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首页> 外文期刊>Environmental Science and Pollution Research >Large scale groundwater flow and hexavalent chromium transport modeling under current and future climatic conditions: the case of Asopos River Basin
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Large scale groundwater flow and hexavalent chromium transport modeling under current and future climatic conditions: the case of Asopos River Basin

机译:当前和未来气候条件下的大规模地下水流和六价铬迁移模型:以阿苏波斯河盆地为例

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In recent years, high concentrations of hexavalent chromium, Cr(VI), have been observed in the groundwater system of the Asopos River Basin, raising public concern regarding the quality of drinking and irrigation water. The work described herein focuses on the development of a groundwater flow and Cr(VI) transport model using hydrologic, geologic, and water quality data collected from various sources. An important dataset for this goal comprised an extensive time series of Cr(VI) concentrations at various locations that provided an indication of areas of high concentration and also served as model calibration locations. Two main sources of Cr(VI) contamination were considered in the area: anthropogenic contamination originating from Cr-rich industrial wastes buried or injected into the aquifer and geogenic contamination from the leaching process of ophiolitic rocks. The aquifer's response under climatic change scenario A2 was also investigated for the next two decades. Under this scenario, it is expected that rainfall, and thus infiltration, will decrease by 7.7 % during the winter and 15 % during the summer periods. The results for two sub-scenarios (linear and variable precipitation reduction) that were implemented based on A2 show that the impact on the study aquifer is moderate, resulting in a mean level decrease less than 1 m in both cases. The drier climatic conditions resulted in higher Cr(VI) concentrations, especially around the industrial areas.
机译:近年来,在阿苏波斯河流域的地下水系统中观察到高浓度的六价铬Cr(VI),引起公众对饮用水和灌溉水质量的关注。本文描述的工作着重于使用从各种来源收集的水文,地质和水质数据开发地下水流量和Cr(VI)传输模型。实现这一目标的重要数据集包括各个位置的Cr(VI)浓度的广泛时间序列,这些时间序列可指示高浓度区域,也可作为模型校准位置。该地区考虑了Cr(VI)污染的两个主要来源:人为污染,源于埋藏或注入含水层中的富含Cr的工业废物,以及来自卵石岩石浸出过程的地质污染。在接下来的二十年中,还研究了在气候变化情景A2下含水层的响应。在这种情况下,预计冬季降雨和入渗量将减少7.7%,夏季减少15%。基于A2实施的两个子方案(线性和可变降水减少)的结果表明,对研究含水层的影响是中等的,导致两种情况下平均水位下降均小于1 m。较干燥的气候条件导致较高的Cr(VI)浓度,尤其是在工业区附近。

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