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- W206467701 abstract "Consider the flow of any tensorially linear and isotropic viscous fluid in a cylindrical channel, parallel to the x-axis. All variables are assumed to be x-independent. Necessary, but not sufficient conditions for this are that the boundary conditions be x-independent, and that the free surface, if there is open flow, be also a cylinder parallel to x. The y-axis is taken horizontal; thus the components of gravity are g x , 0, g z . (If the x-axis is also horizontal, it is the case of plane flow, parallel to the (y - z) plane which is considered). Equilibrium conditions read:$$ frac{partial tau_{!xy}}{partial y},+,frac{partial tau_{!xz}}{partial z},+,varrho g_x, =,0quad quad quadleft|begin{array}{ll} frac{partial sigma_{!y}}{partial y},+,frac{partial tau_{!yz}}{partial z}=,0 frac{partial tau_{!y!z}}{partial y},+,frac{partial sigma_{!z}}{partial z},+,varrho g_z,=,0 end{array} right| $$(7.1)" @default.
- W206467701 created "2016-06-24" @default.
- W206467701 creator A5050073169 @default.
- W206467701 date "1987-01-01" @default.
- W206467701 modified "2023-09-27" @default.
- W206467701 title "Open flow in a cylindrical channel of a power-law viscous fluid, and application to temperate valley glaciers" @default.
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- W206467701 doi "https://doi.org/10.1007/978-94-009-3563-1_7" @default.
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