Pendugaan Potensi Volume Akuifer Menggunakan Metode Geolistrik di Pulau Gili Ketapang, Probolinggo, Jawa Timur

Geoelectric measurement using Schlumberger configuration was carried out in Gili Ketapang Island, a small island with a population density of 12,356 people/km2. The measurement conducted at 8 locations using a vertical electrical sounding (VES) method. The result of geoelectric data processing shows...

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Main Authors: Dino Gunawan Pryambodo, Joko Prihantono
Format: Article
Language:English
Published: Center for Nuclear Minerals Technology 2019-05-01
Series:Eksplorium: Buletin Pusat Pengembangan Bahan Galian Nuklir
Subjects:
Online Access:http://jurnal.batan.go.id/index.php/eksplorium/article/view/5415
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spelling doaj-6ab638f283d34f9e97027eef913925c72020-12-16T07:50:13ZengCenter for Nuclear Minerals TechnologyEksplorium: Buletin Pusat Pengembangan Bahan Galian Nuklir0854-14182503-426X2019-05-014015362http://dx.doi.org/10.17146/eksplorium.2019.40.1.5415Pendugaan Potensi Volume Akuifer Menggunakan Metode Geolistrik di Pulau Gili Ketapang, Probolinggo, Jawa TimurDino Gunawan Pryambodo0Joko Prihantono1Pusat Penelitian dan Pengembangan Sumber Daya Laut dan Pesisir, KKPPusat Penelitian dan Pengembangan Sumber Daya Laut dan Pesisir, KKPGeoelectric measurement using Schlumberger configuration was carried out in Gili Ketapang Island, a small island with a population density of 12,356 people/km2. The measurement conducted at 8 locations using a vertical electrical sounding (VES) method. The result of geoelectric data processing shows aquifer resistivity value ranging from 2.71–206 Ωm at the sandy limestone lithology. The largest aquifer volume potency based on the 2D groundwater aquifer model is in the K-03 and K-17 location. The 3D groundwater aquifer model shows that the aquifer volume is 27,689,400 m3 or about 27.689.400.000 liters. The groundwater inside the aquifer will last within 68 years in a condition where there is no population increase. Besides, the groundwater also lasts even there is no water addition inside the aquifer, by natural or artificial.http://jurnal.batan.go.id/index.php/eksplorium/article/view/5415geoelectricvolumeaquiferschlumberger
collection DOAJ
language English
format Article
sources DOAJ
author Dino Gunawan Pryambodo
Joko Prihantono
spellingShingle Dino Gunawan Pryambodo
Joko Prihantono
Pendugaan Potensi Volume Akuifer Menggunakan Metode Geolistrik di Pulau Gili Ketapang, Probolinggo, Jawa Timur
Eksplorium: Buletin Pusat Pengembangan Bahan Galian Nuklir
geoelectric
volume
aquifer
schlumberger
author_facet Dino Gunawan Pryambodo
Joko Prihantono
author_sort Dino Gunawan Pryambodo
title Pendugaan Potensi Volume Akuifer Menggunakan Metode Geolistrik di Pulau Gili Ketapang, Probolinggo, Jawa Timur
title_short Pendugaan Potensi Volume Akuifer Menggunakan Metode Geolistrik di Pulau Gili Ketapang, Probolinggo, Jawa Timur
title_full Pendugaan Potensi Volume Akuifer Menggunakan Metode Geolistrik di Pulau Gili Ketapang, Probolinggo, Jawa Timur
title_fullStr Pendugaan Potensi Volume Akuifer Menggunakan Metode Geolistrik di Pulau Gili Ketapang, Probolinggo, Jawa Timur
title_full_unstemmed Pendugaan Potensi Volume Akuifer Menggunakan Metode Geolistrik di Pulau Gili Ketapang, Probolinggo, Jawa Timur
title_sort pendugaan potensi volume akuifer menggunakan metode geolistrik di pulau gili ketapang, probolinggo, jawa timur
publisher Center for Nuclear Minerals Technology
series Eksplorium: Buletin Pusat Pengembangan Bahan Galian Nuklir
issn 0854-1418
2503-426X
publishDate 2019-05-01
description Geoelectric measurement using Schlumberger configuration was carried out in Gili Ketapang Island, a small island with a population density of 12,356 people/km2. The measurement conducted at 8 locations using a vertical electrical sounding (VES) method. The result of geoelectric data processing shows aquifer resistivity value ranging from 2.71–206 Ωm at the sandy limestone lithology. The largest aquifer volume potency based on the 2D groundwater aquifer model is in the K-03 and K-17 location. The 3D groundwater aquifer model shows that the aquifer volume is 27,689,400 m3 or about 27.689.400.000 liters. The groundwater inside the aquifer will last within 68 years in a condition where there is no population increase. Besides, the groundwater also lasts even there is no water addition inside the aquifer, by natural or artificial.
topic geoelectric
volume
aquifer
schlumberger
url http://jurnal.batan.go.id/index.php/eksplorium/article/view/5415
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AT jokoprihantono pendugaanpotensivolumeakuifermenggunakanmetodegeolistrikdipulaugiliketapangprobolinggojawatimur
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