2015
DOI: 10.1039/c4ra14087g
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Theoretical study of deuterium isotope effects on acid–base equilibria under ambient and hydrothermal conditions

Abstract: The calculated difference between pKa values in H2O and D2O is in excellent agreement with experiment.

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Cited by 27 publications
(33 citation statements)
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“…This is consistent with the fact that the pK a of an organic acid is in general higher in D 2 O than in H 2 O. 19 The difference in these intensity ratios indicates that the isotopic effects alter the rate of deprotonation of photo-excited pyranine. Releasing of heavier D + from deuterated pyranine and transferring it through the hydrogen-bonding network should be slower, leading to the higher Q.…”
Section: Methodssupporting
confidence: 76%
See 1 more Smart Citation
“…This is consistent with the fact that the pK a of an organic acid is in general higher in D 2 O than in H 2 O. 19 The difference in these intensity ratios indicates that the isotopic effects alter the rate of deprotonation of photo-excited pyranine. Releasing of heavier D + from deuterated pyranine and transferring it through the hydrogen-bonding network should be slower, leading to the higher Q.…”
Section: Methodssupporting
confidence: 76%
“…A higher Q value of deuterated pyranine (relatively higher I PyOD* and lower I PyO−* ) represents that PyOD* is less acidic than PyOH*. This is consistent with the fact that the pK a of an organic acid is in general higher in D 2 O than in H 2 O . The difference in these intensity ratios indicates that the isotopic effects alter the rate of deprotonation of photo‐excited pyranine.…”
Section: Resultssupporting
confidence: 65%
“…57 The deuterium isotope effect due to zero-point energies has been determined both experimentally and computationally to be around 0.5 pK a units for several aromatic acids with varying acidities. 58 This corresponds to a difference of 0.67 kcal mol À1 in DG. If the observed amplitudes of the fast decay components in H 2 O and D 2 O are assumed to reect the relative CIP* populations, the difference in DG is estimated to be 0.55 kcal mol À1 , in close agreement with the above value.…”
Section: Comparison With Experimental Decaysmentioning
confidence: 99%
“…[ 2 ] The fact that the actual percentage of anion is 18% (calculated from the integration value 0.70 of the peak at 4.47 ppm vs a total integration of 3.74 of the signals H20) can be explained considering the lower acidity of the organic compounds in D 2 O with respect to H 2 O. [ 24 ] Calculated chemical shifts for H20, H21, and H22 of the anion are 4.42, 6.12, and 6.55, which are in good agreement with the experimental values.…”
Section: Resultsmentioning
confidence: 99%