Search

Search Funnelback University

Search powered by Funnelback
1 - 10 of 40 search results for KaKaoTalk:PC53 24 / |u:www.itg.cam.ac.uk where 0 match all words and 40 match some words.
  1. Results that match 1 of 2 words

  2. 28 Jul 2006: Geology 186 24.6 1.64 220 12.6 1.80. JFM 197 22.5 1.50 265 11.3 1.61.
  3. PII: 0377-0273(93)90087-8

    www.itg.cam.ac.uk/people/heh/Paper110.pdf
    27 Apr 2006: Subsequently (ap- proximately 40-50 rain from the beginning),. 24 r. KOYa_GUCHI L, kt. ... grade particles with A T = 2 4 C and Co= 1.24 wt.%.
  4. PII: 0012-821X(93)90028-8

    www.itg.cam.ac.uk/people/heh/Paper112.pdf
    27 Apr 2006: 1034 23.0 24.0 0.016 67. K 1.3 w t. % saline s o l u t i o n S e d i m e n t m ... 1034 24.0 10.0 0.012 28. L 1.3 wt.% saline s o l u t i o n Secliment m fresh w a t e r.
  5. Particle-driven gravity currents

    www.itg.cam.ac.uk/people/heh/Paper115.pdf
    30 May 2006: 0, for which case the third term in (24) is negligible and the single-layer shallow-water momentum equation is recovered. ... The two-layer model comprises the three equations (17), (21) and (24) for the three variables h, u and 4 that describe the
  6. PII: 0022-0248(93)90538-8

    www.itg.cam.ac.uk/people/heh/Paper116.pdf
    27 Apr 2006: iments havebeenusedin drawing up fig. 3.) Fig.1 • 24.5 5 then plots the heightsof the mushy layer and. ... 0 24 concentrationsas functions of time for experi-0 100 200 300 400 500 mentswith the six different valuesof the contam-.
  7. PII: 0022-0248(94)90038-8

    www.itg.cam.ac.uk/people/heh/Paper119.pdf
    27 Apr 2006: 2.18), which can be (2.23) and (2.24) more closely.used in (2.22) to show that Segregation is more sensitive to the value of. ... 4.24)mass reduce to and we use this condition together with (4.21)—.
  8. 30 May 2006: J. Fluid Mech. (1995), vol. 289, p p. 263-293 Copyright 0 1995 Cambridge University Press. 263. Sedimentation and entrainment in dense layers of suspended particles stirred by an oscillating grid. By H E R B E R T E. HUPPERT', J. STEWART TURNER' A N
  9. PII: 0022-0248(94)00965-1

    www.itg.cam.ac.uk/people/heh/Paper126.pdf
    27 Apr 2006: f_0q(z,) d z ' = A 2. (3.24) The functional form for the source strength q(z') is d e t e r m i n e d by matching
  10. 30 May 2006: University of Cambridge, Silver Street, Cambridge CB3 9EW, UK. (Received 17 October 1994 and in revised form 24 May 1995). ... Each freezing experiment took on the order of 24 hours, after which the solid crystalline block was cut up into pieces and the
  11. 30 May 2006: J. Fluid Mech. (1996), 001. 308, p p. 289-311 Copyright @ 1996 Cambridge University Press. 289. Entrainment into two-dimensional and axisymmetric turbulent gravity currents. BY M A R K A. H A L L W O R T H ' , H E R B E R T E. H U P P E R T ' , J E

Refine your results

Search history

Recently clicked results

Recently clicked results

Your click history is empty.

Recent searches

Recent searches

Your search history is empty.