It now supports parallel calculations on Pentium 3 and 4 CPUs that significantly reduces the inversion time for very large survey grids. In addition to surveys with a traditional rectangular grid of electrodes, it also supports surveys with trapezoidal grids which is common in rugged and/or forested areas. Email supportaarhusgeosoftware.dk for technical support.
RES2DINV CRACK SOFTWARE SOFTWARE
Starting from 1st April 2018, sales and first-line support of the software will be managed by Aarhus Geosoftware (Denmark).
RES2DINV CRACK SOFTWARE SOFTWARE DOWNLOAD
RES2DINV Download Software Download Specsheet OhmImager Download Software. Support for vector arrays, segmentation of large survey grids and VOI calculations with Enterprise version. It supports surveys with up to about 6240 electrodes and 75000 data points. Software Seismic, Magnetic, and Geoelectrical Data Acquisition & Analysis Software. The inversion of the resistivity and IP data is conducted by least-square method involving finite-element and finite-difference methods. 3D surveys are more time-consuming and expensive to carry out, but could be useful for very complex geological situations. Furthermore a dvd video player is built in which can be used for playing almost all kinds of audio and video files even dvds and hd video.Investment account support manage your investments and download the latest stock quotes. RES2DINV software is designed to interpolate and interpret field data of electrical geophysical prospecting (2D sounding) of electrical resistivity (conductivity) and induced polarization. RES3DINV is the 3D resistivity and IP inversion software, and it is probably the first widely available commercial software of this type. However due to recent developments in field equipment design, interpretation software and microcomputer technology, two-dimensional (2D) and even three-dimensional (3D) surveys are now practical geophysical exploration tools for environmental and engineering studies. Until the early 1990s, the resistivity method has been used as a one-dimensional (1D) tool where quantitative modelling was confined to simple horizontal layers which are not sufficiently accurate for complex geological environments. Over the last 10 years, there has been a revolutionary change in the resistivity (and IP) surveying method.