Pendugaan sebaran intrusi air laut melalui sungai di desa Ujungmanik kecamatan Kawunganten kabupaten Cilacap menggunakan metode geolistrik resistivitas konfigurasi Wenner

Muhammad Sehah, Mitha Syahfitri, S. Sunardi
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引用次数: 1

Abstract

The estimation of the distribution of the sea water intrusion through the rivers in Ujungmanik Village, Kawunganten District, Cilacap Regency has been carried out using the Wenner configuration resistivity geoelectric. This research aims to estimate the distribution of sea water intrusion through rivers in Ujungmanik Village, Kawunganten District, Cilacap Regency based on geoelectric resistivity and conductivity data of groundwater. The geoelectric data acquisition was carried out on four lines. They were Wen1 Line, Wen2 Line, Wen3 Line, and Wen4 Line. Each line had a range of 200 meters. The results of geoelectric data processing showed that the subsurface rock structure consisted of sand, clay, sandy loam, and sandy clay. The Seawater intrusion shown by the sand layer occurred in all trajectories which had a range of resistivity value of 0.20 - 2.79 Ωm. Groundwater samples was carried out at fifteen points with the conductivity value varies between 1363 - 4145 µS / cm so that they can be classified that the water was fresh and brackish due to the sampling done in the rainy season. From this research it can be implied that the entire Ujungmanik  area is evenly intruded by the sea water at the coordinates 7º38ꞌ15.62ꞌꞌLS 108°57ꞌ20.89ꞌꞌBT to 7º39ꞌ22.86ꞌꞌLS 108º56ꞌ35.33ꞌꞌBT.
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利用温纳组态电阻率地电法对西拉喀普县Kawunganten区Ujungmanik村的河流海水入侵分布进行了估算。本研究基于地下水地电阻率和电导率数据,估算了西拉喀普县Kawunganten区Ujungmanik村的河流海水入侵分布。地电数据采集在四条线路上进行。它们是文一线、文二线、文三线和文四线。每条线的范围为200米。地电资料处理结果表明,地下岩石结构由砂、粘土、砂壤土和砂质粘土组成。砂层所显示的海水侵入发生在电阻率范围为0.20 ~ 2.79 Ωm的所有轨迹上。地下水样品在15个点进行,电导率值在1363 - 4145µS / cm之间变化,因此可以将其分类为淡水和微咸水,因为采样是在雨季进行的。从这项研究中可以看出,整个乌永格马里克地区在坐标7º38 15.62 ls108°57 20.89 ls7º39 22.86 ls108º56 35.33 lmbt处被海水均匀侵入。
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