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PHYSICAL REVIEW E 93, 023116 (2016) Flow-induced compaction of ...
www.itg.cam.ac.uk/people/grae/120.pdf21 Mar 2016: Received 24 June 2015; revised manuscript received 1 January 2016; published 24 February 2016). ... 24)] while the effective permeability decreases like H1(cf. (22)). The porosity also approaches an asymptotic profilewith φ0 0 as H. -
PII: 0022-0248(94)90038-8
www.itg.cam.ac.uk/people/grae/22.pdf27 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)—. -
doi: 10.1098/rspa.2009.0496, 1005-1025 first published online 3…
www.itg.cam.ac.uk/people/grae/91.pdf29 Apr 2010: we can make the approximation G(y) π y. Equation (2.24) then becomesπ. ... By dimensionalization of equation (3.24), we findthat the system is stable when. -
Experiments on the low-Reynolds-number settling of a sphere through a …
www.itg.cam.ac.uk/people/heh/Paper265.pdf23 Dec 2021: seal” configurations observed for inertial impacts of spheres ontoair-water [24] and fluid-fluid [26] interfaces. ... Phys. 3, 180. (2007).[23] D. Lee and H. Kim, Impact of a superhydrophobic sphere onto water, Langmuir 24, 142 (2008).[24] J. -
The propagation of two-dimensional and axisymmetric viscous gravity…
www.itg.cam.ac.uk/people/heh/Paper47.pdf30 May 2006: 2.21). (2.22). (2.23). (2.24). where EN is the value of [ at r = rN(t). ... Substituting (2.23) and (2.24) into (2.21) and (2.22), we find that $ ( z ) , where z = c/&, satisfies. -
flm608.dvi
www.itg.cam.ac.uk/people/heh/Paper177.pdf9 Mar 2004: 6.3 6.3 24.3 5.89 1.00 3.86 9.6 6.1 3.8 0.7417 6.3 6.3 24.3 10.71 1.00 ... 86 9.6 8.2 5.2 0.8118 6.3 6.3 24.3 20.37 1.00 3.86 9.6 11.3 7.1 0.8919 13.2 -
PII: 0011-7471(73)90056-9
www.itg.cam.ac.uk/people/heh/Paper15.pdf26 Sep 2011: 24). F o r a solution to be possible the right-hand side o f (24) must be positive, that is (with Yr negative). -
Initial advance of long lava flows in open channels
www.itg.cam.ac.uk/people/heh/Paper222.pdf27 Aug 2010: However, variations in fountain height in episode 4, asplotted in figure 1.24 of Wolfe et al. ... the night of 24–25 July 1983,when the flow front divided into two parallel lobes. -
Viscous free-surface flows past cylinders
www.itg.cam.ac.uk/people/heh/Paper274.pdf26 Mar 2023: The governing Eq. (7) in the rescaledcoordinates is. h3. x̂=. [. x̂. (h3. h. x̂. ). ŷ. (h3. h. ŷ. )]. (24). ... 5.0 24 15 7.14 1.2 0.853.5 48 13.2 4.50 1.72 0.615.0 24 7.9 3.76 1.28 0.773.5 -
High Reynolds number gravity currents along V-shaped valleys
www.itg.cam.ac.uk/people/heh/Paper217.pdf18 Nov 2009: y1=2ð1 þ yÞ1=2ln. y1=2 þffiffiffiffiffiffiffiffiffiffiffiffi1 þ y. p s þ c1; (24). ... Am.Math. Soc. 46 (1940) 615–683. [24] T.B. Benjamin, Gravity currents and related phenomena, J. -
The Fluid Mechanics of Carbon Dioxide Sequestration
www.itg.cam.ac.uk/people/heh/Paper246.pdf24 Apr 2014: 24/. 14. F. or p. erso. nal u. se o. nly. ... n 04. /24/. 14. F. or p. erso. nal u. se o. -
Ageostrophic effects in rotating stratified flow
www.itg.cam.ac.uk/people/heh/Paper17.pdf30 May 2006: 24-2. 372 H. E. Huppert and 144. E. Stern. $1. , //,/,////,//////////////,,,/,////// / ///,/I/ // / / / , // , / , / // , / / / / // / /, /' I -. FIGURE 1. An elevation of the channel, bounded by vertical walls at. ... Moh(x/L) e--ikg. (3.24). While in -
doi:10.1016/j.jcp.2004.11.039
www.itg.cam.ac.uk/people/grae/62.pdf26 Apr 2006: Received 29 March 2004; received in revised form 24 September 2004; accepted 11 November 2004. ... ykumar and Mao [24] again assuming the interface was sharp. The SPH method, as mentioned earlier, does. -
PII: 0022-0248(94)90038-8
www.itg.cam.ac.uk/people/heh/Paper119.pdf27 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)—. -
PII: S0022-0248(99)00290-0
www.itg.cam.ac.uk/people/grae/40.pdf26 Apr 2006: 1.0 [24]. The slope of the linethrough data set (h), for silicon carbide particles in a succino-nitrile melt, is! ... Azouni, W. Kalita, M. Yemmou, J. Crystal Growth. 99 (1990) 201.[24] S. -
flm1000491a
www.itg.cam.ac.uk/people/heh/Paper225.pdf18 Jan 2011: φ̃0(0; λ̄) =. h(0, y)2 dy. (3.24). The solid curve in figure 5 shows the result of substituting the value of φ̃0(0; λ̄)found in this way -
Laminar free convection in confined regions
www.itg.cam.ac.uk/people/grae/4.pdf1 Jun 2006: 1 -. f = 16-21 min. 24.5 25.0 25.5 26.0 26.5 27.0 27.5 28.0 28.5 29.0 T. ... 0 - 1 24.5 25.0 25.5 26.0 26.5 27.0 27.5 28.0 28.5 29.0 29.5 30.0 30.5. -
doi:10.1016/j.jcp.2005.12.002
www.itg.cam.ac.uk/people/grae/74.pdf12 Jun 2006: g. [23,24]). The major difficulties then consist in the formulation of accurate internalboundary conditions and in following the evolution of the interfaces through time. ... 104 This study 19.6 16.2 3.53 0.585 2.24[2] 19.51 16.2 3.53 0.586 2.243[3] -
Thermohaline Steps Induced By Melting of the Erebus Glacier Tongue
www.itg.cam.ac.uk/people/heh/Paper44.pdf16 Jul 2010: Geophys. Res., 79, 1792-1797, 1974. Gebhart, B., and J. C. Molendorf, A new density relationship for pure and saline water, Deep Sea Res., 24(9), 831-848, 1977. ... Glaciol., 24, 259-271, 1979. Tressler, W. L., and A.M. Ommundsen, Seasonal oceanographic -
PII: S0301-9322(98)00062-7
www.itg.cam.ac.uk/people/heh/Paper151.pdf9 Mar 2004: rNt 0 rN0 24. M. Ungarish, H.E. Huppert / International Journal of Multiphase Flow 25 (1999) 715737 725. ... For this case. the box model yields [rN/rN(0)]max=[8Fr/(3 b)]1/4. (This is by about 24% smaller than for.
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