Volume 40 Issue 3
Jun.  2026
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REN Xiufang, LI Kai, QU Bin, WEI Zhiyuan. Correlation between rainfall and surface displacement of shallow loess landslides: a case study of Dongzhangpo Village landslide, Xi’an[J]. GEOTECHNICAL ENGINEERING TECHNIQUE, 2026, 40(3): 366-372. doi: 10.20265/j.cnki.issn.1007-2993.2025-0034
Citation: REN Xiufang, LI Kai, QU Bin, WEI Zhiyuan. Correlation between rainfall and surface displacement of shallow loess landslides: a case study of Dongzhangpo Village landslide, Xi’an[J]. GEOTECHNICAL ENGINEERING TECHNIQUE, 2026, 40(3): 366-372. doi: 10.20265/j.cnki.issn.1007-2993.2025-0034

Correlation between rainfall and surface displacement of shallow loess landslides: a case study of Dongzhangpo Village landslide, Xi’an

doi: 10.20265/j.cnki.issn.1007-2993.2025-0034
  • Received Date: 2025-01-20
  • Accepted Date: 2025-04-09
  • Rev Recd Date: 2025-03-06
  • Available Online: 2026-06-08
  • Publish Date: 2026-06-08
  • The Dongzhangpo Village landslide is a rainfall-triggered shallow loess landslide. To reveal the deformation mechanism of shallow loess landslides induced by rainfall and provide a basis for the early warning of regional shallow loess landslides during the rainy season, monitoring and correlation analysis of rainfall, soil moisture content and slope deformation were carried out on this landslide. The results show that the horizontal and vertical displacements on the landslide surface basically reach their peaks under the condition of rainfall peaks. According to the variation trends of rainfall and slope displacement, the Dongzhangpo Village landslide is a typical rainfall-triggered landslide. The Pearson correlation coefficient analysis indicates that the soil moisture content at depths of 0.2~4.2 m below the ground surface has an extremely strong correlation with rainfall. The lag time of soil moisture content variation ranges from 30 to 196 h, and the lag time gradually increases with the increase of burial depth. The surface displacement has an extremely strong correlation with the increment of soil moisture content at 0.2 m depth, a moderate correlation with that at 0.7 m, 1.2 m and 1.5 m depths, and a weak correlation with that at 2.2 m, 3.2 m and 4.2 m depths, indicating that the landslide deformation is dominated by shallow surface displacement. In terms of the lag of surface displacement behind the increase of moisture content, the peak correlation coefficients at all depths appear within 24 h with very small lag, showing that slope deformation occurs shortly after the increase of soil moisture content.

     

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