Search
Search Funnelback University
- Refined by:
- Date: 2006
1 -
10 of
24
search results for KaKaoTalk:vb20 200 |u:www.itg.cam.ac.uk
where 0
match all words and 24
match some words.
Results that match 1 of 2 words
-
PII: 0022-0248(93)90538-8
www.itg.cam.ac.uk/people/heh/Paper116.pdf27 Apr 2006: The mean volume fraction 4,. 0 I I,,,, I0 100 200 300 400 500. ... whoseheight h ‘ H. Substituting. 0 0 100 200 300 500 M0 M= p0AH (A.4). -
Under consideration for publication in J. Fluid Mech. 1 ...
www.itg.cam.ac.uk/people/heh/jfm50.pdf28 Jul 2006: as to be expected, the figure is much lower for the 200 journals with highest cumulative impact. -
flm145.dvi
www.itg.cam.ac.uk/people/heh/Paper197.pdf11 Oct 2006: 1992). The typical grid has 200 intervals over [0, xN (t)] and a time step of0.04. ... 2 4 6 8 10 12 14 16 18 200. -
On gravity currents driven by constant fluxes of saline and…
www.itg.cam.ac.uk/people/heh/Paper188.pdf5 May 2006: 0 20 40 60 80 100 120. 500400300200100. 0–100–200. 200300. 1000. ... 0 20 40 60 80 100 120. –100–200–300. Time (s)Time (s). -
Magnetic resonance imaging of structure and convection in solidifying …
www.itg.cam.ac.uk/people/heh/Paper192.pdf5 May 2006: pulses, 512 µs in duration and anacquisition width of 200 kHz was used. ... In our velocity imaging experiments the echo time TE was 10.3 ms, while theobservation time was 200 ms. -
flm483.dvi
www.itg.cam.ac.uk/people/heh/Paper186.pdf5 Jan 2006: 3. 4. 5. 6. 100 200 300 400 500. a(cm). t (min). ... b). 1. 2. 3. 4. 5. 0 50 100 150 200 250 300. -
Axisymmetric particle-driven gravity currents
www.itg.cam.ac.uk/people/heh/Paper127.pdf30 May 2006: 200. n 150 W. 50. 1 I I I I 0 20 40 60 80. ... R. Lister. 60 I n g'. (cm s-3 Expt Theory 42 21 11 0 - -. 0 - A. 0. I - - - 9 - - - --.__ I 100 I 150 I 200. -
Particle-driven gravity currents
www.itg.cam.ac.uk/people/heh/Paper115.pdf30 May 2006: initial volume fraction 5 YO of 200 pm-diameter sand and initial height of 20 m, for which us = 2 cm sP1 and gh = 0.81 m s -. The dynamics of ... 400. cl. 200. Y I I I L 0 50 100 150 200. -
Numerical modelling of convection in a reactive porous medium with a…
www.itg.cam.ac.uk/people/heh/Paper191.pdf5 May 2006: Convection in reactive porous media 111. 100 200 300 400 500 600 700 8000. ... 50 100 150 200 250 3000. 0.5. 1.0. 1.5. 2.0. 2.5. -
Ice blocks melting into a salinity gradient
www.itg.cam.ac.uk/people/heh/Paper35.pdf30 May 2006: h. 5 200 - 9. ( b ) 400. 34 4 34 5 34 6 34 1 34 4 34 5 34 6 34 7 S ( % a ) S ( % O ). B I L t<h ... 100 0.0026 0.0061 0.0083 0.0184 150 0.0035 0.0077 0.0092 0.0198 200 0.0041 0.0088 00101 0.0210.
Search history
Recently clicked results
Recently clicked results
Your click history is empty.
Recent searches
Recent searches
Your search history is empty.