Abstract
The efficiency of carbon utilization and storage within the Pennsylvanian Morrow B sandstone, Farnsworth Unit, Texas, is dependent on three-phase oil, brine, and CO2 flow behavior, as well as spatial distributions of reservoir properties and wettability. We show that end member two-phase flow properties, with binary pairs of oil–brine and oil–CO2, are directly dependent on heterogeneity derived from diagenetic processes, and evolve progressively with exposure to CO2 and changing wettability. Morrow B sandstone lithofacies exhibit a range of diagenetic processes, which produce variations in pore types and structures, quantified at the core plug scale using X-ray micro computed tomography imaging and optical petrography. Permeability and porosity relationships in the reservoir permit the classification of sedimentologic and diagenetic heterogeneity into five distinct hydraulic flow units, with characteristic pore types including: macroporosity with little to no clay filling intergranular pores; microporous authigenic clay-dominated regions in which intergranular porosity is filled with clay; and carbonate–cement dominated regions with little intergranular porosity. Steady-state oil–brine and oil–CO2 co-injection experiments using reservoir-extracted oil and brine show that differences in relative permeability persist between flow unit core plugs with near-constant porosity, attributable to contrasts in and the spatial arrangement of diagenetic pore types. Core plugs “aged” by exposure to reservoir oil over time exhibit wettability closer to suspected in situ reservoir conditions, compared to “cleaned” core plugs. Together with contact angle measurements, these results suggest that reservoir wettability is transient and modified quickly by oil recovery and carbon storage operations. Reservoir simulation results for enhanced oil recovery, using a five-spot pattern and water-alternating-with-gas injection history at Farnsworth, compare models for cumulative oil and water production using both a single relative permeability determined from history matching, and flow unit-dependent relative permeability determined from experiments herein. Both match cumulative oil production of the field to a satisfactory degree but underestimate historical cumulative water production. Differences in modeled versus observed water production are interpreted in terms of evolving wettability, which we argue is due to the increasing presence of fast paths (flow pathways with connected higher permeability) as the reservoir becomes increasingly water-wet. The control of such fast-paths is thus critical for efficient carbon storage and sweep efficiency for CO2-enhanced oil recovery in heterogeneous reservoirs.
Highlights
IntroductionEnhanced oil recovery (EOR) utilizing reservoir flooding with high density supercritical carbon dioxide (scCO2 ) is a means to mitigate rising atmospheric carbon dioxide levels while extracting oil as an energy resource, with a net storage of carbon in geologic units (often termed carbon capture, utilization, and storage or CCUS)
Enhanced oil recovery (EOR) utilizing reservoir flooding with high density supercritical carbon dioxide is a means to mitigate rising atmospheric carbon dioxide levels while extracting oil as an energy resource, with a net storage of carbon in geologic units
The efficient management of CCUS in a reservoir or field involves assessing the heterogeneity and behavior of flow for three-phase oil, brine, and scCO2 transport, and to this end, in this paper we examine these for the Morrow B sandstone reservoir of the Farnsworth Unit (FWU)
Summary
Enhanced oil recovery (EOR) utilizing reservoir flooding with high density supercritical carbon dioxide (scCO2 ) is a means to mitigate rising atmospheric carbon dioxide levels while extracting oil as an energy resource, with a net storage of carbon in geologic units (often termed carbon capture, utilization, and storage or CCUS). The focus of EOR/CCUS is on depleted oil reservoirs, and an example of this is the Farnsworth Unit (FWU) of West Texas (Figure 1), which has been in operation since the. The efficient management of CCUS in a reservoir or field involves assessing the heterogeneity and behavior of flow for three-phase oil, brine, and scCO2 transport, and to this end, in this paper we examine these for the Morrow B sandstone reservoir (part of the Pennsylvanian Morrow Formation) of the FWU. The Morrow B sandstone is the target reservoir for the FWU project, located at a depth between 7550 ft (2301 m) and 7950 ft (2432 m) and spanning approximately 28 square miles (72 km2 ) with a mean thickness of 24.3 ft (7.4 m; Figure 1B,C; see [7]). The Morrow B sandstone underlies an upper Morrow Formation shale and the Thirteen
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