Effects of Tectonic Setting and Hydraulic Properties on Silent Large-Scale Landslides: A Case Study of the Zhaobishan Landslide, China
| Primer Autor |
Hu, Guisheng
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| Co-autores |
Tian, Shufeng
Chen, Ningsheng
Rahman, Mahfuzur
Ni, Huayong
Somos-Valenzuela, Marcelo
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| Título |
Effects of Tectonic Setting and Hydraulic Properties on Silent Large-Scale Landslides: A Case Study of the Zhaobishan Landslide, China
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| Editorial |
SPRINGER
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| Revista |
INTERNATIONAL JOURNAL OF DISASTER RISK SCIENCE
|
| Lenguaje |
en
|
| Resumen |
Unlike strong earthquake-triggered or heavy rainfall-triggered landslides, silent large-scale landslides (SLL) occur without significant triggering factors and cause unexpected significant disaster risks and mass casualties. Understanding the initiation mechanism of SLLs is crucial for risk reduction. In this study, the mechanism of the Zhaobishan SLL was investigated, and the SLL was jointly controlled by weak-soil (fractured rock mass) and strong-water (abundant water replenishment) conditions under the impact of active tectonism and complex hydraulic properties. Strong tectonic uplift, high fault density, and historical earthquakes led to weak-soil conditions conducive to the Zhaobishan SLL. The combined effect of unique lithology, antiform, and cultivated land contributed to the water replenishment characteristics of extensive runoff confluence (3.16 times that of the landslide body) and supported long-distance groundwater replenishment, thereby forming strong-water conditions for the landslide. The amplified seepage amount caused the strength of the soil mass on the sliding surface to decrease to 0.4 times its initial strength, eventually triggering the Zhaobishan SLL, which occurred 4.6 days after the peak rainfall. Moreover, the landslide deposits have accumulated on the semi-diagenetic clay rock, thereby controlling the subsequent recurring debris flows in the Lengzi Gully. To reduce disaster risk of SLL in vulnerable mountainous regions, the water confluence area behind the main scarp of the landslides and the hysteresis characteristics between landslides and peak rainfall should be further considered, and recurring debris flows following massive landslides also should be focused.
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| Fecha Publicación |
2023
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| Tipo de Recurso |
artículo original
|
| doi |
10.1007/s13753-023-00502-0
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| Formato Recurso |
PDF
|
| Palabras Claves |
Debris flow
Hydraulic properties
Risk reduction
Runoff amplification
Silent large-scale landslides (SLL)
Tectonic setting
|
| Ubicación del archivo | |
| Categoría OCDE |
Geología
Meteorología y Ciencias Atmosféricas
Recursos Hídricos
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| Materias |
Flujo de escombros
Propiedades hidráulicas
La reducción de riesgos
amplificación de escorrentía
Deslizamientos de tierra silenciosos a gran escala (SLL)
entorno tectónico
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| Página de inicio (Recomendado-único) |
600.0
|
| Página final (Recomendado-único) |
617
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| Identificador del recurso (Mandatado-único) |
artículo original
|
| Versión del recurso (Recomendado-único) |
versión publicada
|
| License |
CC BY 4.0
|
| Condición de la licencia (Recomendado-repetible) |
CC BY 4.0
|
| Derechos de acceso |
acceso abierto
|
| Access Rights |
acceso abierto
|
| Id de Web of Science |
WOS:001059871100002
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| ISSN |
2095-0055
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| Tipo de ruta |
verde# dorada
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| Categoría WOS |
Geología
Meteorología y Ciencias Atmosféricas
Recursos Hídricos
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| Referencia del Financiador (Mandatado si es aplicable-repetible) |
NSFC U20A20110
STEP 2019QZKK0902
YIPA 2020367
CHAS 131C11KYSB20200033
|
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