TY - JOUR
T1 - Workflow for Upscaling Wettability From the Nanoscale to Core Scale
AU - Rucker, Maja
AU - Bartels, Willem-Bart
AU - Bultreys, Tom
AU - Boone, Marijn
AU - Singh, Kamaljit
AU - Garfi, Gaetano
AU - Scanziani, Alessio
AU - Spurin, Catherine
AU - Yesufu-Rufai, Sherifat
AU - Krevor, Samuel
AU - Blunt, Martin J.
AU - Wilson, Ove
AU - Mahani, Hassan
AU - Cnudde, Veerle
AU - Luckham, Paul F.
AU - Georgiadis, Apostolos
AU - Berg, Steffen
PY - 2020/4
Y1 - 2020/4
N2 - Wettability is a key factor influencing multiphase flow in porous media. In addition to the average contact angle, the spatial distribution of contact angles throughout the porous medium is important, as it directly controls the connectivity of wetting and nonwetting phases. The controlling factors may not only relate to the surface chemistry of minerals but also to their texture, which implies that a length-scale range from nanometers to centimeters has to be considered. So far, an integrated workflow addressing wettability consistently through the different scales does not exist. In this study, we demonstrate that such a workflow is possible by combining microcomputed tomography (uCT) imaging with atomic-force microscopy (AFM). We find that in a carbonate rock, consisting of 99.9% calcite with a dual-porosity structure, wettability is ultimately controlled by the surface texture of the mineral. Roughness and texture variation within the rock control the capillary pressure required for initializing proper crude oil-rock contacts that allow aging and subsequent wettability alteration. AFM enables us to characterize such surface-fluid interactions and to investigate the surface texture. In this study, we use AFM to image nanoscale fluid-configurations in 3D at connate water saturation and compare the fluid configuration with simulations on the rock surface, assuming different capillary pressures.
AB - Wettability is a key factor influencing multiphase flow in porous media. In addition to the average contact angle, the spatial distribution of contact angles throughout the porous medium is important, as it directly controls the connectivity of wetting and nonwetting phases. The controlling factors may not only relate to the surface chemistry of minerals but also to their texture, which implies that a length-scale range from nanometers to centimeters has to be considered. So far, an integrated workflow addressing wettability consistently through the different scales does not exist. In this study, we demonstrate that such a workflow is possible by combining microcomputed tomography (uCT) imaging with atomic-force microscopy (AFM). We find that in a carbonate rock, consisting of 99.9% calcite with a dual-porosity structure, wettability is ultimately controlled by the surface texture of the mineral. Roughness and texture variation within the rock control the capillary pressure required for initializing proper crude oil-rock contacts that allow aging and subsequent wettability alteration. AFM enables us to characterize such surface-fluid interactions and to investigate the surface texture. In this study, we use AFM to image nanoscale fluid-configurations in 3D at connate water saturation and compare the fluid configuration with simulations on the rock surface, assuming different capillary pressures.
UR - http://www.scopus.com/inward/record.url?scp=85090587276&partnerID=8YFLogxK
U2 - 10.30632/PJV61N2-2020a5
DO - 10.30632/PJV61N2-2020a5
M3 - Article
SN - 1529-9074
VL - 61
SP - 189
EP - 205
JO - Petrophysics
JF - Petrophysics
IS - 2
ER -