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首页> 外文期刊>Journal of Hydrology >Model-based analysis of dissolved oxygen supply to aquifers within riparian zones during river level fluctuations: Dynamics and influencing factors
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Model-based analysis of dissolved oxygen supply to aquifers within riparian zones during river level fluctuations: Dynamics and influencing factors

机译:基于模型的河水水位波动期间河岸带含水层溶解氧供应分析:动力学及其影响因素

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Dissolved oxygen (DO) largely impacts the environmental function of riparian aquifers. However, the dynamics and influencing factors of DO supply to riparian aquifers are not well understood. In this study, we developed a model considering air-liquid two-phase flow, air entrapment and multi-phase transport of O_2(g) in a riparian aquifer to investigate the hydrologic exchange flows and DO supply during river level fluctuations. A sensitivity analysis was conducted to quantify the influences of hydrological conditions of river, hydrogeological conditions of riparian aquifer, DO consumption rate constant and DO concentration in the river water on DO supply to the riparian aquifer. Results show that the river, the entrapped air and the unsaturated zone all provide a significant amount of DO to the riparian aquifer, and there are also noticeable differences in the spatial distribution of DO from the three different sources. Results also indicate there are a DO-rich strip and a DO-rich plume occurring in the top of the riparian aquifer and the channel-aquifer interface, respectively. Both DO-rich areas are the research focus in evaluating the environmental function of riparian zones. Further, the DO supply amount shows a significant increase as the river amplitude and period increase, and a losing river and increasing hydraulic conductivity also leads to the increasing DO supply flux because these incidents promote infiltration of the river water. In contrast, the high DO concentration in the river water increases the DO flux from river but reduces the DO supply from the entrapped air and the unsaturated zone because of the competition in different supply pathways. Moreover, the model simulations agree with the measurements of DO source in a field that has been reported. This work provides a useful tool for estimating DO supply to riparian aquifers and improves our understanding of the environmental function of riparian zones.
机译:溶解氧(DO)在很大程度上影响了河岸含水层的环境功能。然而,对河岸含水层溶氧供应的动态和影响因素尚不清楚。本研究建立了河岸含水层中O_2(g)的气液两相流、空气滞留和多相输送的模型,研究了河水水位波动过程中的水文交换流和溶氧供应。通过敏感性分析,量化了河流水文条件、河岸含水层水文地质条件、河水中溶氧消耗率常数和溶氧浓度对河岸含水层溶氧供应的影响。结果表明:河流、滞留空气和非饱和带均向河岸含水层提供了大量的溶氧,且3种不同来源的溶氧空间分布也存在明显差异。研究结果还表明,在河岸含水层和河道-含水层界面的顶部分别存在富含溶氧的带状物和富含溶氧物的羽流。这两个富含溶氧层的区域都是河岸带环境功能评价的研究重点。此外,随着河流振幅和周期的增加,溶氧供应量呈显著增加趋势,而河流的流失和水力传导率的增加也导致溶氧供应通量增加,因为这些事件促进了河水的渗透。相反,由于不同供应途径的竞争,河水中的高溶氧浓度增加了河流的溶氧通量,但减少了截留空气和非饱和带的溶氧供应。此外,模型模拟结果与已报道的领域中溶解氧源的测量结果一致。这项工作为估算河岸含水层溶氧供应量提供了有用的工具,提高了我们对河岸带环境功能的认识。

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