Abstract
Due to the huge losses caused by landslides, landslide deformation monitoring has become essential. The change of the tilting angle of the slope surface can reflect the instability process of the landslide. However, there are few studies on the relationship between the instability process of landslides and the tilting angle of the slope surface on the time scale. Therefore, there are even fewer cases in using the inclination angle of the landslide as an early warning method in practice. On August 24, 2018, a wireless tilt sensor network was deployed in the Heifangtai area of Gansu Province in China, to monitor the inclination state of loess landslides to study the relationship between the tilting angle of the slope surface and the landslide instability process. At 4 o’clock on October 5, 2019, the wireless tilt sensor network mentioned above detected a new loess fall landslide. Through the analysis of the monitoring data from the tilting sensor nodes named T3 and T4, we found that the tilting angle of the landslide surface in the pre-sliding stage has significant change compared with the stable stage, which directly verifies that the inclination data can be used for landslide warning. At the same time, we inputted the monitored inclination data into the inclination warning model proposed by **e et al. (Landslides 17:301–312, 2020) for verification and found that the trend of inclination changes matches the model well. However, the forecast time error is large. Therefore, this paper optimizes the inclination early warning model proposed by **e. Using the optimized early warning model, the predicted landslide occurrence time based on the data of the T3 node was 0.517 days, which was about 8 h later than the actual landslide that occurred on October 4, 2019, which is an improvement of forecasting. This case serves as an on-site direct evidence to further verify the feasibility of using the landslide body inclination state as a landslide monitoring and early warning parameter which can be promoted and used in practice.
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs10346-021-01727-0/MediaObjects/10346_2021_1727_Fig1_HTML.png)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs10346-021-01727-0/MediaObjects/10346_2021_1727_Fig2_HTML.png)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs10346-021-01727-0/MediaObjects/10346_2021_1727_Fig3_HTML.png)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs10346-021-01727-0/MediaObjects/10346_2021_1727_Fig4_HTML.png)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs10346-021-01727-0/MediaObjects/10346_2021_1727_Fig5_HTML.png)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs10346-021-01727-0/MediaObjects/10346_2021_1727_Fig6_HTML.png)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs10346-021-01727-0/MediaObjects/10346_2021_1727_Fig7_HTML.jpg)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs10346-021-01727-0/MediaObjects/10346_2021_1727_Fig8_HTML.png)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs10346-021-01727-0/MediaObjects/10346_2021_1727_Fig9_HTML.png)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs10346-021-01727-0/MediaObjects/10346_2021_1727_Fig10_HTML.png)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs10346-021-01727-0/MediaObjects/10346_2021_1727_Fig11_HTML.png)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs10346-021-01727-0/MediaObjects/10346_2021_1727_Fig12_HTML.png)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs10346-021-01727-0/MediaObjects/10346_2021_1727_Fig13_HTML.png)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs10346-021-01727-0/MediaObjects/10346_2021_1727_Fig14_HTML.png)
References
Brabb EE (1991) The world landslide problem. Episodes 14:52–61. https://doi.org/10.18814/epiiugs/1991/v14i1/008
Fan X, Xu Q, Liu J et al (2019) Successful early warning and emergency response of a disastrous rockslide in Guizhou Province, China. Landslides 16:2445–2457. https://doi.org/10.1007/s10346-019-01269-6
Lin M, Yan W, Wassell I (2008) Wireless sensor network: water distribution monitoring system. In: Radio & Wireless Symposium. IEEE. https://doi.org/10.1109/RWS.2008.4463607
Liu Y, Liao M, Shi X et al (2016) Potential loess landslide deformation monitoring using L-band SAR interferometry. Geo-Spatial Inf Sci 19:273–277. https://doi.org/10.1080/10095020.2016.1258202
Lu GY, Chiu LS, Wong DW (2007) Vulnerability assessment of rainfall-induced debris flows in Taiwan. Nat Hazards 43(2):223–244. https://doi.org/10.1007/s11069-006-9105-y
Nadim F, Kjekstad O, Peduzzi P et al (2006) Global landslide and avalanche hotspots. Landslides 3:159–173. https://doi.org/10.1007/s10346-006-0036-1
Pecoraro G, Calvello M, Piciullo L (2018) Monitoring strategies for local landslide early warning systems. Landslides 16:213–231. https://doi.org/10.1007/s10346-018-1068-z
Peng J, Lin H, Wang Q et al (2014) The critical issues and creative concepts in mitigation research of loess geological hazards. J Engingeering Geol 22:684–691. https://doi.org/10.13544/J.CNKI.JEG.2014.04.014
Qi X, **u D, Peng D, Ju Y (2018) Forecasting method of sliding distance of static liquefaction-type loess landslide in Heifangtai, Gansu Province. J Sichuan Univ Sci Eng (Natural Sci Ed) 31(4):83–88. https://doi.org/10.11863/j.suse.2018.04.13
Qi X, Xu Q, Li B et al (2016) Preliminary study on mechanism of surface water infiltration at Heifangtai loess landslide in Gansu. J Eng Geol 24(3):418–424. https://doi.org/10.13544/j.cnki.jeg.2016.03.011
Robinson G, Spieker A (1978) Nature to be commanded…: earth-science maps applied to land and water management
Uchimura T, Towhata I, Lan Anh TT et al (2010) Simple monitoring method for precaution of landslides watching tilting and water contents on slopes surface. Landslides 7:351–357. https://doi.org/10.1007/s10346-009-0178-z
Uchimura T, Towhata I, Wang L et al (2015) Precaution and early warning of surface failure of slopes using tilt sensors. Soils Found 55(5):1086–1099. https://doi.org/10.1016/j.sandf.2015.09.010
Wang H, Zhuo T, Zhong P et al (2021) A novel wireless underground transceiver for landslide internal parameter monitoring based on magnetic induction. Int J Circuit Theory Appl 1–10. https://doi.org/10.1002/cta.2975
**e J, Uchimura T, Wang G et al (2020) A new prediction method for the occurrence of landslides based on the time history of tilting of the slope surface. Landslides 17:301–312. https://doi.org/10.1007/s10346-019-01283-8
Xu Q, Peng D, He C, et al (2020) Theory and method of monitoring and early warning for sudden loess landslide—a case study at Heifangtai terrace. J Eng Geol 28:111–121 (in Chinese). https://doi.org/10.13544/J.CNKI.JEG.2019-038
Yue J (2014) Research on railway slope monitoring and early warning based on instrument for surface inclined deformation. Shijiazhuang Tiedao University. (in Chinese)
Zhao C, Zhang Q, He Y et al (2016) Small-scale loess landslide monitoring with small baseline subsets interferometric synthetic aperture radar technique—case study of **ngyuan landslide. Shaanxi, China J Appl Remote Sens, pp 10–026030. https://doi.org/10.1117/1.JRS.10.026030
Acknowledgements
The authors would like to thank graduate students Tianxiang Zhuo, Dingkang Zou, and Chaoyu Wei for their help during the deployment of the system. We also want to give great thanks to Wisen Innovation Company, Wuxi, China, for offering the Wisen wireless sensor system.
Funding
This work was sponsored by the National Natural Science Foundation of China (41521002), the State Key Laboratory of Geohazard Prevention and Geoenvironment Protection Independent Research Project (SKLGP2019Z012), and the Sichuan Science and Technology Program (2021YFS0324). It was also partially supported by the China Scholarship Council (201808510005).
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Wang, H., Zhong, P., **u, D. et al. Monitoring tilting angle of the slope surface to predict loess fall landslide: an on-site evidence from Heifangtai loess fall landslide in Gansu Province, China. Landslides 19, 719–729 (2022). https://doi.org/10.1007/s10346-021-01727-0
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s10346-021-01727-0