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Seok MW, Kim D, Park GH, Lee K, Kim TH, Jung J, Kim K, Park KT, Kim YH, Mo A, Park S, Ko YH, Kang J, Kim H, Kim TW. Atmospheric deposition of inorganic nutrients to the Western North Pacific Ocean. THE SCIENCE OF THE TOTAL ENVIRONMENT 2021; 793:148401. [PMID: 34166903 DOI: 10.1016/j.scitotenv.2021.148401] [Citation(s) in RCA: 7] [Impact Index Per Article: 2.3] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/11/2021] [Revised: 06/08/2021] [Accepted: 06/08/2021] [Indexed: 06/13/2023]
Abstract
We evaluated the potential impacts of atmospheric deposition on marine productivity and inorganic carbon chemistry in the northwestern Pacific Ocean (8-39°N, 125-157°E). The nutrient concentration in atmospheric total suspended particles decreased exponentially with increasing distance from the closest land-mass (Asia), clearly revealing anthropogenic and terrestrial contributions. The predicted mean depositional fluxes of inorganic nitrogen were approximately 34 and 15 μmol m-2 d-1 to the west and east of 140°E, respectively, which were at least two orders of magnitude greater than the inorganic phosphorus flux. On average, atmospheric particulate deposition would support 3-4% of the net primary production along the surveyed tracks, which is equivalent to ~2% of the dissolved carbon increment caused by the penetration of anthropogenic CO2. Our observations generally fell within the ranges observed over the past 18 years, despite an increasing trend of atmospheric pollution in the source regions during the same period, which implies high temporal and spatial variabilities of atmospheric nutrient concentration in the study area. Continued atmospheric anthropogenic nitrogen deposition may alter the relative abundances of nitrogen and phosphorus.
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Affiliation(s)
- Min-Woo Seok
- Division of Environmental Science and Ecological Engineering, Korea University, Seoul 02841, Republic of Korea
| | - Dongseon Kim
- Marine Environmental Research Center, Korea Institute of Ocean Science & Technology, Busan 49111, Republic of Korea
| | - Geun-Ha Park
- Marine Environmental Research Center, Korea Institute of Ocean Science & Technology, Busan 49111, Republic of Korea
| | - Kitack Lee
- Division of Environmental Science and Engineering, Pohang University of Science & Technology, Pohang 37673, Republic of Korea
| | - Tae-Hoon Kim
- Faculty of Earth Systems and Environmental Sciences, College of Natural Sciences, Chonnam National University, 61186 Gwangju, Republic of Korea
| | - Jinyoung Jung
- Korea Polar Research Institute, Incheon 21990, Republic of Korea
| | - Kitae Kim
- Korea Polar Research Institute, Incheon 21990, Republic of Korea
| | - Ki-Tae Park
- Korea Polar Research Institute, Incheon 21990, Republic of Korea
| | - Yeo-Hun Kim
- Global Ocean Research Center, Korea Institute of Ocean Science & Technology, Busan 49111, Republic of Korea
| | - Ahra Mo
- Division of Environmental Science and Ecological Engineering, Korea University, Seoul 02841, Republic of Korea
| | - Seunghee Park
- Division of Environmental Science and Ecological Engineering, Korea University, Seoul 02841, Republic of Korea
| | - Young Ho Ko
- OJEong Resilience Institute, Korea University, Seoul 02841, Republic of Korea
| | - Jeongwon Kang
- Korean Seas Geosystem Research Unit, Korea Institute of Ocean Science & Technology, Busan 49111, Republic of Korea
| | - Haryun Kim
- East Sea Research Institute, Korea Institute of Ocean Science & Technology, Uljin 36315, Republic of Korea
| | - Tae-Wook Kim
- Division of Environmental Science and Ecological Engineering, Korea University, Seoul 02841, Republic of Korea; OJEong Resilience Institute, Korea University, Seoul 02841, Republic of Korea.
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Duan X, Guo C, Zhang C, Li H, Zhou Y, Gao H, Xia X, He H, McMinn A, Wang M. Effect of East Asian atmospheric particulate matter deposition on bacterial activity and community structure in the oligotrophic Northwest Pacific. ENVIRONMENTAL POLLUTION (BARKING, ESSEX : 1987) 2021; 283:117088. [PMID: 33857882 DOI: 10.1016/j.envpol.2021.117088] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/15/2020] [Revised: 04/01/2021] [Accepted: 04/02/2021] [Indexed: 06/12/2023]
Abstract
Large amounts of anthropogenic East Asian (EA) particulate matters (PM), containing inorganic nutrients and organic matter, are deposited in the oligotrophic Northwest Pacific Ocean. However, the effects of such deposition on marine microbes remain unclear. In this study, the effect of EA PM deposition on marine bacteria was assessed by five on-board microcosm experiments, conducted in oligotrophic basins of the South China Sea. The addition of EA PM to the sampling water induced a clear shift in bacterial community composition from prevailing oligotrophs (i.e., SAR 11 clade, Prochlorococcus, AEGEAN-169 marine group) to less common copiotrophs (i.e., Alteromonas, Ruegeria, Flavobacteriaceae) and thus a slight increase in bacterial diversity. The shift to more active community composition, as well as stimulation of PM nutrients, resulted in a large increase in cell-specific and bulk bacterial production. In contrast, there were only minor changes in bacterial abundance, possibly due to increased top-down mortality. The EA PM also exhibited a stronge toxic effect on pico-cyanobacteria, leading to a significant decrease in their proportion. Moreover, the responses of bacterial metabolism and community composition exhibited significant relationships with the hydrographic condition of the locations. Stronger promotion effects of the EA PM on bacterial production and community shift from oligotrophs to copiotrophs was demonstrated at the more oligotrophic sites with lower chlorophyll a concentrations. These results suggest that PM deposition from polluted areas has the potential to alter the typical oligotrophic microbiomes and change the net metabolic balance of the bacterial community. These will then influence the dynamics of carbon flow in microbial food webs and biogeochemical cycles, especially with the trend of global warming and expansion of low-chlorophyll regions.
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Affiliation(s)
- Xueping Duan
- College of Marine Life Sciences, Frontiers Science Center for Deep Ocean Multispheres and Earth System, Ocean University of China, Qingdao, 266003, China
| | - Cui Guo
- College of Marine Life Sciences, Frontiers Science Center for Deep Ocean Multispheres and Earth System, Ocean University of China, Qingdao, 266003, China; Institute of Evolution and Marine Biodiversity, Ocean University of China, Qingdao, 266003, China.
| | - Chao Zhang
- Key Laboratory of Marine Environment and Ecology, Ministry of Education of China, Ocean University of China, Qingdao, 266100, China
| | - Hongbo Li
- National Marine Environmental Monitoring Center, Dalian, 116023, China
| | - Yao Zhou
- College of Marine Life Sciences, Frontiers Science Center for Deep Ocean Multispheres and Earth System, Ocean University of China, Qingdao, 266003, China
| | - Huiwang Gao
- Key Laboratory of Marine Environment and Ecology, Ministry of Education of China, Ocean University of China, Qingdao, 266100, China
| | - Xiaomin Xia
- Key Laboratory of Tropical Marine Bio-resources and Ecology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, 510301, China
| | - Hui He
- College of Marine Life Sciences, Frontiers Science Center for Deep Ocean Multispheres and Earth System, Ocean University of China, Qingdao, 266003, China; Institute of Evolution and Marine Biodiversity, Ocean University of China, Qingdao, 266003, China
| | - Andrew McMinn
- College of Marine Life Sciences, Frontiers Science Center for Deep Ocean Multispheres and Earth System, Ocean University of China, Qingdao, 266003, China; Institute for Marine and Antarctic Studies, University of Tasmania, Hobart, Tasmania, 7001, Australia
| | - Min Wang
- College of Marine Life Sciences, Frontiers Science Center for Deep Ocean Multispheres and Earth System, Ocean University of China, Qingdao, 266003, China; Institute of Evolution and Marine Biodiversity, Ocean University of China, Qingdao, 266003, China
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Cai M, Lin Y, Chen M, Yang W, Du H, Xu Y, Cheng S, Xu F, Hong J, Chen M, Ke H. Improved source apportionment of PAHs and Pb by integrating Pb stable isotopes and positive matrix factorization application (PAHs): A historical record case study from the northern South China Sea. THE SCIENCE OF THE TOTAL ENVIRONMENT 2017; 609:577-586. [PMID: 28763655 DOI: 10.1016/j.scitotenv.2017.07.190] [Citation(s) in RCA: 4] [Impact Index Per Article: 0.6] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/18/2017] [Revised: 07/20/2017] [Accepted: 07/21/2017] [Indexed: 06/07/2023]
Abstract
To obtain the historical changes of pyrogenic sources, integrated source apportionment methods, which include PAH compositions, diagnostic ratios (DRs), Pb isotopic ratios, and positive matrix factorization (PMF) model, were developed and applied in sediments of the northern South China Sea. These methods provided a gradually clear picture of energy structural change. Spatially, Σ15PAH (11.3 to 95.5ng/g) and Pb (10.2 to 74.6μg/g) generally exhibited decreasing concentration gradient offshore; while the highest levels of PAHs and Pb were observed near the southern Taiwan Strait, which may be induced by accumulation of different fluvial input. Historical records of pollutants followed closely with the economic development of China, with fast growth of Σ15PAH and Pb occurring since the 1980s and 1990s, respectively. The phasing-out of leaded gasoline in China was captured with a sharp decrease of Pb after the mid-1990s. PAHs and Pb correlated well with TOC and clay content for core sediments, which was not observed for surface sediments. There was an up-core increase of high molecular PAH proportions. Coal and biomass burning were then qualitatively identified as the major sources of PAHs with DRs. Furthermore, shift toward less radiogenic signatures of Pb isotopic ratios after 1900 revealed the start and growing importance of industrial sources. Finally, a greater separation and quantification of various input was achieved by a three-factor PMF model, which made it clear that biomass burning, coal combustion, and vehicle emissions accounted for 40±20%, 41±13%, and 19±12% of PAHs through the core. Biomass and coal combustion acted as major sources before 2000, while contributions from vehicle emission soared thereafter. The integrated multi-methodologies here improved the source apportionment by reducing biases with a step-down and cross-validation perspective, which could be similarly applied to other aquatic systems.
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Affiliation(s)
- Minggang Cai
- State Key Laboratory of Marine Environmental Science, Xiamen University, Xiamen 361102, China; Fujian Provincial Key Laboratory for Coastal Ecology and Environmental Studies, Xiamen University, Xiamen 361102, China; College of Ocean and Earth Sciences, Xiamen University, Xiamen 361102, China
| | - Yan Lin
- College of Ocean and Earth Sciences, Xiamen University, Xiamen 361102, China
| | - Meng Chen
- Fujian Provincial Key Laboratory for Coastal Ecology and Environmental Studies, Xiamen University, Xiamen 361102, China; College of the Environment and Ecology, Xiamen University, Xiamen 361102, China
| | - Weifeng Yang
- College of Ocean and Earth Sciences, Xiamen University, Xiamen 361102, China
| | - Huihong Du
- College of Ocean and Earth Sciences, Xiamen University, Xiamen 361102, China
| | - Ye Xu
- College of Ocean and Earth Sciences, Xiamen University, Xiamen 361102, China
| | - Shayen Cheng
- College of Ocean Science and Resource, National Taiwan Ocean University, Keelung 20224, Taiwan
| | - Fangjian Xu
- College of Geosciences, China University of Petroleum, Qingdao 266555, China
| | - Jiajun Hong
- College of the Environment and Ecology, Xiamen University, Xiamen 361102, China
| | - Mian Chen
- College of Ocean and Earth Sciences, Xiamen University, Xiamen 361102, China
| | - Hongwei Ke
- College of Ocean and Earth Sciences, Xiamen University, Xiamen 361102, China.
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Meng J, Liu J, Fan S, Kang C, Yi K, Cheng Y, Shen X, Tao S. Potential health benefits of controlling dust emissions in Beijing. ENVIRONMENTAL POLLUTION (BARKING, ESSEX : 1987) 2016; 213:850-859. [PMID: 27038572 DOI: 10.1016/j.envpol.2016.03.021] [Citation(s) in RCA: 4] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/17/2015] [Revised: 03/04/2016] [Accepted: 03/05/2016] [Indexed: 06/05/2023]
Abstract
Although the adverse impact of fine particulate matter (i.e., PM2.5) on human health has been well acknowledged, little is known of the health effects of its specific constituents. Over the past decade, the annual average dust concentrations in Beijing were approximately ∼14 μg m(-3), a value that poses a great threat to the city's 20 million residents. In this study, we quantify the potential long-term health damages in Beijing resulting from the dust exposure that occurred from 2000 to 2011. Each year in Beijing, nearly 4000 (95% CI: 1000-7000) premature deaths may be associated with long-term dust exposure, and ∼20% of these deaths are attributed to lung cancer. A decomposition analysis of the inter-annual variability of premature deaths in Beijing indicates that dust concentrations determine the year-to-year tendency, whereas population growth and lung cancer mortality rates drive the increasing tendency of premature death. We suggest that if Beijing takes effective measures towards reducing dust concentrations (e.g., controlling the resuspension of road dust and the fugitive dust from construction sites) to a level comparable to that of New York City's, the associated premature deaths will be significantly reduced. This recommendation offers "low-hanging fruit" suggestions for pollution control that would greatly benefit the public health in Beijing.
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Affiliation(s)
- Jing Meng
- Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University, Beijing, China
| | - Junfeng Liu
- Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University, Beijing, China.
| | - Songmiao Fan
- NOAA Geophysical Fluid Dynamics Laboratory, 201 Forrestal Road, Princeton, NJ, 08542, USA
| | - Chuyun Kang
- Department of Child, Adolescent and Women's Health, School of Public Health, Peking University Health Science Center, Beijing, China
| | - Kan Yi
- Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University, Beijing, China
| | - Yanli Cheng
- Chinese Academy of Meteorological Sciences, Beijing, China
| | - Xing Shen
- Tumor (protons) Center, Shanghai Jiao Tong University, Ruijin Hospital, Shanghai, 200025, China
| | - Shu Tao
- Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University, Beijing, China
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5
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Chow JC, Lowenthal DH, Chen LWA, Wang X, Watson JG. Mass reconstruction methods for PM 2.5: a review. AIR QUALITY, ATMOSPHERE, & HEALTH 2015; 8:243-263. [PMID: 26052367 PMCID: PMC4449935 DOI: 10.1007/s11869-015-0338-3] [Citation(s) in RCA: 111] [Impact Index Per Article: 12.3] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 02/18/2015] [Accepted: 03/17/2015] [Indexed: 05/19/2023]
Abstract
Major components of suspended particulate matter (PM) are inorganic ions, organic matter (OM), elemental carbon (EC), geological minerals, salt, non-mineral elements, and water. Since oxygen (O) and hydrogen (H) are not directly measured in chemical speciation networks, more than ten weighting equations have been applied to account for their presence, thereby approximating gravimetric mass. Assumptions for these weights are not the same under all circumstances. OM is estimated from an organic carbon (OC) multiplier (f) that ranges from 1.4 to 1.8 in most studies, but f can be larger for highly polar compounds from biomass burning and secondary organic aerosols. The mineral content of fugitive dust is estimated from elemental markers, while the water-soluble content is accounted for as inorganic ions or salt. Part of the discrepancy between measured and reconstructed PM mass is due to the measurement process, including: (1) organic vapors adsorbed on quartz-fiber filters; (2) evaporation of volatile ammonium nitrate and OM between the weighed Teflon-membrane filter and the nylon-membrane and/or quartz-fiber filters on which ions and carbon are measured; and (3) liquid water retained on soluble constituents during filter weighing. The widely used IMPROVE equations were developed to characterize particle light extinction in U.S. national parks, and variants of this approach have been tested in a large variety of environments. Important factors for improving agreement between measured and reconstructed PM mass are the f multiplier for converting OC to OM and accounting for OC sampling artifacts.
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Affiliation(s)
- Judith C. Chow
- Division of Atmospheric Sciences, Desert Research Institute, Reno, NV 89512 USA
- The State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an, Shaanxi 710075 China
- Graduate Faculty, University of Nevada, Reno, NV 89503 USA
| | - Douglas H. Lowenthal
- Division of Atmospheric Sciences, Desert Research Institute, Reno, NV 89512 USA
- Graduate Faculty, University of Nevada, Reno, NV 89503 USA
| | - L.-W. Antony Chen
- Division of Atmospheric Sciences, Desert Research Institute, Reno, NV 89512 USA
- Department of Environmental and Occupational Health, University of Nevada, Las Vegas, NV 89154 USA
| | - Xiaoliang Wang
- Division of Atmospheric Sciences, Desert Research Institute, Reno, NV 89512 USA
- Graduate Faculty, University of Nevada, Reno, NV 89503 USA
| | - John G. Watson
- Division of Atmospheric Sciences, Desert Research Institute, Reno, NV 89512 USA
- The State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an, Shaanxi 710075 China
- Graduate Faculty, University of Nevada, Reno, NV 89503 USA
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