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Figure 8.3.5 Middle: Photographs of electrolysis products from 20% Fe 2 O 3 or Fe 3 O 4 by mass in 800 C
Li 2 CO 3 : following extended 0.5A electrolysis at a coiled wire (Pt or Fe) cathode with a Ni
anode. Left: cathode restricted CV in Li 2 CO 3 , containing 1:5 by weight of either Fe 2 O 3 or
Fe 3 O 4 . Right: The measured iron electrolysis potentials in molten Li 2 CO 3 , as a function
of the temperature, current density, and the concentration of dissolved Fe(III). Modified
with permission from Licht andWang 2010.
The two principal natural ores of iron are hematite (Fe 2 O 3 ) and the mixed valence
Fe 2 + / 3 + magnetite (Fe 3 O 4 ). We observe that, Fe 3 O 4 is also highly soluble in molten
Li 2 CO 3 , and may also be reduced to iron with the net electrolysis reaction:
E =
+
=
Fe 3 O 4
3Fe
2O 2
1 . 32 V, E thermoneutral
1 . 45 V
(8.3.6)
Fe 3 O 4 electrolysis potentials run parallel, but
0.06 V higher, than those of Fe 2 O 3 in
Figure 8.2.1. The processes are each endothermic; the required electrolysis potential
decreases with increasing temperature. For Fe 3 O 4 in Figure 8.3.5, unlike the single
peak evident for Fe 2 O 3 , two reduction peaks appear in the CV at 800 C. Following
the initial cathodic sweep (indicated by the left arrow), the CV exhibits two reduc-
tion peaks, again more pronounced at an iron electrode (grey curve), which appear
to be consistent with the respective reductions of Fe 2 + and Fe 3 + . In either Fe 2 O 3 ,or
Fe 3 O 4 , the reduction occurs at a potential before we observe any reduction of the
molten Li 2 CO 3 electrolyte, and at constant current, iron is deposited. Following 1
hour of electrolysis at either 200 or 20 mA/cm 2 of iron deposition, as seen in the Fig-
ure 8.3.5 photographs, and as with the Fe 2 O 3 case, the extracted cooled electrode,
following extended electrolysis and iron formation, contains trapped electrolyte. Fol-
lowing washing, the product weight is consistent with the eight electron per Fe 3 O 4
coulombic reduction to iron.
The solid products of the solid reaction of Fe 2 O 3 and Li 2 CO 3 had been char-
acterized (Collongues and Chaudron, 1950; Wijayasinghe et al., 2003). We prepare
and probe the solubility of lithiated iron oxide salts in molten carbonates, and report
high Fe(III) solubilities, in the order of 50% in molten carbonates, are achieved via the
reaction of Li 2 O with Fe 2 O 3 , yielding an effective method for CO 2 free iron production.
Lithium oxide, as well as Fe 2 O 3 or Fe 3 O 4 , each have melting points above 1460 C.
Li 2 O dissolves in 400-1000 C molten carbonates. We find the solubility of Li 2 Oin
molten Li 2 CO 3 increases from 9 to 14 m from 750 to 950 C. Following preparation
of specific iron oxide salts, we add them to molten alkali carbonate. The resultant
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