FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3080999613> ?p ?o ?g. }

• W3080999613 abstract "Abstract Simulation of gas huff-n-puff (HnP) in core models is often simplified by assuming homogenous, isotropic models, which are not representative of fine-grained multi-component shales with multiple types of pore space and anisotropic permeability. According to the previous literaturte, history matching of a 6-cycle HnP process and tuning of cross-phase effective diffusion coefficients using a homogeneous model presented a need for a detailed core-scale geomodel to capture variations in effective diffusion coefficients as a result of heterogeneity experienced during each diffusion cycle. A workflow for reconstructing a corescale volume of Lower Eagle Ford (LEF) shale is presented that combines rock characterization using high-resolution digital images at the micrometer/nanometer scale and transmitted light microscopy to provide models for detailed heterogeneity of the LEF shale for gas huff-n-puff simulation. Core-scale models form LEF are reconstructed using high-resolution SEM-EDS and FIB-SEM images. SEM-EDS and FIB-SEM images were coupled with transmitted light microsocpy and micro-computed tomography (CT) to constrain facies distribution, discrete fracture networks and to distribute petrophysical properties. The reconstruction method produced a more representative core model of the LEF and can be used for simulation of core-scale huff-n-puff experiments conducted in a diffusion cell. Common grain types observed in the SEM-EDS images at different resolutions include detrital quartz, calcite, microfossils and fragments, microfractures, clay minerals, traces of dolomite, and albite. Also common is diagenetic calcite, pyrite, kaolinite, and secondary organic matter (OM) infilling the chambers of foraminifer tests (forams) and other mineral pores. FIB-SEM analysis provided organic bulk transport properties including tortuosity and permeability within the generated pore network models of the LEF shale. Transmitted light microscopy provided the lamina-scale variation of samples from the LEF shale to be incorporated in the core model. A detailed workflow is presented for reconstructtion of a LEF shale core-scale model using high- resolution images and photomicrographs. The model detailed the original core morphology, multiple pore space, and multicomponent mineral distributions for gas huff-n-puff simulation. Several realizations of the geomodel were prepared by varying mineral distributions within the layers as well as the range of petrophysical properties in order to present different gas huff-n-puff simulation scenarios. This provided the compositional model using a sophisticated heterogeneous component of tortuosity/permeability instead of a homogenous and isotropic model." @default.
• W3080999613 created "2020-09-01" @default.
• W3080999613 creator A5002093481 @default.
• W3080999613 creator A5010190979 @default.
• W3080999613 creator A5027314525 @default.
• W3080999613 creator A5028061559 @default.
• W3080999613 creator A5058575019 @default.
• W3080999613 creator A5060011732 @default.
• W3080999613 creator A5065290590 @default.
• W3080999613 creator A5074419885 @default.
• W3080999613 creator A5081814511 @default.
• W3080999613 date "2020-08-30" @default.
• W3080999613 modified "2023-09-27" @default.
• W3080999613 title "A Reconstructed Core-Scale Model of the Lower Eagle Ford Shale Through FIB-SEM, SEM-EDS, and Microscopy for Gas Huff-n-Puff Simulation" @default.
• W3080999613 cites W1255425586 @default.
• W3080999613 cites W1992889808 @default.
• W3080999613 cites W2084087785 @default.
• W3080999613 cites W2317793691 @default.
• W3080999613 cites W2757775752 @default.
• W3080999613 cites W2921252560 @default.
• W3080999613 cites W2969193454 @default.
• W3080999613 doi "https://doi.org/10.2118/200379-ms" @default.
• W3080999613 hasPublicationYear "2020" @default.
• W3080999613 type Work @default.
• W3080999613 sameAs 3080999613 @default.
• W3080999613 citedByCount "1" @default.
• W3080999613 countsByYear W30809996132023 @default.
• W3080999613 crossrefType "proceedings-article" @default.
• W3080999613 hasAuthorship W3080999613A5002093481 @default.
• W3080999613 hasAuthorship W3080999613A5010190979 @default.
• W3080999613 hasAuthorship W3080999613A5027314525 @default.
• W3080999613 hasAuthorship W3080999613A5028061559 @default.
• W3080999613 hasAuthorship W3080999613A5058575019 @default.
• W3080999613 hasAuthorship W3080999613A5060011732 @default.
• W3080999613 hasAuthorship W3080999613A5065290590 @default.
• W3080999613 hasAuthorship W3080999613A5074419885 @default.
• W3080999613 hasAuthorship W3080999613A5081814511 @default.
• W3080999613 hasConcept C127313418 @default.
• W3080999613 hasConcept C187320778 @default.
• W3080999613 hasConcept C192562407 @default.
• W3080999613 hasConcept C199289684 @default.
• W3080999613 hasConcept C2780191791 @default.
• W3080999613 hasConcept C46293882 @default.
• W3080999613 hasConcept C6648577 @default.
• W3080999613 hasConceptScore W3080999613C127313418 @default.
• W3080999613 hasConceptScore W3080999613C187320778 @default.
• W3080999613 hasConceptScore W3080999613C192562407 @default.
• W3080999613 hasConceptScore W3080999613C199289684 @default.
• W3080999613 hasConceptScore W3080999613C2780191791 @default.
• W3080999613 hasConceptScore W3080999613C46293882 @default.
• W3080999613 hasConceptScore W3080999613C6648577 @default.
• W3080999613 hasLocation W30809996131 @default.
• W3080999613 hasOpenAccess W3080999613 @default.
• W3080999613 hasPrimaryLocation W30809996131 @default.
• W3080999613 hasRelatedWork W11584843 @default.
• W3080999613 hasRelatedWork W1421753 @default.
• W3080999613 hasRelatedWork W20818765 @default.
• W3080999613 hasRelatedWork W24335770 @default.
• W3080999613 hasRelatedWork W26174255 @default.
• W3080999613 hasRelatedWork W31293391 @default.
• W3080999613 hasRelatedWork W33801639 @default.
• W3080999613 hasRelatedWork W4872486 @default.
• W3080999613 hasRelatedWork W5904858 @default.
• W3080999613 hasRelatedWork W19190864 @default.
• W3080999613 isParatext "false" @default.
• W3080999613 isRetracted "false" @default.
• W3080999613 magId "3080999613" @default.
• W3080999613 workType "article" @default.