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9 Feb 2004: b 2004 to 131.111.8.96. Redistribution subject to AIP. ns. ’. the. ... The dotted line comes from theasymptotic theory of Sec. V B.b!

18 Jan 2007: G. Worster. (a). (b). (c). 12 cm. (b). (b). (a)(d). (c). ... dz= kl. d2T. dz2 b(T T). (2.3). 72 S. S. L.

30 May 2006: 8 ). ( 4. 8 b ). = 0 (n-reven), (4 8 c ) and Fnr = t w ' q s ,. , g , , r B B / ( b r - b n ). (,4.9). We again suppress the argument. ... 4.10 b ) N ( - )" 23(nw cosh [)-$ sin ( w cosh inn - &I-) sen(?).

30 May 2006: I n the former case. g ( t , y ) (Bt1-l (B-,O), (3.22). ... For B B 1 l,he penetration depth f L / N is much less than the actual depth H , and the critical height varies inversely with B.

7 Aug 2008: a dashed line, is the computational domain, shown in (b). (b) A schematic of the. ... 5(b). Wehave applied the same numerical method to predict the values of.

26 Apr 2006: where. B"B(j, hi)"! hi. Jpej2@4erf(j/2). (35). Eq. (34) is the transcendental equation determin-ing the eigenvalue j. ... Since gH is independent ofhiand B is expressed in closed form, we can calcu-.

7 Aug 2008: a dashed line, is the computational domain, shown in (b). (b) A schematic of the. ... 5(b). Wehave applied the same numerical method to predict the values of.

26 Mar 2023: b) As above, but for a two-dimensional geometry ( 3). 10 % of T. ... b), (b) the height above the input point, h(0, t), scaled by L2 and (c) the aspectratio of the current γ (height over length) as functions of dimensionless time

26 Sep 2011: d T / - d S < z. (5a,b) G = - z z f l d z. ... The Chemical. R u b b e r Co., 1263 pp.

21 Nov 2014: Using (2.14a,b) to evaluate P1 and P2 in (2.11), we obtain. ... its asymptotic value isdependent on all the parameters M, B, D and XF.

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).

15 Sep 2006: Finally (1) and (4) can be written. d r b 4/3 _,d t b b I b b - b •. Equations (8)-(l 1) describe the heat transfer and melting process ... a). 50 100. b). 100. c). 50 100. TIME (yrs). F I G.

25 Jan 2007: Lines of constant density. B. B. FIGURE 1. Phase diagram of a binary alloy. ... b ) Variation of solid composition, 1-4, with depth in the solid, h.

9 Mar 2004: Inthe liquid layer. B = B, C = C. (5.1). In the primary mushy layer. ... B =B. χ, C =. C. χ. (5.2). In the secondary mushy layer.

5 Jan 2006: ρs AH, φg =. mg. ρgAH, φl = 1 (φs φg), (1.1a, b, c). ... a) Ballotini in water, (b) KNO3 in solution,(c) KNO3 ballotini in solution.

23 Dec 2021: Direction of flow. Residual. ImbibitionDrainage. 0.8 1.0. (a) (b). z. FIGURE 1. ... h|rb =h|rb , hFI hr. rb. = hF Dhr. rb. , (2.23a,b).

9 Mar 2004: b). W. g. U. U = (1 – n5/2) 2. s = &(n) =s1/2. ... agreement with independent measurementsof the pump throughput, as shown on figure 4(b).

18 Sep 2006: Sparks: The Fluid Dynamics of a Basaltic M a g m a C h a m b e r. ... The crystals begin to settle, leading to a concentration which increases towards the b o t t o m.

30 May 2006: D = au3,/B, (10). 274 H. E. Huppert, J. S. Turner and M. ... of the layer. Hence. where B, is the buoyancy flux at the origin.

27 Apr 2006: o c k e d b y r u b b l e a n d previous- ly c o o l e d lava. ... p a n d s t o f o r m t h e r u b b l y surface.

26 Sep 2011: Southeast o f it, a smaller hill, casually n am ed " W e b b ' s F o o t " , was discovered in echo soundings taken during the experiment. ... s B u m p " and " W e b b ' s F o o t " is shown in Fig.

19 Jul 2010: S. T U R N E R ET AL. T A B L E 1. ... B. Relatedfigures. 3, 4, 5, 6. A2. A2, A3. A2. 11, 12B1.B2.