Determination of contact angles for three-phase flow in porous media using an energy balance

被引:21
作者
Blunt, Martin J. [1 ]
Alhosani, Abdulla [1 ]
Lin, Qingyang [1 ]
Scanziani, Alessio [1 ]
Bijeljic, Branko [1 ]
机构
[1] Imperial Coll London, Dept Earth Sci & Engn, London SW7 2BP, England
关键词
Contact angle; Imaging; Wettability; Multiphase flow in porous media; Curvature; Three-phase flow; IN-SITU CHARACTERIZATION; PORE-SCALE; WATER; OIL; WETTABILITY; SANDSTONE;
D O I
10.1016/j.jcis.2020.07.152
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Hypothesis: We define contact angles, theta, during displacement of three fluid phases in a porous medium using energy balance, extending previous work on two-phase flow. We test if this theory can be applied to quantify the three contact angles and wettability order in pore-scale images of three-phase displacement. Theory: For three phases labelled 1, 2 and 3, and solid, s, using conservation of energy ignoring viscous dissipation (Delta alpha(1s) cos theta(12) - Delta alpha(12) phi kappa(12)Delta S-1)sigma(12) = (Delta alpha(3s) cos theta(23) Delta alpha(23) phi kappa(23)Delta S-3)sigma(23) Delta alpha(13)sigma(13), where phi is the porosity, sigma is the interfacial tension, alpha is the specific interfacial area, S is the saturation, and kappa is the fluid-fluid interfacial curvature. A represents the change during a displacement. The third contact angle, theta(13) can be found using the Bartell-Osterhof relationship. The energy balance is also extended to an arbitrary number of phases. Findings: X-ray imaging of porous media and the fluids within them, at pore-scale resolution, allows the difference terms in the energy balance equation to be measured. This enables wettability, the contact angles, to be determined for complex displacements, to characterize the behaviour, and for input into pore-scale models. Two synchrotron imaging datasets are used to illustrate the approach, comparing the flow of oil, water and gas in a water-wet and an altered-wettability limestone rock sample. We show that in the water-wet case, as expected, water (phase 1) is the most wetting phase, oil (phase 2) is intermediate wet, while gas (phase 3) is most non-wetting with effective contact angles of theta(12) approximate to 48 degrees and theta(13) 44 degrees, while theta(23) approximate to 0 since oil is always present in spreading layers. In contrast, for the alteredwettability case, oil is most wetting, gas is intermediate-wet, while water is most non-wetting with contact angles of theta(12) approximate to 134 degrees +/- similar to 10 degrees; theta(13) =119 degrees +/-similar to 10 degrees, and theta(23) = 66 degrees +/-similar to 10 degrees. (C) 2020 The Author(s). Published by Elsevier Inc.
引用
收藏
页码:283 / 290
页数:8
相关论文
共 47 条
  • [1] USE OF THE TERM YOUNGS EQUATION FOR CONTACT ANGLES
    ADAM, NK
    [J]. NATURE, 1957, 180 (4590) : 809 - 810
  • [2] Using energy balance to determine pore-scale wettability
    Akai, Takashi
    Lin, Qingyang
    Bijeljic, Branko
    Blunt, Martin J.
    [J]. JOURNAL OF COLLOID AND INTERFACE SCIENCE, 2020, 576 : 486 - 495
  • [3] Quantification of Uncertainty and Best Practice in Computing Interfacial Curvature from Complex Pore Space Images
    Akai, Takashi
    Lin, Qingyang
    Alhosani, Abdulla
    Bijeljic, Branko
    Blunt, Martin J.
    [J]. MATERIALS, 2019, 12 (13)
  • [4] Pore-scale mechanisms of CO2 storage in oilfields
    Alhosani, Abdulla
    Scanziani, Alessio
    Lin, Qingyang
    Raeini, Ali Q.
    Bijeljic, Branko
    Blunt, Martin J.
    [J]. SCIENTIFIC REPORTS, 2020, 10 (01)
  • [5] In situ pore-scale analysis of oil recovery during three-phase near-miscible CO2 injection in a water-wet carbonate rock
    Alhosani, Abdulla
    Scanziani, Alessio
    Lin, Qingyang
    Pan, Ziqing
    Bijeljic, Branko
    Blunt, Martin J.
    [J]. ADVANCES IN WATER RESOURCES, 2019, 134
  • [6] Automatic measurement of contact angle in pore-space images
    AlRatrout, Ahmed
    Raeini, Ali Q.
    Bijeljic, Branko
    Blunt, Martin J.
    [J]. ADVANCES IN WATER RESOURCES, 2017, 109 : 158 - 169
  • [7] Pore-scale imaging of trapped supercritical carbon dioxide in sandstones and carbonates
    Andrew, Matthew
    Bijeljic, Branko
    Blunt, Martin J.
    [J]. INTERNATIONAL JOURNAL OF GREENHOUSE GAS CONTROL, 2014, 22 : 1 - 14
  • [8] Pore-scale contact angle measurements at reservoir conditions using X-ray microtomography
    Andrew, Matthew
    Bijeljic, Branko
    Blunt, Martin J.
    [J]. ADVANCES IN WATER RESOURCES, 2014, 68 : 24 - 31
  • [9] [Anonymous], 2017, A Pore-scale Perspective
  • [10] Linking pore-scale interfacial curvature to column-scale capillary pressure
    Armstrong, Ryan T.
    Porter, Mark L.
    Wildenschild, Dorthe
    [J]. ADVANCES IN WATER RESOURCES, 2012, 46 : 55 - 62