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  2. Tuesday Informal Lunch Seminars

    www.itg.cam.ac.uk/seminars/tue_1.10/lent_2006.html
    24 Jan 2006: 21 February. Stephen Peppin. (ITG). A new type of mushy layer.
  3. A note on shock diffraction by a supersonic wedge

    www.itg.cam.ac.uk/people/heh/Paper2.pdf
    30 May 2006: WRITHAM, G. B. 1957 A new approach to problems of shock dynamics.
  4. PII: 0012-821X(90)90143-L

    www.itg.cam.ac.uk/people/heh/Paper97.pdf
    27 Apr 2006: These c o m p o n e n t s would not necessarily be distinguishable optically because new crystallization would take place on a restite nucleus.
  5. PII: 0022-0248(91)90092-J

    www.itg.cam.ac.uk/people/heh/Paper103.pdf
    27 Apr 2006: T.G.L. Shirtcliffe,. ResearchSchoolof Earth Sciences,Victoria University of Wellington, P.O. Box 600, Wellington I, New Zealand. ... Flemings, Solidification Processing(McGraw-Hill.larly important in caseswhere the fluid in the New York, 1974).
  6. 85230

    www.itg.cam.ac.uk/people/heh/Paper146.pdf
    27 Apr 2006: in Voight, B., ed., Rockslides and avalanches, Volume 1: New York, Elsevier,p. ... 1245–1260. Melosh, H. J., 1979, Acoustic fluidization: A new geological process?: Journal ofGeophysical Research, v.
  7. 28 Jul 2006: developed a new apparatus to analyse turbulent mixing between two plane streams of different. ... to turbulent convection in a low Prandtl number fluid, echoing the new theoretical predictions.
  8. 30 May 2006: The last decade or so has seen considerable excitement develop in aspects of geology that have become more quantitative, and many new intellectually challenging research areas are beginning to emerge. ... Phillips suggests that this process has been
  9. 30 May 2006: 2, pp. 1065-6. New. STEWARTSON, K. 1958 On the motion of a sphere along the axis of a rotating fluid. &.
  10. flm957.dvi

    www.itg.cam.ac.uk/people/heh/Paper195.pdf
    17 May 2006: However, for general values of α, thiscorresponds to a point source that is moving uphill in the new frame, complicatingthe analysis. ... Instead, an additional naturalvelocity scale, (q/φ)1/3, enters the problem. We thus define a new set of
  11. Axisymmetric gravity currents in a porous medium

    www.itg.cam.ac.uk/people/heh/Paper189.pdf
    5 May 2006: In 4 we summarize ourmajor new results and conclusions, and compare our results with a related theoreticalstudy by Bachu, Nordbotten & Celia (2005) and Nordbotten, Celia & Bachu (2005). ... where the new independent variable y is a scaled similarity

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