Deutsch
 
Datenschutzhinweis Impressum
  DetailsucheBrowse

Datensatz

DATENSATZ AKTIONENEXPORT
Zur Ablage hinzufügen
  Lokale TagsFreigabegeschichteDetailsÜbersicht

Freigegeben
Zeitschriftenartikel

Monitoring crack opening via seismic velocity variation to assess that fatal effect of precipitation for landslide motion

Urheber*innen

Liu,  Zhiqiang
External Organizations;

Liang,  Chuntao
External Organizations;

/persons/resource/chris

Sens-Schönfelder,  C.
2.4 Seismology, 2.0 Geophysics, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Hu,  Wei
External Organizations;

Sun,  Xinlei
External Organizations;

/persons/resource/tuo

ZHANG,  TUO
2.4 Seismology, 2.0 Geophysics, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Xu,  Rui
External Organizations;

Jiang,  Zhiyu
External Organizations;

Jiang,  Hao
External Organizations;

Externe Ressourcen
Es sind keine externen Ressourcen hinterlegt
Volltexte (frei zugänglich)
Es sind keine frei zugänglichen Volltexte in GFZpublic verfügbar
Ergänzendes Material (frei zugänglich)
Es sind keine frei zugänglichen Ergänzenden Materialien verfügbar
Zitation

Liu, Z., Liang, C., Sens-Schönfelder, C., Hu, W., Sun, X., ZHANG, T., Xu, R., Jiang, Z., Jiang, H. (2024): Monitoring crack opening via seismic velocity variation to assess that fatal effect of precipitation for landslide motion. - Earth and Planetary Science Letters, 644, 118922.
https://doi.org/10.1016/j.epsl.2024.118922


Zitierlink: https://gfzpublic.gfz-potsdam.de/pubman/item/item_5027646
Zusammenfassung
Numerous potential landslides with slow sliding speeds pose a continuous threat to human safety. The movements of these landslides continuously modify hydrogeological conditions and lead to cracks expansion, making it easier for subsequent rainfall to infiltrate into the landslide interior. Monitoring the tiny variations of structures and pore-water pressure in the interior of landslides can help understanding this coupling mechanism and accessing landslide damage risk. Here, we utilized seismic ambient noise interferometry to assess hourly velocity changes that enable us to quantify the response of landslides to external factors at different depths, including earthquakes, rainfall, and mechanical effects from sliding. In a case of Xishan Village Landslide, Sichuan Province, China, we observed an outstanding velocity drop coinciding with the onset of rainfall and bursts in tremor activity in a period in which the landslide experienced vertical displacement. Our observations highlight the new sight to investigate how the mechanical process of landslide movement modifies hydrogeological conditions and promotes rainfall infiltration, as well as assesses the subsequent recovery process.