2018
DOI: 10.1016/s1876-3804(18)30041-7
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Production prediction for fracture-vug carbonate reservoirs using electric imaging logging data

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Cited by 13 publications
(3 citation statements)
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“…Building upon previous models of singular inclined fractures and inclined slab-like fractures [16,17], we developed three types of fractured formation models according to the geometric relationship between the fracture orientation, borehole radius, and detection depth of the deep lateral resistivity log of the dual laterolog tool: (i) The intersection of the fracture plane with the bottom plane of the electrode column is outside the radial detection depth of the electrode (Figure 2a). The angle between the fracture plane and the bottom plane of the electrode column is the fracture inclination angle θ, in degrees; the vertical distance between the two walls of the fracture represents the fracture width w, in µm; the borehole radius is denoted as r, in m; the radial detection depth of the deep laterolog is r 1 , in m; and the height of the cylindrical main current of the deep laterolog is H, in m, which is typically 0.74 m. In all models, the effective conductive medium is analogous to that of a vuggy reservoir.…”
Section: Fractured Reservoirsmentioning
confidence: 99%
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“…Building upon previous models of singular inclined fractures and inclined slab-like fractures [16,17], we developed three types of fractured formation models according to the geometric relationship between the fracture orientation, borehole radius, and detection depth of the deep lateral resistivity log of the dual laterolog tool: (i) The intersection of the fracture plane with the bottom plane of the electrode column is outside the radial detection depth of the electrode (Figure 2a). The angle between the fracture plane and the bottom plane of the electrode column is the fracture inclination angle θ, in degrees; the vertical distance between the two walls of the fracture represents the fracture width w, in µm; the borehole radius is denoted as r, in m; the radial detection depth of the deep laterolog is r 1 , in m; and the height of the cylindrical main current of the deep laterolog is H, in m, which is typically 0.74 m. In all models, the effective conductive medium is analogous to that of a vuggy reservoir.…”
Section: Fractured Reservoirsmentioning
confidence: 99%
“…Due to their intense heterogeneity, carbonate reservoirs exhibit features of secondary porosity, including dissolution-enhanced Processes 2024, 12, 43 2 of 21 fractures and vugs, making their microscopic pore structures exceedingly complex [6,14,15]. These complex fractured-cavernous structures in carbonate reservoirs result in inexplicable resistivity response patterns [16][17][18], such as numerous layers with anomalously high resistivity, dense layers with low resistivity, and water-bearing layers with high resistivity. Hence, examining the effects of these fractured-cavernous structures on the resistivity of geofluid-saturated rocks is important to deepen the understanding of their resistivity response patterns, identify their fluid properties, and evaluate their fluid saturation state during the exploration and development of complex fractured-cavernous carbonate hydrocarbon reservoirs.…”
Section: Introductionmentioning
confidence: 99%
“…When the pores within a cave are relatively large and exhibit good connectivity, the flow inside the cave can be considered laminar flow. Furthermore, the laminar flow of incompressible viscous fluids in narrow conduits can be equivalent to Hagen-Poiseuille flow (Xie et al, 2018;Lin et al, 2021). Therefore, the fluid flow within the cave can be approximated as Hagen-Poiseuille flow, enabling the coupling of flow between different media.…”
Section: Introductionmentioning
confidence: 99%