Abstract

The poorly crystalline ferrihydrite (Fh) is often associated with organic matter (OM) and metal(loid)s, such as arsenic (As). The transformation of Fh to more stable and, hence, less reactive phases is catalyzed by the surface reaction with Fe(II). However, little is known regarding the impact of various specific OM types and the co-existence of OM and As on the secondary mineralization of Fh. Accordingly, we explored the extent and the resulting secondary minerals of Fe(II)-induced transformation of [As(III)-adsorbed] OM–Fh adsorption and co-precipitation complexes, which were synthesized using two types of OM: dissolved organic matter (DOM) extracted from the O horizon of an ultisol and polygalacturonic acid (PGA) as a proxy for polysaccharides. Regardless of OM type, increased contents of the co-precipitated or adsorbed OM led to a decrease in Fh transformation in both the absence and presence of As(III). Adsorbed As(III) caused a decrease in Fh conversion for both pure Fh and OM–Fh complexes. We obser...

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