Thawing settlement deformation is one of the main freezing damage for the structure in permafrost region. The actual thawing settlement is the superposition of two parts: thaw settlement and compression settlement. The volume compression coefficient is the key calculation parameter in estimating the compression deformation. Basing on the 286 thawing compression test data of undisturbed frozen soil samples
it has put forward various types of regression equations including linear equation
binomial equation and logarithmic equation and these equations represent the relationship of volume compressibility and dry density of six sorts of soil on the two different pressure sections 0−100 kPa and 0−200 kPa. These soil types are fine gravel
sand
silt
clay
peaty clay and peat. On this basis the empirical volume compression data table of the six sorts of soils is given out; meanwhile
the problems in recommended methods of specifications are pointed out.
Experiment study of fractal feature and relationship between fractal dimension and permeability coefficient of gravelly soil in debris flow source area
Research on thermal parameters of different earthen monument soils
Research on dynamic compaction characteristics of aeolian sand in desert region of Keerqin
Experimental research on shear strength characteristics of dispersive clay
Test on soil-water characteristic curves of bentonite-sand mixtures
Related Author
HE Na
CHEN Ning-sheng
ZHU Yun-hua
YANG Jian-yuan
YANG Cheng-lin
ZHANG Hu-yuan
ZHANG Xue-chao
CHEN Xiao-ning
Related Institution
East China Construction Engineering Corporation of Zhejiang
School of Civil Engineering,Henan Polytechnic University
University of Chinese Academy of Sciences
Key Laboratory of Mountain Hazards and Surface Process, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences and Ministry of Water Resources
School of Civil Engineering and Mechanics, Lanzhou University