Phosphorus (P) can be retained in mineral association with ferrous iron (Fe) as vivianite, Fe(II)3(PO4)2 ? 8 H2O, lake sediments. The is formed and remains stable under anoxic non-sulphidogenic conditions and, therefore, acts a long-term P sink. In laboratory experiments conditions, we investigated whether adsorbed to amorphous Fe(III)-hydroxide functioned precursor phase of vivianite when adde...