Compositional changes of dissolved organic molecules along water flow and their influencing factors in the Three Gorges Reservoir

溶解有机碳 微观世界 环境化学 作文(语言) 非生物成分 总有机碳 碳纤维 孵化 α蛋白细菌 霍帕诺类 化学 碳循环 有机质 生态系统 生态学 地质学 生物 有机化学 材料科学 地貌学 烃源岩 16S核糖体RNA 哲学 语言学 构造盆地 复合材料 复合数 基因 生物化学
作者
Jian Yang,Liuqin Huang,Weiyu She,Geng Wu,Yun Wan,Hailiang Dong,Rosalie Chu,Nikola Tolić,Hongchen Jiang
出处
期刊:Chemical Geology [Elsevier BV]
卷期号:639: 121741-121741 被引量:1
标识
DOI:10.1016/j.chemgeo.2023.121741
摘要

Molecular composition of dissolved organic matter (DOM) and its influencing factors in river reservoirs remains elusive. Here, molecular compositions of DOM, bacterial community structures, and water physiochemistry were investigated in the field and microcosm samples of the Three Gorges Reservoir (TGR). The results showed that DOM molecular compositions were significantly (R2 = 0.245, p < 0.001) correlated with bacterial community structures in the studied field samples, suggesting that bacteria may actively interact with DOM molecules. The molecular compositions of DOM in the studied field samples were significantly (p < 0.05) affected by the distance between the sample sites and the Three Gorges Dam and by bacterial groups of Actinobacteria and Alphaproteobacteria, suggesting that both hydrological and bacterial processes may contribute to the variation in DOM molecular composition in the TGR water. Furthermore, microcosm experiments demonstrated that both microbial and abiotic processes may transform and/or produce DOM in the TGR, thereby affecting DOM molecular composition. Microbial process increased the average aromaticity index and decreased the carbon number of DOM molecules with increasing incubation duration; whereas average oxygen number, double bond equivalent, and oxidation state of carbon of DOM molecules increased during the first 14 days of incubation and began to decrease thereafter. Taken together, this study expands our understanding of the impact of microbial process on the DOM molecular composition in reservoir ecosystems, and has great implications for carbon cycling in major rivers.

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