With a slightly different for an ion when it is a reactant and when it is a product it was suggested that a mean value for a be adopted.” “The crystallographic radii of Fe+2, Fe+3, and H2O are [2] 0.75, 0.60, and 0.72. The mean of the first two is 0.68Å.”
The refinements of the theory will take into account the effect of the radii variations on the reaction rate.
When organic ions are considered one has to consider two new features. “First, the ion is far from being spherical and, second, it is possible that that the effective radius a could be quite different when this particle is a charged reactant and when it is an uncharged product. This is discussed later, where it is inferred from entropy data that the effective polarizing radius of a hydroquinone-like ion such as HOC6H4O− is about the same as that of the hydroxyl ion. It is further suggested that the dielectric saturation around this group when it is a charged particle be neglected as a first approximation, and that a equals the crystallographic radius of the oxygen group 1.4Å. This approximation can be removed by a refinement of the theory.”
3.29.Excess Free Energy of Activation
“Experimental values of ΔF* were calculated from the rate constant k given in Table 1, using Eq. (3.1) and setting Z equal to 1013 liter mole−1 sec−1 in that equation. These values are reported in Table I.
Using the effective radii and the ΔF0’s deduced in the preceding section and setting Dop = 1.8 and Ds = 78.5 at 25∘C, values of
An important note: M. later [71] used for Z the value 1011 liter mole−1 sec−1 instead of 1013 liter mole−1 sec−1 of Ref. [72].
3.30.Excess Entropy of Activation
“Experimental values for the excess entropy of activation of reaction (3.99),
It may be instructive to report, from note 26 in Ref. [2], how this calculation was done.
The pseudo-rate constant k1 of Eq. (3.97) has an activation energy E1, say, and a frequency factor A1 so that k1 = A1 exp(−E1/RT). Values of A1 were determined experimentally. The rate constant k, Eq. (3.99), has a frequency factor A, say, which can be calculated from the known A1 [51] and the known [70] entropy of ionization of QH2, ΔS1 say. It is found that A = A1[H+] exp(− S1/R). According to Eq. (3.7),
“The values of
“In this way
(b)AEROBIC OXIDATION OF THE LEUCOINDOPHENOLS
3.31.Excess Free Energy of Activation
“The overall reaction of the leucoindophenols with dissolved oxygen is represented by Eq. (3.102), where QH2 denotes a leucoindophenol such as HOC6H6NHC6H6OH, and Q denotes the corresponding indophenol HOC6H4NC6H4O.
A mechanism consistent with the data [51] involved the ionization of QH2 to QH−, which then transferred an electron to O2:
This