FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2011562040> ?p ?o ?g. }

• W2011562040 abstract "Abstract Using lattice-Boltzmann simulation of steady-state gas flow we show that apparent permeability values of nano-scale capillaries could be significantly higher than those predicted by the Klinkenberg slip theory. The difference is due to kinetic effects of gas molecules that have gone through inelastic collisions with the walls on those molecules that make up the bulk fluid in the capillary. The kinetic energy that the bouncing back molecules have and the associated momentum carried to the bulk fluid is not a trivial matter in capillaries with diameter h less than 100nm. It creates a molecular streaming effect that amplifies velocity profile developing across the diameter of capillary. In a sense, it is not only the molecules interacting with the wall that slip but also the bulk fluid, i.e., double slip. The double-slip effect is shown using measured permeability data of a crushed nanoporous material with a uniform pore size (10&lt;h&lt;40 nm) at varying pore pressures. Using the simulation results we propose a modification to the Klinkenberg equation. New double-slip Klinkenberg equation includes a characteristic length scale (LKE) that is proportional to the kinetic energy per capillary cross-sectional area of the bouncing-back molecules by the walls. The new length scale of the molecular kinetic effects of nano-capillaries is larger than the mean free path of the molecules. The double-slip Klinkenberg equation reduces to the classical equation for slip flow in large capillaries, i.e., h/LKE &gt;&gt;1, and converges to the absolute permeability value at high pressures. Due to nanoporous nature of coals and organic-rich shales, the double-slip effect is likely to be significant near hydraulic fractures and production wells in depleted reservoirs. The presented theoretical work brings new insights into the measurement of crushed particle permeability using gas uptake or release experiments. Although they are fast low-pressure laboratory measurements, there are widely-recognized uncertainties associated with them. In this paper we show that dramatic variation in the measured permeability is possible due to small changes in the measurement cell pressure. Hence, even when the crushed sample is considered to be representative of the reservoir, the measured permeability may not quantitatively be related to flow under the reservoir conditions. The double-slip permeability concept and the modified Klinkenberg theory eliminate some of the uncertainties associated with the laboratory measurement of permeability and lead to development of new measurement protocols for the unconventional resources industry. A double-slip Klinkenberg chart is developed including the effects of nano-capillaries on the permeability, and two procedures are presented with example calculations on how to use the chart to predict permeability of shale sample from its effective pore size and shape." @default.
• W2011562040 created "2016-06-24" @default.
• W2011562040 creator A5052972182 @default.
• W2011562040 creator A5072435239 @default.
• W2011562040 creator A5085176998 @default.
• W2011562040 date "2012-06-05" @default.
• W2011562040 modified "2023-10-02" @default.
• W2011562040 title "Shale Gas Correction to Klinkenberg Slip Theory" @default.
• W2011562040 cites W1969121759 @default.
• W2011562040 cites W2009656120 @default.
• W2011562040 cites W2166031355 @default.
• W2011562040 cites W2600474252 @default.
• W2011562040 cites W4247263453 @default.
• W2011562040 doi "https://doi.org/10.2118/154977-ms" @default.
• W2011562040 hasPublicationYear "2012" @default.
• W2011562040 type Work @default.
• W2011562040 sameAs 2011562040 @default.
• W2011562040 citedByCount "54" @default.
• W2011562040 countsByYear W20115620402012 @default.
• W2011562040 countsByYear W20115620402013 @default.
• W2011562040 countsByYear W20115620402014 @default.
• W2011562040 countsByYear W20115620402015 @default.
• W2011562040 countsByYear W20115620402016 @default.
• W2011562040 countsByYear W20115620402017 @default.
• W2011562040 countsByYear W20115620402018 @default.
• W2011562040 countsByYear W20115620402019 @default.
• W2011562040 countsByYear W20115620402020 @default.
• W2011562040 countsByYear W20115620402021 @default.
• W2011562040 countsByYear W20115620402023 @default.
• W2011562040 crossrefType "proceedings-article" @default.
• W2011562040 hasAuthorship W2011562040A5052972182 @default.
• W2011562040 hasAuthorship W2011562040A5072435239 @default.
• W2011562040 hasAuthorship W2011562040A5085176998 @default.
• W2011562040 hasConcept C121332964 @default.
• W2011562040 hasConcept C135889238 @default.
• W2011562040 hasConcept C139166363 @default.
• W2011562040 hasConcept C185592680 @default.
• W2011562040 hasConcept C192562407 @default.
• W2011562040 hasConcept C195268267 @default.
• W2011562040 hasConcept C196806460 @default.
• W2011562040 hasConcept C21141959 @default.
• W2011562040 hasConcept C21821499 @default.
• W2011562040 hasConcept C57879066 @default.
• W2011562040 hasConcept C74650414 @default.
• W2011562040 hasConcept C97355855 @default.
• W2011562040 hasConceptScore W2011562040C121332964 @default.
• W2011562040 hasConceptScore W2011562040C135889238 @default.
• W2011562040 hasConceptScore W2011562040C139166363 @default.
• W2011562040 hasConceptScore W2011562040C185592680 @default.
• W2011562040 hasConceptScore W2011562040C192562407 @default.
• W2011562040 hasConceptScore W2011562040C195268267 @default.
• W2011562040 hasConceptScore W2011562040C196806460 @default.
• W2011562040 hasConceptScore W2011562040C21141959 @default.
• W2011562040 hasConceptScore W2011562040C21821499 @default.
• W2011562040 hasConceptScore W2011562040C57879066 @default.
• W2011562040 hasConceptScore W2011562040C74650414 @default.
• W2011562040 hasConceptScore W2011562040C97355855 @default.
• W2011562040 hasLocation W20115620401 @default.
• W2011562040 hasOpenAccess W2011562040 @default.
• W2011562040 hasPrimaryLocation W20115620401 @default.
• W2011562040 hasRelatedWork W1968962528 @default.
• W2011562040 hasRelatedWork W2040967328 @default.
• W2011562040 hasRelatedWork W2059539951 @default.
• W2011562040 hasRelatedWork W2083618104 @default.
• W2011562040 hasRelatedWork W2088628882 @default.
• W2011562040 hasRelatedWork W2093324086 @default.
• W2011562040 hasRelatedWork W2114380171 @default.
• W2011562040 hasRelatedWork W2762355484 @default.
• W2011562040 hasRelatedWork W3096556988 @default.
• W2011562040 hasRelatedWork W2885280263 @default.
• W2011562040 isParatext "false" @default.
• W2011562040 isRetracted "false" @default.
• W2011562040 magId "2011562040" @default.
• W2011562040 workType "article" @default.