and DIC contents. With the increase hydrological effects, the soil MBC content decreased by 38.89%-72.22%, while the DOC and DIC contents increased by 15.13%-19.89% and 13.41%-86.70%, respectively. The results of the correlation analysis and structural equation model indicated that wetland types and hydrological effects directly or indirectly (through changes in soil pH, bulk density, water content, and salinity) drove the changes in soil carbon contents in estuarine wetlands. Altogether, our findings implied that the alterations of wetland types and hydrological effects will affect the blue carbon function of estuarine wetlands. In the future, for accurate assessment of a blue carbon budget for estuarine wetlands, the differences in wetland types and hydrological effects of different areas should be considered.
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Affiliation(s)
- Jimin Yu
- College of Environmental Science and Engineering, Qingdao University, Qingdao, 266071, China; Carbon Neutrality and Eco-Environmental Technology Innovation Center of Qingdao, Qingdao, 266071, China
| | - Xiaotong Wang
- College of Environmental Science and Engineering, Qingdao University, Qingdao, 266071, China; Carbon Neutrality and Eco-Environmental Technology Innovation Center of Qingdao, Qingdao, 266071, China.
| | - Shaoxu Yang
- College of Environmental Science and Engineering, Qingdao University, Qingdao, 266071, China; Carbon Neutrality and Eco-Environmental Technology Innovation Center of Qingdao, Qingdao, 266071, China
| | - Yaoyu Guo
- College of Environmental Science and Engineering, Qingdao University, Qingdao, 266071, China; Carbon Neutrality and Eco-Environmental Technology Innovation Center of Qingdao, Qingdao, 266071, China
| | - Mengyan Liu
- College of Environmental Science and Engineering, Qingdao University, Qingdao, 266071, China; Carbon Neutrality and Eco-Environmental Technology Innovation Center of Qingdao, Qingdao, 266071, China
| | - Min Xi
- College of Environmental Science and Engineering, Qingdao University, Qingdao, 266071, China; Carbon Neutrality and Eco-Environmental Technology Innovation Center of Qingdao, Qingdao, 266071, China.
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4
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Zhang E, Tian H, Li M, Le S, Li B, Wu L, Zhang Q, Fan L. Dendrite inhibited and dead lithium activated dual-function additive for lithium metal batteries. Chem Commun (Camb) 2023; 59:10996-10999. [PMID: 37615934 DOI: 10.1039/d3cc03085g] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 08/25/2023]
Abstract
In this study, 2-fluoro-5-iodopyridine (2-F-5-IPy) was used as an electrolyte additive, which can not only protect the negative electrode effectively by forming a stable SEI, but also convert dead lithium into active lithium. Benefits from this are a capacity retention of a Li‖LiFePO4 cell after 300 cycles from 36.5% to 89.4%, and the symmetrical cell can work stably for more than 800 hours. Therefore, the addition of 2-F-5-IPy can effectively improve the performance of lithium metal batteries.
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Affiliation(s)
- Erlei Zhang
- School of Chemistry and Chemical Engineering, Harbin Institute of Technology, Harbin, Heilongjiang, 150080, P. R. China.
| | - Huijie Tian
- School of Chemistry and Chemical Engineering, Harbin Institute of Technology, Harbin, Heilongjiang, 150080, P. R. China.
| | - Meng Li
- School of Chemistry and Chemical Engineering, Harbin Institute of Technology, Harbin, Heilongjiang, 150080, P. R. China.
| | - Shiru Le
- School of Chemistry and Chemical Engineering, Harbin Institute of Technology, Harbin, Heilongjiang, 150080, P. R. China.
| | - Bingjiang Li
- Jiangsu Zhitai New Energy Technology Co., Ltd. Taizhou, Jiangsu, 225314, P. R. China
| | - Lijun Wu
- Jiangsu Zhitai New Energy Technology Co., Ltd. Taizhou, Jiangsu, 225314, P. R. China
| | - Qixian Zhang
- School of Materials Science and Engineering, Shanghai University, Shanghai, 200444, P. R. China
| | - Lishuang Fan
- School of Chemistry and Chemical Engineering, Harbin Institute of Technology, Harbin, Heilongjiang, 150080, P. R. China.
- Jiangsu Zhitai New Energy Technology Co., Ltd. Taizhou, Jiangsu, 225314, P. R. China
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Morgalev SY, Lim AG, Morgaleva TG, Morgalev YN, Manasypov RM, Kuzmina D, Shirokova LS, Orgogozo L, Loiko SV, Pokrovsky OS. Fractionation of organic C, nutrients, metals and bacteria in peat porewater and ice after freezing and thawing. ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH INTERNATIONAL 2023; 30:823-836. [PMID: 35904738 DOI: 10.1007/s11356-022-22219-1] [Citation(s) in RCA: 2] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/22/2021] [Accepted: 07/21/2022] [Indexed: 06/15/2023]
Abstract
To better understand freezing - thawing cycles operating in peat soils of permafrost landscapes, we experimentally modelled bi-directional freezing and thawing of peat collected from a discontinuous permafrost zone in western Siberia. We measured translocation of microorganisms and changes in porewater chemistry (pH, UV absorbance, dissolved organic carbon (DOC), and major and trace element concentrations) after thawing and two-way freezing of the three sections of 90-cm-long peat core. We demonstrate that bi-directional freezing and thawing of a peat core is capable of strongly modifying the vertical pattern of bacteria, DOC, nutrients, and trace element concentrations. Sizeable enrichment (a factor of 2 to 5) of DOC, macro- (P, K, Ca) and micro-nutrients (Ni, Mn, Co, Rb, B), and some low-mobile trace elements in several horizons of ice and peat porewater after freeze/thaw experiment may stem from physical disintegration of peat particles, leaching of peat constituents, and opening of isolated (non-connected) pores during freezing front migration. However, due to the appearance of multiple maxima of element concentration after a freeze-thaw event, the use of peat ice chemical composition as environmental archive for paleo-reconstructions is unwarranted.
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Affiliation(s)
- Sergey Yu Morgalev
- Centre "Biotest-Nano", Tomsk State University, 36 Lenin Avenue, Tomsk, 634050, Russia
| | - Artem G Lim
- BIO-GEO-CLIM Laboratory, Tomsk State University, 35 Lenina Pr, Tomsk, Russia
| | - Tamara G Morgaleva
- Centre "Biotest-Nano", Tomsk State University, 36 Lenin Avenue, Tomsk, 634050, Russia
| | - Yuri N Morgalev
- Centre "Biotest-Nano", Tomsk State University, 36 Lenin Avenue, Tomsk, 634050, Russia
| | - Rinat M Manasypov
- BIO-GEO-CLIM Laboratory, Tomsk State University, 35 Lenina Pr, Tomsk, Russia
| | - Daria Kuzmina
- BIO-GEO-CLIM Laboratory, Tomsk State University, 35 Lenina Pr, Tomsk, Russia
| | - Liudmila S Shirokova
- N. Laverov Federal Center for Integrated Arctic Research of the Ural Branch of the Russian Academy of Sciences, Arkhangelsk, Nab Severnoi Dviny, 23, Russia
- Geosciences and Environment Toulouse, UMR 5563 CNRS, University of Toulouse, 14 Avenue Edouard Belin, 31400, Toulouse, France
| | - Laurent Orgogozo
- Geosciences and Environment Toulouse, UMR 5563 CNRS, University of Toulouse, 14 Avenue Edouard Belin, 31400, Toulouse, France
| | - Sergey V Loiko
- BIO-GEO-CLIM Laboratory, Tomsk State University, 35 Lenina Pr, Tomsk, Russia
| | - Oleg S Pokrovsky
- Geosciences and Environment Toulouse, UMR 5563 CNRS, University of Toulouse, 14 Avenue Edouard Belin, 31400, Toulouse, France.
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Li Y, Chen Z, Chen J, Castellano MJ, Ye C, Zhang N, Miao Y, Zheng H, Li J, Ding W. Oxygen availability regulates the quality of soil dissolved organic matter by mediating microbial metabolism and iron oxidation. GLOBAL CHANGE BIOLOGY 2022; 28:7410-7427. [PMID: 36149390 DOI: 10.1111/gcb.16445] [Citation(s) in RCA: 19] [Impact Index Per Article: 9.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 04/02/2022] [Accepted: 09/16/2022] [Indexed: 06/16/2023]
Abstract
Dissolved organic matter (DOM) plays a vital role in biogeochemical processes and in determining the responses of soil organic matter (SOM) to global change. Although the quantity of soil DOM has been inventoried across diverse spatio-temporal scales, the underlying mechanisms accounting for variability in DOM dynamics remain unclear especially in upland ecosystems. Here, a gradient of SOM storage across 12 croplands in northeast China was used to understand links between DOM dynamics, microbial metabolism, and abiotic conditions. We assessed the composition, biodegradability, and key biodegradable components of DOM. In addition, SOM and mineral-associated organic matter (MAOM) composition, soil enzyme activities, oxygen availability, soil texture, and iron (Fe), Fe-bound organic matter, and nutrient concentrations were quantified to clarify the drivers of DOM quality (composition and biodegradability). The proportion of biodegradable DOM increased exponentially with decreasing initial DOM concentration due to larger fractions of depolymerized DOM that was rich in small-molecular phenols and proteinaceous components. Unexpectedly, the composition of DOM was decoupled from that of SOM or MAOM, but significantly related to enzymatic properties. These results indicate that microbial metabolism exhibited a dominant role in DOM generation. As DOM concentration declined, increased soil oxygen availability regulated DOM composition and enhanced its biodegradability mainly through mediating microbial metabolism and Fe oxidation. The oxygen-induced oxidation of Fe(II) to Fe(III) removed complex DOM compounds with large molecular weight. Moreover, increased oxygen availability stimulated oxidase-catalyzed depolymerization of aromatic substances, and promoted production of protein-like DOM components due to lower enzymatic C/N acquisition ratio. As global changes in temperature and moisture will have large impacts on soil oxygen availability, the role of oxygen in regulating DOM dynamics highlights the importance of integrating soil oxygen supply with microbial metabolism and Fe redox status to improve model predictions of soil carbon under climate change.
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Affiliation(s)
- Ye Li
- State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing, China
- University of Chinese Academy of Sciences, Beijing, China
| | - Zengming Chen
- State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing, China
| | - Ji Chen
- Department of Agroecology, Aarhus University Centre for Circular Bioeconomy, Aarhus University, Tjele, Denmark
| | | | - Chenglong Ye
- Ecosystem Ecology Laboratory, College of Resources and Environmental Sciences, Nanjing Agricultural University, Nanjing, China
| | - Nan Zhang
- State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing, China
- School of Applied Meteorology, Nanjing University of Information Science & Technology, Nanjing, China
| | - Yuncai Miao
- State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing, China
- University of Chinese Academy of Sciences, Beijing, China
| | - Huijie Zheng
- State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing, China
- University of Chinese Academy of Sciences, Beijing, China
| | - Junjie Li
- State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing, China
- University of Chinese Academy of Sciences, Beijing, China
| | - Weixin Ding
- State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing, China
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Niu H, Lu X, Zhang G, Sarangi C. Investigation of water-soluble organic constituents and their spatio-temporal heterogeneity over the Tibetan Plateau. ENVIRONMENTAL POLLUTION (BARKING, ESSEX : 1987) 2022; 302:119093. [PMID: 35245621 DOI: 10.1016/j.envpol.2022.119093] [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: 11/23/2021] [Revised: 01/24/2022] [Accepted: 02/28/2022] [Indexed: 06/14/2023]
Abstract
Investigating the migration and transformation of carbonaceous and nitrogenous matter in the cryosphere areas is crucial for understanding global biogeochemical cycle and earth's climate system. However, water-soluble organic constituents and their transformation in multiple water bodies are barely investigated. Water-soluble organic carbon (WSOC) and organic nitrogen (WSON), and particulate black carbon (PBC) in multiple types of water bodies in eastern Tibetan Plateau (TP) cryosphere for the first time have been systematically investigated. Statistical results exhibited that from south to north and from east to west of this region, WSOC concentrations in alpine river runoff were gradually elevated. WSOC and nitrogenous matter in the alpine river runoff and precipitation in the glacier region presented distinct seasonal variations. WSON was the dominant component (63.4%) of water-soluble total nitrogen in precipitation over high-altitude southeastern TP cryosphere. Water-soluble carbonaceous matter dominated the carbon cycle in the TP cryosphere, but particulate carbonaceous matter in the alpine river runoff had a small fraction of the cryospheric carbon cycle. Analysis of optical properties illustrated that PBC had a much stronger light absorption ability (MAC-PBC: 2.28 ± 0.37 m2 g-1) than WSOC in the alpine river runoff (0.41 ± 0.26 m2 g-1). Ionic composition was dominated by SO42-, NO3-, and NH4+ (average: 45.13 ± 3.75%) in the snow of glaciers, implying important contribution of (fossil fuel) combustion sources over this region. The results of this study have essential implications for understanding the carbon and nitrogen cycles in high altitude cryosphere regions of the world. Future work should be performed based on more robust in-situ observations and measurements from multiple environmental medium over the cryosphere areas, to ensure ecological protection and high-quality development of the high mountain Asia.
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Affiliation(s)
- Hewen Niu
- State Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, 730000, China.
| | - Xixi Lu
- Department of Geography, National University of Singapore, 1 Arts Link, 117570, Singapore
| | - Guotao Zhang
- Key Laboratory of Land Surface Pattern and Simulation, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, 100101, China
| | - Chandan Sarangi
- Department of Civil Engineering, Indian Institute of Technology, Madras, Chennai, India; Laboratory for Atmospheric and Climate Sciences, Indian Institute of Technology Madras, Chennai, India
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Klaes B, Wörner G, Thiele-Bruhn S, Arz HW, Struck J, Dellwig O, Groschopf N, Lorenz M, Wagner JF, Urrea OB, Lamy F, Kilian R. Element mobility related to rock weathering and soil formation at the westward side of the southernmost Patagonian Andes. THE SCIENCE OF THE TOTAL ENVIRONMENT 2022; 817:152977. [PMID: 35016939 DOI: 10.1016/j.scitotenv.2022.152977] [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: 11/05/2021] [Revised: 12/25/2021] [Accepted: 01/04/2022] [Indexed: 06/14/2023]
Abstract
Rock weathering and pedogenesis are fundamental processes for element mobility in terrestrial bio-geochemical cycles and for the regulation of primary productivity in adjacent coastal marine ecosystems. Here, soils developed from volcanic ash under extreme climate conditions could play a particular role. We therefore investigated rock weathering, soil formation and the associated mobilization of trace elements and micronutrients in a pristine South Patagonian ecosystem. Weathered and unweathered basement lithologies, tephra of the 4.216 kyrs BP Mt. Burney eruption and four soil profiles are considered. The approach combines mineralogical (XRD, SEM) and inorganic geochemical (XRF, ICP-OES/MS) with organic geochemical analyses (TOC, TN, δ13C, δ15N, DOC extracts) of representative samples. Chemical weathering is quantified by mass balance calculations and 14C age constraints allow a correlation of pedogenic processes with the paleoenvironmental history of the area. Our data document that pedogenesis with initial peat formation occurred since ~2.5 kyrs BP. In these acidic peaty Andosols, intensive alteration of volcanic glass mobilized large quantities of elements, considerably surpassing leachates provided by basement rock weathering. Clay production is limited in favor of the formation of amorphous Al- and crystalline Fe-(hydr)oxides. However, tephra alteration, soil organic matter turnover rates, enhanced dissolved organic carbon export, and Fe-/Al-(hydr)oxide precipitation are closely linked and ultimately controlled by rainfall-induced water-level fluctuations, highlighting the dominant influence of the southern westerly wind belt. The transport of mobilized trace elements and micronutrients adsorbed onto suspended colloids (dissolved organic carbon, Al-humus complexes and Fe-(hydr)oxides) is redox-pH-dependent, highly variable and ultimately regulated by westerly intensity. Broader implications of this work include a new perspective on the climate-controlled micronutrient delivery for primary productivity in South Patagonian fjords, which is strongly affected by Andosol formation. Furthermore, a careful evaluation of 'ordinary' geochemical proxies in regional paleoenvironmental archives is needed to account for these unique pedogenic processes.
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Affiliation(s)
- Björn Klaes
- Geology Department, Trier University, Campus II (Geozentrum), Behringstraße 21, 54296 Trier, Germany; Soil Science Department, Trier University, Campus II (Geozentrum), Behringstraße 21, 54296 Trier, Germany.
| | - Gerhard Wörner
- Division of Geochemistry and Isotope Geology, GZG, Georg-August-University Göttingen, Goldschmidtstraße 1, 37077 Göttingen, Germany.
| | - Sören Thiele-Bruhn
- Soil Science Department, Trier University, Campus II (Geozentrum), Behringstraße 21, 54296 Trier, Germany.
| | - Helge Wolfgang Arz
- Marine Geology Department, Leibniz Institute for Baltic Sea Research Warnemünde (IOW), Seestraße 15, 18119 Rostock, Germany.
| | - Julian Struck
- Department of Physical Geography, Institute of Geography, Friedrich-Schiller-University Jena, Löbdergraben 32, 07743 Jena, Germany.
| | - Olaf Dellwig
- Marine Geology Department, Leibniz Institute for Baltic Sea Research Warnemünde (IOW), Seestraße 15, 18119 Rostock, Germany.
| | - Nora Groschopf
- Petrology Research Group, Institute of Geosciences, Johannes Gutenberg University Mainz, Johann-Joachim-Becher-Weg 21, 55128 Mainz, Germany.
| | - Marcel Lorenz
- Soil Science Department, Trier University, Campus II (Geozentrum), Behringstraße 21, 54296 Trier, Germany.
| | - Jean-Frank Wagner
- Geology Department, Trier University, Campus II (Geozentrum), Behringstraße 21, 54296 Trier, Germany.
| | - Oscar Baeza Urrea
- Geology Department, Trier University, Campus II (Geozentrum), Behringstraße 21, 54296 Trier, Germany.
| | - Frank Lamy
- Alfred Wegener Institute (AWI) Bremerhaven, Am Alten Hafen 26, 27568 Bremerhaven, Germany.
| | - Rolf Kilian
- Geology Department, Trier University, Campus II (Geozentrum), Behringstraße 21, 54296 Trier, Germany; University of Magallanes, Avenida Bulnes, 01855 Punta Arenas, Chile
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9
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Zhu X, Chen L, Pumpanen J, Ojala A, Zobitz J, Zhou X, Laudon H, Palviainen M, Neitola K, Berninger F. The role of terrestrial productivity and hydrology in regulating aquatic dissolved organic carbon concentrations in boreal catchments. GLOBAL CHANGE BIOLOGY 2022; 28:2764-2778. [PMID: 35060250 PMCID: PMC9303698 DOI: 10.1111/gcb.16094] [Citation(s) in RCA: 3] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 09/10/2021] [Revised: 12/26/2021] [Accepted: 12/26/2021] [Indexed: 06/14/2023]
Abstract
The past decades have witnessed an increase in dissolved organic carbon (DOC) concentrations in the catchments of the Northern Hemisphere. Increasing terrestrial productivity and changing hydrology may be reasons for the increases in DOC concentration. The aim of this study is to investigate the impacts of increased terrestrial productivity and changed hydrology following climate change on DOC concentrations. We tested and quantified the effects of gross primary production (GPP), ecosystem respiration (RE) and discharge on DOC concentrations in boreal catchments over 3 years. As catchment characteristics can regulate the extent of rising DOC concentrations caused by the regional or global environmental changes, we selected four catchments with different sizes (small, medium and large) and landscapes (forest, mire and forest-mire mixed). We applied multiple models: Wavelet coherence analysis detected the delay-effects of terrestrial productivity and discharge on aquatic DOC variations of boreal catchments; thereafter, the distributed-lag linear models quantified the contributions of each factor on DOC variations. Our results showed that the combined impacts of terrestrial productivity and discharge explained 62% of aquatic DOC variations on average across all sites, whereas discharge, gross primary production (GPP) and RE accounted for 26%, 22% and 3%, respectively. The impact of GPP and discharge on DOC changes was directly related to catchment size: GPP dominated DOC fluctuations in small catchments (<1 km2 ), whereas discharge controlled DOC variations in big catchments (>1 km2 ). The direction of the relation between GPP and discharge on DOC varied. Increasing RE always made a positive contribution to DOC concentration. This study reveals that climate change-induced terrestrial greening and shifting hydrology change the DOC export from terrestrial to aquatic ecosystems. The work improves our mechanistic understanding of surface water DOC regulation in boreal catchments and confirms the importance of DOC fluxes in regulating ecosystem C budgets.
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Affiliation(s)
- Xudan Zhu
- Department of Environmental and Biological SciencesJoensuu CampusUniversity of Eastern FinlandJoensuuFinland
| | - Liang Chen
- Department of Environmental and Biological SciencesJoensuu CampusUniversity of Eastern FinlandJoensuuFinland
| | - Jukka Pumpanen
- Department of Environmental and Biological SciencesKuopio CampusUniversity of Eastern FinlandKuopioFinland
| | - Anne Ojala
- Natural Resources Institute Finland (LUKE)HelsinkiFinland
| | - John Zobitz
- Department of Mathematics, Statistics, and Computer ScienceAugsburg UniversityMinneapolisMinnesotaUSA
| | - Xuan Zhou
- Department of Environmental and Biological SciencesJoensuu CampusUniversity of Eastern FinlandJoensuuFinland
| | - Hjalmar Laudon
- Department of Forest Ecology and ManagementSwedish University of Agricultural ScienceUmeåSweden
| | - Marjo Palviainen
- Department of Forest SciencesUniversity of HelsinkiHelsinkiFinland
| | - Kimmo Neitola
- Institute for Atmospheric Earth System Research (INAR)University of HelsinkiHelsinkiFinland
| | - Frank Berninger
- Department of Environmental and Biological SciencesJoensuu CampusUniversity of Eastern FinlandJoensuuFinland
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10
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Lu F, Wu J, Yi B, Xu Z, Wang M, Sundberg S, Bu ZJ. Long-Term Phosphorus Addition Strongly Weakens the Carbon Sink Function of a Temperate Peatland. Ecosystems 2022. [DOI: 10.1007/s10021-022-00754-9] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/03/2022]
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11
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Drivers controlling spatial and temporal variation of microbial properties and dissolved organic forms (DOC and DON) in fen soils with persistently low water tables. Glob Ecol Conserv 2021. [DOI: 10.1016/j.gecco.2021.e01605] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/18/2022] Open
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12
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Dom SP, Ikenaga M, Lau SYL, Radu S, Midot F, Yap ML, Chin MY, Lo ML, Jee MS, Maie N, Melling L. Linking prokaryotic community composition to carbon biogeochemical cycling across a tropical peat dome in Sarawak, Malaysia. Sci Rep 2021; 11:6416. [PMID: 33742002 PMCID: PMC7979770 DOI: 10.1038/s41598-021-81865-6] [Citation(s) in RCA: 7] [Impact Index Per Article: 2.3] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/16/2020] [Accepted: 01/11/2021] [Indexed: 01/31/2023] Open
Abstract
Tropical peat swamp forest is a global store of carbon in a water-saturated, anoxic and acidic environment. This ecosystem holds diverse prokaryotic communities that play a major role in nutrient cycling. A study was conducted in which a total of 24 peat soil samples were collected in three forest types in a tropical peat dome in Sarawak, Malaysia namely, Mixed Peat Swamp (MPS), Alan Batu (ABt), and Alan Bunga (ABg) forests to profile the soil prokaryotic communities through meta 16S amplicon analysis using Illumina Miseq. Results showed these ecosystems were dominated by anaerobes and fermenters such as Acidobacteria, Proteobacteria, Actinobacteria and Firmicutes that cover 80-90% of the total prokaryotic abundance. Overall, the microbial community composition was different amongst forest types and depths. Additionally, this study highlighted the prokaryotic communities' composition in MPS was driven by higher humification level and lower pH whereas in ABt and ABg, the less acidic condition and higher organic matter content were the main factors. It was also observed that prokaryotic diversity and abundance were higher in the more oligotrophic ABt and ABg forest despite the constantly waterlogged condition. In MPS, the methanotroph Methylovirgula ligni was found to be the major species in this forest type that utilize methane (CH4), which could potentially be the contributing factor to the low CH4 gas emissions. Aquitalea magnusonii and Paraburkholderia oxyphila, which can degrade aromatic compounds, were the major species in ABt and ABg forests respectively. This information can be advantageous for future study in understanding the underlying mechanisms of environmental-driven alterations in soil microbial communities and its potential implications on biogeochemical processes in relation to peatland management.
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Affiliation(s)
- Simon Peter Dom
- Sarawak Tropical Peat Research Institute, Lot 6035, Kuching-Samarahan Expressway, 94300, Kota Samarahan, Sarawak, Malaysia
- Department of Food Science, Faculty of Food Science and Technology, Universiti Putra Malaysia, 43400, Serdang, Selangor, Malaysia
| | - Makoto Ikenaga
- Research Field in Agriculture, Agriculture Fisheries and Veterinary Medicine Area, Kagoshima University, 1-21-24, Korimoto, Kagoshima, 890-0065, Japan
| | - Sharon Yu Ling Lau
- Sarawak Tropical Peat Research Institute, Lot 6035, Kuching-Samarahan Expressway, 94300, Kota Samarahan, Sarawak, Malaysia.
| | - Son Radu
- Department of Food Science, Faculty of Food Science and Technology, Universiti Putra Malaysia, 43400, Serdang, Selangor, Malaysia
| | - Frazer Midot
- Sarawak Tropical Peat Research Institute, Lot 6035, Kuching-Samarahan Expressway, 94300, Kota Samarahan, Sarawak, Malaysia
| | - Mui Lan Yap
- Sarawak Tropical Peat Research Institute, Lot 6035, Kuching-Samarahan Expressway, 94300, Kota Samarahan, Sarawak, Malaysia
| | - Mei-Yee Chin
- Sarawak Tropical Peat Research Institute, Lot 6035, Kuching-Samarahan Expressway, 94300, Kota Samarahan, Sarawak, Malaysia
| | - Mei Lieng Lo
- Sarawak Tropical Peat Research Institute, Lot 6035, Kuching-Samarahan Expressway, 94300, Kota Samarahan, Sarawak, Malaysia
| | - Mui Sie Jee
- Sarawak Tropical Peat Research Institute, Lot 6035, Kuching-Samarahan Expressway, 94300, Kota Samarahan, Sarawak, Malaysia
| | - Nagamitsu Maie
- School of Veterinary Medicine, Kitasato University, Towada, Aomori, 034-8628, Japan
| | - Lulie Melling
- Sarawak Tropical Peat Research Institute, Lot 6035, Kuching-Samarahan Expressway, 94300, Kota Samarahan, Sarawak, Malaysia
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13
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Kitson E, Bell NGA. The Response of Microbial Communities to Peatland Drainage and Rewetting. A Review. Front Microbiol 2020; 11:582812. [PMID: 33193221 PMCID: PMC7658402 DOI: 10.3389/fmicb.2020.582812] [Citation(s) in RCA: 7] [Impact Index Per Article: 1.8] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/13/2020] [Accepted: 09/30/2020] [Indexed: 11/13/2022] Open
Abstract
Peatlands are significant global carbon stores and play an important role in mediating the flux of greenhouse gasses into the atmosphere. During the 20th century substantial areas of northern peatlands were drained to repurpose the land for industrial or agricultural use. Drained peatlands have dysfunctional microbial communities, which can lead to net carbon emissions. Rewetting of drained peatlands is therefore an environmental priority, yet our understanding of the effects of peatland drainage and rewetting on microbial communities is still incomplete. Here we summarize the last decade of research into the response of the wider microbial community, methane-cycling microorganisms, and micro-fauna to drainage and rewetting in fens and bogs in Europe and North America. Emphasis is placed on current research methodologies and their limitations. We propose targets for future work including: accounting for timescale of drainage and rewetting events; better vertical and lateral coverage of samples across a peatland; the integration of proteomic and metabolomic datasets into functional community analysis; the use of RNA sequencing to differentiate the active community from legacy DNA; and further study into the response of the viral and micro-faunal communities to peatland drainage and rewetting. This review should benefit researchers embarking on studies in wetland microbiology and non-microbiologists working on peatland drainage and rewetting in general.
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Affiliation(s)
- Ezra Kitson
- EaSTCHEM School of Chemistry, University of Edinburgh, Edinburgh, United Kingdom
| | - Nicholle G A Bell
- EaSTCHEM School of Chemistry, University of Edinburgh, Edinburgh, United Kingdom
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14
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St James AR, Yavitt JB, Zinder SH, Richardson RE. Linking microbial Sphagnum degradation and acetate mineralization in acidic peat bogs: from global insights to a genome-centric case study. ISME JOURNAL 2020; 15:293-303. [PMID: 32951020 DOI: 10.1038/s41396-020-00782-0] [Citation(s) in RCA: 4] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/09/2020] [Revised: 09/09/2020] [Accepted: 09/14/2020] [Indexed: 11/09/2022]
Abstract
Ombrotrophic bogs accumulate large stores of soil carbon that eventually decompose to carbon dioxide and methane. Carbon accumulates because Sphagnum mosses slow microbial carbon decomposition processes, leading to the production of labile intermediate compounds. Acetate is a major product of Sphagnum degradation, yet rates of hydrogenotrophic methanogenesis far exceed rates of aceticlastic methanogenesis, suggesting that alternative acetate mineralization processes exist. Two possible explanations are aerobic respiration and anaerobic respiration via humic acids as electron acceptors. While these processes have been widely observed, microbial community interactions linking Sphagnum degradation and acetate mineralization remain cryptic. In this work, we use ordination and network analysis of functional genes from 110 globally distributed peatland metagenomes to identify conserved metabolic pathways in Sphagnum bogs. We then use metagenome-assembled genomes (MAGs) from McLean Bog, a Sphagnum bog in New York State, as a local case study to reconstruct pathways of Sphagnum degradation and acetate mineralization. We describe metabolically flexible Acidobacteriota MAGs that contain all genes to completely degrade Sphagnum cell wall sugars under both aerobic and anaerobic conditions. Finally, we propose a hypothetical model of acetate oxidation driven by changes in peat redox potential that explain how bogs may circumvent aceticlastic methanogenesis through aerobic and humics-driven respiration.
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Affiliation(s)
- Andrew R St James
- School of Civil and Environmental Engineering, Cornell University, Ithaca, NY, USA.
| | - Joseph B Yavitt
- Department of Natural Resources, Cornell University, Ithaca, NY, USA
| | | | - Ruth E Richardson
- School of Civil and Environmental Engineering, Cornell University, Ithaca, NY, USA
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15
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Byun C, Kim SY, Kang H. Elevated concentrations of CO2 and nitrogen alter DOC release and soil phenolic content in wetland microcosms. ECOSCIENCE 2020. [DOI: 10.1080/11956860.2020.1732802] [Citation(s) in RCA: 4] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 10/24/2022]
Affiliation(s)
- Chaeho Byun
- Department of Biological Sciences and Biotechnology, Andong National University, Andong, South Korea
- School of Civil and Environmental Engineering, Yonsei University, Seoul, South Korea
| | - Seon-Young Kim
- Water Environment Research Department, National Institute of Environmental Research, Incheon, South Korea
| | - Hojeong Kang
- School of Civil and Environmental Engineering, Yonsei University, Seoul, South Korea
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16
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Pschenyckyj CM, Clark JM, Shaw LJ, Griffiths RI, Evans CD. Effects of acidity on dissolved organic carbon in organic soil extracts, pore water and surface litters. THE SCIENCE OF THE TOTAL ENVIRONMENT 2020; 703:135585. [PMID: 31767326 DOI: 10.1016/j.scitotenv.2019.135585] [Citation(s) in RCA: 3] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/12/2019] [Revised: 10/15/2019] [Accepted: 11/15/2019] [Indexed: 06/10/2023]
Abstract
Over the past 30-40 years, dissolved organic carbon (DOC) concentrations have increased in soil solutions and surface waters in many acid-sensitive areas of Europe and North America. This has been linked to recovery from acidification in response to decreasing levels of atmospheric pollution. Evidence from radiocarbon dating suggests that DOC in surface waters is typically derived from recently photosynthesised organic matter such as plant litter and exudates, yet there is little information on the pH-sensitivity of organic matter solubility, or its decomposition, in litter layers and in different organic soils. Therefore the purpose of this study was to determine a) the sensitivity of DOC to acidity in different surface layers and soil types, in order to b) improve understanding of the key sources contributing to the increasing DOC trend. Such information is vital for understanding site specific characteristics contributing to inconsistencies in DOC release between catchments, and for improving predictions of carbon fluxes and budgets. Based on data collected at four established field pH-manipulation experiments in upland areas of the United Kingdom, we examined the sources, composition and acid-sensitivity of DOC export from the litter and organic soils. We found that litter generated nearly three times more DOC than the organic soils, consistent with radiocarbon evidence that recent plant inputs are a major source of DOC. Furthermore, litter derived DOC had lower specific ultraviolet light absorbance (SUVA) than organic soil DOC, suggesting greater biodegradability, and was not acid sensitive. In contrast, organic soil DOC concentrations were more strongly related to experimentally manipulated pH, implying that the mobility of this DOC may be subject to physicochemical rather than biotic controls. Our results suggest that physicochemically mediated controls on organic matter solubility may be a key driver behind the widely observed increases in surface water DOC in areas undergoing recovery from acidification.
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Affiliation(s)
- Catharine M Pschenyckyj
- Department of Geography and Environmental Sciences, Northumbria University, Newcastle upon Tyne NE1 8ST, UK.
| | - Joanna M Clark
- Soil Research Centre, Department of Geography and Environmental Science, School of Archaeology, Geography and Environmental Science, The University of Reading, Whiteknights, PO Box 227, Reading RG6 6AB, UK
| | - Liz J Shaw
- Soil Research Centre, Department of Geography and Environmental Science, School of Archaeology, Geography and Environmental Science, The University of Reading, Whiteknights, PO Box 227, Reading RG6 6AB, UK
| | | | - Chris D Evans
- Centre for Ecology and Hydrology, Deiniol Rd, Bangor LL57 2UP, UK
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17
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Kluber LA, Johnston ER, Allen SA, Hendershot JN, Hanson PJ, Schadt CW. Constraints on microbial communities, decomposition and methane production in deep peat deposits. PLoS One 2020; 15:e0223744. [PMID: 32027653 PMCID: PMC7004313 DOI: 10.1371/journal.pone.0223744] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/25/2019] [Accepted: 01/20/2020] [Indexed: 11/19/2022] Open
Abstract
Peatlands play outsized roles in the global carbon cycle. Despite occupying a rather small fraction of the terrestrial biosphere (~3%), these ecosystems account for roughly one third of the global soil carbon pool. This carbon is largely comprised of undecomposed deposits of plant material (peat) that may be meters thick. The fate of this deep carbon stockpile with ongoing and future climate change is thus of great interest and has large potential to induce positive feedback to climate warming. Recent in situ warming of an ombrotrophic peatland indicated that the deep peat microbial communities and decomposition rates were resistant to elevated temperatures. In this experiment, we sought to understand how nutrient and pH limitations may interact with temperature to limit microbial activity and community composition. Anaerobic microcosms of peat collected from 1.5 to 2 meters in depth were incubated at 6°C and 15°C with elevated pH, nitrogen (NH4Cl), and/or phosphorus (KH2PO4) in a full factorial design. The production of CO2 and CH4 was significantly greater in microcosms incubated at 15°C, although the structure of the microbial community did not differ between the two temperatures. Increasing the pH from ~3.5 to ~5.5 altered microbial community structure, however increases in CH4 production were non-significant. Contrary to expectations, N and P additions did not increase CO2 and CH4 production, indicating that nutrient availability was not a primary constraint in microbial decomposition of deep peat. Our findings indicate that temperature is a key factor limiting the decomposition of deep peat, however other factors such as the availability of O2 or alternative electron donors and high concentrations of phenolic compounds, may also exert constraints. Continued experimental peat warming studies will be necessary to assess if the deep peat carbon bank is susceptible to increased temperatures over the longer time scales.
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Affiliation(s)
- Laurel A. Kluber
- Biosciences Division, Oak Ridge National Laboratory, Oak Ridge, TN, United States of America
- Climate Change Sciences Institute, Oak Ridge National Laboratory, Oak Ridge, TN, United States of America
| | - Eric R. Johnston
- Biosciences Division, Oak Ridge National Laboratory, Oak Ridge, TN, United States of America
- Climate Change Sciences Institute, Oak Ridge National Laboratory, Oak Ridge, TN, United States of America
| | - Samantha A. Allen
- Biosciences Division, Oak Ridge National Laboratory, Oak Ridge, TN, United States of America
- Climate Change Sciences Institute, Oak Ridge National Laboratory, Oak Ridge, TN, United States of America
| | - J. Nicholas Hendershot
- Biosciences Division, Oak Ridge National Laboratory, Oak Ridge, TN, United States of America
- Climate Change Sciences Institute, Oak Ridge National Laboratory, Oak Ridge, TN, United States of America
| | - Paul J. Hanson
- Climate Change Sciences Institute, Oak Ridge National Laboratory, Oak Ridge, TN, United States of America
- Environmental Sciences Division, Oak Ridge National Laboratory, Oak Ridge, TN, United States of America
| | - Christopher W. Schadt
- Biosciences Division, Oak Ridge National Laboratory, Oak Ridge, TN, United States of America
- Climate Change Sciences Institute, Oak Ridge National Laboratory, Oak Ridge, TN, United States of America
- Department of Microbiology, University of Tennessee, Knoxville, TN, United States of America
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18
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Short Term Effects of Salinization on Compound Release from Drained and Restored Coastal Wetlands. WATER 2019. [DOI: 10.3390/w11081549] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.2] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 11/16/2022]
Abstract
Over the past two decades, great efforts have been made to restore coastal wetlands through the removal of dikes, but challenges remain because the effects of flooding with saline water on water quality are unknown. We collected soil samples from two adjacent coastal fen peatlands, one drained and diked, the other open to the sea and rewetted, aiming at assessing the mobility and export of various compounds. Microcosm experiments with constant flow-through conditions were conducted to determine the effluent concentrations of dissolved organic carbon (DOC), ammonium ( NH 4 + ), and phosphate ( PO 4 3 − ) during saline–fresh water cycles. Sodium chloride (NaCl) was used to adjust salinity (saline water, NaCl concentration of 0.12 mol L−1; fresh water, NaCl concentration of 0.008 mol L−1) and served as a tracer. A model analysis of the obtained chloride ( Cl − ) and sodium ( Na + ) breakthrough curves indicated that peat soils have a dual porosity structure. Sodium was retarded in peat soils with a retardation factor of 1.4 ± 0.2 due to adsorption. The leaching tests revealed that water salinity has a large impact on DOC, NH 4 + , and PO 4 3 − release. The concentrations of DOC in the effluent decreased with increasing water salinity because the combination of high ionic strength (NaCl concentration of 0.12 mol L−1) and low pH (3.5 to 4.5) caused a solubility reduction. On the contrary, saline water enhanced NH 4 + release through cation exchange processes. The PO 4 3 − concentrations, however, decreased in the effluent with increasing water salinity. Overall, the decommissioning of dikes at coastal wetlands and the flooding of once drained and agriculturally used sites increase the risk that especially nitrogen may be leached at higher rates to the sea.
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