Skripsi
IDENTIFIKASI ZONA AKUIFER AIR TANAH MENGGUNAKAN METODE TAHANAN JENIS KONFIGURASI WENNER-SCHLUMBERGER (STUDI KASUS DESA GALUK, KECAMATAN KEDUNGTUBAN KABUPATEN BLORA, JAWA TENGAH)
Research has been carried out to identify groundwater aquifer zones using the Wenner-Schlumberger type of resistance method in Galuk village, Kedungtuban district, Blora district, Central Java. The purpose of this study is to identify the depth and type of groundwater aquifer zones. The data processing stage in this study used AGGISAdmin and Res2dinv software. From the results of the study, it was identified that in the research area the groundwater aquifer zone on track 1 was in the blue gradation image of resistivity 0.869 - 1.75 m with a depth of about 19.2 m - 41.9 m at the 28th electrode below the surface with a thickness of about 19.2 m - 41.9 m. aquifer ± 22.7 meters which identified the presence of sand. The type of aquifer in this path is assumed to be a free aquifer. On track 2 the groundwater aquifer zone is thought to be in the blue gradation image of the resistivity 1.12 – 1.90 m with a depth of about 27 m – 41.9 m at the 32nd electrode distance below the surface with an aquifer thickness of ± 14.9 meters. sand is suspected. The type of aquifer in this trajectory is assumed to be a confined aquifer. Groundwater aquifers on paths 1 and 2 are located at a depth of 20 meters, presumably sand is dominant. Meanwhile, at a depth of 19.5 meters, it is suspected that clay and silt are dominant which can store water but cannot pass (flow) water (aqueous). Keywords: Geoelectrical Method of Specific Resistance, Wenner-Schlumberger Configuration, Aquifers, Groundwater
Inventory Code | Barcode | Call Number | Location | Status |
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2107003847 | T58060 | T580602021 | Central Library (Referens) | Available but not for loan - Not for Loan |
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