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Laminar free convection in confined regions
www.itg.cam.ac.uk/people/grae/4.pdf1 Jun 2006: uw,ww, = vw,,ag(T-TJ, ( 1 ). (2) uT, wT, = K T , t Some authors prefer to use the Grashof number 6% = u-l Ra. -
Gravity currents entering a two-layer fluid
www.itg.cam.ac.uk/people/heh/Paper37.pdf30 May 2006: 751. -. -. -. -. -5 - - - - - - - - - - - - _ _ -- -1 - - _ - - --=- _ _ _ - - -. I I";, tJ I 4 1 VI I I I. 0.25 -. ;I tJ 4 1 v. I I I I I. It is also shown that there -
The Generation of Granitic Magmas by Intrusion of Basalt ...
www.itg.cam.ac.uk/people/heh/Paper83.pdf15 Sep 2006: magma layer. TABLE 2. The table lists the time (tj) at which the basalt layer becomes 60% crystalline and ceasesconvection for different basalt layer thicknesses.
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