Extreme Rainfall Events Triggered Loess Collapses and Landslides in Chencang District, Shanxi, China, during June–October 2021

Author:

Zhou Chang12,Xia Zhao3,Chen Debin4,Miao Leqian5,Hu Shenghua6,Yuan Jingjing6,Huang Wei6,Liu Li6,Ai Dong6,Xu Huiyuan6,Xiao Chunjin6

Affiliation:

1. School of Resources and Geosciences, China University of Mining and Technology, Xuzhou 221116, China

2. Badong National Observation and Research Station of Geohazards, China University of Geosciences, Wuhan 430074, China

3. Hunan Water Planning and Design Institute Co., Ltd., Changsha 410008, China

4. Xinjiang Bureau of Geology and Mineral Resources Exploration and Development, The Second Hydrological Engineering Geological Brigade, Changji 831100, China

5. Shaanxi Geological and Mineral Third Team, Baoji 721300, China

6. The Seventh Geological Brigade of Hubei Geological Bureau, Yichang 443000, China

Abstract

In recent years, the increasing frequency of extreme weather events has exacerbated the severity of geological disasters. Therefore, it is important to understand the mechanisms of geological disasters under extreme rainfall conditions. From June to October 2021, Baoji City, Shanxi Province, China, experienced some extreme and continuous heavy rainfalls, which triggered more than 30 geological disasters. Those geo-disasters threatened the lives of 831 people and the safety of 195 houses. The field investigations found that most of these geological disasters were devastating collapses that occurred in the loess layer, primarily due to the cave dwelling construction. The shear strength, montmorillonite content, disintegration degree, and plasticity index of two typical loesses, namely the Sanmen Formation stiff clay and the Hipparion red clay, were analyzed, and their water sensitivities were evaluated. The failure mechanisms of the landslides, ground fissures, and collapses were analyzed and most of them were controlled by the cave dwelling construction and the strong water sensitivity of the loess. This study provides data for understanding shallow geological disasters induced by extreme rainfall in the loess area, which are more threatening than large geological disasters. We proposed an intensity–duration (I–D) rainfall threshold as I = 90 D−0.92, which relates the rainfall intensity (I) to the rainfall event duration (D). The empirical threshold provides some useful information for the early warning of collapses or landslides in similar geological settings in the loess area.

Funder

National Natural Science Foundation of China

Open Fund of Badong National Observation and Research Station of Geohazards

Publisher

MDPI AG

Reference36 articles.

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