2018
DOI: 10.1016/j.fuel.2018.02.059
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Relaxation and relaxation exchange NMR to characterise asphaltene adsorption and wettability dynamics in siliceous systems

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Cited by 33 publications
(46 citation statements)
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“…NMR and MRI have been widely employed to measure a range of transport properties of various fluids in porous media including various hydrocarbons in rock cores (e.g. Mitchell et al 2013;Coates et al 1999;Zhao et al 2016;Ramskill 2018;Li et al 2016;Li et al 2017a, b;Mitchell et al 2018;Shikhov et al 2018). Whilst these have predominately focused on liquid phase measurements, due predominately to signal-tonoise (SNR) considerations, gas phase NMR/MRI has been used; for example by Zecca et al (2018), to determine the restricted diffusion coefficient of ethane in sandstone cores and, hence, their tortuosity.…”
Section: Introductionmentioning
confidence: 99%
“…NMR and MRI have been widely employed to measure a range of transport properties of various fluids in porous media including various hydrocarbons in rock cores (e.g. Mitchell et al 2013;Coates et al 1999;Zhao et al 2016;Ramskill 2018;Li et al 2016;Li et al 2017a, b;Mitchell et al 2018;Shikhov et al 2018). Whilst these have predominately focused on liquid phase measurements, due predominately to signal-tonoise (SNR) considerations, gas phase NMR/MRI has been used; for example by Zecca et al (2018), to determine the restricted diffusion coefficient of ethane in sandstone cores and, hence, their tortuosity.…”
Section: Introductionmentioning
confidence: 99%
“…The transverse relaxation time is related to the specific surface area of the pores. Specifically, the transverse relaxation increases with the enlargement of the specific surface areas of pores . It can be described using the following equation where T 2 is the transverse relaxation time in ms, S is the specific surface area of the pore in nm 2 , V is the specific volume of the pore in nm 3 , ρ 2 is the transverse surface relaxation coefficient in nm/ms, r is the pore radius in nm, and F s represents the geometry factor.…”
Section: Methodsmentioning
confidence: 99%
“…The latter suggests that dynamic changes in surface properties, e.g. as result of wettability alteration (Shikhov et al 2018(Shikhov et al , 2019, may be understood spatially resolved and inform modelling of two-phase flow (Wang et al 2018a). For such an approach, it would be desirable to replace effective clay parameters with clay structure and surface properties.…”
Section: Introductionmentioning
confidence: 99%