Abstract

Information about the long-term spatiotemporal evolution of landslides can improve the understanding of landslides. However, since landslide deformation characteristics differ it is difficult to monitor the entire movement of a landslide using a single method. The Interferometric Synthetic Aperture Radar (InSAR) and pixel offset tracking (POT) method can complement each other when monitoring deformation at different landslide stages. Therefore, the InSAR and improved POT method were adapted to study the pre- and post-failure surface deformation characteristics of the Gaojiawan landslide to deepen understanding of the long-term spatiotemporal evolution characteristics of landslides. The results show that the deformation displacement gradient of the Gaojiawan landslide exhibited rapid movement that exceeded the measurable limit of InSAR during the first disaster. Moreover, the Gaojiawan landslide has experienced long-term creep, and while studying the post-second landslide’s failure stability, the acceleration trend was identified via time series analysis, which can be used as a precursor signal for landslide disaster warning. Our study aims to provide scientific reference for local governments to help prevent and mitigate geological disasters in this region.

Highlights

  • Landslides and related disasters, as complex natural phenomena, cause significant casualties and serious consequences worldwide [1,2,3,4,5]

  • The Gaojiawan landslide is in a state of accelerated deformation, posing a severe threat to the tunnel and the communities at the foot of the mountain

  • In this study, understanding of the Gaojiawan landslide evolution increased by studying the combination of Interferometric Synthetic Aperture Radar (InSAR)

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Summary

Introduction

Landslides and related disasters, as complex natural phenomena, cause significant casualties and serious consequences worldwide [1,2,3,4,5]. Landslides are distributed throughout the mountainous areas of western China [6,7]. In the transition zone between the Qinghai-Tibet Plateau and the Loess Plateau in particular, tectonics are active, the regional stability is fragile, and geological disasters are frequent [8]. Surface deformation measurement is essential to understanding the evolution of landslides and the early warning of catastrophic damage [10,11,12,13,14]. Due to the unpredictability, imperceptibility, and inaccessibility of many landslides, it is often impossible to obtain such information through traditional measurements

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