Reports by Joshua Heitman
Effect of a Subsurface Hydrophobic Layer on the Upward Movement of Water in Response to Surface Freezing Conditions.
Estimation of Bare-Soil Evaporation Using a Calorimetric Approach with Heat Flux Measured at Multiple Depths.
Soil Water Retention Curves of Two Wettable Soils and Their Matched Hydrophobized Counterparts.