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Tracking the monthly changes of dissolved organic matter composition in a newly constructed reservoir and its tributaries during the initial impounding period

机译:追踪初期蓄水期间新建水库及其支流中溶解性有机物组成的每月变化

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Understanding the roles of inland reservoirs becomes increasingly important with respect to global carbon cycling as well as water resource management due to the unprecedented demand for construction in recent decades. In this study, the dissolved organic matter (DOM) quantity and quality in a newly constructed dam reservoir and its tributaries were monitored monthly during the initial impounding period (July to November 2014) using a size exclusion chromatography (SEC) with online organic carbon detector (OCD). The highest values were observed in the month of August with the highest precipitation for the bulk dissolved organic carbon (DOC), specific UV absorbance (SUVA), and most of the assigned size fractions (except for biopolymers) in the tributaries, indicating that allochthonous sources of DOM were dominant in the feeding stream waters of the reservoir. The bulk DOC and high molecular weight humic substance fraction (similar to 1 kDa) were generally co-varied with the monthly precipitation in the tributaries, while building blocks (350-500 Da), and low molecular weight (LMW) acids and neutrals showed different trends. In a dam site, the smaller molecular fractions became more abundant during the dry season (September to November), presumably due to the in-reservoir processes such as photo- and bio-degradation. Our results also revealed that storms mobilized a large amount of highly aromatic soil-derived DOM to the reservoir. A depth profile at the dam site showed the water is well mixed up to a depth of similar to 20 m. The SEC-OCD data coupled with non-metric multidimensional scaling provided a clear visualization of the spatiotemporal variations in DOM composition, which shed new light on the DOM composition formed in a newly constructed dam reservoir and also on the strategies for future water treatment options.
机译:由于近几十年来对建筑的空前需求,了解内陆水库在全球碳循环以及水资源管理方面的作用变得越来越重要。在这项研究中,在初次蓄水期间(2014年7月至2014年11月),使用带有在线有机碳检测器的尺寸排阻色谱(SEC)每月对新建大坝水库及其支流中的溶解有机物(DOM)的数量和质量进行监测。 (OCD)。在8月观察到了最高值,其中支流中的大部分溶解有机碳(DOC),比紫外线吸收率(SUVA)和大多数指定的大小分数(生物聚合物除外)最多,这表明外生DOM的来源在水库的补给水流中占主导地位。 DOC的总含量和高分子量腐殖质分数(约1 kDa)通常与支流中的月降水量共变,而结构单元(350-500 Da)以及低分子量(LMW)酸和中性物质显示不同的趋势。在坝址上,较小的分子部分在干旱季节(9月至11月)变得更加丰富,这大概是由于诸如光降解和生物降解之类的储层内部过程。我们的结果还表明,暴风雨将大量高度芳香的土壤来源的DOM迁移到了水库。坝址处的深度剖面显示,水混合均匀,深度约为20 m。 SEC-OCD数据与非度量多维标度结合使用可以清楚地显示DOM组成的时空变化,这为新建水库中形成的DOM组成以及未来水处理方案的策略提供了新的思路。

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