Predisposition Factor of Safety of Landslide Dams from Typhoon Talas, Kii Peninsula, Japan

Daikai Rikuto, Gomez Christopher, B. Bradák, Aditya Saputra, D. Hadmoko
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Abstract

Landslide dams are less frequent than other landslides, and their very existence is often very-much short-lived, because the temporary dam tends to collapse rapidly. Because of the resulting lack of evidences, there has been less research done on this topic, although the potential catastrophe they can be at the origin of needs assessment. For this purpose, the present contribution aims at differentiating landslides that trigger dams against those that do not inside a group of valleys of the Kii peninsula in Japan, where landslides occurred after the typhoon Talas in 2011. Using topographic map before the event and LiDAR data in its aftermath, the authors have calculated the factor of safety (FS) of different landslides in the same valleys, comparing the data of landslides that created dams against those that did not. The results show that landslides that triggered dams seemed to have a higher FS than those that did not. The authors suggest that it is because larger landslides are needed and thus appear more stable, but also because at the location where the slopes are stable, the riverbed can incise further instead of growing horizontally, and thus the sediments damming the channel have more chances to block it (as it is narrow) and stop the river from flowing.
台风“塔拉斯”对日本纪宜半岛滑坡坝安全的影响因素
与其他滑坡相比,滑坡坝发生的频率较低,而且它们的存在往往非常短暂,因为临时坝往往会迅速坍塌。由于缺乏证据,对这一主题的研究较少,尽管它们可能是需求评估的潜在灾难。为此,目前的贡献旨在区分触发大坝的山体滑坡与那些不会在日本纪井半岛的一组山谷内发生的山体滑坡,这些山体滑坡发生在2011年台风塔拉斯之后。利用地震前的地形图和地震后的激光雷达数据,作者计算了同一山谷中不同滑坡的安全系数(FS),并将造成大坝的滑坡数据与没有造成大坝的滑坡数据进行了比较。结果表明,触发大坝的滑坡似乎比没有触发大坝的滑坡具有更高的FS。作者认为,这是因为需要更大的滑坡,因此看起来更稳定,但也因为在斜坡稳定的地方,河床可以进一步切割,而不是水平生长,因此筑坝的沉积物有更多的机会阻塞它(因为它很窄),阻止河流流动。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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CiteScore
0.10
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0.00%
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11
审稿时长
15 weeks
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