Abstract
Iron (Fe) cycling exerts strong control on the mobility and bioavailability of the key nutrient phosphate (PO4) in soils and sediments. Coprecipitation of PO4 is known to alter the structure of Fe (oxyhydr)oxides (FeOx), however the environmental fate of PO4-bearing FeOx is not well-understood. Here, PO4-bearing FeOx with 9 mol%
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