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Three dimensional block-structured grids are generated by zone method and solving a system of elliptic partial differential equations.
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Local refining grids were generated to represent the hydraulic fractures in the reservoir model.
The grids were generated using the spring dynamics method, and adjustments were made using analytical functions.
Using a similar approach, functional climate grids were generated for chill-hours, growing degree-days and frost risk.
For this condition, 5 different sampling grids were generated from the geological block model of Sungun copper mine.
Dynamic hexahedral orthogonal grids were generated and updated during the solving process to ensure adequate grid layers at the tiny radial clearance of 30 μm.
A set of bathymetric/topographic nested grids was generated in order to cover the areas from the source zone to the target coast (Fig. 2).
Considering square and hexagonal arrays of fibers, two major finite-element grids were generated where the features and the constrains are automatically being assigned.
Grids were generated with GRID [ 129, 130].
To create the initialization location set (Fig. 2 a), regularly spaced Cartesian grids were generated on the flattened PALS-B12 average surface of the left and right hemispheres using the Caret software (Van Essen 2005).
TPS deformation grids were generated in the program MORPHEUS (Slice, 1999; http://www.morphometrics.org/morpheus.html. STATISTICA, version 8.1 (Statsoft 2005) was used for other statistical analyses (i.e., MANCOVA and MANOVA) and NMDS plots were generated using Matlab (The MathWorks 2007).
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