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Potensi Air Tanah pasca Gempa Tektonik di Lereng Merapi Daerah Klaten Jawa Tengah

Forum Geografi · Vol. 22 No. 2 (2008) · hlm. 186–198

DOI
10.23917/forgeo.v22i2.4993
ISSN
2460-3945, 0852-0682
Terbit
2008-12-20
Penerbit
Universitas Muhammadiyah Surakarta
Bahasa
eng
Lisensi
creativecommons.org/licenses/by-nc-nd/4.0

Abstrak

The purpose of this research is to analyze the potency of land water in the post tectonic earchquake at Merapi slope in Klaten regency, Central Java. This research applies a survey method. The result of analysis is made based on the trilinier diagram, Stiff pattern, and the quality standard of drinking water. The collected data are in the form of land form, shallow land water data, suppressed land water, and well or spring. The results of the sesearch show that 1) the land form in Klaten is divided into four sets of landform, they are peak and slope of volcano, feet of volcano, fluvial palin under volcano, and a set of structural morphology. 2) The potency of land water can be tested based on the amount of land water and the quality of land water. The amount of land water in Klaten regency 260,502,274 m3/year or 727,618,722 liter/day. The amount of land water above is taken from free land water 73,301,436 m3/year, suppressed land water 34,138,520 m3/year, and land water taken from well or spring 153,062,784 m3/year. The quality of shallow land water in Klaten regency is proper to consume. 3) The distribution of upland water potency happens in the feet volcano land form, the potency of medium land water happens in the superficial of fluvial under volcano land form, and the potency of lowland water happens in the slope volcano land form and in the structural range of hills at Bayat subdistrict, 4) The tectonic earthquake gives serious effect toward morphological changes, land split, land subsident and the potency of land water in the fluvial plain of land form under volcano and structural range of hills in the area of Bayat subdistrict, and 5) In 2008, the needs of drinking water in Klaten regency is predicted around 1,164,000 people x 150 liter/day = 174,600,000 liter/day.

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  • Muhammadiyah University of Surakarta
  • University of Brawijaya
  • Universitas Gadjah Mada
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Rekan penulisOrganisasiArtikel bersama
‪Kuswaji Dwi PriyonoMuhammadiyah University of Surakarta8
Suharjo SuharjoMuhammadiyah University of Surakarta5
Sugiharto Budi SantosoMuhammadiyah University of Surakarta5
Agus Anggoro SigitMuhammadiyah University of Surakarta3
Priyono PriyonoMuhammadiyah University of Surakarta3
Munawar CholilMuhammadiyah University of Surakarta3
Rohman HakimMuhammadiyah University of Surakarta2
Suharto WidjojoAfiliasi tidak diketahui2
Wahyuni Apri AstutiMuhammadiyah University of Surakarta2
Jumadi JumadiMuhammadiyah University of Surakarta1
Riani LaviatiAfiliasi tidak diketahui1
Reshinta PurnaningsihMuhammadiyah University of Surakarta1
Slamet SuryantoMuhammadiyah University of Surakarta1
Yuliarta Rudi PrasetyoMuhammadiyah University of Surakarta1
Arif JauhariAfiliasi tidak diketahui1
Choirul AminMuhammadiyah University of Surakarta1
Susanto SusantoUniversity of Brawijaya1
Umrotun UmrotunAfiliasi tidak diketahui1
Triana Nur HandayaniAfiliasi tidak diketahui1
Satriyo NugrohoAfiliasi tidak diketahui1
P PriyonoMuhammadiyah University of Surakarta1
Muhammad MusiyamMuhammadiyah University of Surakarta1
T TaryonoMuhammadiyah University of Surakarta1
Taryono TaryonoUniversitas Gadjah Mada1
Retno Woro KaeksMuhammadiyah University of Surakarta1
Adi RusmantoAfiliasi tidak diketahui1
Priyono PriyonoMuhammadiyah University of Surakarta1
Dina SafriningsihMuhammadiyah University of Surakarta1
Pujo Nur CahyoMuhammadiyah University of Surakarta1
M MulyonoMuhammadiyah University of Surakarta1
Heru Sri WidodoMuhammadiyah University of Surakarta1
Soenarso SimoenAfiliasi tidak diketahui1
Suyono SuyonoAfiliasi tidak diketahui1
Arif WidodoMuhammadiyah University of Surakarta1

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Sumber metadata: OAI-PMH (metadata jurnal) http://journals.ums.ac.id/index.php/fg/oai, pertama di-harvest 8 Nov 2026, terakhir terlihat 8 Nov 2026.
Metadata asli (oai_dc) 
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	<dc:title xml:lang="en-US">Potensi Air Tanah pasca Gempa Tektonik di Lereng Merapi Daerah Klaten Jawa Tengah</dc:title>
	<dc:creator>Suharjo, S</dc:creator>
	<dc:creator>Anna, Alif Noor</dc:creator>
	<dc:creator>Kaeksi, Retno Woro</dc:creator>
	<dc:creator>Priyana, Yuli</dc:creator>
	<dc:subject xml:lang="en-US"></dc:subject>
	<dc:subject xml:lang="en-US">potency of land water; tectonic earthquake; land form</dc:subject>
	<dc:subject xml:lang="en-US"></dc:subject>
	<dc:description xml:lang="en-US">The purpose of this research is to analyze the potency of land water in the post tectonic earchquake at Merapi slope in Klaten regency, Central Java. This research applies a survey method. The result of analysis is made based on the trilinier diagram, Stiff pattern, and the quality standard of drinking water. The collected data are in the form of land form, shallow land water data, suppressed land water, and well or spring. The results of the sesearch show that 1) the land form in Klaten is divided into four sets of landform, they are peak and slope of volcano, feet of volcano, fluvial palin under volcano, and a set of structural morphology. 2) The potency of land water can be tested based on the amount of land water and the quality of land water. The amount of land water in Klaten regency 260,502,274 m3/year or 727,618,722 liter/day. The amount of land water above is taken from free land water 73,301,436 m3/year, suppressed land water 34,138,520 m3/year, and land water taken from well or spring 153,062,784 m3/year. The quality of shallow land water in Klaten regency is proper to consume. 3) The distribution of upland water potency happens in the feet volcano land form, the potency of medium land water happens in the superficial of fluvial under volcano land form, and the potency of lowland water happens in the slope volcano land form and in the structural range of hills at Bayat subdistrict, 4) The tectonic earthquake gives serious effect toward morphological changes, land split, land subsident and the potency of land water in the fluvial plain of land form under volcano and structural range of hills in the area of Bayat subdistrict, and 5) In 2008, the needs of drinking water in Klaten regency is predicted around 1,164,000 people x 150 liter/day = 174,600,000 liter/day.</dc:description>
	<dc:publisher xml:lang="en-US">Universitas Muhammadiyah Surakarta</dc:publisher>
	<dc:contributor xml:lang="en-US"></dc:contributor>
	<dc:date>2008-12-20</dc:date>
	<dc:type>info:eu-repo/semantics/article</dc:type>
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	<dc:identifier>https://journals.ums.ac.id/index.php/fg/article/view/4993</dc:identifier>
	<dc:identifier>10.23917/forgeo.v22i2.4993</dc:identifier>
	<dc:source xml:lang="en-US">Forum Geografi; Vol 22, No 2 (2008): December 2008; 186-198</dc:source>
	<dc:source>2460-3945</dc:source>
	<dc:source>0852-0682</dc:source>
	<dc:language>eng</dc:language>
	<dc:relation>https://journals.ums.ac.id/index.php/fg/article/view/4993/3317</dc:relation>
	<dc:coverage xml:lang="en-US"></dc:coverage>
	<dc:coverage xml:lang="en-US"></dc:coverage>
	<dc:coverage xml:lang="en-US"></dc:coverage>
	<dc:rights xml:lang="en-US">Copyright (c) 2017 S Suharjo, Alif Noor Anna, Retno Woro Kaeksi, Yuli Priyana</dc:rights>
	<dc:rights xml:lang="en-US">https://creativecommons.org/licenses/by-nc-nd/4.0</dc:rights>
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