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Lister Publications
www.itg.cam.ac.uk/people/John/pubs.html9 Nov 2017: Falling plumes of point particles in viscous fluid. Phys. Fluids 24, 123101. -
Tuesday Informal Lunch Seminars
www.itg.cam.ac.uk/seminars/tue_1.10/mich_2000.html18 Sep 2001: Czech Republic and ITG). Convective instability of bubbly layers. 24 October. -
doi:
www.itg.cam.ac.uk/people/heh/Paper242.pdf11 Apr 2013: From the exactsolution we have. W0 =. Z2 1 (π2. 24. ... 4.24). This inner solution indeed satisfies the tip condition w0,in = 0 as Z 0, and asZ it reproduces the source term seen in (4.23). -
The effect of confining impermeable boundaries on gravity currents in …
www.itg.cam.ac.uk/people/heh/Paper221.pdf6 May 2010: Sd 75 0.24. V 1 20 200 V a 44 0.20 V 2 60 100 V b 75 0.25V 3 40 150 V 4 40 62. -
Spreading and convective dissolution of carbon dioxide in vertically…
www.itg.cam.ac.uk/people/heh/Paper237.pdf14 Feb 2013: 24] An upscaled model for convective dissolution canthen be incorporated into models such as equation (1) byintroducing a constant loss or sink term [Gasda et al.,2011 ; MacMinn et al., 2011],. -
Solidification of an alloy cooled from above Part 1. Equilibrium…
www.itg.cam.ac.uk/people/heh/Paper93.pdf25 Jan 2007: 0.01 (for Ra, = lo@), convection continues in the melt until t = 0.24, by which time the system is about 40% solidified. -
J. Fluid Mech. (2001), vol. 440, pp. 359–380. Printed ...
www.itg.cam.ac.uk/people/heh/Paper160.pdf9 Mar 2004: Received 24 April 2000 and in revised form 7 December 2000). -
Particle-driven gravity currents
www.itg.cam.ac.uk/people/heh/Paper115.pdf30 May 2006: 0, for which case the third term in (24) is negligible and the single-layer shallow-water momentum equation is recovered. ... The two-layer model comprises the three equations (17), (21) and (24) for the three variables h, u and 4 that describe the -
Magnetic resonance imaging of structure and convection in solidifying …
www.itg.cam.ac.uk/people/heh/Paper192.pdf5 May 2006: T = T(c) 5.176 c 13.27 c2 24.16 c3 75.52 c4 (2.1)for 0 < c < 0.7, where T (. C) is the temperature of the freezing ... 1:47, 2:14, 2:22, 2:49, 2:58, 3:24, 3:33, 3:59, 5:16, 5:43, 6:52, 7:46,. -
Numerical modelling of convection in a reactive porous medium with a…
www.itg.cam.ac.uk/people/heh/Paper191.pdf5 May 2006: J. Fluid Mech. (2006), vol. 549, pp. 99–129. c 2006 Cambridge University Pressdoi:10.1017/S0022112005007500 Printed in the United Kingdom. 99. Numerical modelling of convection ina reactive porous medium with a mobile. mush–liquid interface. By
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