Heavier
alkaline earth (Ae) metal amide complexes Ae(NR2)2 (Ae = Ca, Sr, Ba) were found to be highly active catalysts
for hydrogen isotope exchange (HIE). The activities for D/H exchange
between C6D6 and H2 strongly increase
with metal size (Ca < Sr < Ba) and with amide bulk: N(SiMe3)2 < N(DIPP)(SiiPr3)< N(SiiPr3)2, DIPP = 2,6-diisopropylphenyl.
At 120 °C and pressures of 10–50 bar, no hydrogenation
side-products are produced, and TONs of 205 and TOFs of 268, competitive
with those for precious metal catalysts, have been achieved. The reverse
H/D exchange between C6H6 and D2 is
even faster by a factor 1.5–2. Substrates also include a range
of substituted arenes. Alkyl-substituted aromatic rings are preferably
deuterated in acidic benzylic positions, and this tendency increases
with the number of alkyl-substituents. Although unactivated (sp3)C–H units could not be deuterated, the (sp3)Si–H function in primary, secondary, and tertiary alkylsilanes
could be converted. Two different pathways for C6H6/D2 isotope exchange have been evaluated by DFT
calculations: (A) a deprotonation/protonation mechanism and (B) direct
nucleophilic aromatic substitution. Although the exact nature of the
catalyst(s) is unclear, the first step is the conversion of Ae(NR2)2 with D2 into R2NAeD which
can aggregate to larger clusters. Energy profiles with model catalysts
(iPr3Si)2NAeD and [(Me3Si)2NAeD]2 (Ae = Ca or Ba) show that
the direct nucleophilic aromatic substitution is the most likely mechanism
for deuteration of arenes. The key to this unusual reaction is the
initial formation of a π-arene···Ae complex which
is followed by the generation of an intermediate with a Meisenheimer
anion. Heavier Ae metal amide complexes are, despite the lack of partially
filled d-orbitals for substrate activation, potent
catalysts for HIE.