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▀███▓███▓▀▀ The diGERATi Present ▀▀▓███▓███▀
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█▄▄▄▄▄ RES2DINV_v3.55.35-DIGERATI ▄▄▄▄▄▄█
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███▀ Release Info ▀██▓
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▐█▓▓ Cracker ......: DIGERATI Release-Type..: Incl_Patch ██▓▌
██▓▌ Packager......: DIGPACKER Release-Date..: 27.03.2006 ▐██▓
██▓ Supplier......: DIGERATI Protection....: Time Limit ██▓
▐██ Coder.........: DIGERATI OS............: WinALL █▓▌
██▓ ░ Company.......: Geotomo Software Files.........: xx/02 ░▓█▓
▀██░ ░█▓▀
▀██░ URL: www.geolectrical.com ░█▓▀
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█▄ █▄▀▀████▓▀ ▐█▓▌ ▀ Release Notes ▀ ▐█▓▌ ▀▓████▀▀▄█ ▄█
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██▓ ██▓
██▓ upports on land, underwater and cross-borehole surveys ██▓
██▓ ██▓
██▓ Supports the Wenner (alpha,beta,gamma), ██▓
██▓ Wenner-Schlumberger, pole-pole, pole-dipole, inline ██▓
██▓ dipole-dipole, equatorial dipole-dipole and ██▓
██▓ non-conventional arrays. ██▓
██▓ ██▓
██▓ Supports exact and approximate least-squares optimisation ██▓
██▓ methods ██▓
██▓ ██▓
██▓ Supports smooth and sharp constrasts inversions ██▓
██▓ ██▓
██▓ Supports up to 16000 electrodes and 21000 data points on ██▓
██▓ computers with 1GB RAM ██▓
██▓ ██▓
██▓ Seamless inversion of very long survey lines using sparse ██▓
██▓ inversion techniques ██▓
██▓ ██▓
██▓ (RES2DINV only license includes limited used of RES3DINV ██▓
██▓ 3D inversion program) ██▓
██▓ ██▓
██▓ Two-dimensional (2D) electrical imaging surveys are now ██▓
██▓ widely used to map areas of moderately complex geology ██▓
██▓ where conventional 1D resistivity sounding and profiling ██▓
██▓ techniques are inadequate. The results from such surveys ██▓
██▓ are usually plotted in the form of a pseudosection (Figure ██▓
██▓ 1a) which gives an approximate but distorted picture of ██▓
██▓ the subsurface geology. ██▓
██▓ ██▓
██▓ The RES2DINV program uses the smoothness-constrained ██▓
██▓ least-squares method inversion technique to produce a 2D ██▓
██▓ model of the subsurface from the apparent resistivity data ██▓
██▓ alone. It is completely automatic and the user does not ██▓
██▓ even have to supply a starting model. This program has ██▓
██▓ been optimised for the inversion of large data sets. The ██▓
██▓ use of available memory is optimised so as to reduce the ██▓
██▓ computer time by minimising disk swapping. On a Pentium ██▓
██▓ based microcomputer, the inversion of a single ██▓
██▓ pseudosection is usually completed within minutes. Four ██▓
██▓ different techniques for topographic modelling are ██▓
██▓ available in this program. Together with the free 2D ██▓
██▓ forward modeling program RES2DMOD, it forms a complete 2D ██▓
██▓ resistivity forward modeling and inversion package. ██▓
██▓ ██▓
██▓ The program will automatically choose the optimum ██▓
██▓ inversion parameters for a particular data set. However, ██▓
██▓ the parameters which affects the inversion process can be ██▓
██▓ modified by the user. Three different variations of the ██▓
██▓ least-squares method are provided; a very fast ██▓
██▓ quasi-Newton method, a slower but more accurate ██▓
██▓ Gauss-Newton method, and a moderately fast hybrid ██▓
██▓ technique which incorporates the advantages of the ██▓
██▓ quasi-Newton and Gauss-Newton methods. The smoothing ██▓
██▓ filter can be adjusted to emphasize resistivity variations ██▓
██▓ in the vertical or horizontal directions. Two different ██▓
██▓ variations of the smoothness constrained least-squares ██▓
██▓ method are provided; one optimised for areas where the ██▓
██▓ subsurface resistivity varies in a smooth manner (such as ██▓
██▓ chemical plumes), and another optimised for areas with ██▓
██▓ sharp boundaries (such as massive ore bodies). A robust ██▓
██▓ data inversion option is also available to reduce the ██▓
██▓ effect of noisy data points. Resistivity information from ██▓
██▓ borehole and other sources can also be included to ██▓
██▓ constrain the inversion process. ██▓
██▓ ██▓
██▓ The figure below shows an example from an electrical ██▓
██▓ imaging survey in an area with fairly complex subsurface ██▓
██▓ geology and significant surface topography. This survey ██▓
██▓ was carried out across a circular mound which is thought ██▓
██▓ to contain some important Irish archaeological burial ██▓
██▓ chambers (Waddell, J. and Barton, K, 1995, Seeing beneath ██▓
██▓ Rathcroghan. Archaeology Ireland, Vol. 9, No. 1, 38-41.). ██▓
██▓ The inversion of this data set, which has 67 electrode ██▓
██▓ positions and 339 data points, took about 81seconds on a ██▓
██▓ 266 MHz Pentium II computer. ██▓
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██▓ ░ ▄ ▀▀▄ ▄▀▀ ▄ ░ ▓█▓
▀██▓▄▄ ▐██▄ ▄ Install Notes ▄ ▄█▓▌ ▄▄▓██▀
▄▀▀████▄█▓▓ ▀▀ ▄▄ ▄▄ ▀▀ ██▓▄████▀▀▄
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▄ ▀▀▀▀▀ ▀▀▀▀▀ ▄
█▓ █▓▀ ▀▓█ █▓
█▓▌▀█ 1. Unpack and install the software █▀▐█▓
█▓▌▀█ 2. Unpack crack.rar and copy/overwrite into the █▀▐█▓
█▓▌▀█ installation dir █▀▐█▓
█▓▌▀█ 3. Apply patch.exe to remove all limits █▀▐█▓
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▄██ ██▄
▐█▓▌ ▄██▄ ▄▄█▓▄▄ ▄▄▀▀ ■ ■ ▀▀▄▄ ▄▄██▓▄ ▄██▄ ▐█▓▌
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▀███▓▓▀ ▀▀ ▀▀ ▀▀██▓▓▓▀
▄ ▄▄▄█ Greets to all who work hard to make the scene █▄▄▄ ▄
▄█▓ █▓▌ ▐█▓ █▓▄
█▓▌ ▐█▓ secure and enjoyable for everyone! █▓▌ ▐█▓
▀█▓ █▓▌ ▐█▓ █▓▀
▀▀▄ █▓▌ Some general notes... ▐█▓ ▄▀▀
▐█▓ █▓▌
██▓ █ - we dont want our releases spread via usenet,ftp █ ██▓
▐█▓ ▐█ - we dont want our releases being listed on ▓▌ █▓▌
█▓ █▓ several public dupe-sites like nforce ██▓ █▓
█▓ █▓▓ - we dont want to see our releases on public places ██▓ █▓
▄█▓ ▄█▓▓ - nor do we support one of these points ██▓▄ █▓▄
▐█▓▌ ██▓▓ ██▓▓ ▐█▓▌
▐██▓ ██▓▀ Think about it and try to make the scene as secure... ▀██▓ ██▓▓
▀███▄▄▄░ ... as possible ░▄▄▄█▓▓▀
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▐▓▌ Ascii by Yce*Remorse ▐▓▌
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