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26 Jul 2013: a). (b). (b) (c). (d). (c). (d). 1. 2. FIG. 8. ... New York, 1992.10 B. Chen, P. D. Wu, and H. Gao, Proc.

20 Feb 2013: XB)a (Y B)b for some integers a,b 0. ... b = (bτ )τHom(E,C) by the formula. (bτ,1,. ,bτ,n) = (a1τ,1,.

19 Oct 2013: Km F6 =I QK 6{ K! x== F6Z? ] =4-<4- 0#B6< =I ]? {? 4g :I KK 0 B"L UBJÔ< =;:I KK ITIT B XABUBJÔ<? ... B"K J5,.#G?=II:; IRÂ0==IIKmG KrKÝG= #g 4< X8 K 4- 'F,.#.=II.

30 Jul 2013: 4(b)). B. “Permeation drag” balanced by repulsive surface forces. Next, we consider a neutrally buoyant particle carried toward the surface by the fluid permeatingthrough the surface (at a rate V0) ... Increasing. 1 Equilibrium. 2 Equilibria. (b). 0

22 May 2013: P(xt1 | Xt, Ut) = P(xt1 | xt, ut). (b) Separable (or decomposable) cost function, (i.e. ... s. In the discounted case, with |c(x, u)| < B, imagine subtracting B > 0 fromevery cost.

19 Aug 2013: Rotation of particles – rigid and dilute. Spheroid: axes a, b, b, aspect ratio r = ab. ... Averaged stress. σ = pI 2µE 2µφ[AE : 〈pppp〉. B(E 〈pp〉 〈pp〉E) CE FDrot〈pp〉].

24 Jan 2013: likelihood estimate of θ is (2a b)/(b 2c). 5. (a) Let X1,. ... b) For some n > 2, let X1,. ,Xn be iid with Xi Exponential(θ).

2 Apr 2013: We plot the loglikelihood surface for a = 1.4,. , 1.6 and b =. 06,. ,. 08. a = 0:20 ; a = a(.01) 1.4b = 0:20 ; b = b(.001) 0.06zz = 1: ... k = 3, t = 4, λ = 2, n = 12, b = 4 (in standard notationfor balanced incomplete blocks).

26 Jul 2013: 2x,0 = a cosx t 1 x x,0 b sinx t 1. ... ̃̇1, D12we obtain, after some algebra,. 4 2 =De1De2 De1. 1 De12 b.

31 Oct 2013: However, ‘This also has thepotential to be applied to the forma-tion of other bonds, bothhomoatomic such as Si–Si orC–C, and heteroatomic bondssuch as C–P and

12 Apr 2013: ηN =[. 2π 1. 0. f0. s[ B f (y), z]yd zd y. ... s0( f B) B f (33a)and. F( f B) 2. 4(2 ) ( f B)3 , (33b).

10 Oct 2013: 5. Moreover, if Y ′ also satisfies (a) and (b), then Y = Y ′ a.s. ... Rearranging gives the desired inequality. Proof of Theorem 2.13. Let a < b Q.

22 May 2013: XT. Proof (not examinable). If B is an event determined by X0, X1,. , ... XT n = jn} B {T = m} {XT = i})= Pi({X0 = j0, X1 = j1,. ,

15 Aug 2013: where E F# denotesthe identity matrix. In many cases,thepeakscanbeassumedtruncatedGaussianin shapesuchthat:, (/. JILK ( M ( 0N. POQ M ( 0SRT UVW#XZY[ O M (. ][K ( 0 4_a. B b[bK ( B#cedf0. (3). ... 2.2. State-Space Form. The setof peaksaffecting the

26 Jul 2013: a) (b) (c). 0 1.0 0 1.0–1.0. 1.0. FIGURE 2. Trajectories, ξ(t), of surface material points for stroke A (a), stroke B (b), andstroke C ... a). (b). (c). (d ). (e). ( f ). 0 1.0 0 1.00 1.0.

3 Mar 2013: 189. A. THE SINGLE-DEGREE-OF-FREEDOM MODEL. 196. B. THE BOUNDARY-ELEMENT METHOD. 199.

26 Oct 2013: I objects U A XI maps U A X to V B Y. ... The interaction of identity and existence. Bf. - A. '. Σa A, b B.IdA(f (b), a). -.

5 Aug 2013: For 2 b B, after receiving (y1, y2)b1 throughfeedback, the encoder generates the input xb for block b asfollows. ... C. Decoding. At the end of each block b (2 b B), the decodersreceive y1b and y2b, respectively.

2 Apr 2013: a) SWNT bundle, (b) absorption spectra of SWNTs dispersed in water with sodium docecylbenzenesulfonatesurfactant. ... N.; Yin, Y.;Cronin, S. B.; Unlu, M. S.; Goldberg,B. B.; Swan, A.

26 Jul 2013: a) (b). b/a = 1/2. V (e). qΩ. V (e). qΩ. ... n 1 Anan2. n 1BnanPn1. 49. B. Efficiency and optimization of an entirelyporous sphere.