Fig. 12

Pearson’s correlation and significance between temperature and the strength of frozen silty clay in the Xing’an Baikal permafrost region (Temp: temperature; CS: compression strength; ITM: initial tangent modulus; SM: secant modulus).
Pearson’s correlation and significance between temperature and the strength of frozen silty clay in the Xing’an Baikal permafrost region (Temp: temperature; CS: compression strength; ITM: initial tangent modulus; SM: secant modulus).