UNSAT-H Version 3.0:Unsaturated Soil Water and Heat Flow Model: Theory, User Manual, and Examples

Fayer, Michael J.

Pacific Northwest National Laboratory (U.S.)

关键词: Heat Flux;    Diffusion;    Transpiration;    Water Influx;    Evaporation;   

DOI  :  10.2172/15001068
RP-ID  :  PNNL-13249
RP-ID  :  AC05-76RL01830
RP-ID  :  15001068

美国|英语

来源: UNT Digital Library

【 摘 要 】

The UNSAT-H model was developed at Pacific Northwest National Laboratory (PNNL) to assess the water dynamics of arid sites and, in particular, estimate recharge fluxes for scenarios pertinent to waste disposal facilities. To achieve the above goals for assessing water dynamics and estimating recharge rates, the UNSAT-H addresses soil water infiltration, redistribution, evaporation, plant transpiration, deep drainage, and soil heat flow. The UNSAT-H model simulates liquid water flow using the Richards equation, water vapor diffusion using Fick's law, and sensible heat flow using the Fourier equation. This report documents UNSAT-H Version 3.0. The report includes the bases for the conceptual model and its numerical implementation, benchmark test cases, example simulations involving layered soils and plants, and the code manual. Version 3.0 is an enhanced-capability update of UNSAT-H Version 2.0 (Fayer Jones 1990). New features include hysteresis, an iterative solution of head and temperature, an energy balance check, the modified Picard solution technique, additional hydraulic functions, multiple year simulation capability, and general enhancements. This report includes eight example problems. The first four are verification tests of UNSAT-H capabilities. The second four example problems are demonstrations of real-world situations.