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1 - 10 of 32 search results for tj KaKaotalk:PC53 where 0 match all words and 32 match some words.

  1. Results that match 1 of 2 words

  2. pcm_proof

    www.statslab.cam.ac.uk/~frank/PAPERS/PRINCETON/pcm0052.pdf
    1 May 2006: Tj (yj ) = yj D′j (yj ). Then µj is the generalized cost of using link j, definedas the sum of the toll and the delay, and λs is theminimum generalized cost

  3. The invasion and coexistence of competingWolbachia strains MJ…

    www.jiggins.gen.cam.ac.uk/pdfs/Wolbachia%20Keeling%20model.pdf
    3 Nov 2006: J. T. ðd þ DIÞTI fIðI; J; UÞ. dJ. dt tJ bJ 1 qI. ... We note thatwhen the transmission (tJ) and cytoplasmic incompat-. ibility (qJ) parameters are low; those infected with strain Jcannot out-compete the uninfected individuals; so strainJ is doomed

  4. The Evolution of Parasite Recognition Genes in the Innate Immune…

    www.jiggins.gen.cam.ac.uk/pdfs/JME-pgrp.pdf
    3 Nov 2006: Si-. nauer Associates, Sunderland, MA, pp 33–61. Carius HJ, Little TJ, Ebert D (2001) Genetic variation in a host-.

  5. The Generation of Granitic Magmas by Intrusion of Basalt ...

    www.itg.cam.ac.uk/people/heh/Paper83.pdf
    15 Sep 2006: magma layer. TABLE 2. The table lists the time (tj) at which the basalt layer becomes 60% crystalline and ceasesconvection for different basalt layer thicknesses.

  6. Gravity currents entering a two-layer fluid

    www.itg.cam.ac.uk/people/heh/Paper37.pdf
    30 May 2006: 751. -. -. -. -. -5 - - - - - - - - - - - - _ _ -- -1 - - _ - - --=- _ _ _ - - -. I I";, tJ I 4 1 VI I I I. 0.25 -. ;I tJ 4 1 v. I I I I I. It is also shown that there

  7. Laminar free convection in confined regions

    www.itg.cam.ac.uk/people/grae/4.pdf
    1 Jun 2006: uw,ww, = vw,,ag(T-TJ, ( 1 ). (2) uT, wT, = K T , t Some authors prefer to use the Grashof number 6% = u-l Ra.

  8. This isa super vis or’ sco py ofth enote ...

    www.damtp.cam.ac.uk/user/sjc1/teaching/NSTIB/notes.pdf
    28 Oct 2006: This. isa. super. vis. or’. sco. py. ofth. enote. s.It. isnot. tobe. dis. trib. ute. dto. studen. ts. Natural Sciences Tripos: IB Mathematical Methods I. Contents. 0 Introduction i. 0.1 Schedule. i. 0.2 Books. ii. 0.3 Lectures. ii. 0.4 Printed

  9. This isa super vis or’ sco py ofth enote ...

    www.damtp.cam.ac.uk/user/sjc1/teaching/NSTIB/Michaelmas/notes.pdf
    28 Oct 2006: This. isa. super. vis. or’. sco. py. ofth. enote. s.It. isnot. tobe. dis. trib. ute. dto. studen. ts. Natural Sciences Tripos: IB Mathematical Methods I. Contents. 0 Introduction i. 0.1 Schedule. i. 0.2 Books. ii. 0.3 Lectures. ii. 0.4 Printed

  10. Bnew_BIT.dvi

    www.damtp.cam.ac.uk/user/na/NA_papers/NA2006_04.pdf
    24 Nov 2006: K} such that. ti º tj , j = 1, 2,. , ... K. If ti tj for all j 6= i, we let (ti, ti1,. ,

  11. SOIL MECHANICSArnold Verruijt Delft University of Technology, 2001,…

    www-mdp.eng.cam.ac.uk/web/library/enginfo/textbooks_dvd_only/soilmechs/SoilMechBook.pdf
    3 Mar 2006: SOIL MECHANICSArnold Verruijt. Delft University of Technology, 2001, 2006. This is the screen version of the book SOIL MECHANICS, used at the Delft University of Technology.It can be read using the Adobe Acrobat Reader. Bookmarks are included to

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