FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2897866771> ?p ?o ?g. }

• W2897866771 endingPage "8755" @default.
• W2897866771 startingPage "8734" @default.
• W2897866771 abstract "Flow and transport properties of fractured rock masses are a function of geometrical structures across many scales. These structures result from physical processes and states and are highly anisotropic in nature. Fracture surfaces often tend to be shifted with respect to each other, which is generally a result of stress-induced displacements. This shift controls the fracture's transmissivity through the pore space that forms from the created mismatch between the surfaces. This transmissivity is anisotropic and greater in the direction perpendicular to the displacement. A contact mechanics-based, first-principle numerical approach is developed to investigate the effects that this shear-induced transmissivity anisotropy has on the overall permeability of a fractured rock mass. Deformation of the rock and contact between fracture surfaces is computed in three dimensions at two scales. At the rock mass scale, fractures are treated as planar discontinuities along which displacements and tractions are resolved. Contact between the individual rough fracture surfaces is solved for each fracture at the small scale to find the stiffness and transmissivity that result from shear-induced dilation and elastic compression. Results show that, given isotropic fracture networks, the direction of maximum permeability of a fractured rock mass tends to be aligned with the direction of the intermediate principal stress. This reflects the fact that fractures have the most pronounced slip in the plane of the maximum and minimum principal stresses, and for individual fractures transmissivity is most pronounced in the direction perpendicular to this slip." @default.
• W2897866771 created "2018-10-26" @default.
• W2897866771 creator A5004323790 @default.
• W2897866771 creator A5050117607 @default.
• W2897866771 creator A5064597353 @default.
• W2897866771 creator A5074802884 @default.
• W2897866771 date "2018-11-01" @default.
• W2897866771 modified "2023-10-11" @default.
• W2897866771 title "Relationship Between the Orientation of Maximum Permeability and Intermediate Principal Stress in Fractured Rocks" @default.
• W2897866771 cites W1557000224 @default.
• W2897866771 cites W1566448103 @default.
• W2897866771 cites W1614951384 @default.
• W2897866771 cites W173136342 @default.
• W2897866771 cites W1832889940 @default.
• W2897866771 cites W1895075854 @default.
• W2897866771 cites W1921350826 @default.
• W2897866771 cites W1932406446 @default.
• W2897866771 cites W1964095013 @default.
• W2897866771 cites W1966841131 @default.
• W2897866771 cites W1971987639 @default.
• W2897866771 cites W1971990676 @default.
• W2897866771 cites W1972049983 @default.
• W2897866771 cites W1972326999 @default.
• W2897866771 cites W1977156689 @default.
• W2897866771 cites W1977757375 @default.
• W2897866771 cites W1983246178 @default.
• W2897866771 cites W1985082252 @default.
• W2897866771 cites W1987536503 @default.
• W2897866771 cites W1989730926 @default.
• W2897866771 cites W1992596969 @default.
• W2897866771 cites W1993950371 @default.
• W2897866771 cites W1998203900 @default.
• W2897866771 cites W2001331462 @default.
• W2897866771 cites W2009551225 @default.
• W2897866771 cites W2010196731 @default.
• W2897866771 cites W2012255496 @default.
• W2897866771 cites W2014545097 @default.
• W2897866771 cites W2016412058 @default.
• W2897866771 cites W2017677517 @default.
• W2897866771 cites W2018248030 @default.
• W2897866771 cites W2018618010 @default.
• W2897866771 cites W2020478857 @default.
• W2897866771 cites W2023307199 @default.
• W2897866771 cites W2023778672 @default.
• W2897866771 cites W2024207616 @default.
• W2897866771 cites W2024628241 @default.
• W2897866771 cites W2030064974 @default.
• W2897866771 cites W2033122457 @default.
• W2897866771 cites W2034082479 @default.
• W2897866771 cites W2035104499 @default.
• W2897866771 cites W2043339854 @default.
• W2897866771 cites W2045502922 @default.
• W2897866771 cites W2045956763 @default.
• W2897866771 cites W2046384101 @default.
• W2897866771 cites W2049754061 @default.
• W2897866771 cites W2051875053 @default.
• W2897866771 cites W2053132150 @default.
• W2897866771 cites W2055241639 @default.
• W2897866771 cites W2059400754 @default.
• W2897866771 cites W2062764546 @default.
• W2897866771 cites W2065285415 @default.
• W2897866771 cites W2065505843 @default.
• W2897866771 cites W2067224114 @default.
• W2897866771 cites W2068216186 @default.
• W2897866771 cites W2071864725 @default.
• W2897866771 cites W2073828018 @default.
• W2897866771 cites W2080556419 @default.
• W2897866771 cites W2084490457 @default.
• W2897866771 cites W2086326746 @default.
• W2897866771 cites W2088651667 @default.
• W2897866771 cites W2093333193 @default.
• W2897866771 cites W2096349182 @default.
• W2897866771 cites W2100138383 @default.
• W2897866771 cites W2114051217 @default.
• W2897866771 cites W2123617092 @default.
• W2897866771 cites W2128361235 @default.
• W2897866771 cites W2132814790 @default.
• W2897866771 cites W2138777789 @default.
• W2897866771 cites W2139124365 @default.
• W2897866771 cites W2143252260 @default.
• W2897866771 cites W2152724920 @default.
• W2897866771 cites W2153028948 @default.
• W2897866771 cites W2155360515 @default.
• W2897866771 cites W2163708666 @default.
• W2897866771 cites W2169365228 @default.
• W2897866771 cites W2189782723 @default.
• W2897866771 cites W2227401841 @default.
• W2897866771 cites W2253087389 @default.
• W2897866771 cites W2271128414 @default.
• W2897866771 cites W2330521729 @default.
• W2897866771 cites W2332143918 @default.
• W2897866771 cites W2332606067 @default.
• W2897866771 cites W2338382920 @default.
• W2897866771 cites W2492699551 @default.
• W2897866771 cites W2592006858 @default.
• W2897866771 cites W2745591729 @default.
• W2897866771 cites W2766179339 @default.
• W2897866771 cites W3103158239 @default.

• next