Experimental Study on Compression Characteristics of Soft Soil Based on Temperature Effect
Abstract
Based on the characteristics of long annual freezing time and short suitable construction period of soft soil in cold region, the feasibility of foundation treatment of soft soil in freezing-thawing layer under freezing condition is discussed. The deformation characteristics of soft soil in freezing-thawing layer in HulunBuir area are studied by using two compression test methods of constant temperature and variable temperature and variable load, and the compressibility indexes under different temperatures and consolidation pressures are obtained. The test results show that the frozen-thawed soft soil has great compressibility, the maximum strain of constant temperature and variable load test is 19.89%, and the maximum compression of variable temperature and variable load test can reach 18.16%. The results of both constant temperature and variable temperature compression tests show that when the soil temperature is in the region of severe phase change (-1.5°C-0°C), the temperature change has the greatest influence on the compression coefficient of soil. The results of compression tests under variable temperature and load show that there will be some additional deformation under the action of temperature. When the soil is in a high consolidation pressure and the temperature is in the temperature transition zone (-1.5°C-0°C), the additional deformation is larger.References
Bhatt, U. S., Walker, D. A., Raynolds, M. K., et al, 2010. Circumpolar arctic tundra vegetation change is linked to sea ice decline. Earth Interactions. 14(8):1-20.
Cai L.Z, 2015. Study on creep test of sand powder soil with high temperature and ice content in Qinghai-Tibet. Harbin Institute of Technology.
Cheng G.D., Ma W., 2006. Problems of permafrost engineering in Qinghai-Tibet railway construction. Chinese Journal of Nature. 6:315-320.
Harrison, W.D., 1991. Permafrost response to surface temperature change and its implications for the 40,000-year surface temperature history at Prudhoe Bay, Alaska. Journal of Geophysical Research Atmospheres. 96(B1): 683-695.
Johannessen, O.M., 1999. Satellite Evidence for an Arctic Sea Ice Cover in Transformation. J.Science. 286(5446):1937-1939.
Liu S.W., Zhang J.M., Zhang H., et al, 2011. Preliminary study on pore water pressure force measurement in high temperature permafrost. Journal of Gansu Agricultural University. 46:155-160.
Ma W., Wang D.Y, 2014. Frozen soil mechanics. Beijing, Science Press.
Ruan G.F.; Zhang J.M., Liu S.W., et al, 2014. Compression experimental research on warm and ice-rich permafrost on the Qinghai-Tibet Plateau. Hydrogeology & Engineering Geology. 2:50-56.
Screen, J.A., Simmonds, I.,2010. The central role of diminishing sea ice in recent Arctic temperature amplification. Nature, 464(7293):1334-1337.
Shim, T., Jeong, J.,Kim, B.,Kim, S., et al, 2013. Development of Dynamical Seasonal Prediction System for Northern Winter using the Cryospheric Condition of Late Autumn. Atmosphere. 23(1):73–83.
Shim, T., Jeong, J., Ok, J., Jeong, H., et al, 2015. Development and Assessment of Dynamical Seasonal Forecast System Using the Cryospheric Variables. Atmosphere. 25(1):155–167.
Su K., Zhang J.M., Liu S.W., et al, 2013. Compressibility of warm and ice-rich frozen soil. Journal of Glaciology and Geocryology. 2:369-375.
Tsytovich, N.A.,1975. The mechanics of frozen ground. Scripta Book Company, Washington, D.C.
Pachauri, R.K.; Reisinger, A., 2007. Climate Change 2007: Synthesis Report. Environmental Policy Collection. 27(2):408.
Phukan A, 1983. Long-term creep deformation of roadway embankment on ice-rich permafrost[C]// Proceedings of the 4th International Conference on Permafrost, National Academy Press.994-999.
Yang Z.H., Still B., Ge X.X., 2015. Mechanical properties of seasonally frozen and permafrost soils at high strain rate. Cold Regions Science and Technology, 113:12-19.
Yao X.L., Qi J.L., Zhang J.M., et al, 2018. A one-dimensional creep model for frozen soils taking temperature as an independent variable. Soils and Foundations. S0038080618300374.
Yu W.X., Yan W.P,1986. Preliminary analysis of freeze-thaw deformation of subgrade in permafrost area of Qinghai-Tibet Highway. Journal of Chang an University(Natural Science Edition). 6:49-70.
Zheng B.; Zhang J.M., Ma X.J., et al, 2009. Study on compression deformation of warm and ice-enriched frozen soil. Chinese Journal of Rock Mechanics and Engineering. (S1):3063-3069.
Zhu Y.L., Zhang J.Y., 1982. Elastic deformation and compression deformation of permafrost. Journal of Glaciology and Geocryology. 3:29-39.
Zimov, S.A., Schuur, E.A.G., Chapin, F.S, 2006. Permafrost and the Global Carbon Budget. Science. 312(5780):1612-1613.