To prevent automated spam submissions leave this field empty.Supports on land, underwater and cross-borehole surveys Supports the Wenner alpha,beta,gammaWenner-Schlumberger, pole-pole, pole-dipole, inline dipole-dipole, equatorial dipole-dipole, gradient and non-conventional arrays. Happy New Year! Make your own four-electrode probe for soil mapping Happy New Year ! Supports on land, underwater and cross-borehole surveys Supports the Wenner alpha,beta,gammaWenner-Schlumberger, pole-pole, pole-dipole, inline dipole-dipole, equatorial dipole-dipole, gradient and non-conventional arrays.
#Res2dinv price full#
The full professional version of the program gives your the ability to save your models and inversion data and is protected with a hardware key USB or LP1 dongle.
#Res2dinv price free#
Upgrades are free for one year for existing customers. Option to include boundaries of layers from seismic or borehole surveys added.
New format for batch mode option script file which makesuse of the files containing the inversion parameters produced by the RES2DINV program.
This method inverts the entire data set and model at a single time to produce a continuous and seamless model. The program supports survey lines with up to electrodes and data points. It is probably an order of magnitude faster than some other commercially available 2D inversion software. Interpolate data from land, under water, and cross-borehole surveys.
#Res2dinv price software#
The software can handle data from any electrode array, including Wenner a, b, gdipole-dipole, inline pole-dipole, pole-pole, Wenner-Schlumberger, equatorial pole-dipole and non-conventional arrays. The inversion of the resistivity and IP data is conducted by least-square method involving finite-element and finite-difference methods. RES2DINV software is designed to interpolate and interpret field data of electrical geophysical prospecting 2D sounding of electrical resistivity conductivity and induced polarization. Supports the Wenner alpha,beta,gammaWenner-Schlumberger, pole-pole, pole-dipole, inline dipole-dipole, equatorial dipole-dipole, gradient and non-conventional arrays. Supports on land, underwater and cross-borehole surveys.
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