FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2023184286> ?p ?o ?g. }

• W2023184286 abstract "Abstract The objective of this paper is to investigate the transient pressure behavior of naturally fractured reservoirs with fractal characteristics. This work is based on the findings of previous studies where it is shown that the networks of fractures in some reservoirs are fractals. Thus, using this assumption, an approximate analytical solution for dual-porosity systems is derived in the Laplace space. The approximate solution presented in this work uses a pseudo-steady state matrix-to-fractal fracture transfer function. This solution is compared with a finite element solution and good agreement is found. Short- and long-time approximations are used to obtain procedures in time to determine some fractal parameters. These approximations are compared to the appropriate expressions when an unsteady-state matrix-to-fractal fracture transfer function is used. Synthetic and field examples are presented to illustrate the methodology proposed in this work. This paper also presents an analytical solution for the pseudo-steady-state flow period and demonstrates the importance of analyzing both transient and pseudo-steady-state flow pressure data for a single-well situation in order to fully characterize a naturally fractured reservoir with a fractal geometry. Introduction Reservoir heterogeneity influences fluid flow trajectories. These heterogeneities are present on a wide range of scales. Fractal theory provides a method to describe the network of fractures in a rock and to connect heterogeneities at smaller scales to those at larger scales and vice versa. The simplest fractal models assume a power law scaling procedure where the exponent is related to the fractal dimension, which is the main tool of fractal geometry. The dimension provides a description of how much space the set of fractures fills, it contains much information about the geometrical properties of the set of fractures. Thus, this fractal parameter describes variations over a range of scales and if it can be estimated, reservoir properties such as porosity and permeability can be properly defined. Chang and Yortsos1 applied a fractal model to pressure transient analysis. This model describes a naturally fractured system which has different scales, poor fracture connectivity and disorderly spatial distribution in a proper fashion. Acuña et. al.2 applied this model to analyze pressure transient tests and they (as Ref. 1 did) found out that the change in wellbore pressure is a power-law function of time, where the fracton or spectral dimension can be obtained. This parameter is a function of both fractal dimension and the conductivity index, which is related to the topology of fractures network. Both Refs. 1 and 2 point out that to determine the values of fractal parameters additional information to the transient test is needed. Olarewaju3 also examined the pressure transient response of naturally fractured reservoirs by using a fractal model, but instead of assuming a pseudo-steady state transfer function between matrix and fracture systems as Refs. 1 and 2 did, he used a transient interporosity flow assumption. Beier4 extended the fractal model of Chang and Yortsos1 to consider a hydraulic fractured well. He also observed a power-law behavior during the linear and radial flow periods." @default.
• W2023184286 created "2016-06-24" @default.
• W2023184286 creator A5015346441 @default.
• W2023184286 creator A5075472259 @default.
• W2023184286 date "2001-09-30" @default.
• W2023184286 modified "2023-10-17" @default.
• W2023184286 title "Fractal Transient Pressure Behavior of Naturally Fractured Reservoirs" @default.
• W2023184286 doi "https://doi.org/10.2118/71591-ms" @default.
• W2023184286 hasPublicationYear "2001" @default.
• W2023184286 type Work @default.
• W2023184286 sameAs 2023184286 @default.
• W2023184286 citedByCount "21" @default.
• W2023184286 countsByYear W20231842862012 @default.
• W2023184286 countsByYear W20231842862013 @default.
• W2023184286 countsByYear W20231842862014 @default.
• W2023184286 countsByYear W20231842862015 @default.
• W2023184286 countsByYear W20231842862016 @default.
• W2023184286 countsByYear W20231842862018 @default.
• W2023184286 countsByYear W20231842862019 @default.
• W2023184286 countsByYear W20231842862020 @default.
• W2023184286 countsByYear W20231842862021 @default.
• W2023184286 countsByYear W20231842862022 @default.
• W2023184286 crossrefType "proceedings-article" @default.
• W2023184286 hasAuthorship W2023184286A5015346441 @default.
• W2023184286 hasAuthorship W2023184286A5075472259 @default.
• W2023184286 hasConcept C111919701 @default.
• W2023184286 hasConcept C127313418 @default.
• W2023184286 hasConcept C134306372 @default.
• W2023184286 hasConcept C2780799671 @default.
• W2023184286 hasConcept C33923547 @default.
• W2023184286 hasConcept C40636538 @default.
• W2023184286 hasConcept C41008148 @default.
• W2023184286 hasConceptScore W2023184286C111919701 @default.
• W2023184286 hasConceptScore W2023184286C127313418 @default.
• W2023184286 hasConceptScore W2023184286C134306372 @default.
• W2023184286 hasConceptScore W2023184286C2780799671 @default.
• W2023184286 hasConceptScore W2023184286C33923547 @default.
• W2023184286 hasConceptScore W2023184286C40636538 @default.
• W2023184286 hasConceptScore W2023184286C41008148 @default.
• W2023184286 hasLocation W20231842861 @default.
• W2023184286 hasOpenAccess W2023184286 @default.
• W2023184286 hasPrimaryLocation W20231842861 @default.
• W2023184286 hasRelatedWork W1980505004 @default.
• W2023184286 hasRelatedWork W1983294024 @default.
• W2023184286 hasRelatedWork W2001071460 @default.
• W2023184286 hasRelatedWork W2006206799 @default.
• W2023184286 hasRelatedWork W2010002018 @default.
• W2023184286 hasRelatedWork W2013855261 @default.
• W2023184286 hasRelatedWork W2016088231 @default.
• W2023184286 hasRelatedWork W2028326439 @default.
• W2023184286 hasRelatedWork W2035482989 @default.
• W2023184286 hasRelatedWork W2041994604 @default.
• W2023184286 hasRelatedWork W2053023480 @default.
• W2023184286 hasRelatedWork W2056797718 @default.
• W2023184286 hasRelatedWork W2057342974 @default.
• W2023184286 hasRelatedWork W2062684873 @default.
• W2023184286 hasRelatedWork W2064941759 @default.
• W2023184286 hasRelatedWork W2065085060 @default.
• W2023184286 hasRelatedWork W2084644145 @default.
• W2023184286 hasRelatedWork W2106545844 @default.
• W2023184286 hasRelatedWork W2134837756 @default.
• W2023184286 hasRelatedWork W2169381013 @default.
• W2023184286 isParatext "false" @default.
• W2023184286 isRetracted "false" @default.
• W2023184286 magId "2023184286" @default.
• W2023184286 workType "article" @default.