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• W1976649462 abstract "For a large suite of consolidated sandstone samples low in shale content we have measured the permeability k, irreducible water saturation Swi, porosity φ, electrical-resistivity formation factor F, porosity by NMR, geometric-mean relaxation times T1g, and stretched-exponential relaxation times T1s (or T1s) is the decisive parameter for the estimation of k or Swi of porous sandstones by other than direct measurements of these quantities. The additional use of φ or F brings appreciable, but not decisive, improvement. We show isovalue maps of the error factor δ, which show substantial regions of near-minimum values of δ and show basic compatibility of our estimators for permeability with different published estimators. The exponents of T1g (or T1s) in our power-law estimators and those of various published estimators for k are not very far from 2.0 if either or both of φ and F are also used in the estimators." @default.
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• W1976649462 date "1996-01-01" @default.
• W1976649462 modified "2023-09-25" @default.
• W1976649462 title "Developments in core analysis by NMR measurements" @default.
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• W1976649462 doi "https://doi.org/10.1016/s0730-725x(96)00160-9" @default.
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