The Role of the Mineralogical Composition on Wettability via Flotation Test and Surface Complexation Modeling (SCM)

Minerals are the chief constituents of rocks and have varied properties, such as the surface area, surface charge, site density, etc. Hence, numerous interactions are bound to occur in a reservoir during rock–fluid (i.e., rock, crude oil and brine) interactions. This study seeks to assess the role o...

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Main Authors: Samuel Erzuah, Ingebret Fjelde, Aruoture Voke Omekeh
Format: Article
Language:English
Published: MDPI AG 2024-02-01
Series:Geosciences
Subjects:
Online Access:https://www.mdpi.com/2076-3263/14/2/47
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author Samuel Erzuah
Ingebret Fjelde
Aruoture Voke Omekeh
author_facet Samuel Erzuah
Ingebret Fjelde
Aruoture Voke Omekeh
author_sort Samuel Erzuah
collection DOAJ
description Minerals are the chief constituents of rocks and have varied properties, such as the surface area, surface charge, site density, etc. Hence, numerous interactions are bound to occur in a reservoir during rock–fluid (i.e., rock, crude oil and brine) interactions. This study seeks to assess the role of the mineralogical composition in the wettability of sandstone rocks (SRs) and mineral mixture (MM) using both surface complexation modeling (SCM) and a flotation test. From the considered sandstone rocks, both the experimental results and the simulated counterparts revealed that the SRs were preferentially hydrophilic. For the MM, when the mass fraction of the hydrophobic mineral was increased, the affinity of the MM became slightly hydrophobic, and vice versa. For the dominant sandstone reservoir rock minerals with predominantly negatively charged surfaces, negligible oil adsorption took place due to the interfacial repulsive forces at the oil–brine and mineral–brine interfaces. For the MM with low calcite content, the wetting preference was influenced by the mineral with a prominent surface area. Our developed model portrayed that the main mechanism of oil adhesion onto sandstone minerals was divalent cation bridging. Nonetheless, adhesion of carboxylate (>COO<sup>−</sup>) onto the illite, montmorillonite and calcite sites also took place, with the latter being more pronounced.
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spelling doaj.art-b7bca82116264427941b05ddcbdf0afd2024-02-23T15:18:04ZengMDPI AGGeosciences2076-32632024-02-011424710.3390/geosciences14020047The Role of the Mineralogical Composition on Wettability via Flotation Test and Surface Complexation Modeling (SCM)Samuel Erzuah0Ingebret Fjelde1Aruoture Voke Omekeh2Department of Petroleum Engineering, Faculty of Civil and Geo-Engineering, Kwame Nkrumah University of Science & Technology, Kumasi 00233, GhanaNORCE Norwegian Research Centre, 4068 Stavanger, NorwayNORCE Norwegian Research Centre, 4068 Stavanger, NorwayMinerals are the chief constituents of rocks and have varied properties, such as the surface area, surface charge, site density, etc. Hence, numerous interactions are bound to occur in a reservoir during rock–fluid (i.e., rock, crude oil and brine) interactions. This study seeks to assess the role of the mineralogical composition in the wettability of sandstone rocks (SRs) and mineral mixture (MM) using both surface complexation modeling (SCM) and a flotation test. From the considered sandstone rocks, both the experimental results and the simulated counterparts revealed that the SRs were preferentially hydrophilic. For the MM, when the mass fraction of the hydrophobic mineral was increased, the affinity of the MM became slightly hydrophobic, and vice versa. For the dominant sandstone reservoir rock minerals with predominantly negatively charged surfaces, negligible oil adsorption took place due to the interfacial repulsive forces at the oil–brine and mineral–brine interfaces. For the MM with low calcite content, the wetting preference was influenced by the mineral with a prominent surface area. Our developed model portrayed that the main mechanism of oil adhesion onto sandstone minerals was divalent cation bridging. Nonetheless, adhesion of carboxylate (>COO<sup>−</sup>) onto the illite, montmorillonite and calcite sites also took place, with the latter being more pronounced.https://www.mdpi.com/2076-3263/14/2/47mineralogymineral mixturesurface complexation modeling (SCM)flotation testelectrostatic pair linkagebond product (BP)
spellingShingle Samuel Erzuah
Ingebret Fjelde
Aruoture Voke Omekeh
The Role of the Mineralogical Composition on Wettability via Flotation Test and Surface Complexation Modeling (SCM)
Geosciences
mineralogy
mineral mixture
surface complexation modeling (SCM)
flotation test
electrostatic pair linkage
bond product (BP)
title The Role of the Mineralogical Composition on Wettability via Flotation Test and Surface Complexation Modeling (SCM)
title_full The Role of the Mineralogical Composition on Wettability via Flotation Test and Surface Complexation Modeling (SCM)
title_fullStr The Role of the Mineralogical Composition on Wettability via Flotation Test and Surface Complexation Modeling (SCM)
title_full_unstemmed The Role of the Mineralogical Composition on Wettability via Flotation Test and Surface Complexation Modeling (SCM)
title_short The Role of the Mineralogical Composition on Wettability via Flotation Test and Surface Complexation Modeling (SCM)
title_sort role of the mineralogical composition on wettability via flotation test and surface complexation modeling scm
topic mineralogy
mineral mixture
surface complexation modeling (SCM)
flotation test
electrostatic pair linkage
bond product (BP)
url https://www.mdpi.com/2076-3263/14/2/47
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