Matches in SemOpenAlex for { <https://semopenalex.org/work/W2765370849> ?p ?o ?g. }
- W2765370849 abstract "Abstract The KS reservoir is a naturally fractured, deep, tight gas sandstone reservoir under high tectonic stress. Because the reservoir matrix is very tight, the natural fracture system is the main pathway for gas production. Meanwhile, stimulation is still required for most production wells to provide production rates that sufficiently compensate for the high cost of drilling and completing wells to access this deep reservoir. Large depletion (and related stress change) was expected during the course of the production of the field. The dynamic response of the reservoir and related risks, such as reduction of fracture conductivity, fault reactivation, casing failure etc., would compromise the long-term productivity of the reservoir. To quantify the dynamic response of the reservoir and related risks, a 4D reservoir geomechanics simulation was conducted for KS reservoir by following an integrated workflow. The work started from systematical laboratory fracture conductivity tests performed with fractured cores to measure conductivity versus confining stress for both natural fractures and hydraulic fractures (with proppant placed in the fractures of the core samples). Natural fracture modeling was conducted to generate a discrete fracture network to delineate spacious distribution of the natural fracture system. In addition, hydraulic fracture modeling was conducted to delineate the geometry of hydraulic fracture system for the stimulated wells. Then, a 3D geomechanical model was constructed through integrating geological, petrophysical and geomechanical data, and both the discrete fracture network (DFN) and hydraulic fracture system were incorporated into the 3D geomechanical model. A 4D reservoir geomechanics simulation was conducted through coupling with a reservoir simulator to predict variation of stress and strain of rock matrix as well as natural fractures and hydraulic fractures during the field production. At each study well location, a near- wellbore model was extracted from the full-field model and casing and cement were installed to evaluate well integrity during production. The 4D reservoir geomechanics simulation revealed that there would be large reduction of conductivity for both natural fractures and hydraulic fractures, and some fractures with certain dip/dip azimuth will be reactivated during the course of the field production. The induced stress change will also compromise wellintegrity for those poorly cemented wellbores. The field development plan must consider all these risks to ensure sustainable long-term production. The paper presents a 4D coupled geomechanics simulation study applied to an HP/HT naturally fractured reservoir, which has rarely been published previously. The study adapted several new techniques to quantify the mechanical response of both natural fractures and hydraulic fractures, such as to use laboratory tests to measure stress sensitivity of natural fractures, integrating DFN and hydraulic fracture system into 4D geomechanics simulation, and evaluating well integrity on both the reservoir scale and the near-wellbore scale." @default.
- W2765370849 created "2017-11-10" @default.
- W2765370849 creator A5005975263 @default.
- W2765370849 creator A5019918709 @default.
- W2765370849 creator A5022802322 @default.
- W2765370849 creator A5037488697 @default.
- W2765370849 creator A5039718733 @default.
- W2765370849 creator A5041199459 @default.
- W2765370849 creator A5047714441 @default.
- W2765370849 creator A5057993946 @default.
- W2765370849 creator A5076407502 @default.
- W2765370849 creator A5079719595 @default.
- W2765370849 date "2017-10-15" @default.
- W2765370849 modified "2023-09-25" @default.
- W2765370849 title "Case Study: 4D Reservoir Geomechanics Simulation of an HP/HT Naturally Fractured Reservoir" @default.
- W2765370849 cites W1041340204 @default.
- W2765370849 cites W1608019363 @default.
- W2765370849 cites W1968254189 @default.
- W2765370849 cites W1968364545 @default.
- W2765370849 cites W1969493438 @default.
- W2765370849 cites W1969740536 @default.
- W2765370849 cites W1979577972 @default.
- W2765370849 cites W1989079678 @default.
- W2765370849 cites W1989428118 @default.
- W2765370849 cites W1994856879 @default.
- W2765370849 cites W1999002887 @default.
- W2765370849 cites W2001745934 @default.
- W2765370849 cites W2001911133 @default.
- W2765370849 cites W2012280311 @default.
- W2765370849 cites W2022832162 @default.
- W2765370849 cites W2040143860 @default.
- W2765370849 cites W2042133641 @default.
- W2765370849 cites W2049134998 @default.
- W2765370849 cites W2054248209 @default.
- W2765370849 cites W2056728198 @default.
- W2765370849 cites W2057397064 @default.
- W2765370849 cites W2061410397 @default.
- W2765370849 cites W2066053222 @default.
- W2765370849 cites W2066739090 @default.
- W2765370849 cites W2068372401 @default.
- W2765370849 cites W2070974773 @default.
- W2765370849 cites W2071095224 @default.
- W2765370849 cites W2080452684 @default.
- W2765370849 cites W2081008335 @default.
- W2765370849 cites W2084027138 @default.
- W2765370849 cites W2107059731 @default.
- W2765370849 cites W2173619605 @default.
- W2765370849 cites W2318361274 @default.
- W2765370849 cites W2321689007 @default.
- W2765370849 cites W2485960821 @default.
- W2765370849 cites W2761090796 @default.
- W2765370849 cites W331408911 @default.
- W2765370849 cites W1985918674 @default.
- W2765370849 doi "https://doi.org/10.2118/187606-ms" @default.
- W2765370849 hasPublicationYear "2017" @default.
- W2765370849 type Work @default.
- W2765370849 sameAs 2765370849 @default.
- W2765370849 citedByCount "1" @default.
- W2765370849 countsByYear W27653708492020 @default.
- W2765370849 crossrefType "proceedings-article" @default.
- W2765370849 hasAuthorship W2765370849A5005975263 @default.
- W2765370849 hasAuthorship W2765370849A5019918709 @default.
- W2765370849 hasAuthorship W2765370849A5022802322 @default.
- W2765370849 hasAuthorship W2765370849A5037488697 @default.
- W2765370849 hasAuthorship W2765370849A5039718733 @default.
- W2765370849 hasAuthorship W2765370849A5041199459 @default.
- W2765370849 hasAuthorship W2765370849A5047714441 @default.
- W2765370849 hasAuthorship W2765370849A5057993946 @default.
- W2765370849 hasAuthorship W2765370849A5076407502 @default.
- W2765370849 hasAuthorship W2765370849A5079719595 @default.
- W2765370849 hasConcept C127313418 @default.
- W2765370849 hasConcept C14641988 @default.
- W2765370849 hasConcept C185715996 @default.
- W2765370849 hasConcept C187320778 @default.
- W2765370849 hasConcept C2778668878 @default.
- W2765370849 hasConcept C78762247 @default.
- W2765370849 hasConceptScore W2765370849C127313418 @default.
- W2765370849 hasConceptScore W2765370849C14641988 @default.
- W2765370849 hasConceptScore W2765370849C185715996 @default.
- W2765370849 hasConceptScore W2765370849C187320778 @default.
- W2765370849 hasConceptScore W2765370849C2778668878 @default.
- W2765370849 hasConceptScore W2765370849C78762247 @default.
- W2765370849 hasLocation W27653708491 @default.
- W2765370849 hasOpenAccess W2765370849 @default.
- W2765370849 hasPrimaryLocation W27653708491 @default.
- W2765370849 hasRelatedWork W1564105384 @default.
- W2765370849 hasRelatedWork W1972895052 @default.
- W2765370849 hasRelatedWork W2004293766 @default.
- W2765370849 hasRelatedWork W2055913127 @default.
- W2765370849 hasRelatedWork W2056728198 @default.
- W2765370849 hasRelatedWork W2222308888 @default.
- W2765370849 hasRelatedWork W2312374423 @default.
- W2765370849 hasRelatedWork W2324847095 @default.
- W2765370849 hasRelatedWork W2467186643 @default.
- W2765370849 hasRelatedWork W2553657542 @default.
- W2765370849 hasRelatedWork W2611793254 @default.
- W2765370849 hasRelatedWork W2621194457 @default.
- W2765370849 hasRelatedWork W2733342268 @default.
- W2765370849 hasRelatedWork W2738262872 @default.
- W2765370849 hasRelatedWork W2808717950 @default.