Question

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要确定泥岩的未冻水含量，首先要确定其是否达到了饱和含水量。从查到的资料[25-28]看，泥岩的饱和含水量首先取决于泥岩的风化程度，风化程度越高饱和含水量越大。本文中的泥岩均为风化泥岩，其饱和含水量应该是较大的。从岩芯记录来看，大部分没有出现融后出水的现象，可以认为其还未达到饱和。对于5.0～6.4 m的土层，其虚拟的温度—未冻水含量的回归公式为：
(2-12)
对于6.4 m以下的土层，其虚拟的温度—未冻水含量的回归公式为：

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Answer 1

要确定泥岩的未冻水含量，首先要确定其是否达到了饱和含水量。从查到的资料[25-28]看，泥岩的饱和含水量首先取决于泥岩的风化程度，风化程度越高饱和含水量越大。本文中的泥岩均为风化泥岩，其饱和含水量应该是较大的。从岩芯记录来看，大部分没有出现融后出水的现象，可以认为其还未达到饱和。对于5.0～6.4 m的土层，其虚拟的温度—未冻水含量的回归公式为：
(2-12)
对于6.4 m以下的土层，其虚拟的温度—未冻水含量的回归公式为

To confirm the unfrozen water content in the mudstone, we shall firstly check whether it has reached the saturated water content. From the data found [25-28], it can be concluded that the saturated water content in mudstone is primarily determined by the weathering degree of mudstone, the higher the weathering degree is, the greater the water content will be. All the mudstones mentioned in this thesis are the weathered ones with much saturated water content. From the records of the core, no effluent is observed after melting in most of the mudstones which have not reached saturation yet. For soil layer with thickness between 5.0 to 6.4m, the regression formula of virtual temperature - unfrozen water content is:
(2-12)
for soil layer with thickness less than 6.4 m, the regression formula of virtual temperature - unfrozen water content is:

Answer 2

To confirm the unfrozen water content in the mudstone, we shall firstly check whether it has reached the saturated water content. From the data found [25-28], it can be concluded that the saturated water content in mudstone is primarily determined by the weathering degree of mudstone, the higher the weathering degree is, the greater the water content will be. All the mudstones mentioned in this thesis are the weathered ones with much saturated water content. From the records of the core, no effluent is observed after melting in most of the mudstones which have not reached saturation yet. For soil layer with thickness between 5.0 to 6.4m, the regression formula of virtual temperature - unfrozen water content is: (2-12)
for soil layer with thickness less than 6.4 m, the regression formula of virtual temperature - unfrozen water content is: