Abstract
A multiphysics mathematical model of high‐speed railway (HSR) roadbeds is necessary to facilitate a good level of understanding of the frost heaving mechanism. Based on the classical hydrodynamic model and fundamental thermoelasticity theories, we propose a thermo‐hydro coupled model, based on the soil‐water characteristic curve and solid‐liquid ratio as the relation equations, with the effects of the ice‐water phase change and water migration due to temperature change considered. With the linear expansion coefficient related to the temperature and the mass of ice content in roadbeds as the relation equation, we establish a macroscopic thermal‐hydro‐mechanical model for unsaturated soil to calculate the roadbed deformations. Based upon the field data of a typical cross section of the Harbin‐Dalian HSR roadbed, the variation of the thermal‐hydro‐mechanical characteristics is simulated and studied. The results demonstrate that the increase of water content in the roadbed’s central line mainly appears in soil layers at depths less than 1.2 m and most ice‐containing soil layers are at depths less than 0.6 m. Under the driving force of thermal and hydraulic migration, the vertical displacement of the west shoulder is increased to 18 mm. Then the settled maximum surface unevenness reaches 16 mm between the shoulder and centre line.
Highlights
A multiphysics mathematical model of high-speed railway (HSR) roadbeds is necessary to facilitate a good level of understanding of the frost heaving mechanism
Based upon the field data of a typical cross section of the Harbin-Dalian HSR roadbed, the variation of the thermal-hydro-mechanical characteristics is simulated and studied. e results demonstrate that the increase of water content in the roadbed’s central line mainly appears in soil layers at depths less than 1.2 m and most ice-containing soil layers are at depths less than 0.6 m
The mechanism of freezethaw deformations in roadbeds is most often studied inside a laboratory by considering the frost heaving behaviour of unsaturated coarse-grained soil with respect to macroscopic factors such as particle size and grade [3, 4], but the heat and water migration in HSR roadbeds and the variation of their thermal-hydro-mechanical characteristics have seldom been studied
Summary
A multiphysics mathematical model of high-speed railway (HSR) roadbeds is necessary to facilitate a good level of understanding of the frost heaving mechanism. The mechanism of freezethaw deformations in roadbeds is most often studied inside a laboratory by considering the frost heaving behaviour of unsaturated coarse-grained soil with respect to macroscopic factors such as particle size and grade [3, 4], but the heat and water migration in HSR roadbeds and the variation of their thermal-hydro-mechanical characteristics have seldom been studied. Previous studies explored moisture migration, frost heaving mechanism, and frost heaving variation of frozen soils in different ways, but most of the existing calculation models have only been verified through laboratory tests Few of these consider the variation of the thermal-hydro-mechanical characteristics of HSR roadbeds in seasonally frozen regions, especially those with sunny-shady slopes
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