2021
DOI: 10.1155/2021/8824090
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Numerical Simulation Study on Waterflooding Heavy Oil Based on Variable Threshold Pressure Gradient

Abstract: The heavy-oil flow in porous media is characterized by non-Darcy law with variable threshold pressure gradient (TPG) due to the large fluid viscosity. However, available analytical and numerical models hardly consider this effect, which can lead to erroneous results. This paper is aimed at presenting an innovative approach and establishing a numerical simulator to analyze the heavy-oil flow behavior with waterflooding. The apparent viscosity of the oil phase and flow correction coefficient characterized by the… Show more

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Cited by 2 publications
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“…In general, the water phase exerts resistance on the motion of the oil phase through the oil–water two-phase flow of shale oil, which results in the flow behavior of the whole fluid showing the characteristics of Bingham fluid. , Moreover, due to the adsorption of polar substances in shale oil on the rock surface, a boundary layer is formed, and there is interfacial molecular force η between boundary layer fluid, bulk phase fluid, and pores. , In physical terms, for Bingham fluid flow through an unsaturated porous media with the porosity of ϕ under a pressure drop of Δ P , the Bingham fluid will be subjected to the driving force (i.e., pressure drop Δ P ), capillary pressure, viscous force, and interfacial molecular force. Based on the assumption that the pressure drop and effective stress are uniformly distributed in the pore space, and the oil phase flows through the capillary with constant speed, according to the Newton’s second law, we have , true( normalΔ P F γ nobreak0em0.25em⁡ normalcos nobreak0em.25em⁡ θ normald 2 r · 1 ϕ ϕ true) π false( r δ false) 2 true( τ 0 + μ normald v normald r true) 2 π false( r δ false) L t η r 2 π false( r δ false) L t = 0 where F is the shape factor, which is assigned as 4, γ is the oil–water interfacial tension, θ d denotes the dynamic contact angle, r is the effective pore radius, δ is the thickness of water film attached to the boundary layer, τ 0 is ultimate shear stress, μ is the viscosity of a fluid, v means the velocity, and L t denotes the actual capillary length.…”
Section: Methodsmentioning
confidence: 99%
“…In general, the water phase exerts resistance on the motion of the oil phase through the oil–water two-phase flow of shale oil, which results in the flow behavior of the whole fluid showing the characteristics of Bingham fluid. , Moreover, due to the adsorption of polar substances in shale oil on the rock surface, a boundary layer is formed, and there is interfacial molecular force η between boundary layer fluid, bulk phase fluid, and pores. , In physical terms, for Bingham fluid flow through an unsaturated porous media with the porosity of ϕ under a pressure drop of Δ P , the Bingham fluid will be subjected to the driving force (i.e., pressure drop Δ P ), capillary pressure, viscous force, and interfacial molecular force. Based on the assumption that the pressure drop and effective stress are uniformly distributed in the pore space, and the oil phase flows through the capillary with constant speed, according to the Newton’s second law, we have , true( normalΔ P F γ nobreak0em0.25em⁡ normalcos nobreak0em.25em⁡ θ normald 2 r · 1 ϕ ϕ true) π false( r δ false) 2 true( τ 0 + μ normald v normald r true) 2 π false( r δ false) L t η r 2 π false( r δ false) L t = 0 where F is the shape factor, which is assigned as 4, γ is the oil–water interfacial tension, θ d denotes the dynamic contact angle, r is the effective pore radius, δ is the thickness of water film attached to the boundary layer, τ 0 is ultimate shear stress, μ is the viscosity of a fluid, v means the velocity, and L t denotes the actual capillary length.…”
Section: Methodsmentioning
confidence: 99%