CT provides a possibility for both non-destructive and continuous measurement of materials(rocks and soil etc)and quantitative description of internal structures. In this paper, CT is used to monitor and analyze the change of structures in frozen soil in uniaxial creep process. It is found that the strengthening and softening actions of structures in frozen soil are controlled by the initiation and growth of structural defefcts, which govern the characteristics of creep process. The breaking appears firstly in the weakened area with low density with-in the sample. Aring-like zone with low density is found in a weakened layer within the sample and then extends outwards to result in integral failure of the structure at last.
Wu Ziwang, Ma Wei, Pu Yibin, Chang Xiaoxiao.
Monitoring the Change of Structures in Frozen Soil in Uniaxial Creep Process by CT[J]. Journal of Glaciology and Geocryology, 1996, 18(4): 306-311 https://doi.org/10.7522/j.issn.1000-0240.1996.0045
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