SOLUTRANS
SOLUTRANS is a 32-bit
Windows program for modeling three-dimensional solute
transport based on the the most sophisticated analytic solutions
available. The solutions are those presented
by Leij et. al. (1991) and Leij et. al. (1993).
The interface and input
requirements are so simple that it only takes a few
minutes to develop models and build insight about complex
solute transport problems. With
SOLUTRANS you can, in a matter of minutes, model solute
transport from a variety of source configurations and
build important insights about key processes. SOLUTRANS
offers a quick and simple alternative to complex,
time-consuming three 3-D numerical flow and transport
models.

This is a model of
two superpositioned parallelipiped initial source
volumes with non-equilibrium sorption. The source
areas retain significant non-equilibrium mass, and
are visible at the left side of the plume. This is a
plot of concentration on the plane z=0, which cuts
through the initial source volumes.
In the November-December 1999 issue of Ground Water (v.
37, no. 6: pp.808-809) three independent experts reported
on their review of SOLUTRANS. Overall, their rating of SOLUTRANS, on a scale
of 1-5, 5 being best, is a follows:
Capability 4, Reliability 4.5,
Ease-of-Use 4, Technical support 5
Here are some excerpts
of their review:
"The software provides for
rapid assessment of a variety of solute transport
scenarios. It is stable. It doesnt take long to
learn. It produces reasonable graphics. Overall,
Solutrans is a good package for analytical solutions
to solute transport problems."
"Solutrans provided rapid
solutions to transport problems. Users with previous
TWODAN experience will recognize and be comfortable
with the interface. Otherwise, the learning curve is
on the order of hours and is greatly aided by the
many included solutions. Input data are readily
modified for sensitivity and scenario analyses."
"We liked the availability of
the nonequilibrium (kinetic) solutions. Also, the
linear equilibrium degradation could prove useful in
trying to assess "natural remediation."
Solutrans allows the user to simulate a degrading
source by specifying it in time steps. One reviewer
found this particular capability to be the best of
any of the analytical models he has tried."
The solutions in
SOLUTRANS all assume a uniform one-dimensional flow field
in the positive x direction. There is three-dimensional
dispersion, with different coefficients allowed in all
three directions. One set of solutions assumes
equilibrium in the solute and adsorbed phases (Leij et.
al., 1991), while another set of solutions allows
non-equilibrium (kinetic) conditions (Leij et. al.,
1993).
With the non-equilibrium solutions, the
solute may be out of equilibrium with some of the
adsorption sites. van Genuchten and Wagenet (1989) and
Leij et. al. (1993) describe two common ways of
conceptualizing non-equilibrium transport; a ``two-site''
concept and a ``two-region'' concept. Both concepts lead
to similar partial differential equations that are, in
fact, written as a common dimensionless partial
differential equation. In the two-site concept, some
fraction of adsorption sites are at equilibrium while
other sites are not. At the non-equilibrium (kinetic)
sites, a first-order rate law governs adsorption. In the
two-region concept, there is mobile pore water and
immobile pore water and both are in equilibrium with the
sorption sites that they are in contact with. Solute
migrates by advection and dispersion in the mobile
region, and first-order diffusion transfers solute mass
from the mobile region to the immobile region (Coats and
Smith, 1964; van Genuchten and Wierenga, 1976).
Separate first-order
decay coefficients may be specified for the equilibrium
and the non-equilibrium phases. The non-equilibrium
models allow you to examine the distribution of
equilibrium (mobile water) concentrations,
non-equilibrium (immobile water) concentrations, and the
total (aqueous + adsorbed) concentration.
Unlike the solutions of Domenico and
Robbins (1985, Groundwater,
v. 23, p. 476.) and Domenico (1987, Jour. Hydrol. v.
91, p. 49), these solutions do not
make approximations that cause errors near the source. These are exact solutions which
involve some numerical integration.
Both the equilibrium
and non-equilibrium solutions allow four different source
geometries:
- rectangular inlet
area
- circular inlet
area
- parallelipiped
(rectangular box) initial volume
- cylindrical
initial volume
The ten solutions
implemented in SOLUTRANS are listed below:
- Rectangular inlet,
equilibrium, steady-state
- Rectangular inlet,
equilibrium
- Rectangular inlet,
non- equilibrium
- Circular inlet,
equilibrium, steady-state
- Circular inlet,
equilibrium
- Circular inlet,
non- equilibrium
- Parallelepiped
initial volume, equilibrium
- Parallelepiped
initial volume, non-equilibrium
- Cylinder initial
volume, equilibrium
- Cylinder initial
volume, non-equilibrium
Using the superposition
features built into SOLUTRANS, it is possible to model
contaminant sources that have irregular distributions in
time and space, as shown here. See the figure above for an
example of source superposition.
All of these solutions
may be used to create simpler two-dimensional,
one-dimensional, and diffusion-only solutions, if needed.
SOLUTRANS has a
seamless, Windows-standard user interface. It has been
designed to be very simple and fast to use. Most common
modeling operations are executed at the push of a button
on the main screen. Mathematical model input data
are accessed directly in a spreadsheet-like grid. Data can be imported and
exported using the Windows Clipboard.
SOLUTRANS can produce
three types of plots: 1) concentrations vs. distance
along a line, 2) concentrations vs. time at a point, and
3) surface plots of concentrations vs. location on a
plane. Press here to see examples of plot types
(1) and (2), and see the above plot for an example of
type (3).
Plots are made on the
screen, and may be exported to the Windows Clipboard or
to disk files in either bitmap (.BMP) or metafile (.WMF)
format. Concentration data may also be exported directly
in comma-delimited ASCII files for use with other
visualization software programs. Data may also be
exported in .GRD format files for surface plotting using
SURFER software.
The following forms of
on-line help are available: tips that automatically
display when you pause over a control, context-sensitive
help (F1 key), and a Windows-standard help file. The help
file is indexed, searchable, printable, and it contains
embedded jumps to related topics.
Documentation
Most of the information
about how to use the software is in the on-line help
system. The SOLUTRANS Manual is a 7 x 9 inch spiral bound
booklet containing the following sections.
- Introduction
- describes the software and how to
install it.
- Tutorial -
step-by-step development and
modification of a SOLUTRANS model, showing
screens as they appear in the process.
- Method
Employed - a detailed section describing
the governing equations and the general nature of
the analytic solutions employed.
- Modeling
Tips - includes advice about parameter
units, computational speeds, superposition, 1-D,
2-D, and diffusion-dominated transport models,
etc.
- Program
Checks - 42 separate checks of the
solutions implemented in SOLUTRANS. The model
input files for the check models are included on
the software diskettes.
- References
System Requirements
- 32-bit Windows
operating system (Windows 95/98/NT as of this
writing)
- 4 MB of hard disk
space
- 8 MB of memory
The commercial
SOLUTRANS license is a typical software license; one
license allows installation on one computer at a time.
The academic license is
a site license available for qualified educational
institutions, and is restricted to academic,
non-commercial purposes.
Purchase of either
license includes unlimited support to make sure that
SOLUTRANS operates properly on your system.
The demo version of
SOLUTRANS is contained in one self-extracting
installation file setupst.exe. This file is about 4 MB in
size, so depending on your system, it may take a while to
download. Download setupst.exe to your hard disk, then
execute this file to setup the software. Instructions for
running the demo version are given during the setup
process. The demo is the same as the full SOLUTRANS
software, except that you are restricted to a fixed model
input.
Click here to download the demo
installation file.
Coats, K. H. and B. D. Smith. 1964.
Dead-end pore volume and dispersion in porous media. Soc.
Petrol. Engr. Jour., v. 4, p. 73-84.
Leij, F. J., T. H. Skaggs, and M. Th.
van Genuchten. 1991. Analytical solutions for solute
transport in three-dimensional semi-infinite porous
media. Water Resources Research, v. 27(10), p. 2719-2733.
Leij, F. J., N. Toride, and M. Th. van
Genuchten. 1993. Analytical solutions for non-equilibrium
solute transport in three-dimensional porous media.
Journal of Hydrology, v. 151, p. 193-228.
Leij, F. J. and S. A. Bradford. 1994.
3DADE: A computer program for evaluating
three-dimensional equilibrium solute transport in porous
media. U. S. Salinity Laboratory Research Report No. 134,
Riverside, California.
Leij, F. J. and N. Toride. 1997.
N3DADE: A computer program for evaluating non-equilibrium
three-dimensional solute transport in porous media. U. S.
Salinity Laboratory Research Report No. 143, Riverside,
California.
van Genuchten, M. Th. and J. C. Parker.
1984. Boundary conditions for displacement experiments
through short laboratory soil columns. Soil Science Soc.
of Am. Jour., v. 48, p. 703-708.
van Genuchten, M. Th. and R. J.
Wagenet. 1989. Two site/two region models for pesticide
transport and degradation: theoretical development and
analytical solutions. Soil Science Soc. of Am. Jour., v.
53, p. 1303-1310.
van Genuchten, M. Th. and P. J.
Wierenga. 1976. Mass transfer studies in sorbing porous
media: 1. analytical solutions. Soil Science Soc. of Am.
Jour., v. 40, p. 473-481.
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