The stability of iron ascorbate solutions was investigated, under both
anaerobic and aerobic conditions, with the Fe2+ and Fe3+ indicators,
respectively ferrozine and mimosine, at different pH values. The speci
es present under the differing conditions were investigated by electro
n paramagnetic resonance (EPR) and Mossbauer spectroscopy and by gel-f
iltration chromatography. At physiological pH (6-8-7.4) iron ascorbate
solutions rapidly form mononuclear chelatable Fe2+ species as reflect
ed by indicator studies and EPR. Mossbauer spectroscopy fails to detec
t any Fe2+ species. EPR studies show a time-dependent decrease in rhom
bic Fe3+, particularly in oxygenated buffers, consistent with a conver
sion to polynuclear Fe. O2 uptake studies show that the conversion of
Fe2+ to Fe3+ in Fe-ascorbate solutions at pH > 7.0 was accompanied by
rapid O2 consumption but preceded depletion of ascorbate. Addition of
high concentrations of mannitol (50-200 mm) reduces the O2 consumption
and partly stabilizes the rapidly chelatable Fe form. Gel filtration
studies show that the oxidation of Fe-ascorbate solutions at pH 7.4 is
accompanied by an increase in the apparent relative molecular mass of
the Fe, presumably due to Fe polymer formation. These studies indicat
e the inherent instability of Fe-ascorbate solutions above neutral pH
and clearly have important implications in the use of ascorbate in stu
dies of Fe physiology.