| Development of an Efficient
Mass and Energy Coupled Transport Simulator for the Vadose Zone |
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Figures illustrate the aggregation
of 1D solutions from BREATH covering a 3km x 5km area over a
potential high-level waste repository (white outline).
The figure on the left depicts distribution of mean annual
shallow infiltration (MAI) estimates in present-day climatic
conditions, and the figure on the right depicts estimates in
cooler and wetter climatic conditions. |
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Southwest Research Institute |
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Sponsor: U.S. Nuclear
Regulatory Commission |
| Principal Investigators:
Stuart Stothoff
and Randall Fedors |
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Program Brief
Statement of Problem: The client
required an efficient, integrated energy and mass transport code capable
of modeling shallow infiltration processes for decade time scales in
arid and semiarid environments for both present-day and future climatic
conditions. Modeling shallow infiltration in arid and semiarid
environments must focus on the short time periods when significant
precipitation occurs. A code to satisfy these needs must (i) efficiently
solve Richards equation for liquid flow, (ii) solve for energy transport
in the liquid and vapor phases, (iii) incorporate efficient
time-stepping algorithms between temporally sparse precipitation events,
and (iv) allow the transpiration algorithm to change with climatic
conditions.
Approach and Accomplishments: The
code BREATH was developed to address this problem. Although BREATH can
be used as a general unsaturated flow simulator for humid environments,
it has features that make it particularly well suited for long-time
simulations of shallow infiltration in arid and semiarid environments.
In arid environments, evaporation and transpiration are important
components of the water balance, with annual potential evapotranspiration
often being greater than annual precipitation; yet, water can still
infiltrate and percolate to the water table, particularly in areas of
thin soils over porous or fractured bedrock. During the sparse
precipitation events, capillary and gravity driven flow requires the use
of a numerical solution of the Richards equation. After a short period
of redistribution, timestep size can be significantly relaxed until the
next precipitation event.
BREATH is a 1-dimensional flow simulator
for coupled heat and moisture flow. The simulator couples the Richards
equation with diffusive vapor transport. Heat flow is modeled as
diffusive flux in the matrix and advective flux in the liquid and vapor
phases. BREATH has a transpiration model that allows for changes in
vegetation, as would be expected for past and future climatic
conditions. The simulator is capable of using constant or finely
resolved temporal meteorological data as an upper boundary condition. A
free drainage condition is also included along with other types for the
lower boundary condition to facilitate modeling of large unsaturated
domains.
Client Benefits: BREATH provides a fast, general purpose tool for modeling unsaturated
heat and moisture flow particularly suited for arid and semiarid
climates. The efficient solution techniques employed by BREATH enable
sensitivity and uncertainty analyses to be performed. |