Risiko Kestabilan Lereng Akibat Gempabumi (Studi Area di Kecamatan Patuk, Kabupaten Gunungkidul)

The research about risk of slope stability as an effort to mitigate landslide slopes due to the earthquake, based on the earthquake of Jogja 2006 along the Opak River fault. The methods used in this study refers to the PERKA BNPB number 2 of 2012, which conducts a qualitative assessment of the lands...

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Main Authors: Eka Priangga Hari Suryana, Subagyo Pramumidjojo, Iman Satryarno
Format: Article
Language:English
Published: Universitas Muhammadiyah Yogyakarta 2018-05-01
Series:Semesta Teknika
Subjects:
Online Access:https://journal.umy.ac.id/index.php/st/article/view/4138
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author Eka Priangga Hari Suryana
Subagyo Pramumidjojo
Iman Satryarno
author_facet Eka Priangga Hari Suryana
Subagyo Pramumidjojo
Iman Satryarno
author_sort Eka Priangga Hari Suryana
collection DOAJ
description The research about risk of slope stability as an effort to mitigate landslide slopes due to the earthquake, based on the earthquake of Jogja 2006 along the Opak River fault. The methods used in this study refers to the PERKA BNPB number 2 of 2012, which conducts a qualitative assessment of the landslide control parameters. Slope stability test is done as an effort to see the effect from earthquake to slope using SLOPE / W software. Test results at 3 locations, each slope in a stable state under normal conditions without earthquake. The first slope (1) in Patuk village has a value ofsafety factor is 2.45, while in earthquake condition has safety factor number is 1.27. The value of the safety factor on the second slope (2) in Ngoro-oro village under normal condition safety factor is 2.22 and the earthquake condition has value safety factor is 0.74. The third slope (3) in Ngoro-oro village has a safety factor number is 3.62 while in earthquake condition has value 1.95. The result of landslide risk calculation use first (1) scenario in Patuk sub-district generally has medium class, with yellow color in landslide risk map. Patuk villages has high class level for landslide risk map, meanwhile Terbah and Semoyo villages have low level class for landslide risk map. The slope in Patuk sub-district has stable conditions againts earthquake, but the change from slope material caused by weathering can made trigger landslide in future.
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spelling doaj.art-e8a766ad4b904e98b2ba8717d1aa1e182022-12-21T23:31:45ZengUniversitas Muhammadiyah YogyakartaSemesta Teknika1411-061X2502-54812018-05-012119310510.18196/st.2112152896Risiko Kestabilan Lereng Akibat Gempabumi (Studi Area di Kecamatan Patuk, Kabupaten Gunungkidul)Eka Priangga Hari Suryana0Subagyo Pramumidjojo1Iman Satryarno2Universitas Gadjah Mada YogykartaUniversitas Gadjah MadaUniversitas Gadjah MadaThe research about risk of slope stability as an effort to mitigate landslide slopes due to the earthquake, based on the earthquake of Jogja 2006 along the Opak River fault. The methods used in this study refers to the PERKA BNPB number 2 of 2012, which conducts a qualitative assessment of the landslide control parameters. Slope stability test is done as an effort to see the effect from earthquake to slope using SLOPE / W software. Test results at 3 locations, each slope in a stable state under normal conditions without earthquake. The first slope (1) in Patuk village has a value ofsafety factor is 2.45, while in earthquake condition has safety factor number is 1.27. The value of the safety factor on the second slope (2) in Ngoro-oro village under normal condition safety factor is 2.22 and the earthquake condition has value safety factor is 0.74. The third slope (3) in Ngoro-oro village has a safety factor number is 3.62 while in earthquake condition has value 1.95. The result of landslide risk calculation use first (1) scenario in Patuk sub-district generally has medium class, with yellow color in landslide risk map. Patuk villages has high class level for landslide risk map, meanwhile Terbah and Semoyo villages have low level class for landslide risk map. The slope in Patuk sub-district has stable conditions againts earthquake, but the change from slope material caused by weathering can made trigger landslide in future.https://journal.umy.ac.id/index.php/st/article/view/4138landslide risk map, ahp, slope/w
spellingShingle Eka Priangga Hari Suryana
Subagyo Pramumidjojo
Iman Satryarno
Risiko Kestabilan Lereng Akibat Gempabumi (Studi Area di Kecamatan Patuk, Kabupaten Gunungkidul)
Semesta Teknika
landslide risk map, ahp, slope/w
title Risiko Kestabilan Lereng Akibat Gempabumi (Studi Area di Kecamatan Patuk, Kabupaten Gunungkidul)
title_full Risiko Kestabilan Lereng Akibat Gempabumi (Studi Area di Kecamatan Patuk, Kabupaten Gunungkidul)
title_fullStr Risiko Kestabilan Lereng Akibat Gempabumi (Studi Area di Kecamatan Patuk, Kabupaten Gunungkidul)
title_full_unstemmed Risiko Kestabilan Lereng Akibat Gempabumi (Studi Area di Kecamatan Patuk, Kabupaten Gunungkidul)
title_short Risiko Kestabilan Lereng Akibat Gempabumi (Studi Area di Kecamatan Patuk, Kabupaten Gunungkidul)
title_sort risiko kestabilan lereng akibat gempabumi studi area di kecamatan patuk kabupaten gunungkidul
topic landslide risk map, ahp, slope/w
url https://journal.umy.ac.id/index.php/st/article/view/4138
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AT subagyopramumidjojo risikokestabilanlerengakibatgempabumistudiareadikecamatanpatukkabupatengunungkidul
AT imansatryarno risikokestabilanlerengakibatgempabumistudiareadikecamatanpatukkabupatengunungkidul