“…The distribution of isomer shifts and quadrupole splittings results from the variety of local environments that the iron(III) ions experience in the amorphous xerogel. Both the average isomer shifts and quadrupole splittings are in complete agreement with those previously observed in iron(III) oxide doped aerogels and xerogels [40][41][42][43][44]. The appearance of broadened sextets below $30 K probably does not arise from ordered iron(III) oxides but rather from the onset, upon cooling, of slow paramagnetic relaxation [45,46] of the isolated iron(III) ions known to be present from UVvisible results and studies of magnetic properties, see below.…”