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Tuesday Informal Lunch Seminars
www.itg.cam.ac.uk/seminars/tue_1.10/lent_2006.html24 Jan 2006: Please bring your own lunch. 24 January. Thibaut Putelat. (ITG). On the selection of active fault planes. -
Tuesday Informal Lunch Seminars
www.itg.cam.ac.uk/seminars/tue_1.10/mich_2006.html17 Oct 2006: Exchange flows during the ventilation of buildings. 24 October. Richard Katz. -
On Howards technique for perturbing neutral solutions of the…
www.itg.cam.ac.uk/people/heh/Paper14.pdf30 May 2006: which lead t o the eigenvalue problem? 4" [Jy2(y - c)-2 - $1 $75 = 0) (2.24) = o ( y = T ). ( 2. 2 5 a, b ). There are two infinite families of -
Lee waves in a stratified flow Part 3. Semi-elliptical obstacle
www.itg.cam.ac.uk/people/heh/Paper8.pdf30 May 2006: a$'(@, SY), DPI = { P } [ 1 , 1 , S&I, (4.23) where yil) = P-1Bi/Ms$2) (4.24 a). ... 4.24 b) = 1 1 8 ) K21og K O ( K 2 ). Truncating a t n = N = 2 , we obtain the second approximation. -
PII: 0022-0248(93)90538-8
www.itg.cam.ac.uk/people/heh/Paper116.pdf27 Apr 2006: iments havebeenusedin drawing up fig. 3.) Fig.1 • 24.5 5 then plots the heightsof the mushy layer and. ... 0 24 concentrationsas functions of time for experi-0 100 200 300 400 500 mentswith the six different valuesof the contam-. -
85230
www.itg.cam.ac.uk/people/heh/Paper146.pdf27 Apr 2006: 15, p. 9–24. Eppler, D. B., Fink, J., and Fletcher, R., 1987, Rheologic properties and kinematics ofemplacement of the Chaos Jumbles rockfall avalanche, Lassen Volcanic NationalPark, California: Journal of Geophysical -
Under consideration for publication in J. Fluid Mech. 1 ...
www.itg.cam.ac.uk/people/heh/jfm50.pdf28 Jul 2006: Geology 186 24.6 1.64 220 12.6 1.80. JFM 197 22.5 1.50 265 11.3 1.61. -
flm145.dvi
www.itg.cam.ac.uk/people/heh/Paper197.pdf11 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. -
Some remarks on the initiation of inertial Taylor columns
www.itg.cam.ac.uk/people/heh/Paper19.pdf30 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. -
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. -
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 -
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)—. -
doi:10.1016/j.jcp.2004.11.039
www.itg.cam.ac.uk/people/heh/Paper187.pdf5 May 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. -
The slumping of gravity currents
www.itg.cam.ac.uk/people/heh/Paper32.pdf30 May 2006: head. This Froude number should be 24 according to Benjamin, but Hoult suggests expressing it as a constant A, to be determined from experiment. -
Nonlinear double-diffusive convection
www.itg.cam.ac.uk/people/heh/Paper25.pdf30 May 2006: J. F u i d Xech. (19761, VOZ. 78, part 4? pp. 821-854 Printed in Great Britain. 82 1. Nonlinear double-diffusive convection By H E R B E R T E. H U P P E R T A N D D A N I E L R. MOORE. Department of Applied Mathematics and Theoretical Physics, -
The effect of side walls on homogeneous rotating flow over…
www.itg.cam.ac.uk/people/heh/Paper18.pdf30 May 2006: The situation can be made to appear even more problematic by continuing the analysis further, (2.24)-(2.31), from which i t appears that a full, three-dimensional calculation, incorporating ... 2 [ M o ( [ ) u(l)([)Ir 2 4 v ( ) ” ( [ ) 24. -
The growth and structure of double-diffusive cells adjacent to a…
www.itg.cam.ac.uk/people/heh/Paper183.pdf5 May 2006: 24 48.2 20.9 26 120 0.83 2.6 1760 2.7 1.38 48.2 20.5 20.3 20 1.18 1.5 2250 2.1 ... 34. 32. 30. 28. 26. 24. 22. 20. 18. 16. 14. -
Ice blocks melting into a salinity gradient
www.itg.cam.ac.uk/people/heh/Paper35.pdf30 May 2006: 0 69.5 24.6 30.4 40.8 47.3 62-5 29.2 37.2 51.9 41.7 23.7 29.7 36.5 42.2. ... 29.6 36.6 25.0 34.8 54.0 24.8 33-8 28.2 35.3 24.3. 1 0 3 dp. -
Collapses of two-dimensional granular columns Gert Lube,1 Herbert E.…
www.itg.cam.ac.uk/people/heh/Paper190.pdf5 May 2006: www.damtp.cam.ac.uk/lab/digiflow/ 2005.23 G. S. Campbell, Annu. Rev. Fluid Mech. 22, 57 1990.24 T. -
PII: 0377-0273(93)90087-8
www.itg.cam.ac.uk/people/heh/Paper110.pdf27 Apr 2006: Subsequently (ap- proximately 40-50 rain from the beginning),. 24 r. KOYa_GUCHI L, kt. ... grade particles with A T = 2 4 C and Co= 1.24 wt.%. -
Multiple coexisting states of liquid rope coiling
www.itg.cam.ac.uk/people/heh/Paper194.pdf17 May 2006: 4Laboratoire de Physique Statistique, UMR 8550 CNRS, Ecole Normale Supérieure, 24,rue Lhomond, 75231 Paris cédex 05, France. ... 1. 2. –12. 3. 10. G. I. IG. (ν. /g2 ). 1/3. ̂. H(g/ν2)1/3 Ĥ. ̂ (Ĥ/)10/3Π15/9. Π15/24. Π15/96. Π1–1/6 -
The stability of a large gas bubble rising through liquid
www.itg.cam.ac.uk/people/heh/Paper81.pdf30 May 2006: Stability of a large gas bubble rising through liquid 417. 24. ... 1. oo 1.712 1.26 1.42 1.10 1.24. 13.61 1.200 0.79 1.06 1. -
flm483.dvi
www.itg.cam.ac.uk/people/heh/Paper186.pdf5 Jan 2006: The experimentswere generally left to run for 24 hours, but heat loss to the laboratory became asignificant factor after roughly 10 hours. ... dy. dτ= (1 θ). (1 y)(1 Λθ). (3.24). y(τ = 0) = 1, (3.25). -
Gravity currents entering a two-layer fluid
www.itg.cam.ac.uk/people/heh/Paper37.pdf30 May 2006: 24-2. 740 J. Y. Holyer and H. E. Huppert. model for energy dissipation. ... The wavelengths given by (6.3) and (6.4) are 6.1 cm on the lower interface and 24-1 cm on the upper interface. -
The Generation of Granitic Magmas by Intrusion of Basalt ...
www.itg.cam.ac.uk/people/heh/Paper83.pdf15 Sep 2006: There is also. [Journal of Petrologf, Vol. 29, P t n 3, pp 599-«24, 1988] Oxford Umvcroty Prcu 19S8. ... FJH,. (24). We determined numerical solutions of (15)—(18) in addition to either (19)—(23) or merely (24).The differences were negligible. -
On gravity currents propagating at the base of a stratified ambient:…
www.itg.cam.ac.uk/people/heh/Paper184.pdf5 May 2006: We areinterested in cases with small C2H because otherwise the distance of propagation issmall, see (3.24), and no real gravity current appears. ... Using the approximations (3.19)–(3.24), we find: (i) for S < 1. -
Solidification of a binary alloy of variable viscosity from a…
www.itg.cam.ac.uk/people/heh/Paper129.pdf30 May 2006: University of Cambridge, Silver Street, Cambridge CB3 9EW, UK. (Received 17 October 1994 and in revised form 24 May 1995). ... Each freezing experiment took on the order of 24 hours, after which the solid crystalline block was cut up into pieces and the -
Magnetic resonance imaging of structure and convection in solidifying …
www.itg.cam.ac.uk/people/heh/Paper192.pdf5 May 2006: T = T(c) 5.176 c 13.27 c2 24.16 c3 75.52 c4 (2.1)for 0 < c < 0.7, where T (. C) is the temperature of the freezing ... 1:47, 2:14, 2:22, 2:49, 2:58, 3:24, 3:33, 3:59, 5:16, 5:43, 6:52, 7:46,. -
PII: 0012-821X(89)90063-0
www.itg.cam.ac.uk/people/heh/Paper87.pdf27 Apr 2006: Volcanol. Geothermal Res. 24, 1-24, 1985. 7 R.H. Nilson, A.R. McBirney and B.H. ... Volcanol. Geothermal Res. 24, 25-54, 1985. 8 I.H. Campbell and J.S. -
Gravity currents: a personal perspective
www.itg.cam.ac.uk/people/heh/Paper193.pdf5 May 2006: c). 100. 300. 500. 700. = 0.0500. g′ = 19.24 cm s–2. -
Entrainment into two-dimensional and axisymmetric turbulent gravity…
www.itg.cam.ac.uk/people/heh/Paper131.pdf30 May 2006: J. Fluid Mech. (1996), 001. 308, p p. 289-311 Copyright @ 1996 Cambridge University Press. 289. Entrainment into two-dimensional and axisymmetric turbulent gravity currents. BY M A R K A. H A L L W O R T H ' , H E R B E R T E. H U P P E R T ' , J E -
Particle-driven gravity currents
www.itg.cam.ac.uk/people/heh/Paper115.pdf30 May 2006: 0, for which case the third term in (24) is negligible and the single-layer shallow-water momentum equation is recovered. ... The two-layer model comprises the three equations (17), (21) and (24) for the three variables h, u and 4 that describe the -
Numerical modelling of convection in a reactive porous medium with a…
www.itg.cam.ac.uk/people/heh/Paper191.pdf5 May 2006: J. Fluid Mech. (2006), vol. 549, pp. 99–129. c 2006 Cambridge University Pressdoi:10.1017/S0022112005007500 Printed in the United Kingdom. 99. Numerical modelling of convection ina reactive porous medium with a mobile. mush–liquid interface. By -
On gravity currents driven by constant fluxes of saline and…
www.itg.cam.ac.uk/people/heh/Paper188.pdf5 May 2006: 14 24.4 8.5 380 015 25.2 17.1 276 016 26.2 34.1 204 017 25.9 63.2 171 018 103.3 8.3 90 019 ... 164 2.913 25.6 33.3 0.123 510 2.930 24.6 16.8 0.123 270 2.931 50 16.8 0.123 240 2.932 104.1 -
PII: 0012-821X(90)90126-I
www.itg.cam.ac.uk/people/heh/Paper98.pdf27 Apr 2006: Once the local Rayleigh number based on 8 exceeds a critical value, as determined by Smith [24] for example, the boundary layer breaks down and the magma begins to convect. -
PII: 0022-0248(94)00965-1
www.itg.cam.ac.uk/people/heh/Paper126.pdf27 Apr 2006: f_0q(z,) d z ' = A 2. (3.24) The functional form for the source strength q(z') is d e t e r m i n e d by matching -
Double-diffusive convection
www.itg.cam.ac.uk/people/heh/Paper42.pdf30 May 2006: J. Fluid Me&. (1981), vol. 106, p p. 299-329. Printed in Great Britain 399. Double-diffusive convection. By H E R B E R T E. H U P P E R T Department of Applied Mathematics and Theoretical Physics,. Silver Street, Cambridge CB3 9EW. A N D J. S T E W -
PII: 0012-821X(93)90028-8
www.itg.cam.ac.uk/people/heh/Paper112.pdf27 Apr 2006: 1034 23.0 24.0 0.016 67. K 1.3 w t. % saline s o l u t i o n S e d i m e n t m ... 1034 24.0 10.0 0.012 28. L 1.3 wt.% saline s o l u t i o n Secliment m fresh w a t e r. -
Sedimentation and entrainment in dense layers of suspended particles…
www.itg.cam.ac.uk/people/heh/Paper124.pdf30 May 2006: J. Fluid Mech. (1995), vol. 289, p p. 263-293 Copyright 0 1995 Cambridge University Press. 263. Sedimentation and entrainment in dense layers of suspended particles stirred by an oscillating grid. By H E R B E R T E. HUPPERT', J. STEWART TURNER' A N -
PII: 0377-0273(82)90062-2
www.itg.cam.ac.uk/people/heh/Paper48.pdf27 Apr 2006: r N = c ( ) (gS3/3v) 118 t (3 I)18 (2.24). ... 8 a n d using (2.24}. The results are:. S = 0.
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