FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2227401841> ?p ?o ?g. }

• W2227401841 endingPage "31" @default.
• W2227401841 startingPage "18" @default.
• W2227401841 abstract "In this paper, we present a linked multicontinuum and crack tensor approach for modeling of coupled geomechanics, fluid flow, and solute transport in fractured rock. We used the crack tensor approach to calculate effective block-scale properties, including anisotropic permeability and elastic tensors, as well as multicontinuum properties relevant to fracture–matrix interactions and matrix diffusion. In the modeling, we considered stress dependent properties, through stress-induced changes in fracture apertures, to update permeability and elastic tensors. We evaluated the effectiveness and accuracy of our multicontinuum approach by comparing our modeling results with that of three independent discrete fracture network (DFN) models. In two of the three alternative DFN models, solute transport was simulated by particle tracking, an approach very different from the standard solute transport used in our multicontinuum modeling. We compared the results for flow and solute transport through a 20 m × 20 m model domain of fractured rock, including detailed comparison of total flow rate, its distribution, and solute breakthrough curves. In our modeling, we divided the 20 m × 20 m model domain into regular blocks, or continuum elements. We selected a model discretization of 40 × 40 elements (having a side length of 0.5 m) that resulted in a fluid-flow rate equivalent to that of the DFN models. Our simulation results were in reasonably good agreement with the alternative DFN models, for both advective dominated transport (under high hydraulic gradient) and matrix-diffusion retarded transport (under low hydraulic gradient). However, we found pronounced numerical dispersion when using larger grid blocks, a problem that could be remediated by the use of a finer numerical grid resolution, while maintaining a larger grid for evaluation of equivalent properties, i.e. a property grid overlapping the numerical grid. Finally, we encountered some difficulties in using our approach when element sizes were so small that only one or a few fractures intersect an element—this is an area of possible improvement that will be pursued in future research." @default.
• W2227401841 created "2016-06-24" @default.
• W2227401841 creator A5032630907 @default.
• W2227401841 creator A5034481707 @default.
• W2227401841 creator A5065058975 @default.
• W2227401841 creator A5074533724 @default.
• W2227401841 creator A5075266200 @default.
• W2227401841 date "2013-02-01" @default.
• W2227401841 modified "2023-10-14" @default.
• W2227401841 title "Linked multicontinuum and crack tensor approach for modeling of coupled geomechanics, fluid flow and transport in fractured rock" @default.
• W2227401841 cites W1589087836 @default.
• W2227401841 cites W1679030178 @default.
• W2227401841 cites W1895776853 @default.
• W2227401841 cites W1968833163 @default.
• W2227401841 cites W1972326999 @default.
• W2227401841 cites W1981719774 @default.
• W2227401841 cites W1985082252 @default.
• W2227401841 cites W1986015919 @default.
• W2227401841 cites W1996677148 @default.
• W2227401841 cites W1998623298 @default.
• W2227401841 cites W2009853934 @default.
• W2227401841 cites W2010298998 @default.
• W2227401841 cites W2020478857 @default.
• W2227401841 cites W2022614832 @default.
• W2227401841 cites W2043456568 @default.
• W2227401841 cites W2048569709 @default.
• W2227401841 cites W2049877861 @default.
• W2227401841 cites W2055072688 @default.
• W2227401841 cites W2061751054 @default.
• W2227401841 cites W2071522825 @default.
• W2227401841 cites W2073828018 @default.
• W2227401841 cites W2075038261 @default.
• W2227401841 cites W2075218807 @default.
• W2227401841 cites W2080746477 @default.
• W2227401841 cites W2080973414 @default.
• W2227401841 cites W2082441586 @default.
• W2227401841 cites W2082519018 @default.
• W2227401841 cites W2084304569 @default.
• W2227401841 cites W2093509339 @default.
• W2227401841 cites W2097501083 @default.
• W2227401841 cites W2126979631 @default.
• W2227401841 cites W2139543996 @default.
• W2227401841 cites W2170830696 @default.
• W2227401841 cites W4238652496 @default.
• W2227401841 doi "https://doi.org/10.1016/j.jrmge.2012.08.001" @default.
• W2227401841 hasPublicationYear "2013" @default.
• W2227401841 type Work @default.
• W2227401841 sameAs 2227401841 @default.
• W2227401841 citedByCount "71" @default.
• W2227401841 countsByYear W22274018412014 @default.
• W2227401841 countsByYear W22274018412015 @default.
• W2227401841 countsByYear W22274018412016 @default.
• W2227401841 countsByYear W22274018412017 @default.
• W2227401841 countsByYear W22274018412018 @default.
• W2227401841 countsByYear W22274018412019 @default.
• W2227401841 countsByYear W22274018412020 @default.
• W2227401841 countsByYear W22274018412021 @default.
• W2227401841 countsByYear W22274018412022 @default.
• W2227401841 countsByYear W22274018412023 @default.
• W2227401841 crossrefType "journal-article" @default.
• W2227401841 hasAuthorship W2227401841A5032630907 @default.
• W2227401841 hasAuthorship W2227401841A5034481707 @default.
• W2227401841 hasAuthorship W2227401841A5065058975 @default.
• W2227401841 hasAuthorship W2227401841A5074533724 @default.
• W2227401841 hasAuthorship W2227401841A5075266200 @default.
• W2227401841 hasBestOaLocation W22274018411 @default.
• W2227401841 hasConcept C106487976 @default.
• W2227401841 hasConcept C120882062 @default.
• W2227401841 hasConcept C121332964 @default.
• W2227401841 hasConcept C127313418 @default.
• W2227401841 hasConcept C134306372 @default.
• W2227401841 hasConcept C159985019 @default.
• W2227401841 hasConcept C185592680 @default.
• W2227401841 hasConcept C185715996 @default.
• W2227401841 hasConcept C187320778 @default.
• W2227401841 hasConcept C192562407 @default.
• W2227401841 hasConcept C2524010 @default.
• W2227401841 hasConcept C2779096232 @default.
• W2227401841 hasConcept C33923547 @default.
• W2227401841 hasConcept C38349280 @default.
• W2227401841 hasConcept C41625074 @default.
• W2227401841 hasConcept C43369102 @default.
• W2227401841 hasConcept C55493867 @default.
• W2227401841 hasConcept C57879066 @default.
• W2227401841 hasConcept C62520636 @default.
• W2227401841 hasConcept C73000952 @default.
• W2227401841 hasConcept C85725439 @default.
• W2227401841 hasConcept C90278072 @default.
• W2227401841 hasConcept C99844830 @default.
• W2227401841 hasConceptScore W2227401841C106487976 @default.
• W2227401841 hasConceptScore W2227401841C120882062 @default.
• W2227401841 hasConceptScore W2227401841C121332964 @default.
• W2227401841 hasConceptScore W2227401841C127313418 @default.
• W2227401841 hasConceptScore W2227401841C134306372 @default.
• W2227401841 hasConceptScore W2227401841C159985019 @default.
• W2227401841 hasConceptScore W2227401841C185592680 @default.
• W2227401841 hasConceptScore W2227401841C185715996 @default.
• W2227401841 hasConceptScore W2227401841C187320778 @default.

• next