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A computational model of water migration flux of fine porous soil in frost heave was investigated in a closed system. The model was established with the heat-mass conservation law and from some previous experimental results. Through defining an auxiliary function an empirical function in the water migration flux, which is difficult to get, was replaced. The data needed are about the water content along the soil column after test with enough long time. We adopt the test data of sample soil columns in [1] to verify the model. The result shows it can reflect the real situation on the whole.