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Paper No. 10
Presentation Time: 4:20 PM

SOLUBILITY OF FERROUS OXALATE DIHYDRATE IN MAGNESIUM CHLORIDE AND SODIUM CHLORIDE SOLUTION


JANG, Je-Hun1, NEMER, Martin2 and XIONG, Yong-Liang2, (1)Sandia National Laboratories, Defense Waste Management Programs, 4100 National Parks Highway, Carlsbad, NM 88220, (2)Sandia National Laboratories, Carlsbad Programs Group, 4100 National Parks Highway, Carlsbad, NM 88220, jjang@sandia.gov

Oxalate (C2O4-2) combines with various divalent metal ions to form sparingly soluble minerals such as CaC2O4·H2O (Whewellite), CaC2O4·2H2O (Weddellite), MgC2O4·2H2O (Glushinskite), MnC2O4·2H2O (Lindbergite), and FeC2O4·2H2O (Humboldtine). These minerals are typically found at the lichen-rock interfaces, and sometimes serve as indicators of active chemical weathering driven by oxalate-producing microorganisms. At the Waste Isolation Pilot Plant (WIPP) near Carlsbad, New Mexico, U.S.A., oxalate is present as a waste component, and a significant amount of iron is present in the form of steel waste canisters. Oxalate can solubilize actinides by forming aqueous complexes, increasing their mobility. A favorable removal mechanism for oxalate is its precipitation with benign cations. Under the reducing conditions present at WIPP after closure, it is possible that ferrous oxalate dihydrate (FeC2O4·2H2O, humboldtine) could form if oxalate is available after the formation of whewellite. A limited number of literature articles have dealt with the solubility product for FeC2O4·2H2O. To determine the solubility product for FeC2O4·2H2O, we examined the dissolution of FeC2O4·2H2O by measuring the concentration of dissolved ferrous iron ([Fe(II)]diss) with the Ferrozine method in MgCl2 and NaCl solutions of incremental concentrations. Some reactors took more than 400 days to achieve apparent equilibrium in terms of [Fe(II)]diss. Higher [Fe(II)]diss was observed in MgCl2 and NaCl solutions of higher concentration. At comparable ionic strengths, the [Fe(II)]diss in MgCl2 solution was higher than in NaCl solution. In MgCl2 solution, phenomena such as (i) a color change in reactors of lower solid-to-liquid ratio and (ii) a higher [Fe(II)]diss in reactors of higher solid-to-liquid ratio were observed, which could indicate the presence of reaction(s) other than simple dissolution of FeC2O4·2H2O. Further chemical and theoretical analyses are in progress and will be presented in the meeting together with conclusions.
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