Air-tough: A fully 3-dimensional linking of atmosphere with soil using eddy diffusivity concept and V-TOUGH
Abstract
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.
- Authors:
-
- Multimedia Environmental Technology, Inc., Newport Beach, CA (United States)
- Publication Date:
- OSTI Identifier:
- 127125
- Report Number(s):
- CONF-9504179-
TRN: 96:004766
- Resource Type:
- Conference
- Resource Relation:
- Conference: 6. annual international conference on high level radioactive waste management, Las Vegas, NV (United States), 30 Apr - 5 May 1995; Other Information: PBD: 1995; Related Information: Is Part Of High level radioactive waste management: Proceedings; PB: 811 p.
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 05 NUCLEAR FUELS; 58 GEOSCIENCES; 54 ENVIRONMENTAL SCIENCES; AIR-BIOSPHERE INTERACTIONS; A CODES; FLUID FLOW; SOILS; HIGH-LEVEL RADIOACTIVE WASTES; RADIOACTIVE WASTE DISPOSAL; LOW-LEVEL RADIOACTIVE WASTES; RADIOACTIVE WASTE FACILITIES; UNDERGROUND FACILITIES; ARID LANDS
Citation Formats
Montazer, P. Air-tough: A fully 3-dimensional linking of atmosphere with soil using eddy diffusivity concept and V-TOUGH. United States: N. p., 1995.
Web.
Montazer, P. Air-tough: A fully 3-dimensional linking of atmosphere with soil using eddy diffusivity concept and V-TOUGH. United States.
Montazer, P. 1995.
"Air-tough: A fully 3-dimensional linking of atmosphere with soil using eddy diffusivity concept and V-TOUGH". United States.
@article{osti_127125,
title = {Air-tough: A fully 3-dimensional linking of atmosphere with soil using eddy diffusivity concept and V-TOUGH},
author = {Montazer, P},
abstractNote = {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.},
doi = {},
url = {https://www.osti.gov/biblio/127125},
journal = {},
number = ,
volume = ,
place = {United States},
year = {Fri Dec 01 00:00:00 EST 1995},
month = {Fri Dec 01 00:00:00 EST 1995}
}