Gas diffusion ratio in the soil in compare to diffusion in the atmosphere (DP/D0) and air permeability in the soil (Ka) is a function of soil physical characteristic, including pore size, continuity and air porosity.The results showed that with increase in soil moisture and Se, DP/D0 and Ka decreased as a logarithmic function. Maximum and minimum value are obtained, at low and high humidity (near saturation), respectively
mohamadi, P. (2013). Comparison Of Methods To Estimate The Oxygen Diffusion Ratio And Air Permeability By Using The Effective Saturated And Soil Moisture. Water and Soil, 27(5), 1023-1033. doi: 10.22067/jsw.v0i0.20431
MLA
panah mohamadi. "Comparison Of Methods To Estimate The Oxygen Diffusion Ratio And Air Permeability By Using The Effective Saturated And Soil Moisture". Water and Soil, 27, 5, 2013, 1023-1033. doi: 10.22067/jsw.v0i0.20431
HARVARD
mohamadi, P. (2013). 'Comparison Of Methods To Estimate The Oxygen Diffusion Ratio And Air Permeability By Using The Effective Saturated And Soil Moisture', Water and Soil, 27(5), pp. 1023-1033. doi: 10.22067/jsw.v0i0.20431
VANCOUVER
mohamadi, P. Comparison Of Methods To Estimate The Oxygen Diffusion Ratio And Air Permeability By Using The Effective Saturated And Soil Moisture. Water and Soil, 2013; 27(5): 1023-1033. doi: 10.22067/jsw.v0i0.20431
)
Send comment about this article