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Study on pore pressure and fluidization evaluation method of unsaturated loess in vibration process

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Abstract

The large-scale fluidization failure of a loess slope induced by earthquake has been widely investigated domestically and abroad. Studies on the fluidization failure of loess slopes have mainly focused on the mechanism of loess subsidence and the liquefaction of saturated loess, while fewer studies have investigated the fluidization failure mechanism and evaluation of unsaturated loess with high water content. In this study, a series of dynamic triaxial cyclic shearing tests were carried out on unsaturated loess to elucidate the mechanism of failure resulting from the fluidization of unsaturated loess by considering the dynamic pore-water pressure, dynamic pore-gas pressure, and dynamic strain of unsaturated loess under the influence of different vibration frequency, matric suction, dynamic stress, and saturation. The results reveal the following: under undrained conditions, when subjected to continuous vibration loading, unsaturated loess can also generate extra-static pore-water pressure, which increases hysterically but quickly grows close to the initial confining pressure. At this time, samples with greater saturation are prone to fluidization failure and approach loess liquefaction. A theoretical model applicable to the fluidization of unsaturated loess is proposed according to the liquefied-evaluation method for saturated loess and the Boyle-Charles law for ideal gases. An evaluation method is also proposed. This study has important theoretical value, and practical significance for further understanding the formation mechanism of the fluidized failure of unsaturated loess slopes under vibration conditions, and for preventing and controlling slope geological disasters during earthquakes in loess regions.

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References

  • Bai M, Zhang S (1990) Liquefaction and movement of loess layer during high-intensity earthquakes. Eng Survey 6:5–9 (in Chinese)

    Google Scholar 

  • China Earthquake Administration Lanzhou Institute of Seismology (1980) The 1920 Haiyuan Earthquake. Seismological Press, Beijing

    Google Scholar 

  • Chen Y, Shi Y (2006) Basic characteristics of seismic landslides in the loess area of Northwest China. Seismol Res 29(3):276–280 (in Chinese)

    Google Scholar 

  • Chen Z, Guo N (2019) New progress in research on unsaturated soil and special soil mechanics and engineering applications. Rock Soil Mech 40(01):1–54 (in Chinese)

    Google Scholar 

  • Kazama M, Unno T (2007) Earthquake-induced mudflow mechanism from a viewpoint of unsaturated soil dynamics. Exper Unsaturat Soil Mechan 112(4):437–444

    Article  Google Scholar 

  • Luo Y (2005) Research on structural change characteristics and structural constitutive relationship of unsaturated loess under dynamic and static complex stress conditions. Xi’an University of Technology, Xi’an

    Google Scholar 

  • Liu D (2009) Loess and arid environment. Anhui Science and Technology Press, Hefei

    Google Scholar 

  • Li S, Jia H, Wang X et al (2016) Limitation and error analysis of axis translation technique for measuring and controlling matric suction. Rock Soil Mech 37(11):3089–3095 (in Chinese)

    Google Scholar 

  • Liu W (2016) Study on the background and disaster modes of landslide on loess plateau. Chang’an University, Xi’an

    Google Scholar 

  • Ma P, Peng J, Wang Q et al (2019) The mechanisms of a loess landslide triggered by diversion-based irrigation: a case study of the South Jingyang Platform, China. Bull Eng Geol Environ 78:4945–4963

    Article  Google Scholar 

  • Peng D (2018) Study on early recognition for potentially loess landslide—a case study at Heifangtai Terrace, Gansu Province, China. Chengdu University of Technology, Chengdu

    Google Scholar 

  • Seed HB, Idriss IM, Zhang Z (1988) Ground motion and liquefaction of earth in an earthquake. Seismological Press, Beijing

    Google Scholar 

  • Sun Y, Sun J, Zhu J et al (2016) Laboratory tests on the unified response mechanism of unsaturated and saturated loess under dynamic loadings. Chin J Lanzhou Univ Nat Sci 52(5):577–586 (in Chinese)

    Google Scholar 

  • Tsukamoto Y, Kawabe S, Matsumoto J et al (2014) Cyclic resistance of two unsaturated silty sands against soil liquefaction. Soils Found 54(6):1094–1103

    Article  Google Scholar 

  • Unno T, Kazama M et al (2008) Liquefaction of unsaturated sand considering gas pressure and volume compressibility of the soil particle skeleton. Soils Found 48(1):87–99

    Article  Google Scholar 

  • Wang L, Liu H, Li L et al (2000) Laboratory study on the mechanism and behebiors of saturated loess liquefaction. Chin J Geotech Eng 22(1):89–94 (in Chinese)

    Google Scholar 

  • Wang L, Shi Y, Liu X et al (2003) Loess dynamics. Seismological Press, Beijing

    Google Scholar 

  • Wu B, Sun D (2013) Study of liquefaction characteristics of unsaturated silt. Rock Soil Mech 02:411–416 (in Chinese)

    Google Scholar 

  • Wang L, Liu K, Sun J et al (2015) Shaking table tests on basic characteristics of saturated undisturbed loess liquefaction. J Seismic Eng 37(4):1023–1028 (in Chinese)

    Google Scholar 

  • Xin P, Liang C, Wu S et al (2016) Kinematic characteristics and dynamic mechanisms of large-scale landslides in a loess plateau: a case study for the north bank of the Baoji stream segment of the Wei River, China. Bull Eng Geol Environ 75:659–671

    Article  Google Scholar 

  • Yuan X, Xu Q, Zhu X et al (2018) Deformation characteristics and formation mechanism of static liquefaction No. 8 loess landslide in Chenjia, Heifangtai, Gansu Province. Geol Sci Technol Inform 37(5):234–239 (in Chinese)

    Google Scholar 

  • Zhang D, Takeuchi A, Sassa K (1995) The motion characteristics of loess landslides induced by the Haiyuan Earthquake in Ningxia Province, China. J Jpn Landslide Soc 32(1):12–17 (in Japanese)

    Article  Google Scholar 

  • Zhang D, Wang G (2007) Study of the 1920 Haiyuan Earthquake-induced landslides in loess (China). Eng Geol 94(1):76–88

    Article  Google Scholar 

  • Zhang M, Li T (2011) Study on the inducing factors of loess landslide and its formation mechanism. J Eng Geol 19(04):530–540 (in Chinese)

    Google Scholar 

  • Zhang X (2015) Experimental study on the formation mechanism of low-angle loess landslides induced by earthquake in Shibeiyuan. Chengdu University of Technology, Chengdu

    Google Scholar 

  • Zhuang Y, Xing A, Cheng Q et al (2020) Characteristics and numerical modeling of a catastrophic loess flow slide triggered by the 2013 Minxian–Zhangxian earthquake in Yongguang village, Minxian, Gansu, China. Bull Eng Geol Environ 79:439–449

    Article  Google Scholar 

Download references

Acknowledgements

The authors particularly appreciate the valuable comments made by the editors and reviewers to make a substantial improvement to this manuscript. We thank Liwen Bianji, Edanz Editing China (www.liwenbianji.cn/ac), for editing the English text of a draft of this manuscript.

Funding

This project was partially supported by the National Science Fund for Distinguished Young Scholars of China (grant no. 41702335), the National Key Research and Development Program of China (2018YFC1504702), and the Major Program of the National Natural Science Foundation of China (grant no. 41790445).

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Correspondence to Lijuan Song.

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Highlights

1. The fluidization failure of unsaturated loess with high water content was investigated.

2. The dynamic responses of unsaturated loess were investigated during fluidization failure.

3. A theoretical model applicable to the fluidization of unsaturated loess was investigated.

4. A theoretical fluidization evaluation method of unsaturated loess is proposed.

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Zhang, X., Pei, X., Zhang, Z. et al. Study on pore pressure and fluidization evaluation method of unsaturated loess in vibration process. Bull Eng Geol Environ 80, 5575–5587 (2021). https://doi.org/10.1007/s10064-021-02216-3

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  • DOI: https://doi.org/10.1007/s10064-021-02216-3

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