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Geometry-Based Preliminary Quantification of Landslide-Induced Impulse Wave Attenuation in Mountain Lakes
 
 
Article

The Effects of Rainfall, Soil Type and Slope on the Processes and Mechanisms of Rainfall-Induced Shallow Landslides

State Key Laboratory of Hydraulics and Mountain River Engineering, Sichuan University, Chengdu 610065, China
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Academic Editors: Ricardo Castedo, Miguel Llorente Isidro and David Moncoulon
Appl. Sci. 2021, 11(24), 11652; https://doi.org/10.3390/app112411652
Received: 3 November 2021 / Revised: 24 November 2021 / Accepted: 3 December 2021 / Published: 8 December 2021
(This article belongs to the Special Issue Geohazards: Risk Assessment, Mitigation and Prevention)
Landslides are a serious geohazard worldwide, causing many casualties and considerable economic losses every year. Rainfall-induced shallow landslides commonly occur in mountainous regions. Many factors affect an area’s susceptibility, such as rainfall, the soil, and the slope. In this paper, the effects of rainfall intensity, rainfall pattern, slope gradient, and soil type on landslide susceptibility are studied. Variables including soil volumetric water content, matrix suction, pore water pressure, and the total stress throughout the rainfall were measured. The results show that, under the experimental conditions of this paper, no landslides occurred on a 5° slope. On a 15° slope, when the rainfall intensity was equal to or less than 80 mm/h with a 1 h duration, landslides also did not happen. With a rainfall intensity of 120 mm/h, the rainfall pattern in which the intensity gradually diminishes could not induce landslides. Compared with fine soils, coarser soils with gravels were found to be prone to landslides. As the volumetric water content rose, the matrix suction declined from the time that the level of infiltration reached the position of the matrix. The pore water pressure and the total stress both changed drastically either immediately before or after the landslide. In addition, the sediment yield depended on the above factors. Steeper slopes, stronger rainfall, and coarser soils were all found to increase the amount of sediment yield. View Full-Text
Keywords: landslides; artificial rainfall; grain size; rainfall pattern; pore water pressure landslides; artificial rainfall; grain size; rainfall pattern; pore water pressure
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MDPI and ACS Style

Liu, Y.; Deng, Z.; Wang, X. The Effects of Rainfall, Soil Type and Slope on the Processes and Mechanisms of Rainfall-Induced Shallow Landslides. Appl. Sci. 2021, 11, 11652. https://doi.org/10.3390/app112411652

AMA Style

Liu Y, Deng Z, Wang X. The Effects of Rainfall, Soil Type and Slope on the Processes and Mechanisms of Rainfall-Induced Shallow Landslides. Applied Sciences. 2021; 11(24):11652. https://doi.org/10.3390/app112411652

Chicago/Turabian Style

Liu, Yan, Zhiyuan Deng, and Xiekang Wang. 2021. "The Effects of Rainfall, Soil Type and Slope on the Processes and Mechanisms of Rainfall-Induced Shallow Landslides" Applied Sciences 11, no. 24: 11652. https://doi.org/10.3390/app112411652

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