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Graphics / CAD / Heat3D 4.11.0533
Heat3D 4.11.0533
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Heat3D 4.11.0533 Description
HEAT is a graphically interfaced application written for a PC running Microsoft WindowsTM.
HEAT is a graphically interfaced application written for a PC running Microsoft WindowsTM. Designed to study 2-D and 3-D transient thermal regimes in and around magmatic intrusions, HEAT models a variety of geologic structures and rock properties and their effect on both conductive and convective heat flow. The graphical interface is readily used to develop and tailor the simulation to represent most geological conditions of magma intrusion and geological structure. Calculated thermal regimes are color encoded and updated in graphical display with each update stored as a file for future playback. This modeling goes well beyond that done by analytical solution of 1-D linearized expressions of thermal diffusion in that it calculates the nonlinear effects of heterogeneous media, temporal, spatial, and thermally varying properties, latent and radioactive decay heat, and magma convective heat transfer. As with most geophysical modeling, the results of these calculations are not mathematically unique for inversion applications. However, rigorous application of geological constraints afforded by this code can greatly reduce the number of simulations that might satisfactorily fit observations.
HEAT employs an explicit finite differencing scheme rather than an alternating direction implicit one in order to insure that the original differential equation solved is exactly reproduced by the finite difference equation when time and spatial steps are infinitesimal. Truncation errors that might evolve when using very short time steps are minimized by utilizing double precision. Continuous thermal gradients are assigned along the boundaries where symmetry planes are not specified, and initial conditions use a designated regional thermal gradient. Latent heats of fusion/crystallization are solved for all rocks including magma where temperatures are in that range. New magmas may be introduced into the calculational mesh at any time during the simulation with or without the calculation of heat advection caused by rock displacement necessary to make space for the magma. All rock/magma properties are assigned by the user and they include: density, porosity (fluid saturation), heat capacity, initial temperature, spatially and thermally varying thermal conductivities, and location. As mentioned earlier, the code has been applied to several geologic areas to test its suitability. A version of heat has been adapted for laboratory rock melting experiments involving thermal variations of rocks melted by a moving hot molybdenum probe. Results thus far have shown the method predicts measured temperatures with enough accuracy to make engineering designs based on it. More documentation can be viewed in the file HEAT3D.pdf.
OS: Windows 7, WinXP, Windows Vista
Tags: Simulate Heat Flow - Create Rock Mesh - Heat Graph Creator - Simulate - Heat - Flow
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