RES2DINV software For Windows 98/Me/2000/NT/XP Supports 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, gradient 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.
New in RES2DINV ver. 3.71: Multicore CPU support is now available in RES2DINVx32 and RES3DINVx64. Download: and. New in RES2DINV ver. 3.59: Sparse inversion option for very long survey lines (2000 to 16000 electrode positions) added. This method inverts the entire data set and model at a single time to produce a continuous and seamless model.
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. جهت سفارش دانلود کرک از طریق ثبت درخواست و یا تماس با شرکت اقدام فرمایید.
Demo/Upgrade software: The latest updates to RES2DINV and RES3DINV require the Keylok dongle. Please contact Geotomo Software or one of the authorised software. The 3.57 version of Res2dinv is available as a free download on our website. The latest version of the software can be downloaded for PCs. Cracked Software 2013-3; Cracked Software 2013-4. Res2dinv 3.58 crack; Microsoft fingerprint reader driver 64 bit; Last look at eden europe youtube.
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.
Article citations RES2DINV Program Version 3.55.49. Copyright (1995-2006). Geotomo Software. Www.geoelectrical.com has been cited by the following article: • TITLE: AUTHORS: KEYWORDS:,,, JOURNAL NAME:,, March 8, 2016 ABSTRACT: In 1986, the Egyptian government planned 15th May City, which is located in the southeast of Helwan city. It is considered one of the most propitious cities that pull out the residents who live around the Nile valley in Egypt.
Supports 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, gradient 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) RES2DINV software is designed to interpolate and interpret field data of electrical geophysical prospecting (2D sounding) of electrical resistivity (conductivity) and induced polarization. The inversion of the resistivity and IP data is conducted by least-square method involving finite-element and finite-difference methods.
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.
Resistivity measurements rely on expanding the electrode separation in order to achieve ever deeper measurements, leading to a larger volume of the subsurface material being sampled for each successive depth level. As a result the each resistivity measurement represents the bulk resistive properties of the ground- referred to as the Apparent Resistivity. The recorded Apparent Resistivity is represented as a point measurement in the dataset.
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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.
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.
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The three-dimension electrical imaging method is interpreted in the form of the geoelectric layers’ depths and thicknesses. Accordingly, the interpretation proposes sequences of three layers. Moreover, the borders of the crack can be noticed. The results of shallow seismic refraction method show the same sequences of three seismic layers. The interpreted layers from both techniques are dried limestone “calcite to dolomite” layer; the second is wetted Marley limestone; and the third Layer is semi-wetted Marley limestone.
Download DEMO: Some customers might find the demo version is essential for all their needs. 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). Registered clients/web users can visit for complete downloads.
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.
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. 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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Archaeology Ireland, Vol. 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.
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.
On a more modern 2.4 GHz Core 2 Duo computer, this takes less than 1 day. Example of a 3-D survey using the offset pole-dipole array. (a) Electrodes layout used for the 3-D survey of the Copper Hill area. (b) The IP model obtained from the inversion of the Copper Hill survey data set. Yellow areas have chargeability values of greater than 35 mV/V, while red areas have chargeability values of greater than 45 mV/V (White et al.
New format for batch mode option script file which makesuse of the files containing the inversion parameters produced by the RES2DINV program. Option to include boundaries of layers from seismic or borehole surveys added. Download legacy version: and Upgrades are free for one year for existing customers. After that, the software will operate indefinetely at the version when your support has ended (and Landviser, LLC will still help our customers with data interpretation for free), but to upgrade to the current version and receive software support from GeoTOMO you will need to pay $290 for each additional year of support. $2,900.00 Special Note for USA customers: Landviser's equipment and software qualify for tax deduction under Section 179. You still have time to purchase ERM-01, ERM-02 or RES2DINV/RES3DINV in 2012, before this deduction expires! For prices and product accessories, go to Send us or post a comment below and we will happily provide you with a custom quote.
New in RES3DINV ver. 3.02:Support for electrodes at arbitrary positions added and memory support increased to 128 GB for RES3DINVx64. Upgrades are free for a year existing customers, after that you have an option to use current released versions for 10% of the sale price (annual support fee) or continue to use the version that was current on the date when your initial support ended. You can use your purchased software indefinetely. Landviser, LLC will always offer technical support to our customers regardles of their support status with software developer and our partner, GeoTOMO Software (Malaysia).
The software can handle data from any electrode array, including Wenner (a, b, g), dipole-dipole, inline pole-dipole, pole-pole, Wenner-Schlumberger, equatorial pole-dipole and non-conventional arrays. Interpolate data from land, under water, and cross-borehole surveys. Easy data conversion from the most popular geophysical instruments including ABEM Lund, Syskal, AGI, PASI, IRIS, SCITREX, etc. It is probably an order of magnitude faster than some other commercially available 2D inversion software. The program supports survey lines with up to 16000 electrodes and 27000 data points.
RES2DINV software For Windows 98/Me/2000/NT/XP Supports 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, gradient 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.
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.
You can upgrade your RES2DINV dongle to RES3DINV via email later, but buying a bundle RES2DINV+RES3DINV gives you maximum flexibility in handling your data for the discount price. $5000.00 Special Note for USA customers: Landviser's equipment and software qualify for tax deduction under Section 179. You still have time to purchase ERM-01, ERM-02 or RES2DINV/RES3DINV in 2012, before this deduction expires! For current prices and product accessories, go to Send us or post a comment below and we will happily provide you with a custom quote. Some customers might find the demo version is essential for all their needs. 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. If you are registered user on our website you can visit RES3DINV folder in directory to download current and legacy versions of software.
To handle very large data sets, the program also supports the incomplete Gauss-Newton optimisation method. When used together with a data compression technique, it enables the inversion of very large data sets with over 20000 data points and model cells. Hudson. As an example, a data set with nearly 65000 data points and 32000 model cells was inverted on a 2Ghz P4 computer in slightly less than 2 days.
The arrays supported include the pole-pole, pole-dipole, inline dipole-dipole, equatorial dipole-dipole and Wenner-Schlumberger. The RES3DINV program uses the smoothness-constrained 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. A Pentium 4 (or compatible CPU) based microcomputer with at least 512 megabytes RAM and an 80 gigabyte hard-disk is recommended.
Alternatively, these parameters separate the location into layers of dissimilar competence nature and dissimilar appropriateness. The interpretation of both methods delineates five chinks or cracks. These chinks extend in the study area. These chinks can be watched by naked eyes in the buildings close to the area of the study. This study recommends getting rid of the gardens that is located between buildings to avoid the negative effect of irrigation water.
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.
Create 3D models of subsurface resistivity or IP! For Windows XP/Vista/7 (available for 32- and 64-bit PCs.) 3D surveys for pole-pole, pole-dipole, dipole-dipole, rectangular, trapezoid, Wenner, Wenner-Schlumberger,and non-conventional arrays. Now available as a combined package together with RES2DINV, the 2D Resistivity & IP inversion program. Supports exact and approximate least-squares optimisation methods Supports smooth and sharp constrasts inversions Supports up to 5041 electrodes and 67500 data points on computers with 1GB RAM Supports trapezoidal survey grids Supports parallel calculations on Pentium 4 (and compatible) based computers Multi-core support with RES3DINVx32, 128GB memory support with RES3DINVx64 In areas where the geological structures are approximately two-dimensional (2D), conventional 2D electrical imaging surveys have been successfully used. The main limitation of such surveys is probably the assumption of a 2D structure. In areas with complex structures, there is no substitute for a fully 3D survey. This program is designed to invert data collected with a rectangular grid of electrodes.
Res2dinv Res2dinv 3.5 Supports 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, gradient and non-conventional arrays. Supports 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, gradient 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 Free Download Information: Free Download 64 is not responsible for software you are downloading nor for details provided about the software 'Res2dinv 3.5' listed here, as the developer can modify information without notifying us. Even if we try to check the files for viruses, we cannot guarantee that they are safe and clean. For your own protection always scan downloaded files for viruses, spyware and malware. License: Freeware Size: 8.2 MB Date Added: 14 March, 2012 Category: / Author.