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18 Jan 2011: the current first reaches the sink, as illustrated in figure 2(a, b). ... B). The results of this more detailedmodel are also shown in figure 6.

4 Jun 2009: subscripts 2 and 3 refer to regions b < z < 0 and z < b. ... H = h/SV , L = l/SV , B = b/SV , X = x/SH and T = t/ST ,(2.13a, b, c, d , e).

6 May 2010: q. x u(h) h. x u(b) b. x. ]. (2.27). In the sheet, in which there is a leading-order parabolic shear flow. ... 4(a), and for steep slopes (A > 1), shown in figure 4(b).

30 Jul 2013: 4(b)). B. “Permeation drag” balanced by repulsive surface forces. Next, we consider a neutrally buoyant particle carried toward the surface by the fluid permeatingthrough the surface (at a rate V0) ... Increasing. 1 Equilibrium. 2 Equilibria. (b). 0

18 Nov 2009: vf (x, t) = kf. μ. ρg(h b). b= φγ kf. ... xf = 11 cm. Balance Balance. PumpW = 1.1 cm. b = 2.1 cm.

15 Jul 2010: or potassium carbonate and nitric acid to release small b u b b l e s of CO 2. ... i c h liberate CO2 b u b b l e s o n reaction.

16 Jul 2010: 9 - " I g a b b r o ] / / / =. 1 I I ]. 9 0 8 0 7 0 6 0. ... 8 0 O O = m. 9 0 -. / G a b b r o n o r i t e / / i I I 1 I I.

30 May 2006: b P 2 b FIGURE 1. Finite obstacle in seini-infinite, stratified flow. ... The most interesting special cases are given by. A , = 4 h 2 ( A / 2 m ) ( l o g ( 4 h / b ) - 1}OO(b21og(h/b)} (b/hO) (A 7 ) and.

27 Apr 2006: tems. In addition, crystals an d b u b b l es in m ag m as m a y b e distributed so t h at they create stable den- ... G. F. G i b b , C. M. B. H e n d e r s o n , C.

12 Apr 2013: ηN =[. 2π 1. 0. f0. s[ B f (y), z]yd zd y. ... s0( f B) B f (33a)and. F( f B) 2. 4(2 ) ( f B)3 , (33b).