2007
DOI: 10.1016/j.jmr.2007.03.008
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Quantitative discrimination of water and hydrocarbons in porous media by magnetization prepared centric-scan SPRITE

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Cited by 18 publications
(14 citation statements)
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“…Experimental and analysis methods have been developed to resolve spatial distributions of fundamental properties for describing flow that are unavailable by any other means. These include porosity (Watson et al 2002;Fantazzini et al 2004;Marica et al 2006), permeability Watson 2011, 2013), fluid saturations (Chen et al 1993;Davies et al 1994;Li et al 2007), and fluid velocities (Chang and Watson 1999). Equipment used to conduct experiments in the field normally employs much smaller magnetic fields and more limited radio-frequency controls, and they lack the means to pulse magnetic-field gradients.…”
Section: Introductionmentioning
confidence: 99%
“…Experimental and analysis methods have been developed to resolve spatial distributions of fundamental properties for describing flow that are unavailable by any other means. These include porosity (Watson et al 2002;Fantazzini et al 2004;Marica et al 2006), permeability Watson 2011, 2013), fluid saturations (Chen et al 1993;Davies et al 1994;Li et al 2007), and fluid velocities (Chang and Watson 1999). Equipment used to conduct experiments in the field normally employs much smaller magnetic fields and more limited radio-frequency controls, and they lack the means to pulse magnetic-field gradients.…”
Section: Introductionmentioning
confidence: 99%
“…For the same reason that CTI is not sensitive to field inhomogeneity, CTI suffers from the disadvantage of not being able to distinguish between spin species with different chemical shifts (although it can chemically differentiate based on different molecular dynamics [9,10]). This contrasts with the multitude of chemical shift imaging methods [11] that are implemented with other MRI modulation schemes.…”
Section: Introductionmentioning
confidence: 99%
“…The displacement of spins occurs without T 2 weighting during the z-storage interval of the STE pulse sequence. SPRITE is largely immune to time-evolution effects resulting from background gradients, paramagnetic impurities and chemical shift [19,20,22,[24][25][26][27][28]. Quantitative measurements of 2-D velocity and permeability in model porous materials and sandstone core samples have been reported [22,23].…”
Section: Introductionmentioning
confidence: 99%