FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2038792757> ?p ?o ?g. }

• W2038792757 abstract "[1] In this study, multiscale permeability upscaling is combined with a sensitivity study of model boundary condition to identify an optimal heterogeneity resolution in developing a reservoir model to represent a deep saline aquifer in CO2 storage simulation. A three-dimensional, fully heterogeneous reservoir model is built for a deep saline aquifer in western Wyoming, where each grid cell is identified by multiple material tags. On the basis of these tags, permeability upscaling is conducted to create three increasingly simpler site models, a facies model, a layered model, and a formation model. Accuracy of upscaling is evaluated first, before CO2 simulation is conducted in all models. Since at the injection site, uncertainty exists in the nature of the reservoir compartment, end-member boundary conditions are evaluated, whereby brine production is introduced to control formation fluid pressure. The effect of conceptual model uncertainty on model prediction is then assessed for each boundary condition. Results suggest that for the spatial and temporal scales considered, without brine production, optimal complexity of the upscaled model depends on the prediction metric of interest; the facies model is the most accurate for capturing plume shape, fluid pressure, and CO2 mass profiles, while the formation model is adequate for pressure prediction. The layered model is not accurate for predicting most of the performance metrics. Moreover, boundary condition impacts fluid pressure and the amount of CO2 that can be injected. For the boundary conditions tested, brine production can modulate fluid pressure, affect the direction of mobile gas flow, and influence the accuracy of the upscaled models. In particular, the importance of detailed geologic resolution is weakened when viscous force is strengthened in relation to gravity force. When brine production is active, variability of the predictions by the upscaled models becomes smaller and the predictions are more accurate, suggesting a subtle but important interplay between heterogeneity resolution, fluid driving forces, and model predictions." @default.
• W2038792757 created "2016-06-24" @default.
• W2038792757 creator A5073568638 @default.
• W2038792757 creator A5079484650 @default.
• W2038792757 creator A5082117229 @default.
• W2038792757 date "2011-05-01" @default.
• W2038792757 modified "2023-10-18" @default.
• W2038792757 title "A study of conceptual model uncertainty in large-scale CO₂storage simulation" @default.
• W2038792757 cites W1491951399 @default.
• W2038792757 cites W1533563182 @default.
• W2038792757 cites W1602113245 @default.
• W2038792757 cites W1965810037 @default.
• W2038792757 cites W1967350246 @default.
• W2038792757 cites W1967945388 @default.
• W2038792757 cites W1969422552 @default.
• W2038792757 cites W1974210778 @default.
• W2038792757 cites W1978141567 @default.
• W2038792757 cites W1980020067 @default.
• W2038792757 cites W1985762111 @default.
• W2038792757 cites W2002265740 @default.
• W2038792757 cites W2014951715 @default.
• W2038792757 cites W2015597581 @default.
• W2038792757 cites W2017307986 @default.
• W2038792757 cites W2018969928 @default.
• W2038792757 cites W2021328460 @default.
• W2038792757 cites W2022376256 @default.
• W2038792757 cites W2033935976 @default.
• W2038792757 cites W2042045547 @default.
• W2038792757 cites W2044656391 @default.
• W2038792757 cites W2044734858 @default.
• W2038792757 cites W2050671870 @default.
• W2038792757 cites W2063917512 @default.
• W2038792757 cites W2064551239 @default.
• W2038792757 cites W2067216567 @default.
• W2038792757 cites W2067244284 @default.
• W2038792757 cites W2069326881 @default.
• W2038792757 cites W2073532908 @default.
• W2038792757 cites W2077289100 @default.
• W2038792757 cites W2088391744 @default.
• W2038792757 cites W2100518860 @default.
• W2038792757 cites W2101031513 @default.
• W2038792757 cites W2101967376 @default.
• W2038792757 cites W2102689158 @default.
• W2038792757 cites W2104387409 @default.
• W2038792757 cites W2115102387 @default.
• W2038792757 cites W2119743251 @default.
• W2038792757 cites W2120806788 @default.
• W2038792757 cites W2121826742 @default.
• W2038792757 cites W2134164857 @default.
• W2038792757 cites W2142524517 @default.
• W2038792757 cites W2154719540 @default.
• W2038792757 cites W2157882426 @default.
• W2038792757 cites W2163131601 @default.
• W2038792757 cites W2170670241 @default.
• W2038792757 cites W2173615563 @default.
• W2038792757 cites W2319692794 @default.
• W2038792757 cites W2329064041 @default.
• W2038792757 cites W4244420516 @default.
• W2038792757 cites W4247551942 @default.
• W2038792757 cites W4299935416 @default.
• W2038792757 doi "https://doi.org/10.1029/2010wr009707" @default.
• W2038792757 hasPublicationYear "2011" @default.
• W2038792757 type Work @default.
• W2038792757 sameAs 2038792757 @default.
• W2038792757 citedByCount "22" @default.
• W2038792757 countsByYear W20387927572012 @default.
• W2038792757 countsByYear W20387927572013 @default.
• W2038792757 countsByYear W20387927572014 @default.
• W2038792757 countsByYear W20387927572015 @default.
• W2038792757 countsByYear W20387927572016 @default.
• W2038792757 countsByYear W20387927572017 @default.
• W2038792757 countsByYear W20387927572018 @default.
• W2038792757 countsByYear W20387927572020 @default.
• W2038792757 countsByYear W20387927572021 @default.
• W2038792757 countsByYear W20387927572022 @default.
• W2038792757 countsByYear W20387927572023 @default.
• W2038792757 crossrefType "journal-article" @default.
• W2038792757 hasAuthorship W2038792757A5073568638 @default.
• W2038792757 hasAuthorship W2038792757A5079484650 @default.
• W2038792757 hasAuthorship W2038792757A5082117229 @default.
• W2038792757 hasBestOaLocation W20387927571 @default.
• W2038792757 hasConcept C120882062 @default.
• W2038792757 hasConcept C121332964 @default.
• W2038792757 hasConcept C127313418 @default.
• W2038792757 hasConcept C134306372 @default.
• W2038792757 hasConcept C153294291 @default.
• W2038792757 hasConcept C159390177 @default.
• W2038792757 hasConcept C178790620 @default.
• W2038792757 hasConcept C182310444 @default.
• W2038792757 hasConcept C185592680 @default.
• W2038792757 hasConcept C187320778 @default.
• W2038792757 hasConcept C2775840915 @default.
• W2038792757 hasConcept C2776957854 @default.
• W2038792757 hasConcept C33923547 @default.
• W2038792757 hasConcept C39432304 @default.
• W2038792757 hasConcept C41625074 @default.
• W2038792757 hasConcept C55493867 @default.
• W2038792757 hasConcept C57879066 @default.
• W2038792757 hasConcept C75622301 @default.
• W2038792757 hasConcept C76177295 @default.

• next