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- W2107389935 abstract "Drinking‐water treatment residuals (WTR) control excessive soluble phosphorus (P) concentrations in soils and appear to do so for a long time. Knowledge of the solid phases controlling the solubility of WTR‐immobilized P could enable the prediction of the long‐term stability of WTR‐immobilized P. We hypothesized that stable aluminum (Al)– and iron (Fe)–phosphate minerals control the solubility of WTR‐immobilized P, thus ensuring that WTR‐immobilized P remains stable in the long term. We utilized both artificially (laboratory) and naturally (field) aged WTR‐amended samples to test our hypothesis and the MINTEQA2 geochemical model to perform chemical equilibrium calculations. The field‐aged WTR‐amended soil (Granby loamy sand and Granby sandy loam) samples were obtained from two sites where an alum‐based WTR (Al‐WTR) had been applied 7.5 years ago. Artificial aging of fresh (freshly amended) soil (Immokalee fine sand) samples was achieved through incubation at elevated temperatures (46 or 70 °C) for 4.5 yea..." @default.
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- W2107389935 date "2009-06-01" @default.
- W2107389935 modified "2023-09-23" @default.
- W2107389935 title "Modeling Solid‐Phase Control of Solubility of Drinking‐Water Treatment Residuals — Immobilized Phosphorus in Soils" @default.
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- W2107389935 doi "https://doi.org/10.1080/00103620902896670" @default.
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