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  2. A1La.dvi

    www.damtp.cam.ac.uk/user/examples/A1La.pdf
    25 Jan 2007: mis. sion. P.H.Haynes Mathematics IA Algebra and Geometry Michaelmas Term 2002 24.
  3. O5L.dvi

    www.damtp.cam.ac.uk/user/examples/O5L.pdf
    25 Jan 2007: ithou. t per. mis. sion. where D = 0E; H = 10B: (24)The latter vectors are used to describe non-trivial electrical and magnetic properties ofmedia for which and are callled permittivity ... We might ask: can we obtain an understanding of the elementary
  4. 25 Jan 2007: E. Huppert. Parameter Value Units. a (5.0+ 0.24( T- 20)) x U 0.015 cm2 s-' CC 4.14 J O C - '. 2.66 J cm-3 O C - '
  5. 25 Jan 2007: 0.01 (for Ra, = lo@), convection continues in the melt until t = 0.24, by which time the system is about 40% solidified.
  6. 25 Jan 2007: J. Fluid Mech. (1989), voZ. 198, p p. 293-319. Printed in Great Britain. 293. Phase changes following the initiation of a hot turbulent flow over a cold solid surface. By HERBERT E. HUPPERT Department of Applied Mathematics and Theoretical Physics,
  7. 10858_2006_9117_37_2-web 117..1

    www-vendruscolo.ch.cam.ac.uk/richter07.pdf
    25 Jan 2007: secondary structures (residues 2–7, 12–16, 23–24, 41–45,. 48–49, and 66–71) (Nederveen and Bonvin 2005).
  8. doi:10.1016/j.jmps.2006.08.004

    www-mech.eng.cam.ac.uk/profiles/fleck/papers/227.pdf
    26 Jan 2007: Received 24 April 2006; received in revised form 18 August 2006; accepted 24 August 2006. ... sA 0 and sB 2:9T. r̄2. (24). We shall show below in a case study on the centre-cracked panel subjected to uniaxialtension that the large negative T-stress is
  9. A history of cosmologies and their religious contexts | Faraday

    https://www.faraday.cam.ac.uk/resources/multimedia/a-history-of-cosmologies-and-their-religious-contexts/
    Thumbnail for A history of cosmologies and their religious contexts | Faraday 30 Jan 2007: 480x360. 799.09 MB. WebM. 480x360. 343.01 MB. 480x360. 240.24 MB. 320x240.
  10. ENTROPY PRODUCTION IN THERMOSTATS II NURLAN S. DAIRBEKOV AND ...

    https://www.dpmms.cam.ac.uk/~gpp24/thermo2oct.pdf
    3 Feb 2007: 24) 〈R̃y(Z), Z〉 = 〈Ry(Z), Z〉 〈Z E, Z〉 〈E, Z〉2.Indeed,. ... 7 α and using (24), we deduce:. (31). SM. {|F :u (n/2 1 α)〈E, y〉Z|2 α.
  11. 3 Feb 2007: The problem is open even forgeodesic flows. We refer to [24] for partial results in this direction when k = 2. ... Proc. CambridgePhilos. Soc. 139 (2005) 307–316. [24] V.A. Sharafutdinov, G. Uhlmann, On deformation boundary rigidity and spectral

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