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1 - 10 of 20 search results for TALK:PC53 20 |u:www.itg.cam.ac.uk where 0 match all words and 20 match some words.

  1. Results that match 1 of 2 words

  2. PII: 0012-821X(81)90075-3

    www.itg.cam.ac.uk/people/heh/Paper43.pdf
    16 Jan 2007: 1.40. • 1.3o >,. 1.20. 1.10 I 6 0 5 0 4 0 3 0 2 0 10. ... 149. 1.32 /. 1.31 /. 1. 3 0 /. Eo 1 2 9 /. /. _., / 1. 2 8 1.27. /. 1 2 6 / i , = / • 20 ; 0 35 4'0.

  3. The fluid mechanics of solidification

    www.itg.cam.ac.uk/people/heh/Paper92.pdf
    16 Jan 2007: 0 10 20 30. c, (wt Yo) FIQURE 10. The non-dimensional growth rates A4, A, and A, (determined by Worster 1986) with. ... 20. 15 - v. 3 l 0 - fi 5 -. - -. X I I I I I. 0 10 20 30 40 50.

  4. Steady-state mushy layers: experiments and theory

    www.itg.cam.ac.uk/people/heh/Paper199.pdf
    18 Jan 2007: Peppin, P. Aussillous, H. E. Huppert and M. G. Worster. 5 10 15 20 250. ... J. Cryst. Growth 20, 121–124. Chen, C. F. 1991 Experimental study of convection in a mushy layer during directional solidification.J.

  5. doi:10.1098/rspa.2006.1790

    www.itg.cam.ac.uk/people/grae/77.pdf
    22 Jan 2007: 1 mm. 20 wt% montmorillonite. 1 mm. (a) (b) (c). (d) (e) ( f ). Figure 1. Colloidal suspensions frozen by cooling from below. The system is open at the top to asupply ... where CiZCN/ks. Equation (2.20) can be integrated from zZ0 to z ZN usingequation

  6. Solidification of an alloy cooled from above. Part 3. Compositional…

    www.itg.cam.ac.uk/people/heh/Paper95.pdf
    25 Jan 2007: 2= 307 J 337 J 20.0 "C. A 0.056 -. TABLE 1. ... 10. 5 -. 35 1. -. - h. E 0. 0 10 20 30 40 50.

  7. Melting the roof of a chamber containing a hot, turbulently…

    www.itg.cam.ac.uk/people/heh/Paper82.pdf
    25 Jan 2007: 45. 20 30 40 0 10 20 30 40 0 10 I (min) t (min). ... Melting the roof of a chamber. Finally, (18) and (20) can be written J D.

  8. Solidification of an alloy cooled from above Part 1. Equilibrium…

    www.itg.cam.ac.uk/people/heh/Paper93.pdf
    25 Jan 2007: Huppert. To cooler. - I 20 cm l o - 10 cm I 1 Scale. ... A. - 0. -10. T ("C). -20. -30. 100. Source. E D B, n C D.

  9. Phase changes following the initiation of a hot turbulent flow over a …

    www.itg.cam.ac.uk/people/heh/Paper85.pdf
    25 Jan 2007: which satisfies (2.17b) if B ( z ) = exp ( - 4 V z ) , (2.20). ... This justifies the use of the long-time solutions (2.20) and (2.21) in the geological context.

  10. Solidification of an alloy cooled from above Part 2. Non-equilibrium…

    www.itg.cam.ac.uk/people/heh/Paper94.pdf
    25 Jan 2007: are similar to those derived in P a r t 1 (equations (3.19) and (3.20)), though they now involve the variable 8, and, as mentioned earlier, q5i is no ... Solidijcation of an alloy cooled from above. Part 2. 20. 15.

  11. The growth of compositionally stratified solid above a horizontal…

    www.itg.cam.ac.uk/people/heh/Paper86.pdf
    25 Jan 2007: T, = -20 "C c, = 9.37%. 1. H 01 = -h,(AC)f = 2.40 x 10-4K, s-'. ... 0.04 - (b) -. 0.01. 0 5 10 15 20 25 0 5 10 15 20 25.

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