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flm517.dvi
www.itg.cam.ac.uk/people/heh/Paper175.pdf9 Mar 2004: J. Fluid Mech. (2003), vol. 489, pp. 269–299. c 2003 Cambridge University PressDOI: 10.1017/S0022112003005172 Printed in the United Kingdom. 269. Solidification and convection of a ternarysolution cooled from the side. By LYNN J. BLOOMFIELD AND -
J. Fluid Mech. (1998), vol. 362, pp. 17–51. Printed ...
www.itg.cam.ac.uk/people/heh/Paper142.pdf9 Mar 2004: Of course, at large t, say 1/β = 200, the difference must belarge since all the particles are expected to have settled out, while the homogeneouscurrent maintains its density excess.). -
GeoFluidMech_fin.tex typeset [1]
www.itg.cam.ac.uk/people/heh/Paper154.pdf9 Mar 2004: 1. Geological Fluid Mechanics. By Herbert E. Huppert. (Received 6 February 2000). 1. The Earth. Since antiquity there has been consideration and speculation about the Earth on which. we live. How did it form; how does it evolve; how can its riches -
J. Fluid Mech. (2002), vol. 472, pp. 333–371. c© ...
www.itg.cam.ac.uk/people/heh/Paper172.pdf9 Mar 2004: J. Fluid Mech. (2002), vol. 472, pp. 333–371. c 2002 Cambridge University PressDOI: 10.1017/S0022112002002379 Printed in the United Kingdom. 333. Polydisperse particle-driven gravity currents. By T H O M A S C. H A R R I S1, A N D R E W J. H O G
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