Air-tough [electronic resource] : A fully 3-dimensional linking of atmosphere with soil using eddy diffusivity concept and V-TOUGH
Published
Berkeley, Calif. : Lawrence Berkeley National Laboratory, 1995. Oak Ridge, Tenn. : Distributed by the Office of Scientific and Technical Information, U.S. Dept. of Energy
In arid climates, evapotranspiration is a strongly-coupled thermodynamic process that is controlled by the interaction of the atmospheric boundary layer and the upper soil surface. Simulation of this process requires a fully-coupled thermodynamic multi-phase fluid-flow and energy-transport code. Such a code was developed in a previous investigation using V-TOUGH. The resulting efficient computer code, A-TOUGH, simulates the effect of dynamic atmospheric fluctuations on vapor movement between the soil and the atmosphere and the resulting moisture movement in the soil. However, the coupling between the atmosphere and soil employed eddy diffusivity which was only a function of time and not a function of space. In the present study the code is extended to allow spatial as well as temporal variation of eddy diffusivity.
Report Numbers
E 1.99:lbl--37200 E 1.99: conf-9503110-- conf-9503110-- lbl--37200
Published through SciTech Connect. 03/01/1995. "lbl--37200" " conf-9503110--" "DE95014788" TOUGH 95: transport of unsaturated ground water and heat workshop, Berkeley, CA (United States), 20-22 Mar 1995. Montazer, P. [Multimedia Environmental Technology, Inc., Newport Beach, CA (United States)].