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首页> 外文期刊>Estonian Journal of Earth Sciences >Conceptual model of groundwater quality for the monitoring and management of the Voronka groundwater body, Estonia
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Conceptual model of groundwater quality for the monitoring and management of the Voronka groundwater body, Estonia

机译:监测和管理爱沙尼亚沃龙卡地下水体的地下水水质概念模型

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摘要

A fundamental knowledge of processes that control groundwater composition is required for informed management of water quality. The Voronka groundwater body in northeastern Estonia represents a good example of a complicated, overexploited groundwater system where conceptual understanding of baseline quality and governing hydrogeochemical processes can support sustainable aquifer management. A conceptual understanding or conceptual model is a simplified representation or a working understanding of the real hydrogeological system and its processes. The baseline chemical composition of the Voronka groundwater body was formed during the last glaciations, when glacial meltwater intruded into water-bearing rocks. Two main processes that can change Voronka groundwater body quality at the present day are: (1) seawater intrusion and (2) water exchange between buried valleys and formation's groundwater. Future monitoring and management should focus on changes in the natural composition of groundwater caused by abstraction. The HCO_3 ~-/Cl~-value is the best parameter to describe the fluctuations in natural background chemistry in the Voronka groundwater body and to assess significant trends induced by abstraction. In case of the discovered trends, a suite of isotope methods, especially ~(14)C, ~3H, δ~2H, δ~(18)O and δ~(13) C, can be used to detect whether the intrusion of seawater or exchange of water with buried valleys is taking place.
机译:要对水质进行明智的管理,必须具备控制地下水成分的过程的基础知识。爱沙尼亚东北部的沃龙卡(Voronka)地下水体是复杂,开发过度的地下水系统的一个很好的例子,在该系统中,对基线质量和控制水文地球化学过程的概念理解可以支持可持续的含水层管理。概念理解或概念模型是对实际水文地质系统及其过程的简化表示或工作理解。沃龙卡地下水体的基线化学成分是在末次冰川期形成的,当时冰川融水侵入了含水岩石。目前,可以改变沃龙卡地下水体质量的两个主要过程是:(1)海水入侵和(2)埋谷与地层地下水之间的水交换。未来的监测和管理应集中在由提取引起的地下水自然组成的变化上。 HCO_3〜-/ Cl〜值是描述沃龙卡地下水体中自然本底化学波动并评估抽象引起的重要趋势的最佳参数。在发现趋势的情况下,可以使用一套同位素方法,尤其是〜(14)C,〜3H,δ〜2H,δ〜(18)O和δ〜(13)C,来检测是否存在侵入。海水或与埋谷交换水。

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