Quantification of clay mineral microporosity and its application to water saturation and effective porosity estimation: A case study from Upper Ordovician reservoir, Libya
The relative volume of clay minerals contributing to the microporosity is the main feature that influences the estimation of water saturation in hydrocarbon reservoirs. For developing a genuine understanding of reservoir quality, the present study elucidated the petrography, quantification of clay m...
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doaj-8202d1a6531949a8ab3dfdf5cb46f4a82020-11-25T00:43:34ZengElsevierJournal of Natural Gas Geoscience2468-256X2019-06-0143139150Quantification of clay mineral microporosity and its application to water saturation and effective porosity estimation: A case study from Upper Ordovician reservoir, LibyaAbubaker Alansari0Ahmed Mohamad Ahmed Salim1Hammad Tariq Janjuhah2Abdul Hadi Bin Abd Rahman3Nuri Mohamed Fello4Department of Geosciences, University Technology PETRONAS, 32610, Perak, Malaysia; Corresponding author.Department of Geosciences, University Technology PETRONAS, 32610, Perak, MalaysiaDepartment of Geology, American University of Beirut, Bliss Street., 1107-2020, LebanonDepartment of Geosciences, University Technology PETRONAS, 32610, Perak, MalaysiaNational Oil Corporation (NOC), Tripoli, LibyaThe relative volume of clay minerals contributing to the microporosity is the main feature that influences the estimation of water saturation in hydrocarbon reservoirs. For developing a genuine understanding of reservoir quality, the present study elucidated the petrography, quantification of clay minerals, and microporosity, besides their effect on the petrophysical parameters. The ratified method is an integration of core data, SEM (Scanning Electron Microscopy), XRD, and thin section. The most identified clay minerals in order of decreasing abundance are kaolinite (45%), Illite (35%), a mixed layer (10%), smectite (5%) and others are 5%. The estimation of clay mineral microporosity was based on the SEM photomicrographs. Mixed clay minerals have a variety of textures with microporosity values that range from 10 to 55%. In this regard, the clay microporosity data was used to calculate the effective clay volume; the clay bound water, the effective water saturation and porosity. As a result, the estimated values are decreased when the microporosity is considered, except for the effective volume of clay minerals which is approximately twice (52.5%) as the original dry mineral volume. Moreover, the microporosity based water saturation decreased dramatically when compared to log values up to 22. 37%. The above-estimated values correlated with both core and log readings using linear regression. The derived relationships with a high correlation coefficient (R2) were used to extrapolate microporosity, clay bound water, effective saturation and effective porosity in the uncored well interval. The correlation coefficient R2 is higher than 90%. Keywords: Clay minerals, Microporosity, Effective porosity, Effective saturation, Effective clay volume, Solid clay mineral volumehttp://www.sciencedirect.com/science/article/pii/S2468256X18300749 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Abubaker Alansari Ahmed Mohamad Ahmed Salim Hammad Tariq Janjuhah Abdul Hadi Bin Abd Rahman Nuri Mohamed Fello |
spellingShingle |
Abubaker Alansari Ahmed Mohamad Ahmed Salim Hammad Tariq Janjuhah Abdul Hadi Bin Abd Rahman Nuri Mohamed Fello Quantification of clay mineral microporosity and its application to water saturation and effective porosity estimation: A case study from Upper Ordovician reservoir, Libya Journal of Natural Gas Geoscience |
author_facet |
Abubaker Alansari Ahmed Mohamad Ahmed Salim Hammad Tariq Janjuhah Abdul Hadi Bin Abd Rahman Nuri Mohamed Fello |
author_sort |
Abubaker Alansari |
title |
Quantification of clay mineral microporosity and its application to water saturation and effective porosity estimation: A case study from Upper Ordovician reservoir, Libya |
title_short |
Quantification of clay mineral microporosity and its application to water saturation and effective porosity estimation: A case study from Upper Ordovician reservoir, Libya |
title_full |
Quantification of clay mineral microporosity and its application to water saturation and effective porosity estimation: A case study from Upper Ordovician reservoir, Libya |
title_fullStr |
Quantification of clay mineral microporosity and its application to water saturation and effective porosity estimation: A case study from Upper Ordovician reservoir, Libya |
title_full_unstemmed |
Quantification of clay mineral microporosity and its application to water saturation and effective porosity estimation: A case study from Upper Ordovician reservoir, Libya |
title_sort |
quantification of clay mineral microporosity and its application to water saturation and effective porosity estimation: a case study from upper ordovician reservoir, libya |
publisher |
Elsevier |
series |
Journal of Natural Gas Geoscience |
issn |
2468-256X |
publishDate |
2019-06-01 |
description |
The relative volume of clay minerals contributing to the microporosity is the main feature that influences the estimation of water saturation in hydrocarbon reservoirs. For developing a genuine understanding of reservoir quality, the present study elucidated the petrography, quantification of clay minerals, and microporosity, besides their effect on the petrophysical parameters. The ratified method is an integration of core data, SEM (Scanning Electron Microscopy), XRD, and thin section. The most identified clay minerals in order of decreasing abundance are kaolinite (45%), Illite (35%), a mixed layer (10%), smectite (5%) and others are 5%. The estimation of clay mineral microporosity was based on the SEM photomicrographs. Mixed clay minerals have a variety of textures with microporosity values that range from 10 to 55%. In this regard, the clay microporosity data was used to calculate the effective clay volume; the clay bound water, the effective water saturation and porosity. As a result, the estimated values are decreased when the microporosity is considered, except for the effective volume of clay minerals which is approximately twice (52.5%) as the original dry mineral volume. Moreover, the microporosity based water saturation decreased dramatically when compared to log values up to 22. 37%. The above-estimated values correlated with both core and log readings using linear regression. The derived relationships with a high correlation coefficient (R2) were used to extrapolate microporosity, clay bound water, effective saturation and effective porosity in the uncored well interval. The correlation coefficient R2 is higher than 90%. Keywords: Clay minerals, Microporosity, Effective porosity, Effective saturation, Effective clay volume, Solid clay mineral volume |
url |
http://www.sciencedirect.com/science/article/pii/S2468256X18300749 |
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