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RISEffect of hydrophobicity on colloid transport during two phase flow in a micromodel
ناشر: American Geophysical Union
سال: 2014
The role of contact angle on unstable flow formation during infiltration and drainage in wettable porous media
ناشر: American Geophysical Union
سال: 2013
Evaporation from porous surfaces into turbulent airflows: Coupling eddy characteristics with pore scale vapor diffusion
ناشر: American Geophysical Union
سال: 2013
Lithologic influences on groundwater recharge through incised glacial till from profile to regional scales: Evidence from glaciated Eastern Nebraska
ناشر: American Geophysical Union
سال: 2014
Comparison of simulated water, nitrate, and bromide transport using a Hooghoudt based and a dynamic drainage model
ناشر: American Geophysical Union
سال: 2014
Reply to comment by S. Iden and W. Durner on “Simple consistent models for water retention and hydraulic conductivity in the complete moisture rangeâ€
ناشر: American Geophysical Union
سال: 2014
Imaging and quantification of preferential solute transport in soil macropores
ناشر: American Geophysical Union
سال: 2014
Capillary pressure overshoot for unstable wetting fronts is explained by Hoffman\'s velocity dependent contact angle relationship
ناشر: American Geophysical Union
سال: 2014
Modeling biofilm dynamics and hydraulic properties in variably saturated soils using a channel network model
ناشر: American Geophysical Union
سال: 2014
Moisture profiles of the upper soil layer during evaporation monitored by NMR
ناشر: American Geophysical Union
سال: 2014