I. Grassert, G. Oehme / Journal of Organometallic Chemistry 621 (2001) 158–165
161
phiphile, and we propose a reaction with water or D2O
being activated on the surface of the micelle. The
influence of SDS on activity and enantioselectivity is
quite similar, but the CH and CD exchange is much
lower (9% CH and 5% CD), showing a specific effect of
sulfate as an anionic amphiphile. Sodium dodecanesul-
fonate, in comparison, gave a large increase in enan-
tioselectivity, as well as a slightly higher exchange of
CH or CD during the hydrogenation. The exceptional
position of SDS as an isotope-exchange-inhibiting am-
phiphile is more evident with methyl a-acetamido-acry-
late as the substrate than with methyl (Z)-a-acetamido-
cinnamate (see Tables 1 and 2).
an enhancement of the enantioselectivity. Comparison
of the isotope exchange in water and methanol shows
that there is an extreme solvent effect, which has been
discussed by Sinou and co-workers for 1:1 mixtures of
water and different organic solvents [10]. We were
interested in the investigation of the CH/CD exchange
within a systematically varied mixture of CH3OD–
D2O, the results of which are given in Fig. 2.
The graphical presentation shows a non-linearity be-
tween isotope incorporation and the mole fraction of
D2O in O-deuterated methanol. In the region with a
low CH3OD or D2O content the D incorporation is
significant, and in the large region between 30 and
80 mol% of D2O the exchange is almost constant. We
conclude that the change of the hydrogen bonding
structure in water is extreme, with either a low content
of methanol and, vice versa, in methanol with a low
content of water. This should influence the activity and
reactivity of water in isotope-exchange experiments.
Additionally, the curve of enantioselectivities is approx-
imately constant within the mixtures and drops dramat-
ically only from 10 mol% of methanol to pure D2O,
most probably due to the low solubility of the reactants
in water.
Fig. 3 displays the results of D-labelling experiments
in mixed micelles with different ratios of SDS and
CTA+HSO−4 . The isotopic exchange is almost constant
with an excess of SDS and rapidly increases at a 1:1
mixture to give a high-level exchange, which is charac-
teristic for CTA+HSO4−. The enantioselectivity ob-
served has a minimum at the 1:1 mixture. It is well
known that mixtures of anionic and cationic surfactants
give a precipitation of ion pairs [17]. The concentration
of micelle-forming surfactants should be extremely low
in 1:1 mixtures, with an obvious effect on the enantiose-
lectivity and a less clear effect on the CH/CD exchange.
Comparing CD and CH exchange, we observed an
isotopic effect [16], meaning that the incorporation of
H is faster than the incorporation of D. A graphical
presentation of this effect is given in Fig. 1.
The CH or CD exchange in the catalysed hydrogena-
tion is coupled with the hydrogenation process and not
observable when the educts are substituted by the prod-
ucts (methyl a-acetamidophenylalaninate or methyl a-
acetamidoalaninate) under the reaction conditions.
The ratio of incorporation is noted for each system in
parentheses and was found to be between 1.3 and 1.7.
This is comparable to the isotope effect of 1.22 reported
by Brown and Parker [6] as the ratio of hydrogenation
to deuteration for the reaction of (Z)-a-acetamidocin-
namic acid with HD in methanol using the pre-
catalyst (1.2-bicyclo[2.2.1]heptadiene)(1.2-bis(diphenyl-
phosphino)ethane)rhodium(I) tetrafluoroborate.
Both Table 1 and Fig. 1 show a dependence of the
CH/CD exchange on the type of the amphiphile, with a
decrease of incorporation in the order cationic, non-
ionic, zwitterionic and anionic. Low rates of exchange
occur especially with SDS. In comparison with the
control value in water, the addition of surfactants led to
Fig. 1. Comparison of the H/D exchange within the H2O/D2 and D2O/H2 systems during the hydrogenation of methyl (Z)-a-acetamidocinnamate
in the presence of different amphiphiles.