Page 353 - Advanced Organic Chemistry Part A - Structure and Mechanisms, 5th ed (2007) - Carey _ Sundberg
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334                            Scheme 3.4. Some Representative Kinetic Isotope Effects

     CHAPTER 3                                   Reaction                         k /k D  (°C)
                                                                                   H
     Structural Effects on
     Stability and Reactivity  A. Primary kinetic isotope effects
                          1 b  PhCH 2  H*  +  Br·    Ph  CH · +  H*  Br           4.6 (77)
                                                      2
                                    O                          O –
                          2 c  (CH ) C  C  C(CH ) 2   + OH –  (CH ) C  C  C(CH )  6.1 (25)
                               3 2
                                                                       3 2
                                           3
                                                           3 2
                                 H*    H*                    H*
                          3 d  H*
                                   +
                                   N(CH ) + OH –           +  (CH ) N             4.0 (191)
                                       3 3
                                                                3 3
                          B. Secondary kinetic isotope effects
                          4 e                                           H*
                             CH O        CH*  O  +  HCN     CH O        C  OH     0.73 (25)
                               3
                                                              3
                                                                        C
                                                                        N
                          5   f         H*        O               H*
                                                H 2
                             CH 3       C  Cl          CH 3       C   OH          1.30 (25)
                                              CF CH OH
                                                3
                                                   2
                                        H*                        H*
                                     2
                          6 g      CH *
                                      CH *
                                        2
                                                                                  1.37 (50)
                                                            +  CH2*  CH *
                                                                      2
                          a. Temperature of measurement is indicated in parentheses.
                          b. K. B. Wiberg and L. H. Slaugh, J. Am. Chem. Soc., 80, 3033 (1958).
                          c. R. A. Lynch, S. P. Vincenti, Y. T. Lin, L. D. Smucker, and S. C. Subba Rao, J. Am. Chem. Soc., 94, 8351
                           (1972).
                          d. W. H. Saunders, Jr., and T. A. Ashe, J. Am. Chem. Soc., 91, 473 (1969).
                          e. L. do Amaral, H. G. Bull, and E. H. Cordes, J. Am. Chem. Soc., 94, 7579 (1972).
                          f. V. J. Shiner, Jr., M. W. Rapp, and H. R. Pinnick, Jr., J. Am. Chem. Soc., 92, 232 (1970).
                          g. M. Taagepera and E. R. Thornton, J. Am. Chem. Soc., 94, 1168 (1972).
                       especially in the range between 1 and 2. For these reasons, isotope effects are usually
                       used in conjunction with other criteria in the description of reaction mechanisms. 123
                           A new method for determining KIE using compounds of natural isotopic
                       abundance has been developed. 124  This method makes experimental data more readily
                       available. The method is based on the principle that as the reaction proceeds, the
                                                            2
                       amount of the slower reacting isotope, e.g., Hor  13 C, is enriched in the remaining
                       reactant. For example, an isotope effect of 1.05 leads to ∼ 25% enrichment of the less
                                                                                          2
                       reactive isotope at 99% conversion. The extent of enrichment can be measured by H


                       123   For more complete discussion of isotope effects see: W. H. Saunders, in Investigation of Rates and
                          Mechanisms of Reactions, E. S. Lewis, ed., Techniques of Organic Chemistry, 3rd Edition, Vol. VI, Part
                          1, John Wiley & Sons, New York, 1974, pp. 211–255; L. Melander and W. H. Saunders, Jr., Reaction
                          Rates of Isotopic Molecules, Wiley, New York, 1980; W. H. Saunders, in Investigation of Rates and
                          Mechanisms of Reactions, C. F. Bernasconi, ed., Techniques of Organic Chemistry, 4th Edition, Vol.
                          VI, Part 1, Interscience, New York, 1986, Chap. VIII.
                       124
                          D. A. Singleton and A. A. Thomas, J. Am. Chem. Soc., 117, 9357 (1995).
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