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30 Oct 2015: C. Christodoulou, “Interfacial mixing in stratified flows,” J. Hydraul. Res. 24, 77–92 (1986).4 B. ... Downloaded. to IP: 131.111.16.57 On: Fri, 30 Oct 2015 10:24:16.

26 Apr 2006: 24),so f! 0 as x! 1. The interface shape is deter-mined from the equation for f in the inner regionalone. ... Wettlaufer, Rep. Prog. Phys. 58. (1995) 115. [24] J.S. Wettlaufer, M.G.

27 Apr 2006: 24. Zielinski, G. A. Use of paleo-records in determining variability within the volcanism-climate system.

22 Jan 2007: Inserting equations (2.23) and (2.24) into equations (2.12)–(2.16) andlinearizing in the perturbed quantities leads to the following nonlinear ordinarydifferential equation for the disturbance amplitude:.

21 Nov 2014: 19:. 20:. 21:. 22:. 23:. 24:. 25:. 26:. 27:. 28:. 29:.

13 Apr 2011: 24. The wave speed c is scaledby. ghstop cos θ and the maximal thickness hf by hstop. ... Jop, Y. Forterre, and O. Pouliquen, Nature (London) 441, 727. (2006).[24] I.

23 Dec 2021: Thus,with 1ρ =ρ because the density of the overlying air can be neglected, β = 24.8 or0.295 cm1 s1 and (βV 1/3)1 was between 0.004 s ... A 24). Dow. nloa. ded. from. htt. ps://. ww. w.c. ambr.

18 May 2017: 1γ). 1H(L). (p11/γD p11/γS. )(2.23). (. γ. 1γ). 1H(L). p11/γD. (2.24).

14 Feb 2013: 22:. 23:. 24:. 25:. 26:. 27:. 28:. 29:. 30:. 31:. 32:.

9 Feb 2004: r = (F/πV )1/2. (2.24)In contrast to the instantaneous, fixed volume release of the last section, there is not a finite radius at whichthe mass of particulate matter ... Applying these concepts to the relationship for the density of deposit for a single

18 May 2017: x = h(y) = 16 y3 c1y c2, (4.24)where c1 and c2 are constants. ... angles. SIAM J. Appl. Math. 49, 1009–1028. (doi:10.1137/0149061)24. Vogel TI. 2013 Liquid bridges between balls: the small volume instability.

24 Aug 2012: 0.1. 0 10. 0. 0.4. 101108. x/l0 10. 0. 0.4. S = 3 S = 24. ... σxx = E(1 ν)(1 2ν) [(1 ν)xx νyy ],. σyy = E(1 ν)(1 2ν) [(1 ν)yy νxx ], (24).

14 May 2008: 21. 22. 23. 24. 25. 26. 27. 28. V (µm s–1).

11 Oct 2006: After some algebra and use of(2.24), we obtain. ρD. Dt. [1. ... 374 M. Ungarish and H. E. Huppert. t0 4 8 12 16 20 24.

26 Apr 2006: Leppäranta, pp. 24–104,Univ. of Helsinki Press, Helsinki, 1998. Wettlaufer, J. S., Heat flux at the ice-ocean interface, J. ... E. Huppert, The phase evolution ofyoung sea ice, Geophys. Res. Lett., 24, 1251–1254, 1997a.

26 Mar 2023: as. th/T = 0.63, (2.24)at which time rN /L = 0.92 and h/L = 0.67. ... Illustrative evaluations of the time scales on which the axisymmetric transition from radial tothin-layer regimes occurs, given by (2.21)–(2.24), for a selection of geological

10 Mar 2011: MS received 24 June 2009 and accepted in revised form 10 February 2010.

11 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.

26 Mar 2023: So, was Ruskin simply blaming air pollution on the devil? Ruskin’s biographer notes the fact that[24].

30 May 2006: r 2 ) ( r < 1) 2.94 0.93 1.27 1.00 {(‘i ( r > 1 ). - I Cylindrical Gaussian e-T2 ( f < 00) 3.13 1-12 2.24 0.86. ... If h,R-l > Fmin (2.24) t It is interesting to compare these values with the relationship h0R-l = 2 deduced by.