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富营养化和盐化会提高干旱湖泊中溶解有机物的含量。

Eutrophication and salinization elevate the dissolved organic matter content in arid lakes.

机构信息

School of City and Environment, Northwest University, Xi'an, 710127, China; Key Laboratory of Watershed Geography, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing, 210008, China; Shanxi Key Laboratory of Surface System and Environmental Carrying Capacity, Northwest University, Xi'an, 710127, China.

Key Laboratory of Watershed Geography, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing, 210008, China.

出版信息

Environ Res. 2023 Sep 15;233:116471. doi: 10.1016/j.envres.2023.116471. Epub 2023 Jun 20.

Abstract

Dissolved organic matter (DOM) plays an essential role in the global lake carbon cycle. Understanding DOM composition and monitoring its spatiotemporal dynamics are of great significance for understanding the lake carbon cycle, controlling water pollution, and protecting water resources. However, previous studies have focused mainly on eutrophic freshwater lakes, with limited attention given to saline lakes. Based on in situ data collected in ten lakes in northwestern China, this study reported the changes in DOM components in different lake types. Parallel factor analysis (PARAFAC) was used to analyze the three-dimensional excitation emission matrix (EEMs) to obtain the DOM fluorescence components. The contributions of different environmental factors to the changes in DOM components were quantified by the generalized linear model (GLM). The results showed that the eutrophication index was significantly positively related to dissolved organic carbon (DOC) (R = 0.95, p < 0.01) and colored DOM (CDOM) (R = 0.96, p < 0.01) concentrations. Terrestrial humic-like and tryptophan-like components, which are highly correlated with human activities, explained 62% and 64% of the variations in DOC and CDOM, respectively. In sum, the contributions of human activities to the DOC and CDOM variations were 61% and 57%, respectively. Salinity also showed significant positive correlations with both DOC (R = 0.88, p < 0.01) and CDOM (R = 0.87, p < 0.01). Lake salinization led to increases in DOM concentration, and salinity contributed 20% and 16% to the DOC and CDOM variations, respectively. Therefore, human activities and salinity codetermined the DOM concentration and its composition in the western arid lakes. Based on these findings, this study proposed a feasible flowchart for remotely estimating DOM in saline lakes using satellite data. This study is significant for the long-term monitoring of the carbon cycle and the effective protection of lake water resources in saline lakes.

摘要

溶解有机物质(DOM)在全球湖泊碳循环中起着至关重要的作用。了解 DOM 的组成并监测其时空动态对于理解湖泊碳循环、控制水污染和保护水资源具有重要意义。然而,以前的研究主要集中在富营养化的淡水湖泊上,对盐水湖的关注有限。本研究基于中国西北部十个湖泊的现场数据,报道了不同湖泊类型中 DOM 成分的变化。采用平行因子分析(PARAFAC)对三维激发发射矩阵(EEMs)进行分析,以获得 DOM 荧光成分。通过广义线性模型(GLM)量化了不同环境因素对 DOM 成分变化的贡献。结果表明,富营养化指数与溶解有机碳(DOC)(R = 0.95,p < 0.01)和有色溶解有机物质(CDOM)(R = 0.96,p < 0.01)浓度呈显著正相关。与人类活动高度相关的陆地腐殖质样和色氨酸样成分分别解释了 DOC 和 CDOM 变化的 62%和 64%。总之,人类活动对 DOC 和 CDOM 变化的贡献分别为 61%和 57%。盐度与 DOC(R = 0.88,p < 0.01)和 CDOM(R = 0.87,p < 0.01)均呈显著正相关。湖泊盐化导致 DOM 浓度增加,盐度对 DOC 和 CDOM 变化的贡献分别为 20%和 16%。因此,人类活动和盐度共同决定了西部干旱湖泊中 DOM 的浓度及其组成。基于这些发现,本研究提出了一种利用卫星数据远程估计盐水湖 DOM 的可行流程图。本研究对于长期监测碳循环和有效保护盐水湖水资源具有重要意义。

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