JA Vrugt, PH Stauffer, T Wohling… - Vadose zone …, 2008 - pubs.geoscienceworld.org
Many of the parameters in subsurface flow and transport models cannot be estimated directly at the scale of interest, but can only be derived through inverse modeling. During this …
ABSTRACT Šimůnek, J., M. Th. van Genuchten, and M. Šejna, The HYDRUS Software Package for Simulating Two-and Three Dimensional Movement of Water, Heat, and Multiple …
A complete treatment of the theory and practice of groundwater engineering, The Handbook of Groundwater Engineering, Second Edition provides a current and detailed review of how …
HJ Vogel, K Roth - Advances in water resources, 2001 - Elsevier
Pore-network models are attractive to relate pore geometry and transport processes in soil. In this contribution amorphological path'is presented to generate a network model based on …
Tension disc infiltrometers are becoming increasingly popular devices for in situ measurement of the unsaturated hydraulic properties of soil. Tension infiltration data are …
JG Kroes, JC Van Dam, P Groenendijk, RFA Hendriks… - 2009 - library.wur.nl
SWAP 3.2 simulates transport of water, solutes and heat in the vadose zone. It describes a domain from the top of canopy into the groundwater which may be in interaction with a …
The calculation of the relative hydraulic conductivity function based on water retention data is an attractive and widely used approach, since direct measurements of unsaturated …
This chapter introduces the reader to the theory and applications of inverse modeling for parameter estimation of soil hydraulic functions, using various proven experimental …
A Wayllace, N Lu - Geotechnical Testing Journal, 2012 - asmedigitalcollection.asme.org
A transient water release and imbibitions (TWRI) method for measuring the soil water retention curve (SWRC) and hydraulic conductivity function (HCF) under drying and wetting …