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25 Sep 2008: while the kinematic equation yieldsu = @x@t ; v = @y@t : (20)Van Dommelen & Shen (1980) made the key observation that (19) de-pends only on x and u, and hence that ... 19) and the rst of (20) can besolved independently of the equations governing y and v.

30 Sep 2008: ψ(x, t) = χ(x) exp. (. iEt. ). (20). Substituting for (20) for ψ in the Schrödinger equation yields the time-independent. ... States of the special form (20) are known as stationary states.

29 Jan 2008: The results were staggering,especially the minimization of a periodic function F (x), x Rn, with 100 vari-ables, although problems with n = 20 were considered large at that time. ... The average values of these counts with m = 2n1 are 931, 1809,3159 and

5 Dec 2008: 20. Cop. yrig. ht. 200. 8 U. nive. rsity. of C.

23 Sep 2008: JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 94, NO. D12, PAGES 14,617-14,628, OCTOBER 20, 1989. ... r {-«Z3m a(sin Zm - Zm cos Zm)} (20). lfOZm AA = • -(z 2 - a 2 sin 2 z)dz - 3 -- •Zm q- «a2(zm- sinzm coszm)} (21).

17 Jan 2008: whenever this limit exists. Remarks. • It follows from (1.20) and the definition of a partial deriva-tive (1.14) that. ... To derive (1.52) start from the definition of a directional derivative (1.20), and use the definition of.

24 Apr 2008: 1.4 The ADHM Construction 20. 1.4.1 The Metric on the Higgs Branch 23. ... 20 –. of the D(p 4)-brane [3, 5]. They are the same object!

1 Feb 2008: 0 10 20 30 40 50 600. 5. 10. 15. 20. ... 3è1V6ñEG;=1"J /. i>31Vð@6:v3EF<@> <Cç35è1ENêïé-DF;1þ:C>-A 17>1V6ð"õÂ651V;éDN35;zEF> :@>. 5. 0 10 20 30 400.

1 Apr 2008: 7b) and, with H0 f 20 L. 2D /g, the undisturbed layer depth,.

27 Jan 2008: 20. for sufficiently small t. We will prove this. Let (U,ϕ) be a chart containing p then, in thesecoordinates, τ will have the form.