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IUPAC Kinetic Data Evaluation

Atkinson, R., Baulch, D. L., Cox, R. A., Crowley, J. N., Hampson Jr., R. F., Kerr, J. A., Rossi, M. J., and Troe, J. Summary of Evaluated Kinetic and Photochemical Data for Atmospheric Chemistry, IUPAC Subcommittee on Gas Kinetic Data Evaluation for Atmospheric Chemistry, http //www.iupac-kinetic.ch.cam.ac.uk, December 2001. [Pg.16]

Data for Atmospheric Chemistry Supplement VI—IUPAC Subcommittee on Gas Kinetic Data Evaluation for Atmospheric Chemistry, J. Phys. Chem. Ref. Data, 26, 1329-1499 (1997a). [Pg.337]

Ongoing evaluations of kinetic and photochemical data essential for atmospheric chemistry are provided by the Jet Propulsion Laboratory of the California Institute of Technology, by the IUPAC Subcommittee for Gas Kinetic Data Evaluation [5-12],... [Pg.78]

R. Atkinson, D.L. Baulch, R.A. Cox, R.F. Hampson Jr., J.A. Kerr, M.J. Rossi, J. Troe, Evaluated Kinetic, Photochemical and Heterogeneous Data for Atmospheric Chemistry, Supplement V, IUPAC Subcommittee on Gas Kinetic Data Evaluation for Atmospheric Chemistry, J. Phys. Chem. Ref. Data, 26, 521... [Pg.222]

Imrik, K., Dobe, S., and Berces, T., Int. J. Chem. Kinet., 33,49-55, 2001. lUPAC Subcommittee for Gas Kinetic Data Evaluation, http //www.iupac-kinetic.ch.cam.ac.uk update frequently. [Pg.1598]

Because both forward and reverse reactions involve the participation of air molecules (M), the reaction rale coefficients for the forward and reverse reactions are represented by the general termolecular form (3.25). The reverse (decomposition) reactions in these types of reactions are typically highly temperature-dependent. Reaction rate coefficients for these two reactions are given in both the IUPAC (Atkinson et al. 2004) and JPL (Sander et al. 2003) kinetic data evaluations. In the IUPAC evaluation both forward and reverse rate coefficients are given. The JPL evaluation presents the forward rate coefficients and the equilibrium constants for the reactions. At equilibrium the rates of the forward (/) and reverse (r) reactions are equal, so the equilibrium constant, K r, is directly related to the forward, kf, and reverse, kf, rate coefficients. For example, for N2Os formation,... [Pg.92]

Atkinson, R., Baulch, D.L., Cox, R.A., Crowley, J.N., Hampson, R.F., Hynes, R.G., Jenkin, ME., Rossi, M.J., Troe, J. IUPAC Subcommittee evaluated kinetic and photochemical data for atmospheric chemistry Volume II— gas phase reactions of organic species. Atmos. Chem. Phys. 6, 3625 055 (2006)... [Pg.133]


See other pages where IUPAC Kinetic Data Evaluation is mentioned: [Pg.691]    [Pg.252]    [Pg.460]    [Pg.39]    [Pg.57]    [Pg.360]    [Pg.50]    [Pg.171]    [Pg.173]    [Pg.1392]    [Pg.1428]    [Pg.173]    [Pg.176]    [Pg.1968]    [Pg.279]    [Pg.932]   


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