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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.

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1 Aug 2004: B+32The parti ular ase B̂ = b̂ orresponds to the ase of Dira 'sele tron in magneti eld, onsidered above. ... Consider, for instan e,B = ip W(x)p2 ; B = ip W(x)p2 ;fB;Bg = p2 W2; [B;B+ = W 0:Then, H = p2 W2 W 032 ;or, in the

6 Mar 2004: q. qg. b. b. W-. W+. t. t. Final State (top lifetime too short. ... e-. e+. H0. Z0Z0. b. b. f. f. Dr M.A. Thomson Lent 2004.

19 Apr 2004: σ. (11). The A and B stiffness matrices of CLT and are given by. ( ). ( ). ... grad gradK D D u uψ = = b b b b (23) where b is the unit vector in the direction of the derivative.

29 Nov 2004: B B B ( )( ( )1 0 11)0 1. Figure 2: A magnetic monopole emitting two flux tubes. ... Phys. B 492, 152 (1997) [arXiv:hep-. th/9611230].[15] A. Hanany and K.

6 Jul 2004: I = I and (A B) = B A. on the nose, and similarly for maps. ... a bc d. ). with a C(A, B), b C(C, B), c C(A, C) d C(C, C) using the naturalformula.

3 Jun 2004: Sub-glacial topography rpl B loc J # q0 53674 art a Croot /David G. ... Brian Birley a Beckett /John Angus t Iceland adventure: the double traverse of Vatnajoukull by the Cambridge expedition, with an introduction by B.B.

25 Mar 2004: The Killing form evaluated on a pair of nn skew-symmetric matricesA, B is actually (n 2)trace AB (see (Kobayahsi & Nomizu 1969)). ... . 0 a b ca 0 c bb c 0 ac b a 0.

5 Jan 2004: 100. 50. 0. 50. 100. A. B′. B. C. D. Applied water pressure. ... 100. A. B′. B. C. D. Pressure decreasing. 150 100 50 50 100 1500.