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Landslides and Moisture-Temperature for Cutting Slope Soil in Freeze-Thaw Cycles

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Abstract

It is the main problem for highway in seasonal frozen regions that soil cutting slope instability causing by freeze-thaw, which affected traffic safety and the environment seriously. Relying on the silty clay slope, which is in the Tong-San highway expansion project from Jiamusi to Harbin, using triaxial shear tests, field monitoring, the mechanism of slope instability causing by freeze-thaw was studied. Triaxial test results show that: when the soil water content is less than the optimum water content, the soil cohesion is increased with the increase of moisture. The soil cohesion is decreased with the increase of moisture, when the soil water content is bigger than the optimum water content. The peak value of soil cohesion is near the optimum water content. The internal friction angle of soil is decreased with the increase of moisture. Soil cohesion is decreased with the increase of times of freeze-thaw cycles. Field monitoring results indicates that, during the process of soil freezing, moisture migrates to the freezing-front. In the melting period of spring, because of the accumulating water within the cracks of temperature shrinkage, and longer duration of zero temperature below the slope surface, the melting water was hampered, as well as the water frozen within the soil body melt rapidly when soil body temperature reaches 0.1 °C, all of these results in the water content in shallow slope is too high, and soil shear strength decreases, then occurs cutting slope landslides.

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References

  • Clark MJ (1988) Advance in periglacial geomorphology. Wiley, New York, pp 325–359

    Google Scholar 

  • Li Y, Zhao K (2002) The analysis of landslide in k2023 of QING-Zang highway. J Geol Hazards Environ Preserv 13(4):33–35

    Google Scholar 

  • Liu H, Wang P (2006) Stability analysis of instability caused by freeze-thaw for highway earthen side slopes. J Harbin Inst Technol 38(5):764–766

    Google Scholar 

  • McRoberts EC, Morgenstern NR (1974) The stability of thawing slopes. Can Geotech J 11:447–469

    Article  Google Scholar 

  • Niu FJ, Cheng GD, Xie Q (2002) Study on instability of slopes in permafrost regions of Qinghai-Tibet High plateau. In: Yakutsk C (ed) Proceedings of the 5th international symposium on permafrost engineering, Permafrost Institute/SB RAS Press, pp 192–197

    Google Scholar 

  • Niu F, Cheng G, Lai Y et al (2004) Instability study on thaw slumping in permafrost regions of Qinghai-Tibet plateau. Chin J Geotech Eng 26(3):402–406

    Google Scholar 

  • Shan W, Guo Y, Liu H (2009) Effect of freeze-thaw on strength and microstructure of silty clay. J Harbin Inst Technol 16(Sup. 1):207–211

    Google Scholar 

  • Tarr RS (1897) Rapidity of weathering and stream erosion in the arctilatitudes. American Geologist 19:131–136

    Google Scholar 

  • Wang B, French HM (1995) In situ creep of frozen soil. Tibet pleateau. China Can Geotech J 32:545–552

    Article  Google Scholar 

  • Wu H, Gao W, Wang G et al (2006) Cause and control of soil-cutting’s sliding collapse in frigid zone. J Nat Disasters 15(3):66–70

    Google Scholar 

  • Zhou Y, Guo D (1982) Principal characteristics of permafrost in China. J Glaciol Geocryol 4:1–19

    Google Scholar 

  • Zhu C, ZhangJ X, Cheng P (1996) Rock glaciers in the central Tianshan Mountain, China. Permafrost Periglac Process 7:69–78

    Article  Google Scholar 

Download references

Acknowledgments

The authors would like to thank the financial supports provided by the research project of Heilongjiang provincial Science and Technology Department (GZ07 C401), and the Key project of Heilongjiang provincial Transportation Department “Highway Slope Stability and Greening by Vegetation in Cold Regions”.

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Correspondence to Ying Guo .

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© 2013 Springer-Verlag Berlin Heidelberg

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Guo, Y., Shan, W., Zhang, C., Sun, Y. (2013). Landslides and Moisture-Temperature for Cutting Slope Soil in Freeze-Thaw Cycles. In: Margottini, C., Canuti, P., Sassa, K. (eds) Landslide Science and Practice. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-31337-0_48

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