2008
DOI: 10.3923/jas.2008.4070.4078
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A Damped Least-Squares Inversion Program for the Interpretation of Schlumberger Sounding Curves

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Cited by 47 publications
(40 citation statements)
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“…Inverse modeling, in contrast starts with the data and a general principle or a model, in which the model parameters are estimated by minimizing the error/misfit function set up between the data and model parameters (Menke, 1984). During the past decades researchers have made several attempts to solve the resistivity inverse problems (Ghosh, 1971;Zohdy, 1989;Macias et al, 2000;Qady and Ushijima, 2001;Singh et al, 2005;Ekinci and Demirci, 2008). However, these approaches have some common drawbacks.…”
Section: S Maiti Et Al: Inversion Of DC Resistivity Data Of Koyna Rmentioning
confidence: 99%
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“…Inverse modeling, in contrast starts with the data and a general principle or a model, in which the model parameters are estimated by minimizing the error/misfit function set up between the data and model parameters (Menke, 1984). During the past decades researchers have made several attempts to solve the resistivity inverse problems (Ghosh, 1971;Zohdy, 1989;Macias et al, 2000;Qady and Ushijima, 2001;Singh et al, 2005;Ekinci and Demirci, 2008). However, these approaches have some common drawbacks.…”
Section: S Maiti Et Al: Inversion Of DC Resistivity Data Of Koyna Rmentioning
confidence: 99%
“…The modeling and interpretation of Direct Current (DC) resistivity sounding in this region, therefore, assume a special significance to understand the inhomogeneous infiltrations of fluids through porous media and geologically weak zones, such as faults and fractured zones, near the sub-surface area. The DC resistivity sounding method is one of the most popular methods that has been invariably applied for solving hydrological, geothermal, environmental and engineering problems (Ekinci and Demirci, 2008;Singh et al, 2010). In this method, current is induced directly into the ground through a pair of current electrodes and resulting voltage difference is measured between a pair of potential electrodes.…”
Section: Introductionmentioning
confidence: 99%
“…where g = [g i (m)] is the 1D model response calculated by using the well-known Gosh-Koefoed filters for the Schlumberger array [14,21]. Basically, resolving an inverse problem means finding models associated with the minimum of the misfit or the objective function.…”
Section: Inversion Algorithmmentioning
confidence: 99%
“…The common practice is to linearize the misfit function at the vicinity of a starting model and then update the model iteratively until a convergence to an optimum solution is reached [13,14]. In this study, we developed our algorithm [20] to simultaneously invert the VES data sets distributed along a profile.…”
Section: B Introductionmentioning
confidence: 99%
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