塔朗山火山地貌调查与滑坡潜力测绘

Isra Haryati Diva, Usqo Irwanto, K. Nizam, Latifa Annur, Dhanu Sekarjati, B. G. Putra, Yuliana Safitri, Eggy Arya Giovandi, A. Y. Nofrizal, M. Hanif, Akina Abe
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引用次数: 4

摘要

调查地貌学,是应用地貌学的一个分支。本文对塔朗山地貌景观特征进行了调查,并对滑坡危险性进行了制图。在本研究中采用了一些方法,首先进行了野外观测和采样,对地貌特征进行了研究。其次,利用地理信息系统将物理场数据与空间数据相结合,采用日本MAFF的方法进行滑坡灾害制图。研究结果发现了一些火山形态、火山锥、上斜坡、中斜坡、下斜坡、下斜坡和火山平原。对滑坡灾害,凡涉及到地貌特征研究的观测和采样来源。研究发现,滑坡危险性分为4个区,(I)区土地稳定,低危险性大9 ha, (II)区土地足够稳定,中等危险性大12.295 ha, (III)区土地不太稳定,高危险性大1.118 ha, (IV)区土地不稳定,最高危险性大0.1 ha。它的地貌特征、地貌特征和土地利用特征对滑坡危险性有很大的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Investigation Volcanic Land Form and Mapping Landslide Potential at Mount Talang
The survey geomorphology, it is the one apart of applied geomorphology. In case has done investigation character of geomorphological landscape of Mount Talang and mapping of landslide hazard potential. In this research has used some method, the first field observation and sampling for geomorphology character study were conducted. Second the mapping landslide hazard used method the MAFF Japan where integrating physical field data and spatial data using geographic information system. The results of this study where found some volcanic morphology, volcanic cones, upper slopes, middle slope, lower slopes, foot slope, and volcanic plain. The landslide hazard, where involving sources of observation and sampling for the study of geomorphological characters. From the research has found the landslide hazard in four zone, zone (I) land stable and low hazard potential large 9 ha, zone (II) land enough stable and middle hazard potential large 12.295 ha, zone (III) land less stable and high hazard potential large 1.118 ha, and Zone (IV) land unstable and highest hazard potential 0.1 ha. The typical of geomorphology, morphometry, and land use it has really influence to landslide potential to landslide hazard.
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