Electrolysis of acidic H2O+D2O mixtures has been performed using the well e
stablished mercury drop electrode. The experiment was done in order to stud
y, for the first time in a chemical reaction, a possible cooperative behavi
our of hydrogen species which is evident from neutron and Raman light scatt
ering studies. The electrochemical-kinetic results show a volcano type of d
eviation of the rate constants, centered around [D]/[H+D] = 0.8, from behav
iour expected from nominal D and H concentrations. It can be fitted assumin
g an effective fractionation factor of l* = 0.25, which deviates significan
tly from the established (bulk) fractionation factor of l = 0.69. Basically
, a different D+/H+-ratio is effective for electron transfer on the mercury
drop surface than is present in bulk solution. Various strategies have bee
n followed to explain the observed phenomena on a classical basis. The assu
mption that a reorganisation of the water I mercury interface may generate
the reduced fractionation factor is presently not sustained by convincing e
xperimental or theoretical evidence. We therefore propose to consider limit
ations of the applicability of simple reversible statistical concepts to th
e electrochemical water splitting process being in line with ongoing resear
ch on quantum correlation with H/D systems. (C) 1999 Elsevier Science S.A.
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