Technical Papers
May 17, 2024

Rainfall Infiltration Test and Numerical Simulation Analysis of a Large Unsaturated Soil Slope

Publication: Journal of Hydrologic Engineering
Volume 29, Issue 4

Abstract

Rainfall infiltration is the primary factor affecting slope stability, which may lead to geological hazards such as landslides, collapses, and debris flows. Thus, it is crucial to investigate the rainfall infiltration patterns of unsaturated soil slopes. During a natural rainstorm, the soil volumetric water content at various depths of a significant unsaturated soil slope model was monitored onsite. The soil-water characteristic curve parameters and saturated permeability coefficient of remolded soil were quantified, and the Van Genuchten (VG) model was utilized to forecast the unsaturated permeability coefficient. The numerical simulation method was used to simulate the field rainfall experiment. Based on the mutual verification of the field measurement and numerical simulation, rainfall simulation with different rainfall intensities was added, and its influence on rainfall infiltration depth, pore water pressure, and transient saturated zone was analyzed. The findings revealed that under the rainstorm intensity of the field rainfall test, the rainfall infiltration depth ranged from 0.2 to 0.4 m after a continuous 9-h rainfall period. As the rainfall intensity increased, the range of soil pore water pressure variations expanded, with a maximum value ranging from 9 to 140 kPa under the rainstorm rainfall intensity. By extending the duration of rainstorm rainfall intensity to 14 h, the depth of the transient saturated zone reached 0.2 m. With a duration of 20 h, it reached 0.4 m. The depth reached 0.6 m after 27 h and 1.5 m after 36 h. The research findings of this paper can provide scientific guidance for revealing the hydrological characteristics of slopes during rainfall and for the protection and reinforcement of slopes.

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Data Availability Statement

All data supporting the findings of this study are available from the corresponding author upon reasonable request.

Acknowledgments

This work was supported by the National Natural Science Foundation of China (No. 51978249), the Joint Funds of the National Natural Science Foundation of China (No. U22A20232), and the Innovation Group Project of Hubei Science and Technology Department (No. 2020CFA046).

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Go to Journal of Hydrologic Engineering
Journal of Hydrologic Engineering
Volume 29Issue 4August 2024

History

Received: Oct 20, 2023
Accepted: Feb 20, 2024
Published online: May 17, 2024
Published in print: Aug 1, 2024
Discussion open until: Oct 17, 2024

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Gaoliang Tao, Ph.D. [email protected]
Professor, Innovation Demonstration Base of Ecological Environment Geotechnical and Ecological Restoration of Rivers and Lakes, Hubei Univ. of Technology, Wuhan, Hubei 430068, China; Professor, School of Intelligent Construction, Wuchang Univ. of Technology, Wuhan, Hubei 430223, China. Email: [email protected]
Master’s Student, Innovation Demonstration Base of Ecological Environment Geotechnical and Ecological Restoration of Rivers and Lakes, Hubei Univ. of Technology, Wuhan, Hubei 430068, China. Email: [email protected]
Henglin Xiao, Ph.D. [email protected]
Professor, Innovation Demonstration Base of Ecological Environment Geotechnical and Ecological Restoration of Rivers and Lakes, Hubei Univ. of Technology, Wuhan, Hubei 430068, China (corresponding author). Email: [email protected]
Master’s Student, Innovation Demonstration Base of Ecological Environment Geotechnical and Ecological Restoration of Rivers and Lakes, Hubei Univ. of Technology, Wuhan, Hubei 430068, China. Email: [email protected]
Master’s Student, Innovation Demonstration Base of Ecological Environment Geotechnical and Ecological Restoration of Rivers and Lakes, Hubei Univ. of Technology, Wuhan, Hubei 430068, China. Email: [email protected]

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