This research presents an interpretation of data obtained as part of a previous Electric Power Research Institute (EPRI) field leachate study, with a focus on arsenic leaching behavior. This study is unique in that it is the first to evaluate a large set of field-generated data from CCP management facilities using geochemical equilibrium speciation modeling. Based on the evaluation, two models are presented describing the natural weathering progression of CCPs with initially low pH (<7) and those with initially high pH (>9). For those with initially low pH (<7), scorodite solubility and adsorption limit arsenic concentrations up to pH ~7, the pH at which adsorption plays a key role, depending upon the solubility of the co-precipitated ferric oxide phase. Between pH 7 to 9, scorodite either dissolves incongruently to form ferric oxides that adsorb arsenate, or ferric iron is reduced to ferrous iron, producing symplesite as the arsenic-limiting phase. For CCPs exhibiting initially high pH (>9), calcium arsenate solubility limits arsenic concentrations at pH > ~10. Carbonation reactions favor the precipitation of calcite, and calcium arsenate is unstable below pH ~10, or log pCO2 of 10-6.5 bar. Arsenic released by calcium arsenate is either adsorbed to existing metal oxides or clays, or, in the presence of elevated ferrous iron, may be precipitated as symplesite.
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