我国北方典型湖库水体溶解性有机质赋存特征及影响因素
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1.中国环境科学研究院;2.成都理工大学生态环境学院

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国家科技基础性工作专项( 2015FY110900-005)


Distribution characteristics and environmental controls of dissolved organic matter in typical northern Chinese lakes and reservoirs
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1.State Key Laboratory of Environmental Benchmarks and Risk Assessment,Chinese Academy of Environmental Sciences;2.China;3.Institute of Water Ecology and Environment,Chinese Academy of Environmental Sciences;4.College of Ecology and Environment,Chengdu University of Technology

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National Science and Technology Basic Work Project (2015FY110900-005)

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    摘要:

    溶解性有机质(DOM)在水生生态系统和生物地球化学过程中起着至关重要的作用。解析我国北方典型湖库水体溶解性有机质组分特征、来源及影响因素对湖泊水体有机物污染及防治具有十分重要的意义。该论文共采集了130个点位的表层水样,采集区域如下:小兴凯湖(XXKH)、 松花湖(SHH)、大伙房水库(DHF)、官厅水库(GT)、于桥水库(YQ)、白洋淀(BYD)、衡水湖(HSH)、南四湖(NSH)。结果显示:①采用平行因子分析(PARAFAC)从北方八个湖库水体的DOM中分离出3个组分:类腐殖质(C1)、类色氨酸(C2)、类酪氨酸(C3)。其中东北湖库的DOM具有较强的腐殖化和较低的自生源特征,华北地区湖库的DOM具有较强的自生源特征;相较于其他湖库,BYD的DOM具有强烈的自生源特征,且DOM含量和类蛋白质占比偏高。 ②人类活动等外源带来的类腐殖质输入与COD、HIX有显著正相关(p<0.01);类蛋白质组分C2、C3含量与DOC浓度、FI、BIX指数有显著正相关(p<0.01),以及与HIX指数有显著负相关性(p<0.01);DOM各组分与氮营养盐的相关性比磷营养盐高。③较大的流域面积会延长DOM在湖内的滞留时间,并促进内源DOM组分的积累;较深的水体有利于DOM组分的保存。温度升高会增强DOM的湖内转化,增强内源特征,减弱外源特征;降水量较多的地区,雨水径流将陆源腐殖质输入水体,增强外源DOM特征。藻类、水生植被和微生物主要通过内源过程来影响DOM的动态变化,共同调节水体的营养循环和生态功能。人类活动较高的地区,会促进湖库水体产生内源性DOM。植被覆盖度较高的地区,会给湖库水体带来更多的类腐殖质组分。

    Abstract:

    Dissolved organic matter (DOM) plays a pivotal role in aquatic ecosystems and biogeochemical cycles. Understanding the composition characteristics, sources, and influencing factors of DOM in typical lakes and reservoirs across northern China is crucial for effective organic matter pollution control and ensuring safe water transfer. This study collected 130 surface water samples from eight representative water bodies: Xiaoxingkai Lake (XXKH), Songhua Lake (SHH), Dahuofang Reservoir (DHF), Guanting Reservoir (GT), Yuqiao Reservoir (YQ), Baiyangdian Lake (BYD), Hengshui Lake (HSH), and Nansi Lake (NSH). The key findings are as follows: (1) Through parallel factor analysis (PARAFAC), three distinct fluorescent components were identified in the DOM of these lakes and reservoirs: humic-like substances (C1), tryptophan-like substances (C2), and tyrosine-like substances (C3). DOM in northeastern lakes and reservoirs exhibited strong humification characteristics with relatively low autochthonous contributions, while those in North China demonstrated pronounced autochthonous features. Notably, BYD displayed unique DOM characteristics with higher DOM content and protein-like components compared to other studied water bodies. (2) Humic-like substances from anthropogenic sources significantly positively correlated with COD and HIX (p < 0.01). Protein-like components (C2, C3) showed significant positive correlations with DOC, FI, and BIX (p < 0.01), but negative correlations with HIX (p < 0.01). DOM components correlated more strongly with nitrogen than phosphorus nutrients. (3) Environmental factors significantly influenced DOM dynamics. Larger drainage areas prolonged DOM retention time, promoting the accumulation of autochthonous DOM components. Greater water depth facilitated DOM preservation. Elevated temperatures enhanced DOM transformation within lakes, strengthening autochthonous characteristics while weakening allochthonous features. In high-precipitation regions, terrestrial humic substances were transported into water bodies through runoff, enhancing exogenous DOM characteristics. Biological factors, including algae, aquatic vegetation, and microorganisms, primarily influenced DOM dynamics through endogenous processes, collectively regulating nutrient cycling and ecological functions. In areas with intensive human activities, increased endogenous DOM production was observed in lake and reservoir waters. Furthermore, regions with higher vegetation coverage contributed more humic-like components to aquatic systems. This comprehensive analysis provides valuable insights into DOM dynamics in northern China"s lakes and reservoirs, offering scientific basis for water quality management and pollution control strategies.

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  • 收稿日期:2024-12-02
  • 最后修改日期:2025-02-24
  • 录用日期:2025-04-02
  • 在线发布日期: 2025-05-26
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