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Piezometric and hydrogeochemical characterization of groundwater circulation in complex karst aquifers. A case study: the Mancha Real-Pegalajar aquifer (Southern Spain)

机译:复杂岩溶含水层地下水循环的测压和水文地球化学特征。案例研究:Mancha Real-Pegalajar含水层(西班牙南部)

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摘要

A small karst aquifer of great structural com plexity has been subjected to significant resource with drawal over recent decades. This exploitation aroused social conflict due to the effect it has had on emblematic springs. This research has analysed piezometric data col lected over the course of 12 years and the spatial hydro chemical data supplied by the main water points associated with it. The spatial and temporal evolution of the main chemical species in the groundwater and the hydrogeo chemical processes affecting them have been studied, modelling them with the programme PHREEQC. These data suggest a complicated model of hydrogeological function with sectors storing water at different depths and connected to each other locally as determined by the geological structure.
机译:近几十年来,一个结构复杂的小型岩溶含水层受到了大量资源的吸引。这种剥削由于对象征泉源的影响而引起了社会冲突。这项研究分析了过去12年中收集的测压数据以及与之相关的主要水位提供的空间水化学数据。研究了地下水中主要化学物质的时空演化及其影响的水文地质化学过程,并使用PHREEQC程序对其进行了建模。这些数据表明了一个复杂的水文地质功能模型,其中区段存储着不同深度的水,并根据地质结构确定了局部相互连接的位置。

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