云南杞麓湖底泥营养物质分布及释放特征
CSTR:
作者:
作者单位:

1.云南省生态环境科学研究院/云南省重金属污染控制工程技术研究中心;2.中国科学院南京地理与湖泊研究所/湖泊与流域水安全重点实验室

作者简介:

通讯作者:

中图分类号:

基金项目:

国家自然科学基金联合基金项目(U220220245),云南省科技厅重点研发计划“生态补水影响下程海水生态系统安全评估研究与示范”(202303AC100019),兴滇英才支持计划2025年度青年人才项目(530000251100004339966),云南典型工业园区地下水中特征新污染物精准识别与风险评估研究项目。


On the Distribution and Release Characteristics of Nutrients in the Sediments of Qilu Lake,Yunnan Province
Author:
Affiliation:

1.Yunnan Provincial Academy of Eco-Environmental Sciences;2.Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences

Fund Project:

This work was supported by the Joint Fund of the National Natural Science Foundation of China (No. U220220245); the Key Research and Development Program of Yunnan Province (No. 202303AC100019); the

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 附件
  • |
  • 文章评论
    摘要:

    摘要:为系统揭示云南高原重污染湖泊杞麓湖的底泥污染特征、内源释放风险及主要污染来源,为湖泊的科学精准治理提供理论依据,本研究于2024至2025年对杞麓湖全湖进行了系统的底泥调查。研究共布设20个采样点,测定了底泥总氮(TN)、总磷(TP)、有机质(OM)及多种重金属的含量,并结合GIS分析了其空间分布格局;同时选取西部河口、湖心及东北部三个典型区域,通过室内静态培养模拟实验,定量评估了氮磷营养盐的释放通量与形态转化规律;最终运用内梅罗综合污染指数法和主成分分析(PCA)等方法,对污染程度进行评价并解析了主要污染来源。结果表明:杞麓湖底泥是污染物的巨大“储藏库”,污染极其严重,表层底泥TN、TP、OM含量分别介于2120-11300 mg/kg、270-2280 mg/kg与41.4-260 g/kg。内梅罗指数评价显示,70%的采样点达到中度及以上污染水平(PN > 2.0),且总氮是导致污染的首要决定性因子。污染物空间分布呈现显著的异质性,在承接陆源输入的西南部入湖河口区和作为内源生物沉降中心的湖心区域形成“污染热点”。主成分分析清晰地区分两大类污染来源:一是以TP和多种重金属(特别是Cd、Pb、Cu、Zn)为特征的农业面源与工业源复合污染;二是以TN和OM为特征的生活污水与内源生物贡献的有机污染。静态释放实验证实,底泥是强烈的氮磷内源,湖心与东北部是主要的“高效释放区”,总磷释放通量最高可达2.80 mg/(m2·d),氨氮释放通量高达146.1 mg/(m2·d);而西部入湖河口区则表现出独特的总氮净吸收现象,是潜在的“脱氮功能区”。本研究的核心创新在于首次揭示了杞麓湖内源污染“存量”与“风险”在空间上的非均一性与功能分异。研究发现,污染物存量最高的西部入湖河口区,在释放机制上却表现为独特的总氮净吸收,是一个潜在的“脱氮功能区”。与之相对,湖心与东北部虽部分区域存量并非最高,却是氮磷“高效释放区”。这一发现不仅深化了对重污染浅水湖泊生物地球化学过程复杂性的理解,更重要的是,为湖泊内源治理从传统的单一片面的整体修复模式,转向基于“源-汇”格局和功能分异的精准分区管控策略,提供了关键的科学依据。

    Abstract:

    Abstract:To systematically reveal the sediment pollution characteristics, endogenous release risks, and primary pollution sources in Qilu Lake, a heavily polluted plateau lake in Yunnan, and to provide a scientific basis for its precise and effective management, a comprehensive sediment investigation was conducted across the entire lake from 2024 to 2025. This study involved collecting samples from 20 sites to determine the concentrations of total nitrogen (TN), total phosphorus (TP), organic matter (OM), and various heavy metals, with their spatial distribution patterns analyzed using GIS. Concurrently, laboratory static incubation experiments were performed on sediments from three typical areas—the western estuary, the lake"s center, and the northeastern region—to quantify the release fluxes and transformation patterns of nitrogen and phosphorus. Finally, methods such as Nemerow"s comprehensive pollution index and Principal Component Analysis (PCA) were employed to assess the pollution degree and identify the main sources. The results indicated that the sediments of Qilu Lake act as a massive "pollution reservoir" and are extremely polluted, with surface sediment concentrations of TN, TP, and OM ranging from 2120–11300 mg/kg, 270–2280 mg/kg, and 41.4–260 g/kg, respectively. The Nemerow"s index assessment revealed that 70% of the sampling sites reached moderate to severe pollution levels (PN > 2.0), with TN being the primary determining factor for the pollution. The pollutant distribution exhibited significant spatial heterogeneity, forming "pollution hotspots" in the southwestern estuary area, which receives terrestrial inputs, and in the central lake area, which serves as a deposition center for endogenous biomass. PCA clearly distinguished two major categories of pollution sources: (1) a composite source of agricultural non-point and industrial pollution, characterized by TP and various heavy metals (especially Cd, Pb, Cu, Zn); and (2) an organic pollution source, characterized by TN and OM, originating from domestic sewage and endogenous biological contributions. The static release experiments confirmed that the sediment is a strong internal source of nitrogen and phosphorus. The central and northeastern parts of the lake were identified as the main "high-efficiency release zones," with a maximum TP release flux of up to 2.80 mg/(m2·d) and an ammonia nitrogen release flux as high as 146.1 mg/(m2·d). In contrast, the western estuary area exhibited a unique net absorption of total nitrogen, suggesting its potential as a "denitrification functional zone." The core innovation of this study lies in revealing, for the first time, the spatial heterogeneity and functional differentiation between the "stock" (pollutant storage) and "risk" (release potential) of internal pollution in Qilu Lake. The study found that the western estuary area, despite having the highest pollutant stock, exhibited unique net total nitrogen absorption in its release mechanisms, identifying it as a potential "denitrification functional zone." Conversely, the central and northeastern areas, although some parts do not have the highest pollutant stock, function as the "high-efficiency release zones" for nitrogen and phosphorus. This finding not only deepens the understanding of the complexity of biogeochemical processes in heavily polluted shallow lakes but, more importantly, This provides the critical scientific evidence for evolving endogenous pollution remediation in lakes, moving away from conventional, simplistic, holistic approaches to a precision, zone-based management and control strategy informed by "source-sink" patterns and functional differentiation.

    参考文献
    相似文献
    引证文献
引用本文
相关视频

分享
文章指标
  • 点击次数:
  • 下载次数:
  • HTML阅读次数:
  • 引用次数:
历史
  • 收稿日期:2025-08-25
  • 最后修改日期:2025-12-02
  • 录用日期:2025-12-31
  • 在线发布日期: 2026-04-28
  • 出版日期:
文章二维码
您是第    位访问者
地址:南京市江宁区麒麟街道创展路299号    邮政编码:211135
电话:025-86882041;86882040     传真:025-57714759     Email:jlakes@niglas.ac.cn
Copyright:中国科学院南京地理与湖泊研究所《湖泊科学》 版权所有:All Rights Reserved
技术支持:北京勤云科技发展有限公司

苏公网安备 32010202010073号

     苏ICP备09024011号-2