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Hydrogeological research on intensively exploited deep aquifers in the 'Loma de úbeda' area (Jaén, southern Spain)

机译:“ Loma deúbeda”地区(西班牙南部哈恩)密集开采的深层含水层的水文地质研究

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摘要

The intensive use of groundwater for irrigation in the area of úbeda ('Loma de úbeda', Jaén, southern Spain) has transformed an area of traditionally rain-fed dry farmland into fields with some of the highest olive oil productivity in the world. Early hydrogeological research studies, initiated just after the beginning of the groundwater exploitation, revealed that the water was collected from three different overlapping aquifers occupying an area of over 1,100 km2, with the lower aquifers located at depths from 300 to over 700 m in an area of 440 km2. Multidisciplinary research, based on geological characterization, and piezometric, hydrochemical and isotopic data, has led to a conceptual model of functioning in this complex hydrogeological system. The proposed model allows for the identification of the recharge areas, and the discharge, which is at present mainly associated with the groundwater pumping. Areas of mixing of waters from the different aquifers and the main hydrogeochemical processes affecting groundwater quality are described.
机译:乌贝达地区(西班牙南部哈恩省的“洛马德乌贝达”,洛马德乌贝达地区)大量使用地下水进行灌溉,已将传统上靠雨水灌溉的旱田变成了世界上橄榄油产量最高的田地。在地下水开采开始后不久就开始的早期水文地质研究表明,水是从三个不同的重叠含水层中收集的,这些含水层面积超过1100 km2,而较低的含水层位于该区域300至700 m以上的深度440平方公里。基于地质特征以及测压,水化学和同位素数据的多学科研究,导致了在这个复杂的水文地质系统中发挥作用的概念模型。所提出的模型允许识别补给区域和排放,目前主要与地下水抽取有关。描述了来自不同含水层的水的混合区域以及影响地下水质量的主要水文地球化学过程。

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