“…This variation indicates a progressive decrease of the number of low-l eff species, consistent with the degradation of the iron dextran akaganéite particles, together with an increase of high-l eff species, most likely associated to the synthesis of ferritin or some paramagnetic iron containing molecules. At this point, we must remind that previous magnetic experiments on deoxyhaemoglobin and methemoglobin, which contain Fe 2+ and Fe 3+ , respectively, resulted in paramagnetic effective moments 5.46 l B and 5.80 l B , which are very close to the corresponding single ion values, while oxyhaemoglobin appears to be diamagnetic [3,48].…”