Dian Chandrasasi, Runi Asmaranto, Ni Made Candra Partarini
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摘要

有近百年历史的格林能大坝,从大坝下游的滑坡中可以看到主坝的渗水情况。本研究旨在通过温纳-斯伦贝谢电气地质配置,确定格林能坝主坝的可见渗流,并找出渗流模式在格林能坝体坡和坝基上的位置。视觉上有6(6)个渗漏点,其中一个渗漏点被怀疑是地下水流动的结果。渗漏位置的指示全部位于主坝下游。温纳-斯伦贝谢电性地质组态测量结果经RES2DINV应用程序处理,得到了以最低电阻率值为代表的渗流位置的蓝色渐变结果。从四条工作线的结果可以看出,每条工作线表示不同的渗流势,但可以看出,主坝格林能坝各区域均存在渗流势,其特征为低电阻率,以蓝色标记。
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PENERAPAN METODE GEOLISTRIK KONFIGURASI WENNER – SCHLUMBERGER UNTUK ANALISIS REMBESAN PADA MAINDAM WADUK GRENENG, KABUPATEN BLORA
The nearly 100-year-old Greneng dam is indicated by seepage in the main dam visible from landslides on the downstream of the dam wall. This study aims to determine visible seepage in the main dam of Greneng Dam and to find out the position of seepage pattern on the body slope and foundation of Greneng Dam by Electrical Geology configuration of Wenner-Schlumberger. Visually there are 6 (six) spot seepage where, one spot of seepage is suspected as a result of groundwater flow. The indication of the seepage position is entirely located on the downstream of the main dam. The measurement result by Electrical Geology configuration of Wenner-Schlumberger with the processing of RES2DINV application obtained the result of seepage position which is represented by the lowest resistivity value with blue gradation. The results of the four work lines can be observed that each line shows the potential for different seepage, however, it can be seen that there is a potential flow of seepage in each area of Main Dam Greneng Dam which is characterized by low resistivity marked with blue color.
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