Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/3691
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dc.contributor.authorallTong, M.en
dc.contributor.authorallTao, H.en
dc.date.accessioned2008-03-04T02:21:00Zen
dc.date.available2008-03-04T02:21:00Zen
dc.date.issued2008-03-04T02:21:00Zen
dc.identifier.urihttp://hdl.handle.net/2122/3691en
dc.description.abstractThe induced polarization (IP) decay curve of natural shaly sand can be modeled as a weighted superposition of exponential relaxations with different relaxation time constant. The IP relaxation time spectrum, which is defined as plot of weight versus the relaxation time constant, has been previously demonstrated as a significant tool for capillary pressure curve, pore size distribution and permeability of reservoir. Earlier works successfully used singular value decomposition (SVD) method to extract the relaxation time spectra from the decay data. However, those works were obtained from the measured data with very high signal to noise ratio (SNR). The developed algorithm is suitable for these data. But for the practice use downhole, the obtained decay data have low SNR and then the obtained spectra from these decay data using the algorithm may be unstable and invalid. In this work, the method of regularization is applied to extracting continuous IP relaxation time spectra from decay data. The regularization operator is a unit matrix. To illustrate the influences of regularization parameters on the inversion of IP relaxation time spectra, the used decay data is generated from starting relaxation time spectra. Varying levels of random noise are added to these data sets and the IP relaxation time spectra are calculated for comparison to the starting distribution. Results show that for the data contains noise, the obtained spectra of the simulated decay data become smoother with increasing the regularization parameter. There exists an optimum regularization parameter which can be used to get the most reasonable spectrum. The logarithmical optimum parameter decreases linearly with increasing the logarithmical SNR. The developed algorithm and the prediction of the optimum parameter are very reasonable for the real rock sample. The results also show that the best number of relaxation distribution points ranges from 16 to 64.en
dc.language.isoEnglishen
dc.relation.ispartofAnnals of Geophysicsen
dc.subjectinduced polarizationen
dc.subjectrelaxation time spectrumen
dc.subjectinversionen
dc.subjectregularization methoden
dc.subjectshaly sanden
dc.titleMulti-exponential inversion of induced polarization relaxation signal of shaly sanden
dc.typemanuscripten
dc.description.statusUnpublisheden
dc.type.QualityControlUnreferreden
dc.subject.INGV04. Solid Earth::04.02. Exploration geophysics::04.02.04. Magnetic and electrical methodsen
dc.relation.referencesBöner, F. D., Schopper, J. R. and Weller A., 1996, Evaluation of transport and storage properties in the soil and groundwater zone from induced polarization measurements: Geophysical Prospecting, 44, 583-602. de Lima O.A.L. and Niwas S., 2000, Estimation of hydraulic parameters of shaly sandstone aquifers form geoelectrical measurements: Journal of hydrology, 235, 12-26. Marshall, D. J. and Madden, T. R., 1959, Induced polarization, a study of its causes. Geophysics, 24, 790-816. Prammer, M.G. 1994, NMR pore size distributions and permeability at the well site: SPE28368. Slater, L. and Lesmes, D. P., 2002, Electical-hydraulic relationships observed for unconsolidated sediments: Water Resources Research 38, 31-1 - 31-10. Titov, K., Kemna, A., Tarasov, A. and Vereecken, H., 2004, Theoretical and experimental study of time domain-induced polarization in water-saturated sands: Journal of Applied Geophysics, 50, 417-433. Tong, M.S., Wang, W.N., Li, L., Jiang, Y.Z. and Shi, D.Q., 2004. Estimation of permeability of shaly sand reservoir from induced polarization relaxation time spectra. Journal of Petroleum Science and Engineering, 45, 1-10. Tong, M.S., Li, L., Wang, W.N. and Jiang, Y.Z., 2006. A time-domain induced-polarization method for estimating permeability of a shaly sand reservoir. Geophysical Prospecting, 54, 623-631. Vinegar, H. J. and Waxman, M. H., 1984, Induced polarization of shaly sands. Geophysics, 49, 1267-1287. Vinegar, H. J., and Waxman, M. H., 1987, In-situ method for determining pore size distribution, capillary pressure and permeability: U.S. Patent 4,644,283. Vinegar, H. J., and Waxman, M. H., 1988, In-situ method for determining formation permeability: U.S. Patent 4,743,854. Weng A.,Xu S. Xu and Wang X., 2006, On inversion method of surface nuclear magnetic resonance data, Goephysical Solutions for Environment and Engineering----Proceedings of the 2nd International Conference on Environmental and Engineering Geophysics(Vol.1), Wuhan, China, 456-459.en
dc.description.fulltextopenen
dc.contributor.authorTong, M.en
dc.contributor.authorTao, H.en
item.openairetypemanuscript-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.classification.parent04. Solid Earth-
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