Pore-Scale Imaging of the Oil Cluster Dynamic during Drainage and Imbibition Using In Situ X-Ray Microtomography

被引:18
作者
Li, Junjian [1 ]
Gao, Yajun [1 ,2 ]
Jiang, Hanqiao [1 ]
Liu, Yang [1 ]
Dong, Hu [3 ]
机构
[1] China Univ Petr, State Key Lab Petr Resources & Prospecting, Beijing 102249, Peoples R China
[2] CNOOC Res Inst Co Ltd, Beijing 100028, Peoples R China
[3] iRock Technol Co Ltd, Beijing 100094, Peoples R China
关键词
MIXED-WET; MULTIPHASE FLOW; CONTACT-ANGLE; PERCOLATION; SATURATION; CAPILLARY; WETTABILITY; MORPHOLOGY; CURVATURE; SANDSTONE;
D O I
10.1155/2018/7679607
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We imaged water-wet and oil-wet sandstones under two-phase flow conditions for different flooding states by means of X-ray computed microtomography (mu CT) with a spatial resolution of 2.1 mu m/pixel. We systematically study pore-scale trapping of the nonwetting phase as well as size and distribution of its connected clusters and disconnected globules. We found a lower S-or, 19.8%, for the oil-wet plug than for water-wet plug (25.2%). Approximate power-law distributions of the water and oil cluster sizes were observed in the pore space. Besides, the tau value of the wetting phase gradually decreased and the nonwetting phase gradually increased during the core-flood experiment. The remaining oil has been divided into five categories; we explored the pore fluid occupancies and studied size and distribution of the five types of trapped oil clusters during different drainage stage. The result shows that only the relative volume of the clustered oil is reduced, and the other four types of remaining oil all increased. Pore structure, wettability, and its connectivity have a significant effect on the trapped oil distribution. In the water sandstone, the trapped oil tends to occupy the center of the larger pores during the water imbibition process, leading to a stable specific surface area and a gradually decreasing oil capillary pressure. Meanwhile, in oil-wet sandstone, the trapped oil blobs that tend to occupy the pores corner and attach to the walls of the pores have a large specific surface area, and the change of the oil capillary pressure was not obvious. These results have revealed the well-known complexity of multiphase flow in rocks and preliminarily show the pore-level displacement physics of the process.
引用
收藏
页数:13
相关论文
共 40 条
  • [1] AMOTT E, 1959, T AM I MIN MET ENG, V216, P156
  • [2] 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
  • [3] 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
  • [4] Pore-scale imaging of geological carbon dioxide storage under in situ conditions
    Andrew, Matthew
    Bijeljic, Branko
    Blunt, Martin J.
    [J]. GEOPHYSICAL RESEARCH LETTERS, 2013, 40 (15) : 3915 - 3918
  • [5] 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
  • [6] BLUNT M, 1991, TRANSPORT POROUS MED, V6, P407, DOI 10.1007/BF00136349
  • [7] Blunt M. J., 1992, PHYS REV A, V46, P12
  • [8] A non-local algorithm for image denoising
    Buades, A
    Coll, B
    Morel, JM
    [J]. 2005 IEEE COMPUTER SOCIETY CONFERENCE ON COMPUTER VISION AND PATTERN RECOGNITION, VOL 2, PROCEEDINGS, 2005, : 60 - 65
  • [9] The impact of transitions between two-fluid and three-fluid phases on fluid configuration and fluid-fluid interfacial area in porous media
    Carroll, Kenneth C.
    McDonald, Kieran
    Marble, Justin
    Russo, Ann E.
    Brusseau, Mark L.
    [J]. WATER RESOURCES RESEARCH, 2015, 51 (09) : 7189 - 7201
  • [10] Pore-scale multiphase flow experiments in bead packs of variable wettability
    Celauro, J. G.
    Torrealba, V. A.
    Karpyn, Z. T.
    Klise, K. A.
    McKenna, S. A.
    [J]. GEOFLUIDS, 2014, 14 (01) : 95 - 105