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首页> 外文期刊>Journal of Geochemical Exploration: Journal of the Association of Exploration Geochemists >Hydrogeochemical characteristics of a volcanic-sedimentary aquifer with special emphasis on Fe and Mn content: A case study in Mexico
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Hydrogeochemical characteristics of a volcanic-sedimentary aquifer with special emphasis on Fe and Mn content: A case study in Mexico

机译:对Fe和Mn内容特别强调的火山沉积含水层的水力代科学特征 - 以墨西哥为例

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摘要

Previous studies performed on the volcanic-sedimentary aquifer of the Tenancingo Valley (Mexico) reports high concentrations of Fe, Mn, and NO3-, and water from several wells receives purification treatments due to presence of Fe and Mn. These studies have not achieved conclusive results regarding the origin of Fe and Mn, nor have hydrogeochemical evaluations of the aquifer been performed. The present study aimed to evaluate the physicochemical characteristics of the water and identify the geochemical processes that determine presence of Fe and Mn in groundwater. This characterization was based on physicochemical data from well and spring samples (16 samples) during dry and rainy seasons (June and November 2012, respectively).
机译:先前对特纳辛戈河谷(墨西哥)火山沉积含水层进行的研究报告显示,铁、锰和NO3-的浓度较高,由于铁和锰的存在,来自几口井的水接受了净化处理。这些研究尚未就铁和锰的来源取得结论性结果,也没有对含水层进行水文地球化学评估。本研究旨在评估水的物理化学特征,并确定决定地下水中铁和锰存在的地球化学过程。该特征基于旱季和雨季(分别为2012年6月和11月)期间油井和春季样本(16个样本)的物理化学数据。

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