4.7 Article

MPM evaluation of the dynamic runout process of the giant Daguangbao landslide

期刊

LANDSLIDES
卷 18, 期 4, 页码 1509-1518

出版社

SPRINGER HEIDELBERG
DOI: 10.1007/s10346-020-01569-2

关键词

Landslide; Runout analysis; Material point method; Friction degradation

资金

  1. NSFC [41877291, 41672356]
  2. National Key R&D Program of China [2020YFC1512005]
  3. Belt & Road international cooperation team for the Light of West program of CAS
  4. Key Research Program of the Chinese Academy of Sciences [KFZD-SW-424]

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This study investigates the runout process of the Daguangbao landslide triggered by the 2008 Wenchuan earthquake. It finds that the landslide mass initially slides along the bedding-plane as a whole body before disintegrating during the runout process. The duration of sliding is 64 seconds with a maximum velocity of 60 m/s. Friction degradation of the slip surface has a significant impact on the final runout distance and depth of the deposit zone.
Giant landslides can cause significant damage to their dynamic runout processes. Understanding the mechanics of the runout process is essential for landslide risk assessment and mitigation design. This paper investigates the runout process of the 1.16 x 10(9) m(3) giant Daguangbao landslide triggered by the 2008 Ms 8.0 Wenchuan earthquake. The Daguangbao landslide is a typical bedding-plane slide and the properties of basal sliding surface play a key role in the runout behaviors of the landslide. The material point method (MPM) is adopted as a numerical tool of the simulations. A thermal-based velocity-weakening friction law is used to simulate the contact between the sliding body and the basal sliding surface. A strain-softening constitutive model is used to evaluate the damages inside the landslide body and their effects on the runout behaviors of the landslide. Numerical results reveal that landslide mass slides along the bedding-plane as a whole body initially and then disintegrates during the runout process. The calculated duration of sliding is 64 s and the maximum velocity reaches 60 m/s. The friction coefficient of the slip surface decreases sharply as the landslide body starts to move, and a steady-state friction coefficient mu approximate to 0.06 is reached when the velocity exceeds approximately 20 m/s. Friction degradation of the slip surface shows a sensible influence on the final runout distance and the depth of the deposit zone. The dynamic fragmentation of the landslide body, the final runout distance, and deposition topography are also significantly affected by material softening.

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