Chemists at Texas A&M University,
College Station, have devised a way to
employ NMR to simultaneously measure
small kinetic isotope effects of all
atoms involved in a reaction, using
natural abundances of the elements [J.
Am. Chem. Soc. 117, 9357 (1995)].
According to the researchers, the
technique may make determination of
all kinetic isotope effects routine
features of investigating reactions.
The key step in the method of organic
chemistry professor Daniel A.
Singleton and graduate student Allen
A. Thomas is to isolate the starting
materials after the reaction has gone
almost to completion. In this way,
positive isotope effects show up as
great enrichment at each atom
position, whereas negative effects
show up as great depletion -
differences easily seen in NMR. They
demonstrated their method with a study
of the Diels-Alder reaction of maleic
anhydride with isoprene. At 98.9%
completion, they distilled off the
unreacted isoprene and determined the
amount of deuterium and carbon-13 at
each position, using the presumably
uninvolved methyl group as an internal
standard.