CONVERT
CONCEPTUAL MODEL TO A MODFLOW CONSTRUCT
Switch from the 3D Grid Module to the Map Module
Select Map->MODFLOW
Confirm that ALL APPLICABLE COVERAGES is SELECTED
OK
Now that we have the grid defined, the final steps remaining before we have a
usable MODFLOW model is definition of the layer elevations and the starting heads.
If you have a data set (x,y,z scatter data) defining a surface, then this is the
best way to enter elevations.
Sometimes we work with two data sets, for example a digitized surface elevation
and depth to the bottom of a unit in a borehole.
To expedite progress to convergence on the steady state solution we will define
starting heads at a constant depth below ground surface rather than an arbitrary
horizontal surface.
OPEN THE SCATTER POINT DATA DEFINING THE GROUND SURFACE
The file terrain.sp2 (*.sp2 for scatter point 2D) is a simple ascii file containing
the x,y,z data defining the ground surface. You can create such data sets for
your own data by using the same format. Click here to
view the format of a scatter point data set
Use the DATA CALCULATOR to create a set of starting heads that are 10 ft below
the ground surface using
Data>DataCalculator
INTERPOLATE HEADS AND ELEVATIONS TO THE MODFLOW GRIDS
While in the 2D Scatter Data Module
Select Interpolation->toMODFLOWLayers
Highlight the ground elevations and the top of layer 1
Select Map
Select OK to initiate the interpolation
NOW, import the data defining the elevations of the units in boreholes by File>Import,
select, elevs.sp2 open, and notice the new set of points that appear. The scatter
point data for the units in boreholes is another ASCII file, much smaller then
the ground surface data set. click here to view the unit
elevations scatter point data set
By now, your screen should look like this:
While in the 2D Scatter Data Module
Select Interpolation->toMODFLOWLayers
Select OK to initiate the interpolation
Now clean up the display by hiding the scatter data points
and by hiding the grid frame
Now check the model cross section:
Notice that you can switch to various
orientations and toggle through rows, columns and layers in the tool palette.
Try to digest what you are viewing. Notice the various symbols representing the
sources and sinks. Look at the layer relationships. Notice
that toward the limestone hillside, where the lower sediment pinch out, the bottom
elevations are above the top elevations for layer 2, so the layer looks like it
is "turned inside out".
Correct these problems by:
make all cells that fall below the bottom layer inactive by:
also view the correction from the plan view perspective:
notice the inactive cells in layer 2 and return to viewing
layer 1.
REVISIT THE MODEL CHECKER ONCE MORE TO CONSIDER OTHER ERRORS
If there are no errors, close the dialog
If there are errors, highlight the error you want to work on and follow the steps
in the lower panel. The model checker window can be left open while you make the
corrections.
Select DONE