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Deny Juanda P.
Kelompok Keahlian Geologi Terapan, Institut Teknologi Bandung
Aerospace Engineering Astronomy Automotive Engineering Biochemistry, Genetics & Molecular Biology Chemical Engineering, Chemistry & Bioengineering Chemistry Civil Engineering, Building, Construction & Architecture Computer Science & IT Control & Systems Engineering Decision Sciences, Operations Research & Management Earth & Planetary Sciences Electrical & Electronics Engineering Energy Engineering Immunology & microbiology Industrial & Manufacturing Engineering Library & Information Science Materials Science & Nanotechnology Mechanical Engineering Neuroscience Physics

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ANALISIS HIDROKIMIA UNTUK INTERPRETASI SISTEM HIDROGEOLOGI DAERAH KARS Taat Setiawan; Deny Juanda P.; Budi Brahmantyo; D. Erwin Irawan
Widyariset Vol 13, No 3 (2010): Widyariset
Publisher : Pusbindiklat - LIPI

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (4901.296 KB) | DOI: 10.14203/widyariset.13.3.2010.1-8

Abstract

Cijulang and its surrounding area represent as karst morphology with the cavity network development as the result of groundwater dissolution process. The research of karst hydrogeology in Cijulang area was conducted by using hydrochemical analysis and compiled with the field hydrogeological observation data to identify the hydrogeological system. Based on hydrochemical analysis data as degree of acidity (pH), partial pressure of CO2 (Pco2), and saturation index of calcite (SIkalsit) that compiled with hydrogeological characteristics shown the change of groundwater flow mechanism on the spanning of certainly elevation. Diffusion flow mechanism happened at theelevation of 110–65 masl (transition zone-1) and then changed into conduit flow mechanism at the elevation of 65–35 masl (transition zone -2) and at the elevation of 35–20 masl (zone of continuous water circulation).
ANALISIS HIDROKIMIA UNTUK INTERPRETASI SISTEM HIDROGEOLOGI DAERAH KARS Taat Setiawan; Deny Juanda P.; Budi Brahmantyo; D. Erwin Irawan
Widyariset Vol 13, No 3 (2010): Widyariset
Publisher : Pusbindiklat - LIPI

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.14203/widyariset.13.3.2010.1-8

Abstract

Cijulang and its surrounding area represent as karst morphology with the cavity network development as the result of groundwater dissolution process. The research of karst hydrogeology in Cijulang area was conducted by using hydrochemical analysis and compiled with the field hydrogeological observation data to identify the hydrogeological system. Based on hydrochemical analysis data as degree of acidity (pH), partial pressure of CO2 (Pco2), and saturation index of calcite (SIkalsit) that compiled with hydrogeological characteristics shown the change of groundwater flow mechanism on the spanning of certainly elevation. Diffusion flow mechanism happened at theelevation of 110–65 masl (transition zone-1) and then changed into conduit flow mechanism at the elevation of 65–35 masl (transition zone -2) and at the elevation of 35–20 masl (zone of continuous water circulation).
Co-Authors Budi Brahmantyo D. Erwin Irawan Taat Setiawan