Computation method for frost heaving characteristic for deep seasonal frozen ground subgrade
A technology of deep seasonality and calculation methods, applied in calculation, special data processing applications, instruments, etc., can solve problems such as lack of guiding significance and insufficient micro-mechanism research, and achieve the effect of stable quality
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[0008] The present invention will be described in detail below in conjunction with examples.
[0009] The frost heave of the soil is caused by the freezing volume expansion of some water in the original pores of the soil when the soil temperature drops below the freezing point, and more importantly, the migration and accumulation of water in the unfrozen area to the freezing front under the action of the soil water potential gradient. And freeze, caused by volume expansion. The ratio of frost heave amount to the thickness of the frozen soil layer is often used as the characteristic value of soil frost heave deformation, that is, the frost heave rate η (or frost heave strength, frost heave coefficient), expressed in percentage.
[0010] η = Δh h × 100 ( % )
[0011] In the formula: h—thickness of frozen soil, mm;
[0012] △h—Incremental va...
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