2017
DOI: 10.1021/acs.energyfuels.7b00433
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Permeability Estimation from NMR Time Dependent Methane Saturation Monitoring in Shales

Abstract: This paper consists of multiple approaches to develop a new model to determine the porosity, permeability, and rate of desorption of 1.5-in. shale samples. Permeability measurements of very tight rocks is difficult and uncertain, and no clear industry standard has yet been agreed upon. Therefore, this technique will investigate a new way to determine the porosity and permeability in shales. The raw NMR signal of the sample is measured before methane injection and is used as a base signal. During the injection … Show more

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Cited by 19 publications
(10 citation statements)
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“…Another (more recent) conundrum is the origin of the NMR surface relaxation for hydrocarbons confined in organic-rich shales, where large ratios T 1S / T 2S ≳ 4 for the hydrocarbons were previously reported, as well as dispersion T 1S (ω 0 ) , for the saturating hydrocarbons. In order to shed light on this, we analyze the isolated heptane signal in the polymer–heptane mixes, and we interpret the heptane relaxation as surface relaxation T 1S and T 2S , where the polymer is considered as the “surface” for heptane.…”
Section: Introductionmentioning
confidence: 95%
“…Another (more recent) conundrum is the origin of the NMR surface relaxation for hydrocarbons confined in organic-rich shales, where large ratios T 1S / T 2S ≳ 4 for the hydrocarbons were previously reported, as well as dispersion T 1S (ω 0 ) , for the saturating hydrocarbons. In order to shed light on this, we analyze the isolated heptane signal in the polymer–heptane mixes, and we interpret the heptane relaxation as surface relaxation T 1S and T 2S , where the polymer is considered as the “surface” for heptane.…”
Section: Introductionmentioning
confidence: 95%
“…Aside from bulk fluids, another major conundrum in petrophysics is the origin of the NMR surface relaxation T 1S and T 2S of fluids confined in organic-rich shales. For instance, Ozen and Sigal first reported that light hydrocarbons exhibit large ratios T 1S / T 2S ≳ 4 when confined in organic shale, while small ratios T 1S / T 2S ≃ 2 are found for water. While this provides a good contrast mechanism for fluid typing and saturation estimates in organic-rich shale, the mechanism behind this observation is still not well understood.…”
Section: Introductionmentioning
confidence: 99%
“…This is in stark contrast to the 1 H-1 H dipole-dipole relaxation T 1RT which increases with T , for all hydrocarbons, including methane. Also of interest recently is the influence of pore confinement on the NMR response of methane [25][26][27][28][29][30][31][32][33][34], which has practical applications for characterizing the light hydrocarbons in the organic nano-pores of kerogen and bitumen in organic-rich shale. One of the current mysteries is why the T 1S /T 2S ratio for surface-relaxation of methane in organic-shale is typically T 1S /T 2S 2, while for higherorder alkanes it is typically higher T 1S /T 2S 4.…”
Section: Introductionmentioning
confidence: 99%