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flm1100071a
www.itg.cam.ac.uk/people/heh/Paper228.pdf21 Oct 2011: r10 20 30 40. r. t. 0. 0.4. 0.8. 1.2. Vel. ... 5 10 15 20 25 30. rf. (b)(a). Figure 5. Experimental comparison. -
PII: S0022-0248(01)00595-4
www.itg.cam.ac.uk/people/grae/45.pdf26 Apr 2006: Curvature effects can be neglected whenR4Rc and analytical expressions for Vc arereadily derived [20]. ... Cambridge, 1999, p. 339. [20] A.W. Rempel, M.G. Worster, J. Crystal Growth 205. -
jc004333 1..7
www.itg.cam.ac.uk/people/grae/82.pdf7 Aug 2008: The measurements were carried out with very high vertical and temporalresolution over the course of a few days until the ice had reached a thickness ofaround 20 cm. ... 2002], indicating thatequation (3) might also be a good approximation for theaverage -
Instruments and Methods A non-destructive method for measuring the ...
www.itg.cam.ac.uk/people/grae/61.pdf28 Apr 2006: up. The resistance between thewires is almost negligible, and hence the functional form ofthe conductivity at a fixed temperature 20 is. ... 20 0:0015T: ð7ÞHere T is the temperature deficit below 20 C, S is in ppt. -
grl50082 307..311
www.itg.cam.ac.uk/people/grae/105.pdf9 Apr 2013: since the model includes a number of idealiza-tions, for quantitative implementation we propose tuningthis factor with experimental results.[20] In conclusion, the dimensional vertical component of. -
OP-QJMA190019
www.itg.cam.ac.uk/people/heh/Paper269.pdf23 Dec 2021: Therefore, we rewrite our expression as. p = 100a0(g′V)1/2 x3/20 t1. ... tmax = T1β1A1/2γ 5/20 , (4.2)for T1 a dimensionless constant to be determined. -
Flow and Reactions in Permeable Rocks. By O. M. P HILLIPS .…
www.itg.cam.ac.uk/people/heh/Paper106.pdf30 May 2006: I found only one obvious error. I n Section 6.6 the angle q5 is used in the text, while it is depicted as 8 in figure 6.20 ; and qi -
PHYSICAL REVIEW E 83, 031306 (2011) Shallow granular flows ...
www.itg.cam.ac.uk/people/heh/Paper226.pdf13 Apr 2011: y (mm). u (m. m/s. ). t=3 mint=5 mint=12 mint=20 min. ... FIG. 20. The minimum flow rate required for steady flow isestimated by Eq. -
Viscous gravity currents inside confining channels and…
www.itg.cam.ac.uk/people/heh/Paper210.pdf5 Mar 2008: 023104-2 D. Takagi and H. E. Huppert Phys. Fluids 20, 023104 2008. ... 023104-4 D. Takagi and H. E. Huppert Phys. Fluids 20, 023104 2008. -
PII: 0011-7471(73)90056-9
www.itg.cam.ac.uk/people/heh/Paper15.pdf26 Sep 2011: 20 = 0"874 K25 , (1)t. where C2o (c25) signifies the diffusivity at 20C (25C). ... 22). The system (20) to (22) is now linear and has solutions o f the form.
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