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1 - 21 of 21 search results for `some B B` |u:www.itg.cam.ac.uk
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  2. M411_31c 568..571

    www.itg.cam.ac.uk/people/grae/47.pdf
    27 Apr 2006: Even these frigid temperatures are muchhigher than the eutectic temperatures of some of the aqueoussolutions that are likely to be present. ... Some. researchers have referred to solidication experiments20 and assumed that most of the.
  3. Some remarks on the initiation of inertial Taylor columns

    www.itg.cam.ac.uk/people/heh/Paper19.pdf
    30 May 2006: Printed in Great Britain. 397. Some remarks on the initiation of inertial Taylor columns. ... Thus further compression is needed for some of the vortex lines to be able to flow over the obstacle.
  4. 1 Jun 2006: The predictions of the compositional layering in the solid produced by this convection were successfully compared with some experimental investigations using aqueous sodium carbonate. ... For example, figure 7 shows some measurements of the variation of
  5. PII: 0012-821X(82)90155-8

    www.itg.cam.ac.uk/people/heh/Paper45.pdf
    27 Apr 2006: With time, some dense input fluid spreads along the b o t t o m so that locally the situation is the same as the one considered in the previous studies, ... h o u s layer on the container floor continued for quite some time.
  6. 30 May 2006: This fluid convects into the upper layer and carries with it some of the particles. ... b ) Calculated positions of some of t h e layers of constant bulk density for t h e differential sedimentation of a suspension of type-1 particles.
  7. Natural convection in a mushy layer

    www.itg.cam.ac.uk/people/grae/14.pdf
    1 Jun 2006: Some aspects of the flow structure have been analysed previously by Roberts & Loper (1983) b u t they did not include the thermodynamic interactions between the flow and the growth of ... moving with some prescribed, constant speed V , as illustrated in
  8. 30 May 2006: Substituting MIA = E , (7.1)) and (7.8) into (5.21), we obtain (after some manipulation). ... into (3.8), we obtain (after some reduction). c,, = 2K/02Kx-fH1(x)dx ( E O ) (9.2a) 63. =
  9. The stability of a large gas bubble rising through liquid

    www.itg.cam.ac.uk/people/heh/Paper81.pdf
    30 May 2006: by some external means, because a n eigenmode grows indefinitely regardless of its initial amplitude. ... some by turning over a bucket of air, remained intact for values of R up to about 15 em.
  10. PII: 0012-821X(90)90126-I

    www.itg.cam.ac.uk/people/heh/Paper98.pdf
    27 Apr 2006: This partially solidi- fied region has b e e n co n si d ered b y some authors to b e p a r t o f the t h ... roof into the interior of the chamber causes some 45% of the chamber to solidify at the floor, even though it is being cooled only from the roof.
  11. PREMELTING DYNAMICS

    www.itg.cam.ac.uk/people/grae/68.pdf
    26 Apr 2006: Figure 2a shows a state in which thesolid-liquid interface intersects the boundary of the wedge at some contact angleβ. ... determine values for these quantities separately. Moreover, although the trappingprocess is not instantaneous, the particle is
  12. 5 May 2006: There isalso some evidence of mixing between the ambient and the particle-laden fluids, butthis is of insufficient strength to mix the particles throughout the entire water depth. ... the structure and nature of the turbulent fluctuations. Arita & Jirka
  13. PII: 0377-0273(82)90062-2

    www.itg.cam.ac.uk/people/heh/Paper48.pdf
    27 Apr 2006: n t s ; or, possibly, some c o m b i n a t i o n o f (2.8a,b,c). ... some c a u t i o n is necessary in i n t e r p r e t i n g this viscosity e s t i m a
  14. Nonlinear double-diffusive convection

    www.itg.cam.ac.uk/people/heh/Paper25.pdf
    30 May 2006: Some solutions of 8 were obtained by Veronis (1965, 19686) in terms of truncated Fourier expansions. ... For some values of a, T and B, this time- independent form occurs before the solution passes through the two-maxima- per-cycle form of motion or the
  15. Particle-driven gravity currents

    www.itg.cam.ac.uk/people/heh/Paper115.pdf
    30 May 2006: Some turbidites (the sedimentary deposits of ancient turbidity currents) have become oil reservoirs (Perrodon 1985). ... It is convenient to non-dimensionalize (2)-(6) with some of the initial parameters of the current.
  16. CONVECTION IN MUSHY LAYERS

    www.itg.cam.ac.uk/people/grae/30.pdf
    26 Apr 2006: There is experimental evidence, too, that some mushy layersbehave differently from the ideal. ... discussion of some of the applications of thetheory of natural convection in mushy layers.
  17. Axisymmetric particle-driven gravity currents

    www.itg.cam.ac.uk/people/heh/Paper127.pdf
    30 May 2006: In some cases the sedimentary deposits from ancient turbidity currents have become valuable oil reservoirs (Perrodon 1985). ... or constant flux of suspension; (b) sector tank with true apex; and (c) large rectangular tank with semi-circular lock for
  18. PII: 0012-821X(93)90029-9

    www.itg.cam.ac.uk/people/heh/Paper113.pdf
    27 Apr 2006: c h e d the stage w h e r e some particles have settled on the bottom. ... In some e x p e r i m e n t s with the larger values of M 0, the grid, if b r o u g h t to
  19. PII: 0012-821X(89)90063-0

    www.itg.cam.ac.uk/people/heh/Paper87.pdf
    27 Apr 2006: T h e heat transfer, H, will be some function of (Too - Tf), which can be expressed as:. ... T h e actual variation o f heat flux o u t o f a growing intrusion will follow some general path, as de- p i ct ed b y curve
  20. PII: 0012-821X(90)90126-I

    www.itg.cam.ac.uk/people/grae/13.pdf
    27 Apr 2006: This partially solidi- fied region has b e e n co n si d ered b y some authors to b e p a r t o f the t h ... roof into the interior of the chamber causes some 45% of the chamber to solidify at the floor, even though it is being cooled only from the roof.
  21. Double-diffusive convection

    www.itg.cam.ac.uk/people/heh/Paper42.pdf
    30 May 2006: and theory, except for some mechanistic models which have been developed specifically t o interpret experiments. ... The predictions have already received some confirmation from recent observations off the Erebus Glacier tongue in the Antarctic (Jacobs
  22. 5 May 2006: Aqueous salt solutions have been used for some time as laboratory analogues forgeological systems (e.g. ... If the frozen solute becomes immersed in fluid whose temperature isgreater than the liquidus temperature for its concentration, then some quantity

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