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000009456 0247_ $$2DOI$$a10.1016/j.jappgeo.2010.01.008
000009456 0247_ $$2WOS$$aWOS:000276417700008
000009456 037__ $$aPreJuSER-9456
000009456 041__ $$aeng
000009456 082__ $$a620
000009456 084__ $$2WoS$$aGeosciences, Multidisciplinary
000009456 084__ $$2WoS$$aMining & Mineral Processing
000009456 1001_ $$0P:(DE-HGF)0$$aNyari, Z.$$b0
000009456 245__ $$aThe use of non-conventional CPTe data in determination of 3-D electrical resistivity distribution
000009456 260__ $$aAmsterdam [u.a.]$$bElsevier Science$$c2010
000009456 300__ $$a255 - 265
000009456 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article
000009456 3367_ $$2DataCite$$aOutput Types/Journal article
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000009456 3367_ $$2BibTeX$$aARTICLE
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000009456 440_0 $$014681$$aJournal of Applied Geophysics$$v70$$x0926-9851$$y3
000009456 500__ $$aThis work is funded partly by the NATO Collaborative Linkage Grant No. 979868. This paper presents partly the results of research project GVOP-3.1.1-2004-05-0187/3.0 supported by the National Development Plan, the EU co-financed part of the Europe Plan. This work was supported by the Research Fund of Istanbul University, project number: UDP-4295/23092009. We would like to thank Klaus Holliger (Editor-in-Chief) and the reviewers for their constructive remarks.
000009456 520__ $$aThe spatial distribution of the electrical resistivity data provides useful information for investigating and modeling the fluid transport processes. 3D electrical resistivity distribution provides information about water flow and changes in electrical resistivity of the pore fluid.Therefore, to assist in understanding and modeling of the fluid transport process, 3D spatial distribution of the electrical resistivity data with the corresponded 3D geological section were mapped and interpreted in the test site located in western Germany. A process of deriving electrical resistivity values from the mechanical and radioactive parameters of cone penetration tests (CPT) and geological information of boreholes was presented. A reliable method which gives accurate resistivity values in cases of near surface sediments was introduced. Then a field test was executed where the calculated resistivity values were compared with the measured CPTe resistivity data. The CPTe (cone penetration test with electrical extension) data were also used in correlating to the ERT (electrical resistivity tomography) data. Consequently, obtained dense CPT surveys give us the possibility to determine a high resolution resistivity distribution of the investigated area. (C) 2010 Elsevier B.V. All rights reserved.
000009456 536__ $$0G:(DE-Juel1)FUEK407$$2G:(DE-HGF)$$aTerrestrische Umwelt$$cP24$$x0
000009456 588__ $$aDataset connected to Web of Science
000009456 65320 $$2Author$$aCPTe resistivity
000009456 65320 $$2Author$$aWell-log interpretation
000009456 65320 $$2Author$$aERT
000009456 65320 $$2Author$$a3D resistivity distribution
000009456 65320 $$2Author$$aContamination
000009456 650_7 $$2WoSType$$aJ
000009456 7001_ $$0P:(DE-HGF)0$$aKanli, AI.$$b1
000009456 7001_ $$0P:(DE-HGF)0$$aJanos, S.$$b2
000009456 7001_ $$0P:(DE-Juel1)VDB9304$$aTillmann, A.$$b3$$uFZJ
000009456 773__ $$0PERI:(DE-600)1496997-x$$a10.1016/j.jappgeo.2010.01.008$$gVol. 70, p. 255 - 265$$p255 - 265$$q70<255 - 265$$tJournal of applied geophysics$$v70$$x0926-9851$$y2010
000009456 8567_ $$uhttp://dx.doi.org/10.1016/j.jappgeo.2010.01.008
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