By use of naturally occurring C12 and C13 isotopes in carbon monoxide, the effect of carbon mass on the rate of the reactionhas been studied in a 15–1 Vycor flask, in the temperature range 540–727°K, and at pressures between 1 and 20 mm. The rate constant for the reaction was k=12×1012 exp (—31,600/RT) cc mole—1 sec—1. The ratio of rate constants k12/k13 was 1.022 at 540°K, 1.019 at 638°K, and 1.016 at 727°K. An activated complex was set up with normal bond distances and normal force constants, and with the reaction coordinate explicitly given in terms of internal coordinates with an interaction term such that the restoring force on an antisymmetric stretching symmetry coordinate is reduced to zero. By means of E. B. Wilson's FG matrix methods, a vibrational analysis was made of the activated complex, all vibration frequencies were determined for one species, and shifts in frequency due to isotopic substitution were computed by a perturbation method. Similarly, the ratio of effective mass of the reaction coordinate was evaluated, and calculations were checked by the Teller‐Redlich product rule. The isotope rate effect was computed by Bigeleisen's formulation of the activated complex theory. For a set of force constants well within the range of normal values and for normal bond radii, calculated isotope rate ratios at all temperatures are in excellent agreement with observed ones.
REFERENCES
1.
2.
3.
4.
Wilson, Decius, and Cross, Molecular Vibrations (McGraw‐Hill Book Company, Inc., New York, 1955), p. 184.
5.
Glasstone, Laidler, and Eyring, Theory of Rate Processes (McGraw‐Hill Book Company, Inc., New York, 1941).
6.
7.
8.
Herschbach
, Johnston
, Powell
, and Pitzer
, J. Chem. Phys.
25
, 736
(1956
).9.
Linus Pauling, Nature of the Chemical Bond (Cornell University Press, Ithaca, 1940).
10.
See reference 4, p. 188.
11.
See reference 4, pp. 175–176.
12.
13.
These ratios are based on reference 11 and on analogy to nitrogen tetroxide and to ethers. Other ratios could be used within the range of examples from normal molecules.
14.
15.
See reference 4, p. 68.
16.
Bigeleisen and Mayer7 give extensive tables of a function they call This function employs the approximation, Because of the very small isotope effect observed here, we found this approximation to be extremely poor for this case. In making these computations we kept all figures to six significant figures, rounding off only at the end. Unless extreme care is taken in these computations, rounding‐off errors can easily become as large as the isotope effect itself. In these calculations the ratio of kappas was taken as one.
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© 1957 American Institute of Physics.
1957
American Institute of Physics
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