The Forms of Phosphorus in Sediments of Large Lakes (Poyang Lake) and Its Impact on Endogenous Release

The release and retention of phosphorus (P) in sediments play a crucial role in determining whole-system P dynamics and balance in eutrophic lakes. Using Poyang Lake (China’s largest freshwater lake) as a subject for a case study, we performed field investigations and collected data on specific P fo...

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Published inACS ES&T water Vol. 4; no. 8; pp. 3163 - 3177
Main Authors Liu, Wei, Xiao, Huoqing, Yin, Junbao, Qin, Tian, Liu, Zugen, Li, Zhiwen, Wu, Xinying, Abakumov, Evgeny, ANJUM, HANNAN AHMAD, Zhang, Meng, Zhang, Yuanyan, Wu, Daishe, Zhang, Yondong, Kong, Ming, Ma, Zhifei, He, Liang, Yan, Feng, Xie, Xianchuan
Format Journal Article
LanguageEnglish
Published American Chemical Society 09.08.2024
Subjects
Biogeochemical transformation
Lake endogenous phosphorus
Sediment phosphorus forms
Lake phosphorus cycling
Lake eutrophication
Online AccessGet full text
ISSN2690-0637
2690-0637
DOI10.1021/acsestwater.3c00836

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Abstract The release and retention of phosphorus (P) in sediments play a crucial role in determining whole-system P dynamics and balance in eutrophic lakes. Using Poyang Lake (China’s largest freshwater lake) as a subject for a case study, we performed field investigations and collected data on specific P forms in the overlying water, interstitial water, and sediment phases. The vertical concentration variations of the aforementioned P forms in the columnar sediment of Poyang Lake reflect distinct surface enrichment characteristics, primarily attributed to external P inputs. The average flux of dissolved total P at the monitored sites was 0.49 mg/(m2·d), and the estimated P release from Poyang Lake to the overlying water was 447.13–587.7 t/a, which is comparable to the release from typical eutrophic lakes in China. Sediment P release serves as a significant P source for interstitial water and plays a crucial role in the upward release of dissolved IP (interstitial water) from the overlying water. Fe–P (accounting for 47.07% of TP) is the P form in Poyang Lake sediments that is most involved in the migration and transformation process, with a large amount of activated P being transformed into Fe–P and released into the overlying water.
AbstractList The release and retention of phosphorus (P) in sediments play a crucial role in determining whole-system P dynamics and balance in eutrophic lakes. Using Poyang Lake (China’s largest freshwater lake) as a subject for a case study, we performed field investigations and collected data on specific P forms in the overlying water, interstitial water, and sediment phases. The vertical concentration variations of the aforementioned P forms in the columnar sediment of Poyang Lake reflect distinct surface enrichment characteristics, primarily attributed to external P inputs. The average flux of dissolved total P at the monitored sites was 0.49 mg/(m2·d), and the estimated P release from Poyang Lake to the overlying water was 447.13–587.7 t/a, which is comparable to the release from typical eutrophic lakes in China. Sediment P release serves as a significant P source for interstitial water and plays a crucial role in the upward release of dissolved IP (interstitial water) from the overlying water. Fe–P (accounting for 47.07% of TP) is the P form in Poyang Lake sediments that is most involved in the migration and transformation process, with a large amount of activated P being transformed into Fe–P and released into the overlying water.
Author Qin, Tian
Zhang, Yuanyan
Liu, Wei
Xiao, Huoqing
Ma, Zhifei
Liu, Zugen
Abakumov, Evgeny
Li, Zhiwen
He, Liang
Yin, Junbao
Yan, Feng
Zhang, Yondong
Xie, Xianchuan
Kong, Ming
ANJUM, HANNAN AHMAD
Zhang, Meng
Wu, Xinying
Wu, Daishe
AuthorAffiliation School of Materials and Chemical Engineering
Ministry of Ecology and Environment
Saint Petersburg State University
Jiangxi Nanxin Environmental Protection Technology Co. LTD
Nanjing Institute of Environmental Sciences
Pingxiang University
Department of Applied Ecology
Key Laboratory of Poyang Lake Environment and Resource Utilization, Ministry of Education, School of Resource and Environment
AuthorAffiliation_xml – name: School of Materials and Chemical Engineering
– name: Pingxiang University
– name: Ministry of Ecology and Environment
– name: Key Laboratory of Poyang Lake Environment and Resource Utilization, Ministry of Education, School of Resource and Environment
– name: Department of Applied Ecology
– name: Nanjing Institute of Environmental Sciences
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– name: Saint Petersburg State University
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  givenname: Xianchuan
  orcidid: 0000-0002-0664-7193
  surname: Xie
  fullname: Xie, Xianchuan
  email: xchxie@ncu.edu.cn
  organization: Key Laboratory of Poyang Lake Environment and Resource Utilization, Ministry of Education, School of Resource and Environment
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Lake endogenous phosphorus
Sediment phosphorus forms
Lake phosphorus cycling
Lake eutrophication
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