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Multidimensional Flow and Transport in a Drained, Dual-Porosity Soil
Published by the American Society of Agricultural and Biological Engineers, St. Joseph, Michigan www.asabe.orgCitation: Pp. 241-244 in Preferential Flow, Water Movement and Chemical Transport in the Environment, Proc. 2nd Int. Symp. (3-5 January 2001, Honolulu, Hawaii, USA), eds. D. D. Bosch and K. W. King. St. Joseph, Michigan: ASAE 701P0006.(doi:10.13031/2013.2140)
Authors: G.A.P.H. van den Eertwegh, J.L. Nieber, and R.A. Feddes
Keywords: preferential flow and solute transport, dual-porosity soil, computer modeling
Preferential flow of water and transport of solutes in a drained, dual-porosity soil, occurs due to macropores present in a ripened and structured clay field soil. Concentrations of the stable, natural isotope