Geotomo Software RES3DINV Pro v3.14 2024
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Geotomo Software RES3DINV Pro v3.14 2024
RES3DINVx64 Pro 2024
In areas where the geologic structures are nearly 2D, conventional 2D imaging can be used successfully, but in areas with complex structures, there is no substitute for a full 3D survey.
The task of RES3DINV software from Geotomo Software is to create 3D models of the earth. Arrays supported in the program include pole pole, dipole, inline dipole, equatorial dipole, and Wenner-Schlumberger and non-conventional arrays.
RES3DINV uses an exclusive Gauss-Newton least-squares inversion technique to generate a 3D subsurface model from the apparent resistivity data alone.
The program is completely automatic and the user does not even need to provide an initial model. By supporting parallel calculations in the program, the inversion time is significantly reduced. Also, the effects of topography can be modeled using a finite element mesh so that the surface of the mesh matches the topography.
Key features of RES3DINV software
: – Support for exact and approximate least squares optimization methods
– Support for inversion with smooth and sensitive contrast
– Support for 5041 electrodes and 67500 data points on computers with one gigabyte of RAM
– Support for more than 20000 electrodes and 100000 data on computers with 16 GB of RAM
– support for trapezoidal mapping networks
– support for mapping with electrodes in arbitrary positions
– support for parallel computing on Intel and compatible computers
– and..
RES2DINV&RES3DINV bring users advanced data processing and inversion software toolkits for resistivity and induced polarization (IP) data processing and inversion.
It supports automatic inversion of underground three-dimensional (3-D) apparent resistivity models using data obtained from three-dimensional electrical exploration.
Through simple operations, you can immediately start using three different terrain modeling techniques and complex resistivity methods for high-density resistivity data inversion and induced polarization data inversion.
It complies with standard rules and regulations, is easy to operate, and improves productivity. It perfectly supports both conventional arrays and unconventional electrode arrays!
RES3DINVx64 Pro 2024
In areas where the geological structures are approximately two-dimensional (2D), conventional 2D electrical imaging surveys have been successfully used. In areas with complex structures, there is no substitute for a fully 3D survey. The arrays supported include the pole-pole, pole-dipole, inline dipole-dipole, equatorial dipole-dipole and Wenner-Schlumberger and non-conventional arrays. The RES3DINVx32/x64 programs use the smoothness-constrained Gauss-Newton least-squares inversion technique to produce a 3D model of the subsurface from the apparent resistivity data alone. Like RES2DINV, it is completely automatic and the user does not even have to supply a starting model. It supports parallel calculations that significantly reduces the inversion time. Topographic effects can be modeled by using a distorted finite-element grid such that the surface of the grid matches the topography.
Key Features:
– Supports exact and approximate least-squares optimization methods
– Supports smooth and sharp contrasts inversions
– Supports up to 5041 electrodes and 67500 data points on computers with 1GB RAM
– Supports more than 20000 electrodes and 100000 data points on computers with 16GB RAM
– Supports trapezoidal survey grids
– Supports surveys with electrodes at arbitrary positions
– Supports parallel calculations on Intel (and compatible) based computers
– And more
