Theoretical Relationship between Saturated Hydraulic Conductivity and Air Permeability under Dry Conditions: Continuum Percolation Theory
The saturated hydraulic conductivity, Ks, is a fundamental characteristic of subsurface flow and the hydrologic cycle. However, direct measurement of Ks is time consuming. Recently, air permeability measurements at 50 and 100 cm of H2O tension, a relatively dry condition in coarse and medium‐texture...
Main Authors: | Behzad Ghanbarian, Allen G. Hunt, Robert P. Ewing, Thomas E. Skinner |
---|---|
Format: | Article |
Language: | English |
Published: |
Wiley
2014-08-01
|
Series: | Vadose Zone Journal |
Online Access: | https://doi.org/10.2136/vzj2014.03.0029 |
Similar Items
-
Predicting Streamflow Elasticity Based on Percolation Theory and Ecological Optimality
by: Allen G. Hunt, et al.
Published: (2023-08-01) -
Robust calibration and evaluation of a percolation-based effective‐medium approximation model for thermal conductivity of unsaturated soils
by: Yongwei Fu, et al.
Published: (2023-10-01) -
The Percolation Properties of Electrical Conductivity and Permeability for Fractal Porous Media
by: He Meng, et al.
Published: (2019-03-01) -
Woody Vegetation Increases Saturated Hydraulic Conductivity in Dry Tropical Nicaragua
by: R.J. Niemeyer, et al.
Published: (2014-01-01) -
Saturation in the hypercube and bootstrap percolation
by: Morrison, N, et al.
Published: (2016)