GFLOW 2000®
is an analytic element code that belongs in the arsenal of commonly used groundwater
modeling tools. It solves groundwater flow problems by superimposing analytic
solutions under Dupuit-Forchheimer assumptions. In its most simple dress the
code facilitates rapid construction and solution of a steady-state single-layer
groundwater model containing multiple recharge and transmissivity zones with
complicated internal boundary conditions. However, one of its most innovative
aspects is its ability to perform conjunctive surface water/groundwater modeling.
GFLOW 2000® uses
stream networks to route baseflow so that available streamflow responds to stresses
such as pumping, an option that is particularly useful in determining the effect
of wells on the headwaters of streams. It has several ways of simulating the
interaction of groundwater with lakes, including the ability to perform detailed
water balances in the presence of through-flowing streams, a capacity not yet
available in other analytic element codes or MODFLOW2000. Together these options
make it particularly useful in modeling unconfined flow in terrains (e.g. glacial)
with closely spaced surface-water bodies. A second innovation of the code is
to facilitate use of the "stepwise" modeling approach. Often Dupuit-Forchheimer
assumptions are more valid for regional flow problems than for site-specific
problems where vertical head gradients are important. To allow the speed of
analytic elements to be mated with the flexibility of finite-differences, GFLOW
2000®
supports automatic conversion of part of its domain to a local MODFLOW model
with flux or constant head boundary conditions around the inset grid. Once the
conversion is made, the user can add more complexity to geometry and properties
inside the MODFLOW model. Another advanced feature of the code is particle tracking
that takes advantage of mass balance considerations to simulate flow lines from
the water table below a stream to a well. There are "tricks" that
are needed to most effectively perform analytic element modeling; the ample
HELP material introduces the user to the technique's special vocabulary (e.g.,
"linesinks") and also provides a general guide to modeling, which
makes the code a first-rate teaching tool. The GUI, compatible with all versions
of Windowsâ, is workmanlike with excellent visualization tools related
to surface water and calibration. A lot of thought has gone into converting
readily available maps such as USGS coverages into base maps. GFLOW 2000®
is available for $450 from: www.haitjema.com.
|
Rating
System |
|||
|
Ease
of Use
|
5
|
GUI
|
4
|
|
Application
|
5
|
Output/Plotting
|
4
|
|
Documentation
|
5
|
Best
Feature
|
GW/SW
interactions
|
|
Speed
|
4
|
Worst
Feature
|
Editing
linesinks
|
|
Overall
Rating
|
5
|
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Last Update: February, 2004