IMPROVED WATER SATURATION ESTIMATION IN SHALY SANDSTONE THROUGH CLAY MINERALS ELECTROCHEMICAL STUDY
Petrophysical interpretation in shaly sandstone is a complex process. Previous studies suggested that excess conductivity from clay minerals causes different conductivity characteristic in shaly sandstone, hence the Archie’s Law for formation factor-porosity correlation is no longer applicable. This...
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2021
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oai:utpedia.utp.edu.my:246812023-07-05T03:01:54Z http://utpedia.utp.edu.my/id/eprint/24681/ IMPROVED WATER SATURATION ESTIMATION IN SHALY SANDSTONE THROUGH CLAY MINERALS ELECTROCHEMICAL STUDY WAN BAKAR, WAN ZAIRANI TA Engineering (General). Civil engineering (General) Petrophysical interpretation in shaly sandstone is a complex process. Previous studies suggested that excess conductivity from clay minerals causes different conductivity characteristic in shaly sandstone, hence the Archie’s Law for formation factor-porosity correlation is no longer applicable. This study aims to propose an improvement to the mathematical correlation of formation factor-porosity in shaly sandstone. The equation was derived based on the physical theory of clay surface conduction in combination with geometric effect. It furnishes a variable cementation factor m that explains the data deviation from Archie’s straight line on the log-log plot of formation factor versus porosity; thus providing possible solution for the non-linear part of shaly sandstone conductivity curve. The proposed mathematical equation provides good estimation of shaly sandstone formation factor F* for different types of data used for validation i.e established core data, field core data at overburden pressure from different regions and experimental data of collected shaly sandstone samples. 2021-04 Thesis NonPeerReviewed text en http://utpedia.utp.edu.my/id/eprint/24681/1/Wan%20Zairani%20Wan%20Bakar_G03281.pdf WAN BAKAR, WAN ZAIRANI (2021) IMPROVED WATER SATURATION ESTIMATION IN SHALY SANDSTONE THROUGH CLAY MINERALS ELECTROCHEMICAL STUDY. Doctoral thesis, UNSPECIFIED. |
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Petrophysical interpretation in shaly sandstone is a complex process. Previous studies suggested that excess conductivity from clay minerals causes different conductivity characteristic in shaly sandstone, hence the Archie’s Law for formation factor-porosity correlation is no longer applicable. This study aims to propose an improvement to the mathematical correlation of formation factor-porosity in shaly sandstone. The equation was derived based on the physical theory of clay surface conduction in combination with geometric effect. It furnishes a variable cementation factor m that explains the data deviation from Archie’s straight line on the log-log plot of formation factor versus porosity; thus providing possible solution for the non-linear part of shaly sandstone conductivity curve. The proposed mathematical equation provides good estimation of shaly sandstone formation factor F* for different types of data used for validation i.e established core data, field core data at overburden pressure from different regions and experimental data of collected shaly sandstone samples. |
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Thesis |
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WAN BAKAR, WAN ZAIRANI |
author_facet |
WAN BAKAR, WAN ZAIRANI |
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WAN BAKAR, WAN ZAIRANI |
title |
IMPROVED WATER SATURATION ESTIMATION IN SHALY SANDSTONE THROUGH CLAY MINERALS ELECTROCHEMICAL STUDY |
title_short |
IMPROVED WATER SATURATION ESTIMATION IN SHALY SANDSTONE THROUGH CLAY MINERALS ELECTROCHEMICAL STUDY |
title_full |
IMPROVED WATER SATURATION ESTIMATION IN SHALY SANDSTONE THROUGH CLAY MINERALS ELECTROCHEMICAL STUDY |
title_fullStr |
IMPROVED WATER SATURATION ESTIMATION IN SHALY SANDSTONE THROUGH CLAY MINERALS ELECTROCHEMICAL STUDY |
title_full_unstemmed |
IMPROVED WATER SATURATION ESTIMATION IN SHALY SANDSTONE THROUGH CLAY MINERALS ELECTROCHEMICAL STUDY |
title_sort |
improved water saturation estimation in shaly sandstone through clay minerals electrochemical study |
publishDate |
2021 |
url |
http://utpedia.utp.edu.my/id/eprint/24681/1/Wan%20Zairani%20Wan%20Bakar_G03281.pdf http://utpedia.utp.edu.my/id/eprint/24681/ |
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1770553580333301760 |
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13.214268 |