印尼Kulonprogo县Samigaluh区Gerbosari村风化层厚度和坡度对潜在滑坡区域的影响

Novia Nurul Khayati, Sudarmaji, E. Hartantyo
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引用次数: 0

摘要

Gerbosari村有山体滑坡的历史,其强度和风险在5年内发生了56次。Gerbosari Village, Samigaluh District, Kulonprogo Regency位于地理坐标7◦38 '45.33 "- 7◦41' 35.24" LS和100◦9 '20.80 "- 110◦11' 16.52" BT,地形条件在海拔500 - 1000 mdpl左右。本研究旨在以风化层厚度的形式确定滑坡易发区的地下结构以及滑坡易发区坡度的影响,为滑坡易发区微分区图的制作提供依据。本研究使用43个点间距为650 m的微震数据。采用水平与垂直频谱比(HVSR)方法对微震信号进行了分析。测量结果表明,主频率范围为1 ~ 22 Hz,放大系数范围为1 ~ 10.5,峰值地加速度范围为60 ~ 300 cm/s2,风化层厚度范围为12 ~ 22 m。根据坡度分析结果,研究区处于略陡-极陡的坡度上。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Effect of Weathered Layer Thickness and Slope on Potential Areas of Landslides in Gerbosari Village, Samigaluh District, Kulonprogo Regency, Indonesia
Gerbosari Village has a history of landslides with intensity and risk of 56 occurrences over 5 years. Gerbosari Village, Samigaluh District, Kulonprogo Regency is located at geographic coordinates 7◦ 38 '45.33 "- 7◦ 41' 35.24" LS and 100◦ 9 '20.80 "- 110◦ 11' 16.52" BT with topographic conditions at an altitude around 500 - 1000 mdpl. This study aims to determine the subsurface structure of landslide-prone areas in the form of weathered layer thickness and the effect of slope in landslide-prone areas so that it can be used in making micro zonation maps of landslide-prone areas. This study uses 43 microtremor data with a distance between points of 650 m. The microtremor signal was analysed using the horizontal to vertical spectrum ratio ( HVSR) method. From the measurement results, it is obtained that the value of the dominant frequency ranges from 1 - 22 Hz, the value of the amplification factor is obtained in the range of 1 - 10.5, the value of the peak ground acceleration ranges from 60 - 300 cm/s2, the thickness of the weathered layer is obtained in the range of 12 - 22 meters. Based on the results of the slope analysis, the study area is on a slope classified as a bit steep - very steep.
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