In Situ Vivianite Formation in Intertidal Sediments: Ferrihydrite-Adsorbed P Triggers Vivianite Formation.

ABSTRACT: Coastal sediments are a key contributor to oceanic phosphorus (P) removal, impacting P bioavailability and primary productivity. Vivianite, an Fe(II)-phosphate mineral, can be a major P sink in nonsulfidic, reducing coastal sediments. Despite its importance, vivianite formation processes in sediments remain poorly understood. Here, we applied a novel approach to detect and quantify in situ vivianite formation in three intertidal flats. We conducted 7-week long incubations of mesh-bags filled with sediments mixed with (1) ⁵⁷Fe-ferrihydrite, (2) ⁵⁷Fe-ferrihydrite with adsorbed phosphate, and (3) ⁵⁷Fe-ferrihydrite with adsorbed phosphate and some vivianite (natural Fe isotope abundance), which could serve as crystal growth sites. Synthesizing the ferrihydrite

SUBMITTER: Kubeneck LJ 

PROVIDER: S-EPMC11741103 | biostudies-literature | 2025 Jan

REPOSITORIES: biostudies-literature