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Relation of NMR parameters with specific surface and resistivity of shaly sandstone and siltstone samples : experimental study. / Shumskayte, M. Y.; Glinskikh, V. N.

в: Russian Geology and Geophysics, Том 57, № 10, 01.10.2016, стр. 1509-1514.

Результаты исследований: Научные публикации в периодических изданияхстатьяРецензирование

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Shumskayte MY, Glinskikh VN. Relation of NMR parameters with specific surface and resistivity of shaly sandstone and siltstone samples: experimental study. Russian Geology and Geophysics. 2016 окт. 1;57(10):1509-1514. doi: 10.1016/j.rgg.2016.01.019

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Shumskayte, M. Y. ; Glinskikh, V. N. / Relation of NMR parameters with specific surface and resistivity of shaly sandstone and siltstone samples : experimental study. в: Russian Geology and Geophysics. 2016 ; Том 57, № 10. стр. 1509-1514.

BibTeX

@article{a5a64646a48848468500fafa839a7768,
title = "Relation of NMR parameters with specific surface and resistivity of shaly sandstone and siltstone samples: experimental study",
abstract = "Using an MST-05 NMR relaxometer, we determined the dependence of NMR parameters on the specific surface and resistivity of water-saturated shaly sandstone and siltstone core samples. The influence of the type and quantity of clay minerals was evaluated at residual water saturation, because the main contribution to the measured NMR signal in this case is made by clay content. Based on NMR relaxometry data, we obtained quantitative estimates of the specific surface with clay- and capillary-bound fluids. The surface relaxivity was estimated from thermal-desorption and NMR relaxometry data. The high degree of reliability of its values was confirmed by the agreement between the pore size distributions determined by NMR relaxometry and by capillarimetry and granulometry. We have established that the parameters of NMR spectra depend on the specific surface and resistivity, which are, in turn, a function of the surface properties of both clay and sandstone/siltstone particles.",
keywords = "clay minerals, nuclear magnetic resonance, relaxometry, resistivity, specific surface, surface relaxivity",
author = "Shumskayte, {M. Y.} and Glinskikh, {V. N.}",
year = "2016",
month = oct,
day = "1",
doi = "10.1016/j.rgg.2016.01.019",
language = "English",
volume = "57",
pages = "1509--1514",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "10",

}

RIS

TY - JOUR

T1 - Relation of NMR parameters with specific surface and resistivity of shaly sandstone and siltstone samples

T2 - experimental study

AU - Shumskayte, M. Y.

AU - Glinskikh, V. N.

PY - 2016/10/1

Y1 - 2016/10/1

N2 - Using an MST-05 NMR relaxometer, we determined the dependence of NMR parameters on the specific surface and resistivity of water-saturated shaly sandstone and siltstone core samples. The influence of the type and quantity of clay minerals was evaluated at residual water saturation, because the main contribution to the measured NMR signal in this case is made by clay content. Based on NMR relaxometry data, we obtained quantitative estimates of the specific surface with clay- and capillary-bound fluids. The surface relaxivity was estimated from thermal-desorption and NMR relaxometry data. The high degree of reliability of its values was confirmed by the agreement between the pore size distributions determined by NMR relaxometry and by capillarimetry and granulometry. We have established that the parameters of NMR spectra depend on the specific surface and resistivity, which are, in turn, a function of the surface properties of both clay and sandstone/siltstone particles.

AB - Using an MST-05 NMR relaxometer, we determined the dependence of NMR parameters on the specific surface and resistivity of water-saturated shaly sandstone and siltstone core samples. The influence of the type and quantity of clay minerals was evaluated at residual water saturation, because the main contribution to the measured NMR signal in this case is made by clay content. Based on NMR relaxometry data, we obtained quantitative estimates of the specific surface with clay- and capillary-bound fluids. The surface relaxivity was estimated from thermal-desorption and NMR relaxometry data. The high degree of reliability of its values was confirmed by the agreement between the pore size distributions determined by NMR relaxometry and by capillarimetry and granulometry. We have established that the parameters of NMR spectra depend on the specific surface and resistivity, which are, in turn, a function of the surface properties of both clay and sandstone/siltstone particles.

KW - clay minerals

KW - nuclear magnetic resonance

KW - relaxometry

KW - resistivity

KW - specific surface

KW - surface relaxivity

UR - http://www.scopus.com/inward/record.url?scp=84992390860&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2016.01.019

DO - 10.1016/j.rgg.2016.01.019

M3 - Article

AN - SCOPUS:84992390860

VL - 57

SP - 1509

EP - 1514

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 10

ER -

ID: 25477300