A New Model for Simulating the Imbibition of a Wetting-Phase Fluid in a Matrix-Fracture Dual Connectivity System

Journal Article · 31 January 2022 · Geofluids

DOI: https://doi.org/10.1155/2022/7408123 · OSTI ID:1843071

Ning, Xuewei ^[1]; Ewing, Robert ^[2]; Hu, Qinhong  ^[1]; Wang, Qiming ^[1]; Zhang, Xiaoming ^[3]; Chen, ed., Zhiming

---

1. Department of Earth and Environmental Sciences, The University of Texas at Arlington, TX 76019, USA
2. The Climate Corporation, 710 2nd Ave., Seattle, WA 98104, USA
3. Department of Earth and Environmental Sciences, The University of Texas at Arlington, TX 76019, USA, Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, China University of Geosciences, Wuhan 430074, China, Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China

The imbibition experiment is an effective approach for measuring petrophysical properties of porous media, with many such experiments performed over the past decade. Quite some empirical, analytical, and numerical models have been developed to simulate spontaneous imbibition of the wetting phase fluid into porous media, but limitations still exist. In previous studies, the imbibition process has been considered to give a piston-like displacement or the porous medium modeled as multiply-sized pores linked with bonds; both approaches fail to yield comprehensive results due to their neglect of the presence of irregular fractures or nonuniform flow paths through the matrix. By building a numerical model for simulating laboratory-scale experimental data, we performed imbibition tests on several fractured Barnett Shale samples having fractures either parallel ( $P$ ) or transverse ( $T$ ) to the bedding plane and used MATLAB to build a new numerical model by combining the imbibition process in fractures and the matrix using concepts from percolation theory. The experimental data show that the rocks with $P$ -direction fractures have a more steady increase of imbibition rates than the case of $T$ -direction one. As the shale matrix with low pore connectivity hampers the upward water movement, the imbibition rate of shales with $T$ -direction fractures will decrease suddenly after the bottom layer in contact with water is saturated during the initial period. This wetting phase movement (WPM) model can simulate 3D porous media with 2D fractures. The rate of imbibition by fractured porous media is associated with physical parameters such as porosity and fracture distribution (e.g., the number and angle of fractures). Using Monte Carlo methods, we examined fracture parameters and predicted elapsed time and cumulative water imbibition, for the Barnett Shale samples. The results show that the rate of imbibed water mass is sensitive to the number of fractures directly connected to water source, and the connectivity between two neighboring grid cells is a key parameter for the wetting-front progression. The findings of this study can help to better understand the imbibition process with multiple influencing processes and factors in fractured-matrix rocks. Although the experiments, data simulation, and prediction results are based only on Barnett Shale samples, the model is readily applicable to imbibition tests of other fractured rocks to show the spatial and temporal behavior during a dynamic imbibition process that are not easily captured experimentally.

• Research Organization: Univ. of Texas, Arlington, TX (United States)
• Sponsoring Organization: USDOE; USDOE Office of Nuclear Energy (NE)
• Grant/Contract Number: NE0008797
• OSTI ID: 1843071
• Journal Information: Geofluids, Journal Name: Geofluids Vol. 2022; ISSN 1468-8115
• Publisher: Hindawi Publishing CorporationCopyright Statement
• Country of Publication: Canada
• Language: English