ZHANG Xiang-dong, FU Qiang. Experimental study of triaxial creep properties of frozen soil and thickness determination of flat frozen soil wall[J]. 2011, 32(8).
ZHANG Xiang-dong, FU Qiang. Experimental study of triaxial creep properties of frozen soil and thickness determination of flat frozen soil wall[J]. 2011, 32(8).DOI:
In order to determine the thickness of flat frozen soil wall with evident rheological properties
the triaxial creep properties of frozen soil are analyzed. Through theoretical analysis of rheological properties of frozen soil
the logarithmic creep equation of frozen clay is established under complex stress state. The triaxial creep tests for manual prepared frozen clay specimens are carried out by “cold box-triaxial pressure chamber” light test equipment system; so that the creep curves of frozen clay under complex stress state are obtained. According to the test results
the logarithmic creep equation parameters of frozen clay are obtained through regression analysis of logarithmical nonlinear creep equation. According to the rheological theory of frozen soil and the established creep equation
as well as the thickness formula of flat frozen soil wall
through adopting Visualc++ 6.0 and Matlab 6.0
the computer application software is exploited which can calculate thickness of frozen clay wall. With the software
the relationships between the thickness and the span
the pit exposure time
and the pit excavation depth are analyzed. The thickness of flat frozen soil wall possesses rapid growth trend with time extension in the short term and then gradually becomes stable. The thickness of flat frozen soil wall is affected lightly by the span; but it possesses gradual upward trend with the increasing of excavation depth of pit. The temperature affects the thickness of flat frozen soil wall significantly; the higher the temperature is
the larger the thickness is. Consequently
controlling the temperature is the key to the design of flat frozen soil wall. Thus
the results provide a basis for thickness determination of flat frozen soil wall with a large creep deformation.