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PHYSICAL REVIEW E 84, 036111 (2011) Elastic response of ...
www.itg.cam.ac.uk/people/grae/98.pdf24 Aug 2012: The elastic sheets and the salt solution were containedinside an acrylic rectangular tank of dimensions 200 20 25 cm, with an opaque base. -
SOME EFFECTS OF VISCOSITY ON THE DYNAMICS OF REPLENISHED MAGMA…
www.itg.cam.ac.uk/people/heh/Paper60.pdf16 Jul 2010: Plexiglas tank of internal dimensions 200 x 106. Two different experiments described in our ear- mmx •00 mm deep. ... which crystallization is taking place [Chen and Accordingly, we built a tank, 200 x 106 x •00 mm Turner, 1980]. -
Solidification of an alloy cooled from above Part 1. Equilibrium…
www.itg.cam.ac.uk/people/heh/Paper93.pdf25 Jan 2007: I I I. I I I I 0 200 400 600 800. ... about half a year (hi = 200 cm and T / = 1016 "C). -
flm608.dvi
www.itg.cam.ac.uk/people/heh/Paper177.pdf9 Mar 2004: Each new time step rN (t) is updated using(12). Typically, we used 200 y-intervals and a time step of 0.002, but the convergenceand resolution (accurate to at least ... 4.2. H = 1. 0 50 100 150 200. –uN. Figure 14. -
The effect of confining impermeable boundaries on gravity currents in …
www.itg.cam.ac.uk/people/heh/Paper221.pdf6 May 2010: Sd 75 0.24. V 1 20 200 V a 44 0.20 V 2 60 100 V b 75 0.25V 3 40 150 V 4 40 62. ... 200 400 600 800 10000. 50. 100. 150. t (s). x N(t. ) -
PII: S0022-0248(99)00290-0
www.itg.cam.ac.uk/people/grae/40.pdf26 Apr 2006: Journal of Crystal Growth 205 (1999) 427}440. The interaction between a particle and an advancingsolidi"cation front. A.W. Rempel, M.G. Worster. Department of Applied Mathematics and Theoretical Physics, Institute of Theoretical Geophysics, -
PII: 0012-821X(90)90126-I
www.itg.cam.ac.uk/people/heh/Paper98.pdf27 Apr 2006: 0 0. c) loo. 50 100 150 200. TIME (yrs). 50 100 150 200. ... 100. 8O. 60. 40. 20. O " '. ". ' ". " ' -. 0 50 100 150 200. TIME (yrs) Fig. -
Solidification of leads: Theory, experiment,and field observations J. …
www.itg.cam.ac.uk/people/grae/43.pdf26 Apr 2006: 1125WETTLAUFER ET AL.: SOLIDIFICATION OF LEADS. profile was taken after the buoy had reached the oceanic tem-perature, and each subsequent profile is separated by 200 min.A quantitative analysis of ... The initial profile was taken after the buoy had -
Spatial and temporal evolution of injected CO2 at the Sleipner Field, …
www.itg.cam.ac.uk/people/heh/Paper232.pdf8 Jun 2012: Adjacent to the Sleipner field,this sandstone formation is 200–300 m thick [Chadwicket al., 2004] (Figure 1). ... The highestintrareservoir mudstone is 5 m thick, although the ultimateseal is the Nordland Shale, which is 200 m thick [Zweigelet al., 2000 -
880183.qxd
www.itg.cam.ac.uk/people/heh/Paper170.pdf9 Mar 2004: 100 m abovethe valley floor on the southern margins of the depres-sion, more than 200 m above the eastern slope of GuaneGuane Hill (12 km west of the source area,
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