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A kinetic isotope effect (KIE) is an effect observed due to differences in the chemical reaction rates of a molecule with a heavier isotope (k H) relative to one containing a lighter isotope (k L):
Molecules with different isotopic compositions generally react with other molecules in the same manner, but their reaction rates show differences due to their mass differences and sometimes also due to the lower natural abundance of certain isotopes. For example, 13C16O2 is heavier than 12C16O2 by about 2.3 %, and the abundance ratio of 13C16O2/12C16O2 is about 1.1 %. In photosynthesis by plants, the fixation rate of 13C16O2 is slower than that of 12C16O2, which causes a decrease of the 13C/12C ratio in biosynthesized glucose. Thus, the isotopic composition of natural samples is an important parameter in studying their origins. For example, the isotopic composition of organic carbon can be used...
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© 2014 Springer-Verlag Berlin Heidelberg
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Kobayashi, K. (2014). Kinetic Isotope Effect. In: Amils, R., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27833-4_5240-1
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DOI: https://doi.org/10.1007/978-3-642-27833-4_5240-1
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Publisher Name: Springer, Berlin, Heidelberg
Online ISBN: 978-3-642-27833-4
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