Mapping groundwater potential zones in Cilongok Area, Banyumas, Central Java using 2D geoelectrical resistivity

S. Herho, Plato Martuani Siregar, Iqbal Syarief, Dasapta Erwin Irawan, Marlison Justiana Sinaga
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Abstract

The aim of this study is to investigate the presence of potential aquifer layers that would be used as a source of clean water for residents in Cilongok sub-district. We conducted a ground water potential survey at two locations in the sub-district, i.e. Cikidang and Kalisari villages. At each location, geoelectric measurements were taken with the Wenner configuration and the horizontal distance of 900 meters, so that we can get the estimation of lithology layers that potentially store groundwater up to the depth of $\pm 100$ meters. Then the measurement result was processed by using Res2DInv software to get the 2D resistivity images of rock layers. Based on the resistivity estimation and observation of regional geological conditions in that area, then we conducted 2D interpretation about potential lithology layers that economically potential for water well drilling and to be utilized as a source of clean water for the residents. Based on the interpretation of lithology, it was known that the aquifer layer that has the potential as a source of clean water is a layer that consists of coarse and porous tuffs from volcanic eruption products that can easily drain groundwater on the average about 28 to 45 meters depth in Cikidang village and about 45 to 60 meters depth in Kalisari village.
利用二维地电阻率在中爪哇Banyumas的Cilongok地区绘制地下水潜在带
这项研究的目的是调查潜在的含水层的存在,这些含水层将被用作Cilongok街道居民的清洁水源。我们在街道的两个地点,即Cikidang村和Kalisari村进行了地下水势调查。在每个位置,采用Wenner配置和900米的水平距离进行地电测量,这样我们就可以得到可能储存地下水至100米深度的岩性层的估计。然后利用Res2DInv软件对测量结果进行处理,得到岩层的二维电阻率图像。在电阻率估算和区域地质条件观测的基础上,对该区具有钻井经济潜力、可作为居民清洁水源的潜在岩性层进行了二维解释。根据岩性解释,具有清洁水源潜力的含水层是由火山喷发产物的粗糙多孔凝灰岩组成的含水层,在池池塘村平均深度为28 ~ 45米,在卡利萨里村平均深度为45 ~ 60米,很容易排走地下水。
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