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10 Nov 2012: ISSN: 1525-2027. Copyright 2006 by the American Geophysical Union 1 of 24. ... GeochemistryGeophysicsGeosystems G3G3 poore et al.: neogene overflow of ncw 10.1029/2005GC001085. 4 of 24.

8 Mar 2012: 4 QUANTUM SCATTERING IN 3D 24. where δl is a function of k. ... γl =κaj′l(κa). jl(κa). (4.1.2.2). As k 0 have γl const, jl(ka) (ka)l, nl(ka) (ka)(l1) and, as before, getδl (ka)2l1.

27 Jul 2012: the various coefficients appearing in (3.24), (3.25) depend on the dimensionless couplingsgi. ... Thus we find. 2χei = Yi Ui iβjUj 12 (Vij Sij )βj θai ka. =

28 Jan 2012: welding parameters [44]. 24. Fig 2.16 several examples of external discontinuities in RSW [44]. ... 820 483 660 30 40. 840 486 665 30 39. 860 470 640 24 34.

17 Jan 2012: The microstructures of the weld nuggets are given inFig. 7 for cases where the current was 0?5 kA less thanImax. ... Table 4 Joint properties for commercial and investigated alloys. Carbon/wt-%Thickness/mm. Minimum weldcurrent/kA.

14 Aug 2012: kf(min1) ka(m3(n1)mole(n1)min1) n Aggregation Degradation. ADPr ADPr+ ADPr ADPr+. mol/24 h mol/24 h0.2 5 3 136.6 107.7 314.6 ... The effects of changing the rate of folding (kf) or the terms governing the concentration dependence of aggregation (ka and n)

15 Jan 2012: 0.82 kB T) and polar-polar (P-P, 24% of all contacts,21.69 kBT, s.d. ... Biochemistry 24: 1501–1509. 12. Dobson CM (1999) Protein misfolding, evolution and disease.

2 Sep 2012: Kachar & Reese 1989; Lichtscheidl & Balu ka 2000).Nevertheless, ‘relatively little is known about the biogene-sis, dynamics, maintenance, and inheritance of the organelleitself’ (Powell & Latterich 2000). ... al. 1999); and (v) thatthe actin

5 Sep 2012: 49) , and open 3D bulk suspensions (7, 18,24, 25), bacteria were confined in closed microfluidic chambers to. ... 6. Berg HC (1997) Motile behavior of bacteria. Phys Today 53:24–29.7.

10 Oct 2012: 24 CHAPTER 2. SECOND QUANTISATION. Our aim is to find an operator V̂ in second quantised form whose action on a many-bodystate gives. ... Ĥ = JN S2 B.Z.Xk! ka†kak O(S0) (2.16). where! k = 2JS(1 cos k) = 4JS sin2(k/2) represents the dispersion