Volumes and movement distances of earthquake and rainfall-induced catastrophic landslides
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Volumes and movement distances of earthquake and rainfall-induced catastrophic landslides
Vol. 33, Issue 10, (2012)
作者机构:
1. 成都理工大学 地质灾害防治与地质环境保护国家重点实验室,成都,610059
2. 西南科技大学 土木工程与建筑学院,四川,绵阳,621010
3. 中国科学院 成都山地灾害与环境研究所,成都,610041
作者简介:
基金信息:
DOI:
CLC:P642.22
Online First:19 October 2012,
Published:2012
稿件说明:
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FAN Xiao-yi, QIAO Jian-ping, HAN Meng, et al. Volumes and movement distances of earthquake and rainfall-induced catastrophic landslides[J]. 2012, 33(10).
DOI:
FAN Xiao-yi, QIAO Jian-ping, HAN Meng, et al. Volumes and movement distances of earthquake and rainfall-induced catastrophic landslides[J]. 2012, 33(10).DOI:
Volumes and movement distances of earthquake and rainfall-induced catastrophic landslides
To forecast and assess the hazard mechanism of catastrophic landslides
based on the data of earthquake and rainfall-induced catastrophic landslides
the relationships including the equivalent friction coefficient (H/L)
the maximum horizontal distance (L)
the maximum vertical distance (H) and the landslide volume (V) are studied. The relationships among H/L
L
H and V are power laws
in which there are negative power laws between H/L and V and the positive power laws among L
H and V. The horizontal and vertical movement distances of the seismic and the rainfall catastrophic landslides are different in the same scale. The H/L=0.42 is taken into consideration in the standard of landslide long-runout. It is not significant between seismic induced catastrophic landslides and the landslide long-runout
but there is remarkable relationship between rainfall induced catastrophic landslides and the landslide long-runout. The dominate distance of landslide movement can be analyzed based on the movement distances of the 80% landslides; the dominant distances of the horizontal and vertical movements of seismic and rainfall catastrophic landslides are different in the same scale. The results indicate that the movement distances of catastrophic landslides are not only controlled by the volumes but also related to occurrence mechanism. And they can provide references for forecasting and evaluating the hazard region and strength induced by the earthquake and the rainfall catastrophic landslides.