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Applying a Method for Assessing Deep-Seated Rapid Landslide Susceptibility in Jember District, East Java Province, Indonesia

机译:在印度尼西亚东爪哇省Jember区采用一种评估深层快速滑坡敏感性的方法

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A deep-seated rapid (catastrophic) landslide is a phenomenon that may cause serious damage due to the large amount of sediment movement, such as the formation of a landslide dam and debris flows. In Japan, a method for estimating deep-seated rapid (catastrophic) landslide susceptibilities for many small catchments (ca. 1 km2) over relatively large areas (ca. hundreds of km2) was proposed in 2008. In the present study, we applied the Japanese method to the northern part of Jember, East Java, Indonesia, where a debris flow disaster occurred due to the collapse of a landslide dam formed by a deep-seated rapid (catastrophic) landslide in 2004. Although there were several limitations related to data availability, we successfully assessed susceptibility to deep-seated rapid landslides.
机译:根深蒂固的快速(灾难性)滑坡是一种现象,由于大量的泥沙运动(例如形成滑坡坝和泥石流),可能导致严重破坏。在日本,2008年提出了一种方法来估算相对较大区域(约数百平方公里)中许多小流域(约1平方公里)的深层快速(灾难性)滑坡敏感性。在本研究中,我们应用了在印度尼西亚东爪哇省Jember北部的日本方法,那里的泥石流灾害是由于2004年由深部快速(灾难性)滑坡形成的滑坡坝倒塌而引起的。尽管存在与数据相关的一些局限性可用性方面,我们成功评估了对深层快速滑坡的敏感性。

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