Layered double metal hydroxides belonging to the pyroaurite group (pyr
oaurite-type compounds, abbreviated PTCs) consist of positively charge
d trioctahedral metal hydroxide layers, [M(a 1-x)(II)M(b x)(III)(OH)(2
)](x+), with interlayers of charge-compensating anions and water molec
ules,(1,2) [A(x/n).yH(2)O](x-), with 0.15 < x < 0.70. Compounds with h
ydroxide layers of mono- and trivalent metal cations are also known,(3
) and the possible existence of PTCs containing tetravalent cations (S
i, Ti(IV), V(IV)) has been indicated.(4) Recently we described the syn
thesis of a (CoFeIII)-Fe-II-PTC with the composition Fe0.309III)-Fe-II
(OH)(2)][(CO3)(0.140).yH(2)O].(5) The blue variety of Co(OH)2 also has
a layered structure which on anodic oxidation transforms topotactical
ly to the layered CoOOH.(6) Hence it is likely that the Co(II)-dominat
ed Co-II-Fe-III-PTC also can be oxidized electrochemically and still r
etain its layered structure. The oxyhydroxide formed by the electroche
mical reaction will. be described here with emphasis on the oxidation
state of the cations.