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The fluid mechanics of solidification
www.itg.cam.ac.uk/people/heh/Paper92.pdf16 Jan 2007: J. Fluid M e c h. (1990). vol. 212, p p. 209-240. Printed in Great Britain 209. The fluid mechanics of solidification. By H E R B E R T E. H U P P E R T Institute of Theoretical Geophysics and Department of Applied Mathematics and Theoretical. -
Phase changes following the initiation of a hot turbulent flow over a …
www.itg.cam.ac.uk/people/heh/Paper85.pdf25 Jan 2007: J. Fluid Mech. (1989), voZ. 198, p p. 293-319. Printed in Great Britain. 293. Phase changes following the initiation of a hot turbulent flow over a cold solid surface. By HERBERT E. HUPPERT Department of Applied Mathematics and Theoretical Physics, -
Melting the roof of a chamber containing a hot, turbulently…
www.itg.cam.ac.uk/people/heh/Paper82.pdf25 Jan 2007: Substituting (18), (19) and (24) into (21), we obtain the following implicit relationship between T and Tl :. ( 2 5 ). Substituting (20) and (21) into ( 2 2 ) , and using (23a, c ) in ... a = pcDH;' (To--T). (24). Tl = Tmp2c2k' D J H i l ( T o - T ) (T-T, -
PII: 0012-821X(81)90075-3
www.itg.cam.ac.uk/people/heh/Paper43.pdf16 Jan 2007: expressed as wt.%, as a function of the amount of K2CO 3 or NaNO 3 present in solution at 24.2C. ... Lower and upper layer properties were: initial temperatures 46 and 15C; initial concentrations 37 and 24%; initial densities 1.26 and 1.23 g cm 3; and -
Static and flowing regions in granular collapses down…
www.itg.cam.ac.uk/people/heh/Paper208.pdf13 Nov 2007: Method. Glass beads 24 Rotating drume. 0.25–0.35 24 Smooth inclined planef. ... 0.5 0.04 24–31 Rough inclined planeg. 1.26 9–11 Shear gauge, smooth chute flowh. -
The effect of confining boundaries on viscous gravity currents
www.itg.cam.ac.uk/people/heh/Paper201.pdf8 May 2007: 2(m2 1). 2u. XY= Mm2h2. (2.24). We posit a solution in the form. ... 4.1) for openchannel flow is replaced by 24/105 = 0.229 for a circular constraining geometry andK/m = 0.137m2/(1 m2) for a V-shaped constrainer. -
doi:10.1098/rspa.2006.1790
www.itg.cam.ac.uk/people/grae/77.pdf22 Jan 2007: Inserting equations (2.23) and (2.24) into equations (2.12)–(2.16) andlinearizing in the perturbed quantities leads to the following nonlinear ordinarydifferential equation for the disturbance amplitude:. -
new_notes_12.dvi
www.damtp.cam.ac.uk/user/wingate/SFT/2007/RRHqstat.pdf6 Nov 2007: A =. kT log 2 1β. log[. 1 β2(qJM h)2/2 β4(qJM h)4/24. ]. ... hA1/24. |A2|3/2. A4 is not particularly interesting: the denominator |A2| is the interesting part. -
LQCDsupplement.dvi
www.damtp.cam.ac.uk/user/wingate/Part3Essay/2007LQCDsupplement.pdf5 Feb 2007: L. Jaffe, Phys. Today 48N9, 24 (1995). [15] D. B. Renner et al. -
vortex.dvi
www.damtp.cam.ac.uk/user/tong/tasi/vortex.pdf19 Jun 2007: 1. e2=. x6 ls2gs. (3.24). where ls is the string length, and gs the string coupling. ... with worldvolume 039, as shown in figure 6 [24]. The x3.
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