Impact of Moisture Migration on Thermal Resistivity Testing in Unsaturated Soil

Author(s):  
N. R. Woodward ◽  
J. M. Tinjum
2011 ◽  
Vol 261-263 ◽  
pp. 1773-1777
Author(s):  
Ying Cui ◽  
Lin Chang Miao

The coefficient of permeability of unsaturated soil is an important parameter which is used to analyze moisture migration. For complexity and diversity of unsaturated soil behaviors, it is difficult to perform test of unsaturated soil because of many factors. With GDS system, the permeability characteristics of unsaturated soil are tested and studied in this paper which makes it possible to directly measure the coefficient of permeability at various combinations of net normal stresses and matric suction values. The research shows the coefficient of permeability of unsaturated soil is the function of suction and cell pressure.


2013 ◽  
Vol 36 (6) ◽  
pp. 20120151 ◽  
Author(s):  
Nikki R. Woodward ◽  
James M. Tinjum ◽  
Ray Wu

Open Physics ◽  
2018 ◽  
Vol 16 (1) ◽  
pp. 75-83 ◽  
Author(s):  
Fei Xu ◽  
Yaning Zhang ◽  
Guangri Jin ◽  
Bingxi Li ◽  
Yong-Song Kim ◽  
...  

Abstract A three-phase model capable of predicting the heat transfer and moisture migration for soil freezing process was developed based on the Shen-Chen model and the mechanisms of heat and mass transfer in unsaturated soil freezing. The pre-melted film was taken into consideration, and the relationship between film thickness and soil temperature was used to calculate the liquid water fraction in both frozen zone and freezing fringe. The force that causes the moisture migration was calculated by the sum of several interactive forces and the suction in the pre-melted film was regarded as an interactive force between ice and water. Two kinds of resistance were regarded as a kind of body force related to the water films between the ice grains and soil grains, and a block force instead of gravity was introduced to keep balance with gravity before soil freezing. Lattice Boltzmann method was used in the simulation, and the input variables for the simulation included the size of computational domain, obstacle fraction, liquid water fraction, air fraction and soil porosity. The model is capable of predicting the water content distribution along soil depth and variations in water content and temperature during soil freezing process.


1997 ◽  
Author(s):  
Leonard W. Lion ◽  
Brent Alspach ◽  
Jason Gilbert ◽  
Sean Lorden

Crop Science ◽  
1981 ◽  
Vol 21 (5) ◽  
pp. 791-793 ◽  
Author(s):  
R. W. Yaklich ◽  
P. B. Cregan
Keyword(s):  

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