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  2. Tuesday Informal Lunch Seminars

    www.itg.cam.ac.uk/seminars/tue_1.10/mich_2007.html
    9 Oct 2007: 20 November. No seminar. 27 November. Jessica Irving. (ITG). Inner core anisotropy.
  3. Tuesday Informal Lunch Seminars

    www.itg.cam.ac.uk/seminars/tue_1.10/lent_2007.html
    30 Jan 2007: 20 February. John Rudge. (ITG/Bullard). Solitary waves and melt migration in the mantle.
  4. 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.
  5. 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.
  6. 8 May 2007: h. t+. 8g sin β. 15νh2. h. z= 0. (2.20). The effect of confining boundaries on viscous gravity currents 499. ... 10. 20(a) (b). t/(v/ga). 103 104 105. t/(v/ga). z N /. (V/a. )1/2. 10. 100. z N /. (V4 s. in3 β.
  7. 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.
  8. 23 Apr 2007: Received 15 November 2005; accepted 9 January 2007; published online 20 April 2007. ... Thewidely accepted reason for this scaling relationship is theconstant ratio of shear stress and normal stress.20.
  9. Static and flowing regions in granular collapses down…

    www.itg.cam.ac.uk/people/heh/Paper208.pdf
    13 Nov 2007: Received 20 November 2006; accepted 11 July 2007; published online 2 October 2007. ... For Ls= 0.20 m / s and = 0.4 it is reduced to 0.08 s.
  10. 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.
  11. 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.

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