富营养化削弱了我国东部浅水湖泊沉积物的稳定态磷累积
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1.云南师范大学地理学部;2.中国科学院南京地理与湖泊研究所;3.南京信息工程大学地理科学学院;4.南京大学地理与海洋科学学院

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基金项目:

国家重点研发计划项目(2022YFF0801100);国家自然科学基金项目(42507663)


Eutrophication weakens the stable phosphorus accumulation in sediments of shallow lakes in eastern China
Author:
Affiliation:

1.Faculty of Geography, Yunnan Normal University;2.Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences;3.Nanjing University of Information Science and Technology;4.School of Geography and Ocean Science, Nanjing University

Fund Project:

National Key Research and Development Program of China (2022YFF0801100); National Natural Science Foundation of China (42507663)

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    摘要:

    浅水湖泊富营养化已成为全球性环境问题。磷是湖泊富营养化的关键因子,其在沉积物中的分布以及不同形态间的转化直接影响内源磷释放潜力和生态恢复进程。现有研究多聚焦于浅水湖泊内源磷释放,对长尺度下湖泊富营养化对沉积物磷赋存特征的改变及其生态反馈机制仍然缺乏研究。本研究以我国东部平原37个浅水湖泊为研究对象,基于沉积柱记录,结合现代观测水体理化指标,重建了百年来湖泊沉积物磷形态的演变历史,探讨了其环境效应。结果表明,富营养化使得藻类生物量升高,表层沉积物中高释放风险的活性态磷对含量与比例上升,相对稳定的钙磷(Ca-P)含量和比例下降。同时,Ca-P与钙(Ca)的比值在时间序列上持续降低,表明与碳酸钙相关的磷固定过程逐渐减弱,包括磷酸根离子(PO43-)对碳酸钙(CaCO3)晶体结构中的部分碳酸根离子的替换(CO32-),以及难溶性钙磷矿物在CaCO3晶体表面或内部形成,这进一步说明富营养化背景下浅水湖泊沉积物惰性态磷累积能力可能被削弱。研究认为沉积物中活性磷比例升高将增强湖泊内源释放风险,加强湖泊浊水态正反馈过程,使得湖泊生态系统修复更加困难。

    Abstract:

    The eutrophication of shallow lakes has become a global environmental issue. Phosphorus (P) is a key driver of lake eutrophication, and its distribution within sediments, as well as the transformation among its different fractions, directly influences the potential for internal P release and the trajectory of ecological restoration. While existing studies predominantly focus on internal phosphorus (P) release in shallow lakes, the long-term alterations in sedimentary P speciation driven by eutrophication and the underlying ecological feedback mechanisms remain poorly understood. In this study, 37 shallow lakes in the Eastern Plain of China were selected as research subjects. Based on sediment core records and combined with contemporary physicochemical water quality observations, we reconstructed the centennial evolutionary history of P fractions in lake sediments and explored their environmental implications. The results indicate that eutrophication has led to an increase in algal biomass, leading to an increase in the content and proportion of high-release-risk active phosphorus in surface sediments, alongside a decrease in the content and proportion of relatively stable calcium-bound phosphorus (Ca-P). Furthermore, the ratio of Ca-P to calcium (Ca) continuously decreased over the time series, indicating a gradual weakening of phosphorus fixation processes associated with calcium carbonate. These processes include the substitution of phosphate ions (PO43-) for partial carbonate ions (CO32-) within the crystal structure of calcium carbonate (CaCO3), as well as the formation of insoluble calcium-phosphate minerals on the surface or within the interior of CaCO3 crystals. This further suggests that the accumulation capacity for inert phosphorus in shallow lake sediments may be impaired under eutrophic conditions. This study concludes that the elevated proportion of labile P in sediments will exacerbate the risk of internal P release and intensify the positive feedback loop of the turbid water state, thereby making the restoration of lake ecosystems significantly more difficult.

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  • 收稿日期:2026-05-19
  • 最后修改日期:2026-06-29
  • 录用日期:2026-06-29
  • 在线发布日期: 2026-07-31
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