Supercharge, Invasion, and Mudcake Growth in Downhole Applications. Группа авторов
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injection rate.Figure 5.15c. Q = 1, constant rate, high inertia flow.Figure 5.15d. Q = 2, constant rate, high inertia flow.Figure 5.15e. Q = 3, constant rate, high inertia flow.Figure 5.16. Mudcake-dominated invasion.Figure 5.17a. High filtration rate mudcake model (α = 1).Figure 5.17b. Very high filtration rate mudcake model (α = 5).Figure 5.17c. Very slow filtration rate model (α = 0.001).Figure 5.18. “Un-shocking” a steep gradient.Figure 5.19a. Forward shock formation.Figure 5.19b. Backward shock migration.Figure 5.20. Implicit pressure – implicit saturation solver.Figure 5.21a. Early time saturation and pressure.Figure 5.21b. Intermediate time saturation and pressure.Figure 5.21c. Late time saturation and pressure.Figure 5.22. Two-layer mudcake-rock, immiscible flow model.Figure 5.23a. Early time solution.Figure 5.23b. Intermediate time solution.Figure 5.23c. Late time solution.Figure 5.24a. Early time solution.Figure 5.24b. Intermediate time solution.Figure 5.24c. Late time solution.Figure 5.25a. COSL formation testing software platform.Figure 5.25b. COSL formation testing software platform.Figure 5.25c. COSL formation testing software platform.Figure 5.25d. COSL formation testing software platform.Figure 5.25e. COSL formation testing software platform.
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