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www.itg.cam.ac.uk/people/heh/Paper240.pdf14 Feb 2013: 22:. 23:. 24:. 25:. 26:. 27:. 28:. 29:. 30:. 31:. 32:. -
PHYSICAL REVIEW E 87, 023015 (2013) Interface pinning of ...
www.itg.cam.ac.uk/people/heh/Paper239.pdf11 Apr 2013: In a related context, the classical modelhas been modified to replace the sharp interface by a capillarytransition zone [24–26]. ... Porous Media 18, 107 (1995).[24] L. W. Lake, Enhanced Oil Recovery (Prentice-Hall, Englewood. -
Hogg, Charlie A. R., Clelia L. Marti, Herbert E. Huppert, and…
www.itg.cam.ac.uk/people/heh/Paper238.pdf12 Apr 2013: Parameter Value. Inflow channel width (m) 49Inflow channel depth (m) 1.7Inflow velocity (m s21) 0.48Inflow reduced gravity (m s22) 0.021Inflow temperature (uC) 13.0Lake surface temperature (uC) -
Handbook of Environmental Fluid Dynamics: Overview and Fundamentals
www.itg.cam.ac.uk/people/heh/Paper236.pdf11 Apr 2013: 2 2 2. 24/.467. 35.1 Introduction. -
Spreading and convective dissolution of carbon dioxide in vertically…
www.itg.cam.ac.uk/people/heh/Paper237.pdf14 Feb 2013: 24] An upscaled model for convective dissolution canthen be incorporated into models such as equation (1) byintroducing a constant loss or sink term [Gasda et al.,2011 ; MacMinn et al., 2011],. -
On the hydrodynamic interaction between a particle and a ...
www.itg.cam.ac.uk/people/heh/Paper244.pdf30 Jul 2013: 24). The perturbation equations are given, at O(βN), by. 1. η. -
doi:
www.itg.cam.ac.uk/people/heh/Paper242.pdf11 Apr 2013: From the exactsolution we have. W0 =. Z2 1 (π2. 24. ... 4.24). This inner solution indeed satisfies the tip condition w0,in = 0 as Z 0, and asZ it reproduces the source term seen in (4.23). -
The effects of capillary forces on the axisymmetric propagation ...
www.itg.cam.ac.uk/people/heh/Paper243.pdf12 Apr 2013: H = (Q/ub)1/2, (24)and the dimensionless height profile f is solely a function of y, the scaled similarity variable, definedas.
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