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浅水富营养化湖泊(太湖)中颗粒态磷的时空分布及其与环境因子的关系

Spatial and Temporal Distribution of Particulate Phosphorus and Their Correlation with Environmental Factors in a Shallow Eutrophic Chinese Lake (Lake Taihu).

机构信息

Nanjing Institute of Environmental Sciences, Ministry of Environmental Protection, No. 8 Jiang Wang Miao Street, Nanjing 210042, China.

Key Laboratory of Integrated Regulation and Resources Development on Shallow Lakes, Ministry of Education, Hohai University, Nanjing 210098, China.

出版信息

Int J Environ Res Public Health. 2018 Oct 25;15(11):2355. doi: 10.3390/ijerph15112355.

DOI:10.3390/ijerph15112355
PMID:30366408
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC6266604/
Abstract

Spatial and seasonal variations of particulate phosphorus (PP) in a large shallow, eutrophic Lake Taihu with different ecotypes (including a phytoplankton-dominated zone, lake center zone, estuary zone and macrophyte-dominated zone) were investigated. The results showed that particulate organic phosphorus (POP) was the dominant form of PP (>88.0%). The concentration of POP showed higher levels in the bloom-sensitive northwestern zone (phytoplankton-dominated zone and estuary zone) during warm seasons, phytoplankton blooms and input of exogenous particulate matter were the main sources of POP in the lake water. Based on P nuclear magnetic resonance (P NMR) analysis, orthophosphate (Ortho-P) was the dominant molecular species of PP and positively correlated with soluble reactive phosphorus (SRP) ( < 0.01). This suggested that the release of Ortho-P from suspended particulate matter (SPM) was the main source of SRP in the lake water. Pyrophosphate (Pyro-P), which is regarded as a highly labile species of P compounds, represented a large fraction of PP, and its significant positive correlations with chlorophyll (Chl ), indicated that the concentration of Pyro-P could be used as an important indicator for the degree of eutrophication of Lake Taihu. These results proved that PP in lake water was a significant factor supporting lake eutrophication and must be controlled.

摘要

研究了不同生态型(包括浮游植物优势区、湖中心区、河口区和大型植物优势区)的太湖大型浅水富营养化湖泊中颗粒态磷(PP)的时空变化。结果表明,颗粒有机磷(POP)是 PP 的主要存在形式(>88.0%)。在温暖季节、浮游植物水华和外源颗粒物质输入期间,富营养化敏感的西北部区域(浮游植物优势区和河口区)的 POP 浓度较高,浮游植物水华是湖水中 POP 的主要来源。基于磷核磁共振(P NMR)分析,正磷酸盐(Ortho-P)是 PP 的主要分子种类,与可溶解性反应磷(SRP)呈正相关(<0.01)。这表明悬浮颗粒物(SPM)中 Ortho-P 的释放是湖水中 SRP 的主要来源。焦磷酸盐(Pyro-P)被认为是一种高度不稳定的磷化合物,它代表了 PP 的很大一部分,并且与叶绿素(Chl)呈显著正相关,这表明 Pyro-P 的浓度可以作为太湖富营养化程度的重要指标。这些结果证明了湖水中的 PP 是支持湖泊富营养化的重要因素,必须加以控制。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e8b2/6266604/ebc3080fcb7c/ijerph-15-02355-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e8b2/6266604/7ec36349076c/ijerph-15-02355-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e8b2/6266604/6a283ab8f0c0/ijerph-15-02355-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e8b2/6266604/5350218720e6/ijerph-15-02355-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e8b2/6266604/ebc3080fcb7c/ijerph-15-02355-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e8b2/6266604/7ec36349076c/ijerph-15-02355-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e8b2/6266604/6a283ab8f0c0/ijerph-15-02355-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e8b2/6266604/5350218720e6/ijerph-15-02355-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e8b2/6266604/ebc3080fcb7c/ijerph-15-02355-g004.jpg

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Forms of phosphorus in suspended particulate matter in agriculture-dominated lowland catchments: Iron as phosphorus carrier.农业为主的低地集水区悬浮颗粒物中的磷形态:铁作为磷的载体。
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Variations of different dissolved and particulate phosphorus classes during an algae bloom in a eutrophic lake by P NMR spectroscopy.
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