Designing Aquifer Model for the Banks of the Serayu River, Sokawera, Somagede, Banyumas, Indonesia by Means of 1D-Electrical Resistivity Data

A geoelectric survey using the 1D-electrical resistivity method was applied to design a groundwater aquifer model for the banks of the Serayu River in Sokawera Village, Somagede District, Banyumas Regency, Indonesia. The aim of this research was to identify the characteristics of aquifers in the re...

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Autores principales:	Sehah Sehah, Hartono, Zaroh Irayani, Urip Nurwijayanto Prabowo
Formato:	article
Lenguaje:	EN
Publicado:	ITB Journal Publisher 2021
Materias:	1D-Electrical Resistivity aquifer hydrostratigraphic model Serayu riverbanks Sokawera Science Q Science (General) Q1-390
Acceso en línea:	https://doaj.org/article/1ebca258a6d64ec194c9315c7cdf7716
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spelling	oai:doaj.org-article:1ebca258a6d64ec194c9315c7cdf77162021-12-03T07:44:08ZDesigning Aquifer Model for the Banks of the Serayu River, Sokawera, Somagede, Banyumas, Indonesia by Means of 1D-Electrical Resistivity Data10.5614/j.math.fund.sci.2021.53.3.12337-57602338-5510https://doaj.org/article/1ebca258a6d64ec194c9315c7cdf77162021-12-01T00:00:00Zhttps://journals.itb.ac.id/index.php/jmfs/article/view/15192https://doaj.org/toc/2337-5760https://doaj.org/toc/2338-5510 A geoelectric survey using the 1D-electrical resistivity method was applied to design a groundwater aquifer model for the banks of the Serayu River in Sokawera Village, Somagede District, Banyumas Regency, Indonesia. The aim of this research was to identify the characteristics of aquifers in the research area based on resistivity log data. Acquisition, modeling, and interpretation of resistivity data were carried out and the results were lithological logs at seven sounding points. Correlation between the lithological logs resulted in a hydrostratigraphic model. This model is composed of several hydrological units, i.e. shallow aquifer, aquitard, and deep aquifer. The shallow aquifers are composed of sandy clay (10.81-18.21 Wm) and clayey sand (3.04-7.43 Wm) with a depth of groundwater from the water table to 27.51 m. The deep aquifers are composed of sandstone with variation of porosity (2.24-12.04 Wm) at a depth of more than 54.98 m. Based on this model, potential shallow aquifers were estimated to be at sounding points Sch-5, Sch-6, and Sch-7. This hydrostratigraphic model shows that the two types of aquifers are separated by an aquitard layer, allowing groundwater infiltration from the shallow aquifer to the deep aquifer and vice versa. Moreover, the Serayu riverbanks in this research area are estimated to be a groundwater discharge area. Sehah SehahHartonoZaroh IrayaniUrip Nurwijayanto PrabowoITB Journal Publisherarticle1D-Electrical Resistivityaquiferhydrostratigraphic modelSerayu riverbanksSokaweraScienceQScience (General)Q1-390ENJournal of Mathematical and Fundamental Sciences, Vol 53, Iss 3 (2021)
institution	DOAJ
collection	DOAJ
language	EN
topic	1D-Electrical Resistivity aquifer hydrostratigraphic model Serayu riverbanks Sokawera Science Q Science (General) Q1-390
spellingShingle	1D-Electrical Resistivity aquifer hydrostratigraphic model Serayu riverbanks Sokawera Science Q Science (General) Q1-390 Sehah Sehah Hartono Zaroh Irayani Urip Nurwijayanto Prabowo Designing Aquifer Model for the Banks of the Serayu River, Sokawera, Somagede, Banyumas, Indonesia by Means of 1D-Electrical Resistivity Data
description	A geoelectric survey using the 1D-electrical resistivity method was applied to design a groundwater aquifer model for the banks of the Serayu River in Sokawera Village, Somagede District, Banyumas Regency, Indonesia. The aim of this research was to identify the characteristics of aquifers in the research area based on resistivity log data. Acquisition, modeling, and interpretation of resistivity data were carried out and the results were lithological logs at seven sounding points. Correlation between the lithological logs resulted in a hydrostratigraphic model. This model is composed of several hydrological units, i.e. shallow aquifer, aquitard, and deep aquifer. The shallow aquifers are composed of sandy clay (10.81-18.21 Wm) and clayey sand (3.04-7.43 Wm) with a depth of groundwater from the water table to 27.51 m. The deep aquifers are composed of sandstone with variation of porosity (2.24-12.04 Wm) at a depth of more than 54.98 m. Based on this model, potential shallow aquifers were estimated to be at sounding points Sch-5, Sch-6, and Sch-7. This hydrostratigraphic model shows that the two types of aquifers are separated by an aquitard layer, allowing groundwater infiltration from the shallow aquifer to the deep aquifer and vice versa. Moreover, the Serayu riverbanks in this research area are estimated to be a groundwater discharge area.
format	article
author	Sehah Sehah Hartono Zaroh Irayani Urip Nurwijayanto Prabowo
author_facet	Sehah Sehah Hartono Zaroh Irayani Urip Nurwijayanto Prabowo
author_sort	Sehah Sehah
title	Designing Aquifer Model for the Banks of the Serayu River, Sokawera, Somagede, Banyumas, Indonesia by Means of 1D-Electrical Resistivity Data
title_short	Designing Aquifer Model for the Banks of the Serayu River, Sokawera, Somagede, Banyumas, Indonesia by Means of 1D-Electrical Resistivity Data
title_full	Designing Aquifer Model for the Banks of the Serayu River, Sokawera, Somagede, Banyumas, Indonesia by Means of 1D-Electrical Resistivity Data
title_fullStr	Designing Aquifer Model for the Banks of the Serayu River, Sokawera, Somagede, Banyumas, Indonesia by Means of 1D-Electrical Resistivity Data
title_full_unstemmed	Designing Aquifer Model for the Banks of the Serayu River, Sokawera, Somagede, Banyumas, Indonesia by Means of 1D-Electrical Resistivity Data
title_sort	designing aquifer model for the banks of the serayu river, sokawera, somagede, banyumas, indonesia by means of 1d-electrical resistivity data
publisher	ITB Journal Publisher
publishDate	2021
url	https://doaj.org/article/1ebca258a6d64ec194c9315c7cdf7716
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Designing Aquifer Model for the Banks of the Serayu River, Sokawera, Somagede, Banyumas, Indonesia by Means of 1D-Electrical Resistivity Data

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