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Preliminary analysis of the catastrophic February 22nd 2023 Xinjing open-pit mine landslide, Inner Mongolia, China
Preliminary analysis of the catastrophic February 22nd 2023 Xinjing open-pit mine landslide, Inner Mongolia, China
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Preliminary analysis of the catastrophic February 22nd 2023 Xinjing open-pit mine landslide, Inner Mongolia, China
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Preliminary analysis of the catastrophic February 22nd 2023 Xinjing open-pit mine landslide, Inner Mongolia, China
Preliminary analysis of the catastrophic February 22nd 2023 Xinjing open-pit mine landslide, Inner Mongolia, China

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Preliminary analysis of the catastrophic February 22nd 2023 Xinjing open-pit mine landslide, Inner Mongolia, China
Preliminary analysis of the catastrophic February 22nd 2023 Xinjing open-pit mine landslide, Inner Mongolia, China
Journal Article

Preliminary analysis of the catastrophic February 22nd 2023 Xinjing open-pit mine landslide, Inner Mongolia, China

2024
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Overview
On February 22, 2023, a devastating landslide occurred on the mining slope of an open-pit coal mine in Inner Mongolia, China, leading to the mining area being buried and 53 fatalities. The source area of the landslide measured approximately 500 m in both length and width, with an estimated volume of the deposited material reaching approximately 5 million cubic metres. Based on the severe impact of this incident, our study conducted preliminary research using a combination of methodologies, including particle image analysis, synthetic aperture radar interferometry, interpretation of optical remote sensing data, and post-event news reports analysis. The results indicated that the landslide lasted 23 s from initiation to cessation of movement. The historical deformation indicated that prior to the resumption of the mining activities, only localized deformation was observed at the rear edge of the landslide. However, when mining activities resumed in April 2021 and extended to the vicinity of the north slope, the deformation range and rate in the source area of the landslide rapidly increased. The investigation deduced that the soft foundation at the slope bottom and mining activities are the primary causative factors of this event. Mining activities, which stripped coal seams within the slope and surface rock masses, led to the expansion of tension cracks within the landslide body, weakening resisting forces at the leading edge and thus playing a significant role in destabilizing the landslide body. The evolution of the landslide from incubation to instability could be divided into four stages: early microcrack development, slow creep, accelerated deformation after resumption of mining, and ultimate instability. Therefore, it is of great significance to advance real-time deformation monitoring and early warning systems specifically those designed for mining slope areas by comprehensive measures. Furthermore, enhancing the high-frequency monitoring capabilities of synthetic aperture radar satellites is crucial to reducing the occurrence of these catastrophic events.