Aquifer system and groundwater potency in coastal area of Kretek, Bantul Regency, Indonesia

The existence of groundwater in coastal areas really needs attention because of its vulnerability to sea water intrusion. Utilization and good management are needed to maintain its sustainability. The purpose of this research is to determine the aquifer system in the study area and to calculate the...

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Autores principales: Saleh Isa La Ode, Setyawan Purnama Ignasius Loyola
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Publicado: EDP Sciences 2021
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spelling oai:doaj.org-article:c1c2f27a150c4e0985c9586f170219622021-12-02T17:11:57ZAquifer system and groundwater potency in coastal area of Kretek, Bantul Regency, Indonesia2267-124210.1051/e3sconf/202132508001https://doaj.org/article/c1c2f27a150c4e0985c9586f170219622021-01-01T00:00:00Zhttps://www.e3s-conferences.org/articles/e3sconf/pdf/2021/101/e3sconf_icst2021_08001.pdfhttps://doaj.org/toc/2267-1242The existence of groundwater in coastal areas really needs attention because of its vulnerability to sea water intrusion. Utilization and good management are needed to maintain its sustainability. The purpose of this research is to determine the aquifer system in the study area and to calculate the groundwater potency. The aquifer system is determined by processing geoelectric sounding data using Rockworks 16 software. Groundwater potency is calculated using a static approach. The safe yield of groundwater is calculated by multiplying of groundwater fluctuation, village area and the specific yield. Water requirement is calculated base on domestic, livestock and tourism water requirement. The results showed that the Kretek District had two aquifer units, namely the fluvio marin plains and sand dunes. In the fluvio marin plains, most of the constituent material is sand with clay as inserts, while in the aquifer unit the sand dune has constituent material in the form of unconsolidated sand originating from the Merapi Volcano. The groundwater potency of the study area is 234,448,0000 m3/year and the safe yield is 11,772,400 m3/year. With the water requirement for domestic, livestock and tourism are 555,044 m3/year, the groundwater potency in the study area is still sufficient. However, it is recommended that the well drilling does not exceed a depth of 40 meters, because at several locations there has been detected an interface. In addition, in several locations there were also detected connate water originating from ancient marines during the deposition process of the fluvio marin plains in the past.Saleh Isa La OdeSetyawan Purnama Ignasius LoyolaEDP Sciencesarticleaquifergroundwatercoastal areakretek districtbantul regencyEnvironmental sciencesGE1-350ENFRE3S Web of Conferences, Vol 325, p 08001 (2021)
institution DOAJ
collection DOAJ
language EN
FR
topic aquifer
groundwater
coastal area
kretek district
bantul regency
Environmental sciences
GE1-350
spellingShingle aquifer
groundwater
coastal area
kretek district
bantul regency
Environmental sciences
GE1-350
Saleh Isa La Ode
Setyawan Purnama Ignasius Loyola
Aquifer system and groundwater potency in coastal area of Kretek, Bantul Regency, Indonesia
description The existence of groundwater in coastal areas really needs attention because of its vulnerability to sea water intrusion. Utilization and good management are needed to maintain its sustainability. The purpose of this research is to determine the aquifer system in the study area and to calculate the groundwater potency. The aquifer system is determined by processing geoelectric sounding data using Rockworks 16 software. Groundwater potency is calculated using a static approach. The safe yield of groundwater is calculated by multiplying of groundwater fluctuation, village area and the specific yield. Water requirement is calculated base on domestic, livestock and tourism water requirement. The results showed that the Kretek District had two aquifer units, namely the fluvio marin plains and sand dunes. In the fluvio marin plains, most of the constituent material is sand with clay as inserts, while in the aquifer unit the sand dune has constituent material in the form of unconsolidated sand originating from the Merapi Volcano. The groundwater potency of the study area is 234,448,0000 m3/year and the safe yield is 11,772,400 m3/year. With the water requirement for domestic, livestock and tourism are 555,044 m3/year, the groundwater potency in the study area is still sufficient. However, it is recommended that the well drilling does not exceed a depth of 40 meters, because at several locations there has been detected an interface. In addition, in several locations there were also detected connate water originating from ancient marines during the deposition process of the fluvio marin plains in the past.
format article
author Saleh Isa La Ode
Setyawan Purnama Ignasius Loyola
author_facet Saleh Isa La Ode
Setyawan Purnama Ignasius Loyola
author_sort Saleh Isa La Ode
title Aquifer system and groundwater potency in coastal area of Kretek, Bantul Regency, Indonesia
title_short Aquifer system and groundwater potency in coastal area of Kretek, Bantul Regency, Indonesia
title_full Aquifer system and groundwater potency in coastal area of Kretek, Bantul Regency, Indonesia
title_fullStr Aquifer system and groundwater potency in coastal area of Kretek, Bantul Regency, Indonesia
title_full_unstemmed Aquifer system and groundwater potency in coastal area of Kretek, Bantul Regency, Indonesia
title_sort aquifer system and groundwater potency in coastal area of kretek, bantul regency, indonesia
publisher EDP Sciences
publishDate 2021
url https://doaj.org/article/c1c2f27a150c4e0985c9586f17021962
work_keys_str_mv AT salehisalaode aquifersystemandgroundwaterpotencyincoastalareaofkretekbantulregencyindonesia
AT setyawanpurnamaignasiusloyola aquifersystemandgroundwaterpotencyincoastalareaofkretekbantulregencyindonesia
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