FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2766188841> ?p ?o ?g. }

• W2766188841 endingPage "523" @default.
• W2766188841 startingPage "513" @default.
• W2766188841 abstract "Overflushing is a common practice in multistage completions of horizontal wells in unconventional formations. It consists in displacing the suspension by a thin fluid, away from the wellbore and into the fracture. It can, however, overly displace proppant and leave a significant portion of the fracture unsupported near the wellbore, or trigger gravity slumping, again leaving unpropped area near the wellbore. That unpropped area can then close during production, damaging the performance of the fracture. A novel modeling approach was investigated to gain insight into the overflush process and determine secure bounds for maintaining the fracture performance. From a fluid mechanics viewpoint, overflushing is the displacement of a Hershel-Bulkley fluid by a power law fluid in a Hele-Shaw cell, leading to Saffman-Taylor instability at the fluids interface. Whereas most hydraulic fracturing simulators use power-law rheology model, we used a novel numerical approach accounting for the yield-stress behavior of the slurry. Using the lubrication approximation, we derived a model, which includes transport equations for fluid volume fractions and a nonlinear elliptic equation for pressure with mixed-type boundary conditions. Validation was previously performed against three sets of experiments in Hele-Shaw cells, comprising gravitational slumping and displacement of fluids with fingering. Based on fracture mechanics, we analyzed how large a portion of the fracture may be left unsupported before it is severely pinched during drawdown. A parametric study was performed on the displacement of the yield-stress slurry by the overflushing fluid. Qualitatively, when fingers of the overflushing fluid can be created at the overflush/slurry interface, large slurry pillars are preserved in the near-wellbore area, which may keep the fracture open. Three main scenarios of fluids distribution are identified and classified in terms of the oveflush fluid-to-slurry viscosity ratio ξ: (i) the slumping-dominated regime, where light clean overflush fluid goes on top of sedimenting heavy proppant-laden suspension (ξ≳0.1), (ii) an intermediate scenario of slumping combined with fingering (ξ∼0.01), and, finally, (iii) a pure fingering-dominated scenario, when the slurry viscosity is high (ξ<10−3). The third scenario minimizes the geomechanical risks of overflushing by providing tiny fingers that are unlikely to be pinched out during fracture closure." @default.
• W2766188841 created "2017-11-10" @default.
• W2766188841 creator A5025202765 @default.
• W2766188841 creator A5031833898 @default.
• W2766188841 creator A5052628693 @default.
• W2766188841 creator A5075290429 @default.
• W2766188841 date "2018-03-01" @default.
• W2766188841 modified "2023-10-01" @default.
• W2766188841 title "Managed Saffman-Taylor instability during overflush in hydraulic fracturing" @default.
• W2766188841 cites W1964642193 @default.
• W2766188841 cites W1984437679 @default.
• W2766188841 cites W1987994143 @default.
• W2766188841 cites W1993311670 @default.
• W2766188841 cites W1999002887 @default.
• W2766188841 cites W2003404840 @default.
• W2766188841 cites W2004716724 @default.
• W2766188841 cites W2012541063 @default.
• W2766188841 cites W2012939980 @default.
• W2766188841 cites W2024853778 @default.
• W2766188841 cites W2025203524 @default.
• W2766188841 cites W2029862731 @default.
• W2766188841 cites W2084223864 @default.
• W2766188841 cites W2093690869 @default.
• W2766188841 cites W2094704878 @default.
• W2766188841 cites W2102369828 @default.
• W2766188841 cites W2113941137 @default.
• W2766188841 cites W2620425902 @default.
• W2766188841 cites W4229836285 @default.
• W2766188841 cites W4362235792 @default.
• W2766188841 cites W852357326 @default.
• W2766188841 doi "https://doi.org/10.1016/j.petrol.2017.10.018" @default.
• W2766188841 hasPublicationYear "2018" @default.
• W2766188841 type Work @default.
• W2766188841 sameAs 2766188841 @default.
• W2766188841 citedByCount "3" @default.
• W2766188841 countsByYear W27661888412019 @default.
• W2766188841 countsByYear W27661888412020 @default.
• W2766188841 countsByYear W27661888412023 @default.
• W2766188841 crossrefType "journal-article" @default.
• W2766188841 hasAuthorship W2766188841A5025202765 @default.
• W2766188841 hasAuthorship W2766188841A5031833898 @default.
• W2766188841 hasAuthorship W2766188841A5052628693 @default.
• W2766188841 hasAuthorship W2766188841A5075290429 @default.
• W2766188841 hasConcept C107551265 @default.
• W2766188841 hasConcept C114793014 @default.
• W2766188841 hasConcept C121332964 @default.
• W2766188841 hasConcept C127313418 @default.
• W2766188841 hasConcept C15744967 @default.
• W2766188841 hasConcept C187320778 @default.
• W2766188841 hasConcept C191236761 @default.
• W2766188841 hasConcept C200990466 @default.
• W2766188841 hasConcept C207821765 @default.
• W2766188841 hasConcept C2779096232 @default.
• W2766188841 hasConcept C43369102 @default.
• W2766188841 hasConcept C50050167 @default.
• W2766188841 hasConcept C542102704 @default.
• W2766188841 hasConcept C57879066 @default.
• W2766188841 hasConcept C90278072 @default.
• W2766188841 hasConcept C97355855 @default.
• W2766188841 hasConcept C98156149 @default.
• W2766188841 hasConceptScore W2766188841C107551265 @default.
• W2766188841 hasConceptScore W2766188841C114793014 @default.
• W2766188841 hasConceptScore W2766188841C121332964 @default.
• W2766188841 hasConceptScore W2766188841C127313418 @default.
• W2766188841 hasConceptScore W2766188841C15744967 @default.
• W2766188841 hasConceptScore W2766188841C187320778 @default.
• W2766188841 hasConceptScore W2766188841C191236761 @default.
• W2766188841 hasConceptScore W2766188841C200990466 @default.
• W2766188841 hasConceptScore W2766188841C207821765 @default.
• W2766188841 hasConceptScore W2766188841C2779096232 @default.
• W2766188841 hasConceptScore W2766188841C43369102 @default.
• W2766188841 hasConceptScore W2766188841C50050167 @default.
• W2766188841 hasConceptScore W2766188841C542102704 @default.
• W2766188841 hasConceptScore W2766188841C57879066 @default.
• W2766188841 hasConceptScore W2766188841C90278072 @default.
• W2766188841 hasConceptScore W2766188841C97355855 @default.
• W2766188841 hasConceptScore W2766188841C98156149 @default.
• W2766188841 hasLocation W27661888411 @default.
• W2766188841 hasOpenAccess W2766188841 @default.
• W2766188841 hasPrimaryLocation W27661888411 @default.
• W2766188841 hasRelatedWork W148948974 @default.
• W2766188841 hasRelatedWork W1966760705 @default.
• W2766188841 hasRelatedWork W2004649918 @default.
• W2766188841 hasRelatedWork W2040643360 @default.
• W2766188841 hasRelatedWork W2072345938 @default.
• W2766188841 hasRelatedWork W2074993277 @default.
• W2766188841 hasRelatedWork W2091619476 @default.
• W2766188841 hasRelatedWork W2755300875 @default.
• W2766188841 hasRelatedWork W2955202669 @default.
• W2766188841 hasRelatedWork W1979898714 @default.
• W2766188841 hasVolume "162" @default.
• W2766188841 isParatext "false" @default.
• W2766188841 isRetracted "false" @default.
• W2766188841 magId "2766188841" @default.
• W2766188841 workType "article" @default.