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生态学杂志 ›› 2026, Vol. 45 ›› Issue (5): 1604-1615.

• 研究报告 • 上一篇    下一篇

浓江流域排水期溶解性有机质光学特征及来源解析

李莉莉1,2,肖敏2*   

  1. 1天津师范大学地理与环境科学学院, 天津 300387; 2天津师范大学水资源与水环境重点实验室, 天津 300387)
  • 出版日期:2026-05-10 发布日期:2026-05-08

Optical characterization and source analysis of dissolved organic matter during drainage period in the Nongjiang River Basin.

LI Lili1,2, XIAO Min2*   

  1. (1School of Geography and Environmental Sciences, Tianjin Normal University, Tianjin 300387, China; 2Key Laboratory of Water Resources and Environment, Tianjin Normal University, Tianjin 300387, China).

  • Online:2026-05-10 Published:2026-05-08

摘要: 目前对农业流域水体溶解性有机质(DOM)组分、来源及其关键影响因素的认识仍不充分。本研究选择我国三江平原典型农业流域——浓江流域农业排水期河水和湿地水体,借助紫外可见吸收光谱以及三维荧光光谱结合平行因子法,对流域DOM的光谱特征和物质组成开展研究,解析水体DOM来源,探讨人为活动和自然因素对河流湿地系统水体DOM的影响。结果表明:浓江流域水体DOM由4种组分组成,微生物腐殖质组分C1为最主要的荧光组分,组分C2和C3均为陆源类腐殖质化合物,而C4组分为类色氨酸化合物,流域水体DOM组分以类腐殖物质为主。紫外和荧光参数进一步表明,流域水体DOM以类腐殖质中的富里酸物质为主。流域水体DOM整体表现为内外源混合特征,其中,稻田水体DOM表现为较强的自生源特征,而湿地水体DOM的芳香性与疏水性较高,呈强腐殖化特征,陆源特征更明显。相关性分析表明,水体基本理化参数和光学参数与DOM表现出不同程度的相关性,说明湿地碳埋藏及微生物代谢等自然过程,以及农业活动和污水输入等人为活动,共同影响着浓江流域水体DOM的组成和分布。研究结果可为未来东北典型农业流域水体物质循环、碳收支平衡及碳库评价提供数据参考。


关键词: 溶解性有机质, 排水期, 三维荧光光谱, 平行因子分析

Abstract: Dissolved organic matter (DOM) is an important component of aquatic ecosystems, playing an indispensable role in material cycling. However, the DOM components and sources in agricultural watershed waters and their key influencing factors largely remain unknown. In the Nongjiang River Basin, a typical agricultural watershed in the Sanjiang Plain of China, we examined the spectral characteristics and composition of DOM in the watershed during the period of agricultural drainage, using UV-visible absorption spectroscopy (UV-vis) and three-dimensional fluorescence spectroscopy (3D-EEMs) combined with the parallel factor method. We analyzed the sources of DOM in the watershed, and investigated the impacts of anthropogenic and natural factors on the DOM of waters in the river-wetland system. The results showed that the water body DOM in the Nongjiang River Basin consisted of four components. The microbial humus component C1 was the dominant fluorescence component. Components C2 and C3 were terrestrial-source humus-like compounds, while component C4 was tryptophanlike compound. The DOM component of the watershed water body was dominated by humus-like substances. The UV and fluorescence parameters indicated that DOM in the watershed water body was dominated by fulvic acid substances in humus-like substances. The DOM in the watershed water bodies generally exhibited a mixed characteristic of endogenous and exogenous sources. Specifically, DOM in paddy water bodies showed a relatively strong endogenous source feature, while the aromaticity and hydrophobicity of DOM in wetland water bodies were higher, presenting a strong humification feature, with more obvious exogenous source feature. The basic physicochemical and optical parameters of water bodies showed different degrees of correlation with DOM, indicating that natural processes (such as carbon burial and microbial metabolism in wetlands) and anthropogenic activities (such as agricultural activities and sewage inputs) jointly influenced the composition and distribution of water body DOM in the Nongjiang River Basin. Our results can provide reference for the future evaluation of water body material cycling, carbon balance, and carbon pool in typical agricultural watersheds in Northeast China.


Key words: dissolved organic matter, drainage period, three-dimensional fluorescence spectroscopy, parallel factor analysis