Controls on Post?Seismic Landslide Behavior in Brittle Rocks

نویسندگان

چکیده

Earthquakes trigger widespread landsliding in tectonically active landscapes. The effects of strong ground shaking on hillslope stability persist into the post-seismic stage; rates remain elevated years following an earthquake. mechanisms that control spatial pattern and rate ongoing are poorly constrained, hindering our ability to reliably forecast how landscapes landslide hazard evolve. To address this, we undertook a detailed geotechnical investigation which subjected representative rock samples dynamic loading, simulating earthquake hillslopes different configuration. Our results indicate strength is not intrinsic property; rather, it responds amplitude imposed loads degree pre-existing shear surface formation within rock. This path-dependent behavior from differences character fractures generated by amplitude, ways apertures mobilized or degraded subsequent (post-seismic) shearing. Sensitivity loading greater shallow landslides surfaces yet fully form; such can be strengthened weakened events, depending their characteristics. In contrast, deeper steeper have largely developed less likely display response because strain accumulation along dominant. demonstrate need consider numerical models used respond earthquakes evolves.

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ژورنال

عنوان ژورنال: Journal Of Geophysical Research: Earth Surface

سال: 2021

ISSN: ['2169-9011', '2169-9003']

DOI: https://doi.org/10.1029/2021jf006242