The possible diffusion and localization of copper in hexagonal cordier
ite structure, either by Cu(I) insertion within the hexagonal channels
or by Cu(II) substitution for Mg in octahedral sites have been studie
d. Limited amounts of Cu(I) (about 30% of theoretical values) can be i
nserted within the cordierite channels in statistically occupied 4e si
tes (0, 0, z with z = 0.06 and 0.10 respectively for Cu0.5Mg2Al4.5Si4.
5O18 and CuMg2Al5Si4O18). Cu2+/Mg2+ substitution is limited by the com
petitive formation of mullite and spinel phases.