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10 Apr 2006: in difficult multi-jet environment. Some preliminary. Compare with LEPee- WW-ee- Z and dominate. ... Philosophy:. Will describe this in some detail to highlight some of the issues involved….

30 May 2006: 0.2 0.4 0.6 0.8. 1 1.2 1.4 1.6 1.8. 2(a) (b). ... a) (b). FIG. 7: (a) p(λ|mDM h2 ), the probability distribution assumed for λ, the ratio of predicted SUSY dark matter to total darkmatter, given some measured value mDM h2.

30 May 2006: Printed in Great Britain. 397. Some remarks on the initiation of inertial Taylor columns. ... Thus further compression is needed for some of the vortex lines to be able to flow over the obstacle.

27 Apr 2006: With time, some dense input fluid spreads along the b o t t o m so that locally the situation is the same as the one considered in the previous studies, ... h o u s layer on the container floor continued for quite some time.

13 Oct 2006: ON SOME -ADIC REPRESENTATIONS OF Gal(Q/Q)ATTACHED TO NONCONGRUENCE SUBGROUPS. A. J. ... Therefore for some a, b Z, azHT b is asemisimple element of g with exactly 2 eigenvalues.

17 Aug 2006: 39]. As a result, a fraction of some proteins (e.g. hepatitis B virus precore and. ... b,c) The cleaved signal peptides of some viral. glycoproteins mediate functions that are essential for the viral life cycle.

23 Nov 2006: with the addition of some material. These notes are for the exclusive use of Cambridge Part III students and they are not intendedfor wider distribution. ... Inother words, the solution is forced (at the price of tying down some degrees of freedom)

30 Nov 2006: of the first part. 1. The square matrices A and B over the field F are congruent if B = P tAP for some invertible matrixP over F. ... 7. Let S be a real symmetric matrix with Sk = I for some k 1.

6 Apr 2006: Sk musthave the same colour; say cm = cn for some 0 m < n k. ... Now, suppose that we have already constructed Ui1 as required for some i,.

30 May 2006: This fluid convects into the upper layer and carries with it some of the particles. ... b ) Calculated positions of some of t h e layers of constant bulk density for t h e differential sedimentation of a suspension of type-1 particles.