Conceptual Model Tools > Zones > Zone=DM
Borehole Simulation Result File
A borehole simulation result (.tp file extension) can be imported/uploaded by checking the box next to and clicking 'Import' to browse to the file location on your local machine.The .tp file is contained in the .zip folder created when the user saves the latest TP model result:
Other Tools > SaveModel > TP Model Results
Within the downloaded .zip folder, the 'TPROGS_SIM_RESULT.dat' file should be renamed with a .tp file extension before attempting to upload as a Borehole Simulation Result File.
Flow Property
Transformation Options
There are two options for calculating the properties (e.g., horizontal conductivity, vertical conductivity, porosity, etc.) in each groundwater model cell based on the TP cell/3D grid system.The first option, Nearest , assigns the properties of the TP cell located nearest to the groundwater model cell.
The 2nd option, Bilinear uses an average of the properties from surrounding TP cells to calculated the properties of the groundwater model cell.
For example, if one groundwater model cell contained two or more geologic model cells in the horizontal direction, the resulting horizontal conductivity of the groundwater cell was the arithmetic average of the horizontal conductivity values from the geologic model cells. If the groundwater cell contained two or more geologic model cells in the vertical direction, a harmonic average was utilized to calculate vertical conductivity for the groundwater model cell.
Number of Materials
By default, IGW-NET assumes there are 4 material types used in the Borehole simulation result file. Change the input value and click the 'Edit Material Property' button to update the number of materials listed in the Flow Property table (see next).Flow Property Table
Kxx is the x- (west-to-east) direction horizontal conductivity assigned to the material IDKxx/Kyy is the horizontal anisotropy ratio of x-direction conductivity to y- (north-to-south) direction conductivity. The default value of 1 assumes no horizontal anisotropy is present.
Kxx/Kzz is the vertical anisotropy ratio of x-direction conductivity to z- (vertical) direction conductivity. The default value of 10 means that x-direction conductivity is assumed to be 10 times larger than the vertical anisotropy.
n is the effective porosity assigned to the material ID.
Sy is the specific yield assigned to the material ID. (This is used in the case that the TP cell is located in an unconfined layer of the groundwater model.)
Ss is the specific storage assigned to the material ID. (This is used in the case that the TP cell is located in an unconfined layer of the groundwater model.)