Liang Jian, Jiang Tao, Lu Song, Wei Shi-Qiang, Wang Ding-Yong, Chen Xue-Shuang, Wang Qi-Lei
Key Laboratory of Eco-environments in Three Gorges Reservoir Region, Ministry of Education, Chongqing Key Laboratory of Agricultural Resources and Environment, College of Resources and Environment, Southwest University, Chongqing 400716, China.
Department of Forest Ecology and Management, Swedish University of Agricultural Sciences, Umeå SE-90183, Sweden.
Huan Jing Ke Xue. 2016 Jul 8;37(7):2506-2514. doi: 10.13227/j.hjkx.2016.07.012.
As an important sources of dissolved organic matter (DOM) in aquatic system, DOM releases from flooding or submerged soils is a key process in water-level fluctuation zones. In this study, four typical sites in water-level fluctuation zones of Three Gorges Reservoir areas were selected to conduct simulated soil flooding experiments, under ambient (open air) and anoxic conditions. By using fluorescence spectrum technique, the dynamic and geochemical characteristics of DOM releases from flooding soils were investigated. Results showed that the trend or model of DOM releases observed by fluorescence spectrum in all soils from four sampling sites was similar to the observation by UV-Vis spectrum. Fluorescence property of DOM releases showed an important contribution to DOM fluorescence in overlying waters. The rapid releases at initial stage and removal mechanism for later dynamic equilibrium were crucial to explain the dynamic "source-sink" equilibrium in whole flooding period. Effect of inorganic mineral adsorption-desorption on humic-like components (A and C peaks) was significant. Also, impact of microbial utilization on protein-like components (B and T peaks) was confirmative. Additionally, all DOM samples had "autochthonousness plus allochthonousness" property. Except Shibaozhai (SB) site in Zhongxian county, during the whole flooding period, all three other sites didn't show any significant difference between ambient and anoxic conditions. They could be explained by the high heterogeneity of soil property including minerals and organic components. Meanwhile, both the UV-Vis and fluorescence spectra were complementary for each other, and they evidentially showed that the "source-sink" (release and removal) mechanism in DOM releases from submerged soils was the core to decide the dynamics of DOM in overlying waters. Importantly, DOM showed higher aromaticity and humification at the initial release stage when flooding occurred, as well as the greater terrestrial source characteristics, which further helped to explain the environmental fates of pollutants in these environmental sensitive areas. It would also be useful for unveiling the role of DOM in environmental system in future.
作为水生系统中溶解有机物(DOM)的重要来源,淹没土壤中DOM的释放是水位波动带的一个关键过程。本研究选取三峡库区水位波动带的四个典型位点,在有氧(露天)和缺氧条件下进行模拟土壤淹水实验。利用荧光光谱技术,研究了淹水土壤中DOM释放的动态和地球化学特征。结果表明,四个采样位点所有土壤中通过荧光光谱观测到的DOM释放趋势或模型与紫外可见光谱观测结果相似。DOM释放的荧光特性对上覆水体中DOM荧光有重要贡献。初始阶段的快速释放以及后期动态平衡的去除机制对于解释整个淹水期的动态“源 - 汇”平衡至关重要。无机矿物吸附 - 解吸对类腐殖质组分(A峰和C峰)的影响显著。此外,微生物利用对类蛋白质组分(B峰和T峰)的影响也得到了证实。另外,所有DOM样品都具有“自源加外源”特性。除忠县石宝寨(SB)位点外,在整个淹水期,其他三个位点在有氧和缺氧条件下均未表现出显著差异。这可以用包括矿物质和有机组分在内的土壤性质的高度异质性来解释。同时,紫外可见光谱和荧光光谱相互补充,它们清楚地表明淹没土壤中DOM释放的“源 - 汇”(释放和去除)机制是决定上覆水体中DOM动态的核心。重要的是,淹水发生时DOM在初始释放阶段表现出更高的芳香性和腐殖化程度,以及更强的陆源特征,这进一步有助于解释这些环境敏感区域中污染物的环境归宿。这对于未来揭示DOM在环境系统中的作用也将是有用的。