Identifikasi keberadaan cekungan air tanah ciomas Bogor, berdasarkan hasil pendugaan geolistrik  

Oleh:

Padmawidjaja, Tatang

Jenis: Article from Journal - ilmiah nasional - tidak terakreditasi DIKTI
Dalam koleksi: Jurnal Sumber Daya Air vol. 6 no. 02 (Nov. 2010), page 161.
Topik: Geo-electric; Ground Water Basin; Clay Sedimentary; Aquifer

Ketersediaan

Perpustakaan PKPM Nomor Panggil: J128 Non-tandon: 1 (dapat dipinjam: 0) Tandon: tidak ada

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Isi artikel

Geo-electric research to estimate ground water basins and aquifer was conducted in kecamatan Ciomas, kabupaten Bogor. The geological conditions in this location include the Bogor Basin and Bogor linement, with rocks of the Quaternary Volcanic and the Bojongmanik formation which mainly consist of coarse sand to fine clay and calcareous rocks. Resistivity shows the boundary curves at depths greater than 200 meters which indicate the boundary between conductive and resistive areas. Resistivity has a value smaller than 10 ohm m of sandy clay material as groundwater mineral deposit. Based on the resistivity data, Ciomas area can be considered as a rare soil water aquifer trapped in impermeable clay layers

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