Identification Of Locking Segment In A High-Locality Landslide In Shidaguan, Southwest China
Abstract Identification of the locking segments is crucial for assessing the potential runout risk and the overall stability of the high-locality landslide. However, during the field investigation, it is difficult to identify the locking segments before landslide failure due to their concealment. Tizicao landslide, a high-locality landslide, is used as the field example for the locking segments identification analysis in this study. Based on the geomorphology and spatial-temporal deformation in the landslide, the identification characteristics of the locking segments of the landslide are analyzed macroscopically, and the location and area of the locking segments are determined based on the analysis results. The field investigation methods are used to verify the identification results, including the monitoring of surface and deep displacement, geological borehole drilling, and oblique photography using drones. The results show that the locking segment of the Tizicao landslide lies at the southern slope toe, which covers an area of about 4.69 × 104 m2, accounting for 15.2% of the total area of the landslide. The significant different developmental characteristics are observed in respect of the surface displacement, deep displacement, surface crack, and sliding zone soil between locking and non-locking segments. It is concluded that the formation and evolution of the locking rock masses in the Tizicao landslide are closely related to the development of local folds and S-shaped river valleys, differential unloading due to river cutting, and earthquake-induced damage to rock masses in the landslide area.