All Days 1991
DOI: 10.2118/22723-ms
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The Magnetic Resonance Imaging Log Characterized by Comparison with Petrophysical Properties and Laboratory Core Data

Abstract: Core samples are examined using a 10 MHz NMR spectrometer and results are compared with those from the Magnetic Resonance Imaging Log*(MRIL) (operating frequency 1 MHz) in the same rock formations. The frequency dependence of this technology and its link to petrophysics is investigated, thus offering the first link between core and log NMR data for this new tool.

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Cited by 82 publications
(24 citation statements)
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“…However, a logging technique is less attractive if one needs core data of the same bore hole for calibration. In the present case of low Allermoehe sandstone, permeability prediction with an empirical equation of the type of the so-called TimurCoates equation (COATES et al, 1991) was not satisfactory, as it yielded much lower values than directly measured gas permeabilities. Therefore, we used a permeability equation of the Kozeny-Carman type (KOZENY, 1927, CARMAN, 1957, which involves porosity, tortuosity and effective hydraulic pore radius r eff .…”
Section: Introductioncontrasting
confidence: 70%
“…However, a logging technique is less attractive if one needs core data of the same bore hole for calibration. In the present case of low Allermoehe sandstone, permeability prediction with an empirical equation of the type of the so-called TimurCoates equation (COATES et al, 1991) was not satisfactory, as it yielded much lower values than directly measured gas permeabilities. Therefore, we used a permeability equation of the Kozeny-Carman type (KOZENY, 1927, CARMAN, 1957, which involves porosity, tortuosity and effective hydraulic pore radius r eff .…”
Section: Introductioncontrasting
confidence: 70%
“…The permeability is often related to porosity through empirical relations since it depends upon on various porous media characteristics including porosity, distribution, pore shape, and pore connectivity. These relations are developed based on pore or grain sizes and on surface-area measurements, (Carman 1937;Chauvetea and Zaitoun 1981;Van Baaren 1979;Coates et al 1991) The Kozeny-Carman equation (Carman 1937;Bear 1972;Batu 1998,), provides relationship between permeability (ε) and the effective grain diameter (d eff ) as…”
Section: Porosity and Permeability Relationsmentioning
confidence: 99%
“…The permeability of the porous matrix may be calculated using the traditional equations based on the relationships between the permeability and pore geometry and concentration established for homogeneous well-sorted formations (Carman 1956;Timur 1968;Coates et al 1991). However, the introduction of the secondary-pore permeability represented by inclusions of different form and size is a complicated question, because, at present, the permeability is only defined for bodies with, at least, one infinite size as cylinder, slab, and layer limited by two parallel planes (Gueguen and Palciauskas 1994).…”
Section: Introductionmentioning
confidence: 99%