Imaging porosity evolution of tight sandstone during spontaneous water imbibition by X-ray Micro-CT

被引:4
作者
Miletic, Marta [1 ]
Kucukuysal, Ceren [2 ,3 ]
Gulcan, Merve [2 ,3 ]
Garcia, Randy [1 ]
机构
[1] San Diego State Univ, Dept Civil Contruct & Environm Engn, San Diego, CA 92182 USA
[2] Mugla Sitki Kocman Univ, Engn Fac, Geol Engn Dept, Mugla, Turkiye
[3] Mugla Sitki Kocman Univ, Res Lab Ctr, Nat & Engn Geomat Lab, Mugla, Turkiye
关键词
Spontaneous capillary imbibition; X-ray computed tomography; Tight sandstone; Segmentation; Low permeability; Pore surface mineralogy; CENTRAL JUNGGAR BASIN; CLAY-MINERALS; WETTABILITY; MODEL; ROCKS; DISSOLUTION;
D O I
10.1016/j.heliyon.2024.e31844
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Water imbibition is an important process in reservoir rocks during hydraulic fracturing and waterbased enhanced oil recovery operations. However, the water imbibition behavior in tight sandstones has not been fully understood due to their complex pore structure, including the presence of nano and micron-sized pores and throats, surface properties, and wide variation in mineralogy. The present study focuses on the effect of spontaneous water imbibition on the porosity evolution of a tight sandstone. Within this context, a core of Torrey Buff sandstone was characterized by using a combination of multiscale imaging methods (X-ray Computed Tomography, Scanning Electron Microscopy), laboratory experiments (porosity-permeability measurements), and analytical techniques (X-ray Diffraction, Fourier Transform Infrared Spectroscopy, Scanning Electron Microscopy-Energy Dispersive Spectroscopy, and Thermogravimetry). The studied tight sandstone core has a porosity of 12.3 % and permeability of 2.05mD with minerals of quartz (58 %), clays (kaolinite and illite, 23 %), K-feldspar (7 %), dolomite (7 %) and calcite (5 %). Primary and secondary pores, ranging in size from 60 to 140 mu m and 30-50 mu m, respectively, are mostly filled with highly-soluble carbonate minerals and hydrophilic illite, which influence the spontaneous water imbibition capacity of the tight sandstone. The multiscale imaging technique indicates that after a 10-h long water imbibition experiment, the average pore size of the tight sandstone increased by 1.28 %, reaching 2.35 % at the rock-water contact and 0.13 % at the top of the core. In other words, throughout the core, the porosity changes upon water imbibition are not uniform but show an almost linear trend. This observation could be explained by the significant contribution of highly-soluble carbonates and hydrophilic illite on the microstructure of the tight sandstone. This study implies that multiscale imaging techniques, crucial in examining spontaneous water imbibition, hold promise for further research in enhanced oil recovery or hydraulic fracking in tight sandstones.
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页数:9
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