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Assessing Groundwater Quality for Multiuse and Geochemical Evolution in the South Banat Area of Serbia, Pannonian Basin

机译:潘诺尼亚盆地塞尔维亚南巴纳特地区地下水水质综合利用与地球化学演化评估

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摘要

The study includes an assessment of groundwater quality from one shallow and two deeper aquifers in the Danube left bank, under the conditions of coexistence of the open coal mine, arable lands with increasing irrigation needs and potential regional water supply system for the Banat region. The spatial distribution maps of the targeted parameters were used as a starting point in the identification of nine zones in the study area. The Piper plot and the specific ionic plots pointed out that dissolution of carbonate and silicate minerals, as well as cation exchange, plays a significant role in the groundwater chemistry. Although the geological and hydrogeological complexity of the study area highlighted the considerable vertical and horizontal zonations when it comes to groundwater quality, waters have a desirable quality for drinking while for irrigation the eastern zone of the study area is better. Vertical mixing of shallow and deeper groundwaters confirmed the post-sedimentary faulting and erosion of coal seams in the central part of the study area. Generally, the results of determining the origin and quality of groundwaters throughout the study area could greatly help in making decisions regarding the regional water supply and expansion of irrigated lands in the future.
机译:该研究包括在露天煤矿与土地并存,灌溉需求不断增加以及巴纳特地区潜在的区域供水系统共存的条件下,对多瑙河左岸一处浅水层和两处深水层的地下水水质进行评估。目标参数的空间分布图被用作识别研究区域中九个区域的起点。 Piper图和特定离子图指出,碳酸盐和硅酸盐矿物的溶解以及阳离子交换在地下水化学中起着重要作用。尽管研究区域的地质和水文地质复杂性突出显示了涉及地下水质量的相当大的垂直和水平区域,但是水的饮用质量令人满意,而研究区域东部的灌溉条件则更好。浅层和深层地下水的垂直混合证实了研究区中部的沉积后断层和煤层的侵蚀。通常,确定整个研究区域地下水的来源和质量的结果将极大地有助于将来就区域供水和灌溉土地的扩张做出决策。

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