Skip to main content
Log in

Response of landslide deformation to rainfall based on multi-index monitoring: a case of the Tanjiawan landslide in the Three Gorges Reservoir

  • Original Paper
  • Published:
Bulletin of Engineering Geology and the Environment Aims and scope Submit manuscript

A Correction to this article was published on 08 October 2022

This article has been updated

Abstract

Landslide deformation in the Three Gorges Reservoir Area (TGRA) is mainly caused by water level fluctuations; however, it is also influenced by rainfall. The Tanjiawan landslide is one of the most notable landslides affected by rainfall in the TGRA. This study investigates the landslide’s deformation mechanism by analysing reconnaissance data, which are surface deformation survey data, and GPS displacement data for the last 16 years along with several types of monitoring data from equipment installed in 2020. The landslide has undergone significant deformation since September 2014. Subsequent rainfall events have caused severe deformation, and tension cracks have appeared in many parts of the landslide. Owing to the slope structure and rainfall events, a deformation feature has developed, in which sliding masses no. 1 and no. 2 are the active and secondary deformation zones, respectively. The surface displacement of the landslide is clearly step-like, and its episodic deformation is controlled by rainfall. Landslide deformation leads to the development of cracks in the slope, producing dominant seepage channels. As rainwater enters belowground along the cracks and with the influence of the bedrock morphology, the groundwater level in the middle and rear parts, and hence, the hydrodynamic pressure, increase, thereby activating landslide deformation. Both continuous rainfall and heavy rain are responsible for this phenomenon; sliding mass no. 1 shows an overall downward motion. Finally, the seismic data recorded by microcore piles and the change rate in soil moisture content after rainfalls can currently be used for reliable early warnings of landslide instability.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9
Fig. 10
Fig. 11
Fig. 12
Fig. 13
Fig. 14
Fig. 15
Fig. 16
Fig. 17
Fig. 18
Fig. 19

Similar content being viewed by others

Change history

References

Download references

Acknowledgements

Some data of the manuscript were collected with the assistance of Yichang Geological Environment Monitoring and Protection station.

Funding

This work was supported by the National Natural Science Foundation Key Projects of China (No. U21A2031) and the China Postdoctoral Science Foundation (2021M701969).

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Shimei Wang.

Ethics declarations

Conflict of interest

The authors declare no competing interests.

Additional information

The original online version of this article was revised: Originally, the article was published with problem in the organization name of the authors. "China" has been omitted from the affiliations 1 and 2 during processing.

Rights and permissions

Springer Nature or its licensor holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Wang, L., Chen, Y., Wang, S. et al. Response of landslide deformation to rainfall based on multi-index monitoring: a case of the Tanjiawan landslide in the Three Gorges Reservoir. Bull Eng Geol Environ 81, 231 (2022). https://doi.org/10.1007/s10064-022-02732-w

Download citation

  • Received:

  • Accepted:

  • Published:

  • DOI: https://doi.org/10.1007/s10064-022-02732-w

Keywords

Navigation