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Introduction E.J. Hinch D.A.M.T.P. Cambridge University Mobile…
www.damtp.cam.ac.uk/user/hinch/teaching/mobile.pdf23 Apr 2004: In long drums (some of the model experimentshave been with very short drums which permit just a monolayer of particles), Fauvredescribes in chapter 20 an axial instability which leads to a ... For thin layers of grains,Fauvre shows in chapter 20 that air -
report.dvi
www.damtp.cam.ac.uk/user/na/NA_papers/NA2004_01.pdf7 Jan 2004: 2eTt H et = 1 αβ τ2. Hence, by. taking determinants of the matrix equation (2.20), we obtain the condition. ... 20. defined by formula (2.12), where α = eTt Het and σ = αβ τ2, the value of σ being. -
Appendix I: Rossby-wave propagation and shear instability M. E. ...
www.damtp.cam.ac.uk/user/mem/GEFD-SUMMER-shear-instability.pdf30 Sep 2004: Batchelor’s textbook, eq. (7.1.20)). The fact that small Kmeans radian wavelength k1 À 2b suggests that the disturbance should see the whole shear layeras being thin; i.e. ... Rev. Fluid Mech., 20, especially pages381–384. 9. Suppression of shear -
IserlesNorsett2.dvi
www.damtp.cam.ac.uk/user/na/NA_papers/NA2004_05.pdf17 Jun 2004: ω. 500480400. 20. 10. 440420. 30. 40. Figure 2.1: The error for QA1 (bottom) and three different Filon-type methodsQF1 (from the second plot up), scaled by ω. -
Chapter 2 Poisson’s Equation 2.1 Physical Origins Poisson’s equation, …
www.damtp.cam.ac.uk/user/reh10/lectures/nst-mmii-chapter2.pdf8 Mar 2004: 2=. e2. 20. (G. x. )2,. and we calculate G/x as in the worked example in the next section. ... e2. 20. x20. 4π2(x20 (y y0)2 (z z0)2. )3 dy dz = = e216π0x20.
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