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Landslide Susceptibility Mapping and Their Rainfall Thresholds Model in Tinalah Watershed, Kulon Progo District, Yogyakarta Special Region, Indonesia Thema Arrisaldi; Wahyu Wilopo; Teuku Faisal Fathani
Journal of Applied Geology Vol 6, No 2 (2021)
Publisher : Geological Engineering Department Universitas Gadjah Mada

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1320.544 KB) | DOI: 10.22146/jag.59185

Abstract

Landslide often occurred in Tinalah watershed, Kulon Progo District, every year. The frequency of landslide events is increasing after high rainfall intensity. Some factors control landslides such as slope gradient, land use, geological structure, slope hydrology, and geological condition. This research has an objective to develop the susceptibility map of Tinalah watershed and to identify the rainfall threshold to trigger a landslide. The development of the susceptibility map using frequency ratio method with four parameters including slope, type of rock, land use, and lineament density. The landslide data were collected during the field survey and from regional disaster management authority (BPBD) Kulon Progo. Rainfall data were collected from BMKG and GSMap. Soil analysis also was conducted to develop a numerical model to verify the rainfall threshold value. The result shows a high susceptibility of the landslide area is dominated in Tinalah watershed. The rainfall threshold for the low susceptibility of the landslide zone is I=490.14 D-1.404with 5-7 days antecedent rain. The rainfall threshold for medium susceptibility map is I=164.32D-0,689 3-7 days antecedent rain. Moreover, the rainfall threshold for the high susceptibility of the landslide zone is 111.62 D-0.779, with 2-7 days antecedent rain.
ANALISIS PERHITUNGAN WAKTU RUNTUH DAN DIMENSI KERUNTUHAN TEROWONGAN BAWAH TANAH BERDASARKAN PERHITUNGAN RMR DI LOKASI CIBITUNG, KABUPATEN PANDEGLANG, PROVINSI BANTEN Daniel Radityo, S.T., M.T.; Thema Arrisaldi; Hasan Tri Atmojo; Adam Raka Ekasara; Lilik Eko Saputro
Jurnal Ilmiah MTG Vol 13, No 2 (2022): Jurnal Ilmiah MTG Volume 13 No. 2, Desember 2022
Publisher : Jurusan Teknik Geologi Fakultas Teknologi Mineral UPN "Veteran" Yogyakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31315/jmtg.v13i3.9393

Abstract

ABSTRAK - Pengamanan kegiatan penambangan bawah tanah dilakukan bertujuan untuk menjaga stabilitas dan keamanan lubang bukaan terowongan dari reruntuhan batuan. Pengamanan kegiatan penambangan bawah tanah diperlukan kajian rekayasa geologi teknik seperti pemetaan lapangan, perhitungan Rock Mass Rating (RMR), tinggi bukaan terowongan bawah tanah, waktu runtuh (stand-up time), serta dimensi keruntuhan (beban runtuh, tinggi runtuh, dan beban luas atap). Penelitian ini menggunakan data kondisi geologi secara umum, pemetaan lapangan, perhitungan Rock Mass Rating (RMR), waktu runtuh (stand-up time), dimensi keruntuhan (beban runtuh, tinggi runtuh, dan beban luas atap). Kondisi geologi secara umum di daerah produksi CBT_1106_RMU_NTH dan CBT_1106_RMU_STH berupa batuan porfiritik andesit dengan dominan mineral kuarsa, memiliki jenis tekstur kuarsa crusiform, terdapat beberapa kekar menerus dengan panjang 1-3 m yang terisi dengan mineral hard filling lebar 1-5 mm, kekuatan batuan termasuk medium strong, sebagian teralterasi oleh mineral silika. Nilai RMR untuk daerah CBT_1106_RMU_NTH lebih tinggi dibandingkan CBT_1106_RMU_STH karena adanya pengaruh kondisi air tanah dengan tingkat pelapukan yang berbeda. Waktu runtuh daerah CBT_1106_RMU_NTH dapat bertahan lebih lama dibandingkan CBT_1106_RMU_STH karena daerah tersebut lebih stabil. Dimensi keruntuhan CBT_1106_RMU_NTH lebih pendek dan lebih ringan dibandingkan daerah CBT_1106_RMU_STH. Penelitian ini memberikan rekomendasi tinggi bukaan efektif tanpa penguatan.Kata kunci: geologi teknik, RMR, waktu runtuh, tinggi runtuh, beban runtuh. ABSTRACT - Securing underground mining activities is done purposely to maintain the stability and safety of underground mining openings from rock debris. Securing underground mining activities requires geological engineering studies such as field mapping, calculation of Rock Mass Rating (RMR), underground tunnel height, stand-up time, and collapse dimensions (collapse load, collapse height, and roof area load). This study uses data on general geological conditions, field mapping, calculation of Rock Mass Rating (RMR), stand-up time, collapse dimensions (collapse load, collapse height, and roof area load). The general geological conditions in the CBT_1106_RMU_NTH and CBT_1106_RMU_STH production areas are porphyritic andesitic rocks with dominant quartz minerals, have a crusiform quartz texture type, there are several continuous joints with a length of 1-3 m filled with hard filling minerals 1-5 mm wide, rock strength including medium strong, partially altered by silica minerals. The RMR value for the CBT_1106_RMU_NTH area is higher than CBT_1106_RMU_STH due to the influence of groundwater conditions with different levels of weathering. The collapse time for the CBT_1106_RMU_NTH area can last longer than CBT_1106_RMU_STH because this area is more stable. The CBT_1106_RMU_NTH collapse dimension is shorter and lighter than the CBT_1106_RMU_STH region. This study provides a high recommendation of effective aperture without reinforcement.Keywords: engineering geology, RMR, stand-up time, collapse height, collapse load
GIS for Landslide Risk Assessment, Study Case Pengasih and Sentolo District, Kulon Progo, Indonesia Thema Arrisaldi; Puji Pratiknyo; Wahyu Wilopo
International Journal of Disaster Management Vol 6, No 1 (2023): April
Publisher : TDMRC, Universitas Syiah Kuala

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.24815/ijdm.v6i1.30595

Abstract

Landslide is a natural phenomenon that often occurs as a disaster in Kulon Progo Region. This research is located in Pengasih and Sentolo District, Kulon Progo. The aim of the study is landslide risk mapping in the research area. The landslide risk map has 3 parameters, such as potential landslide condition, vulnerable situations, and community capacity to cope with the landslide disaster. Potential landslide obtained from Geographic Information System (GIS )overlay analysis using Analytical Hierarchy Process (AHP) consists of 4 sub-parameters: slope gradient (55.49%), geological condition (25.16%), stream density (9.67%), land use (9.67%). The vulnerability was obtained from 3 sub-parameters, such as economic vulnerability (33.33%), infrastructure vulnerability (33.34%), and population density (33.33%). The community capacity in the research area was obtained from The activity of the Region Disaster Management Authority (BPBD) of Kulon Progo to strengthen community awareness to cope with landslide disasters, such as socialization about landslides and simulation during an emergency landslide. The input in overlay analysis used GIS for the parameters are all sub-parameters from each parameter. Landslide risk map obtained from overlay analysis using GIS based on landslide potential map, vulnerability map, and capacity map. The result is that Pengasih and Sentolo Districts have low to moderate landslide risk conditions. Several landslides occur in each landslide risk zone.