Recharge Zone of Shallow Groundwater at Southeastern Part of Kulon Progo District Area based on Groundwater Facies

T. A, I. A. Prabowo
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Abstract

The Galur and Lendah areas are in the southeastern part of Kulon Progo Regency, Yogyakarta, Indonesia. This area has become a developing area because of the new airport in this district. Along with its development, the need for groundwater in this area is increasing, so groundwater research is also increasingly needed. A study on groundwater is required to support the development of this region. This time, a groundwater study was conducted to determine the potential for the recharge-discharge zone, also groundwater flow patterns based on the chemical facies of the groundwater. The hydrogeological survey was carried out with groundwater sampling from 9 (nine) dug wells and 1 () spring for physical/chemical testing of groundwater in the laboratory. The results showed groundwater in the study area generally flows south or northwest, with a radial pattern anomaly in the north. The shallow groundwater studied was bicarbonate type with Ca, Na, and Mg cations variations. The groundwater facies characterizes groundwater that is typical in the catchment
基于地下水相的库仑普罗戈区东南部浅层地下水补给带
Galur和Lendah地区位于印度尼西亚日惹市Kulon Progo Regency的东南部。由于这个地区有了新机场,这个地区已成为一个发展中的地区。随着其发展,该地区对地下水的需求越来越大,因此对地下水研究的需求也越来越大。为了支持这个地区的发展,需要对地下水进行研究。这一次,进行了地下水研究,以确定补给-排放区的潜力,以及基于地下水化学相的地下水流动模式。水文地质调查从9口挖井和1口井抽取地下水,在实验室对地下水进行物理/化学测试。结果表明:研究区地下水总体向南或向西北流动,北部呈放射状异常;研究的浅层地下水为碳酸氢盐型,存在Ca、Na、Mg阳离子的变化。地下水相是集水区典型地下水的特征
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