Seasonal Soil Freezing Characters in Daxinganling

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Abstract:

For understanding the transport of groundwater existing in the seasonal freezing soil,laboratory test and field monitoring (frozen depth、moisture content and ground temperature in five months) were carried out in Daxinganling. A translocation model is built to analyze water behavior. The result shows that thermal conductivity will increase approximately one percent when temperature decreases 1°C. A transition function is used to prevent non-convergence in the numerical simulation. The simulation proves that the modified numerical simulation can reveal the law of moisture and heat translocation, and further offer guidance in practice.

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Advanced Materials Research (Volumes 652-654)

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1668-1672

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January 2013

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© 2013 Trans Tech Publications Ltd. All Rights Reserved

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[1] Jones P D, Wigley T M and Wright P B. Nature, Vol. 322(1986), p.430–434.

Google Scholar

[2] Anisimov O A, Nelson F E. Global Planet Change, Vol. 14(1996), p.59–72.

Google Scholar

[3] H. J. Jin, Q .H. Yu, L .Z. Lv. Permafrost Periglac Process, Vol. 18(2007), p.245–258.

Google Scholar

[4] Z. Wei, H. J. Jin, et al. In: Proceeding of 9th International Conference on Permafrost(2008), p.1939–(1944).

Google Scholar

[5] Y .J. Ding. In: Proceeding of 7th International Permafrost Conference (1998), p.225–230.

Google Scholar

[6] Nekrasov I A, Klimovskii I V. Science Press (Siberia Branch), (1978).

Google Scholar

[7] Keller F. Permafrost Periglac Process, Vol. 3(1992), p.139–142.

Google Scholar

[8] X. Li , et al. Cold Reg Sci Technol, Vol. 36(2003), p.1–9.

Google Scholar

[9] S. Q. An , et al. Ambio, Vol. 36(2007), p.335–342.

Google Scholar

[10] S. Q. Zhang , et al. Wetlands, Vol. 29 (2009), p.302–313.

Google Scholar