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A shift from drought to extreme rainfall drives a stable landslide to catastrophic failure
The addition of water on or below the earth’s surface generates changes in stress that can trigger both stable and unstable sliding of landslides and faults. While these sliding behaviours are well-described by commonly used mechanical models developed from laboratory testing (e.g., critical-state s...
| Autores principales: | , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2019
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6367458/ https://www.ncbi.nlm.nih.gov/pubmed/30733588 http://dx.doi.org/10.1038/s41598-018-38300-0 |