The anisotropic coefficient, -/: for the onsct of convection in a porous box with the isothermalĪnd impermeable lower boundary adiabatic and impermeable side walls, and both permeableĪnd impermeable upper boundary which is isothermal before convection takes place.26įig. 1.3: Critical Ra-number Ra,: aud the aspect-ratio of the cells, O, as functions of 1.2: Onset of convection in a porous, anisotropic porous box with the permeable upperįig. 1.1: Fractional density, p f / p f o, and viscosity, /i//iO, of water as functions of tenlpera-įig. Methanc is relnoved from rising pore fluids to form hydrate as the pore fluids move into theįig. 3: Fluid expulsion model for gas hydrate formation [Hyndman and Davis, 19921. 2: I
0 Comments
Leave a Reply. |