2001
DOI: 10.1016/b978-0-88415-317-7.x5000-3
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Geologic Analysis of Naturally Fractured Reservoirs

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Cited by 206 publications
(8 citation statements)
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“…We consider a fully penetrated well in an infinite porous media with a single porosity system, i.e., a Type I fractured system of Nelson [19], constant initial pressure, permeability, density and viscosity. Furthermore, we consider that the fluid flow at a given point is governed not only by the properties of the pressure field at that specific position but also depends on the global spatial distribution of that field, and lastly, we consider that the radial symmetry is valid.…”
Section: Model Developmentmentioning
confidence: 99%
“…We consider a fully penetrated well in an infinite porous media with a single porosity system, i.e., a Type I fractured system of Nelson [19], constant initial pressure, permeability, density and viscosity. Furthermore, we consider that the fluid flow at a given point is governed not only by the properties of the pressure field at that specific position but also depends on the global spatial distribution of that field, and lastly, we consider that the radial symmetry is valid.…”
Section: Model Developmentmentioning
confidence: 99%
“…Naturally Fractured Reservoirs (NFRs) are reservoirs with naturally occurring fractures that significantly impact porosity, permeability, production rate, and recovery (Narr et al, 2006;Nelson, 2001). Therefore, they differ considerably in many areas, including geology, geophysics, performance, and economics (Warren & Root, 1963).…”
Section: Implication Of Fracturesmentioning
confidence: 99%
“…Therefore, they differ considerably in many areas, including geology, geophysics, performance, and economics (Warren & Root, 1963). Nelson (2001) defined fractured reservoirs based on the impact of the fracture on porosity and permeability (He, Santoso, et al, 2021;He, Sinan, et al, 2021;Lyons et al, 2015;Nelson, 2001). The four types of fractures are summarized in Table 2 (Nelson, 2001).…”
Section: Implication Of Fracturesmentioning
confidence: 99%
“…Fault zones may cut across several geological units and provide catchment scale preferential flow paths in the form of strongly connected clusters of fractures (Bodvarsson et al, 1997;Flint et al, 2001; H. H. Liu et al, 2004). Tectonically induced stress fields and stress field changes generally promote the formation of local discontinuities, such as fractures, joints and fault zones in consolidated porous rocks (Ford & Williams, 2013;Neslon, 2001). What sets such features apart from typical pore space geometries is their strong anisotropic character, i.e., their length or spatial extent is orders of magnitude larger than their aperture.…”
Section: Accepted Articlementioning
confidence: 99%
“…H. Liu et al, 2004). Tectonically induced stress fields and stress field changes generally promote the formation of local discontinuities, such as fractures, joints, and fault zones in consolidated porous rocks (Ford & Williams, 2013;Neslon, 2001). What sets such features apart from typical pore space geometries is their strong anisotropic character, that is, their length or spatial extent is orders of magnitude larger than their aperture.…”
mentioning
confidence: 99%