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VOLUME 87, NUMBER 8 P H Y S I ...
www.itg.cam.ac.uk/people/grae/49.pdf26 Apr 2006: A static force experiment using a probe with awell-characterized geometry would be more amenable toa quantitative test of this theory. -
Double-diffusive convection
www.itg.cam.ac.uk/people/heh/Paper42.pdf30 May 2006: J. Fluid Me&. (1981), vol. 106, p p. 299-329. Printed in Great Britain 399. Double-diffusive convection. By H E R B E R T E. H U P P E R T Department of Applied Mathematics and Theoretical Physics,. Silver Street, Cambridge CB3 9EW. A N D J. S T E W -
Particle-driven gravity currents
www.itg.cam.ac.uk/people/heh/Paper115.pdf30 May 2006: To test the theory, several experiments were performed to measure the length of particle-driven gravity currents as a function of time and their deposition patterns for a variety of particle -
Komatiites II: Experimental and Theoretical Investigations of…
www.itg.cam.ac.uk/people/heh/Paper69.pdf19 Jul 2010: test a quantitative theory on laboratory data, and thenuse this theory to describe the time history of a solidifying lava. ... The extent to which the first two (internal) observations can bepredicted from one or more of the roof temperature records will -
The fluid mechanics of solidification
www.itg.cam.ac.uk/people/heh/Paper92.pdf16 Jan 2007: J. Fluid M e c h. (1990). vol. 212, p p. 209-240. Printed in Great Britain 209. The fluid mechanics of solidification. By H E R B E R T E. H U P P E R T Institute of Theoretical Geophysics and Department of Applied Mathematics and Theoretical. -
PII: 0377-0273(93)90087-8
www.itg.cam.ac.uk/people/heh/Paper110.pdf27 Apr 2006: 0.1 wt.%, were carried o u t in o r d e r to test the effect o f the intensity o f c o n v e c t -
gl019950 1..4
www.itg.cam.ac.uk/people/heh/Paper182.pdf7 Jul 2004: 2. The Experiments. [3] To test these ideas we conducted a series of experi-ments in a Perspex tank with internal horizontal dimensionsof 2 cm by 30 cm, and a depth -
PII: 0022-0248(94)00965-1
www.itg.cam.ac.uk/people/heh/Paper126.pdf27 Apr 2006: n c o n d u c t e d at small e n o u g h u n d erco o l i n g s to test the -
M411_31c 568..571
www.itg.cam.ac.uk/people/grae/47.pdf27 Apr 2006: Themodel presented here should be regarded as a test of the potentialfor diffusion in the unfrozen liquid to disrupt palaeoclimaticrecords and a challenge to motivate further high-resolution exami-nations of ... peaks is needed to test theories for the -
GeoFluidMech_fin.tex typeset [1]
www.itg.cam.ac.uk/people/heh/Paper154.pdf9 Mar 2004: Geological Fluid Mechanics 17. mas, the origin of some economic ore deposits, such as platinum sulphides (Campbell,. -
PII: 0198-0149(81)90135-7
www.itg.cam.ac.uk/people/heh/Paper41.pdf26 Sep 2011: Deep-Sea Research, Vol. 28A, No. 5, pp. 409 to 440, 1981. 0198-0149/81/050409-32 $02,00/0 Printed in Great Britain. Pergamon Press Ltd. An abyssal topographic experiment. W. JOHN G O U L D t , ROSS HENDRY a n d HERBERT E. HUPPERT. (Received 3 April -
PII: 0377-0273(82)90062-2
www.itg.cam.ac.uk/people/heh/Paper48.pdf27 Apr 2006: t y t o test m o d e l s for t h e e x t r u s i o n m e c h a n i -
Elastic Relaxation of Fluid-Driven Cracks and the Resulting Backflow…
www.itg.cam.ac.uk/people/heh/Paper257.pdf18 May 2017: Young’s moduli E ranging from 66 6.6. to 104 10.4 kPa, as measured via indentation tests [11],were used in our experiments. -
Axisymmetric gravity currents in a porous medium
www.itg.cam.ac.uk/people/heh/Paper189.pdf5 May 2006: current and test the results againstlaboratory experiments. ... 3. Experimental observationsTo test the theoretical model we conducted a series of laboratory experiments in. -
Instruments and Methods A non-destructive method for measuring the ...
www.itg.cam.ac.uk/people/grae/61.pdf28 Apr 2006: Toprovide reliable tests for such a model, accurate andextensive measurements of salinity in growing sea ice arerequired. ... derived from the directly measured par-ameters (impedance and temperature), and to test theunderlying assumptions against -
PII: 0022-0248(91)90092-J
www.itg.cam.ac.uk/people/grae/15.pdf27 Apr 2006: First, we wished to apply an concentration,the z. 1 werechosentobe(10, 20, 30)additional test to the theory by measuring the mm, but otherwisethey wereset at (5, 15, 25)
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