Hydrogeology of Mangsri Cave, Gunungsewu Karst Area, Java Island, Indonesia

A. Cahyadi, H. Reinhart, A. W. Ristiawan, Reza Putra, M. Labib, M. Naufal, I. Riyanto, F. Ramadhan, Angga Dwi Laksono
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引用次数: 1

Abstract

The Gunungsewu karst area is not only known for its unique landscape but also its recurring drought events. To meet the water supply, the local population utilizes several water potentials, namely doline pond, spring, and underground river. This study was designed to analyze the hydrogeological conditions of Mbangsri Cave, following its accidental discovery by the community at the end of 2018. The hydrogeological analysis was conducted by geological surveys, which consisted of rocks collection and structural measurements, cave mapping, and recharge area delineation based on remote sensing images acquired by unmanned aerial vehicles. The results showed that Mbangsri Cave, in the hydrogeological perspective, had low water resources potential. It is believed to be the result of (1) relatively small catchment area, (2) a fault in the southern part of Mbangsri Cave, creating a small groundwater basin, and (3) the thin epikarst layer, limiting the water storage.
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印度尼西亚爪哇岛Gunungsewu喀斯特地区Mangsri洞的水文地质
Gunungsewu喀斯特地区不仅以其独特的景观而闻名,而且经常发生干旱事件。为了满足当地的供水需求,当地居民利用了几种水势,即碱塘、泉水和地下河。本研究旨在分析Mbangsri洞穴的水文地质条件,该洞穴于2018年底被社区意外发现。水文地质分析是通过地质调查进行的,包括岩石收集和构造测量、洞穴测绘和基于无人机遥感图像的补给区划定。结果表明,从水文地质角度看,姆邦斯里洞水资源潜力较低。这被认为是:(1)相对较小的集水区;(2)Mbangsri洞南部的断层形成了一个较小的地下水盆地;(3)薄的表溶层,限制了水的储存。
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