Under anoxic conditions, the interactions
between As-bearing ferrihydrite
(Fh) and As(V)-reducing bacteria are known to cause Fh transformations
and As mobilization. However, the impact of different types of organic
matter (OM) on microbial As/Fe transformation in As-bearing Fh-organic
associations remains unclear. In our study, we therefore exposed arsenate-adsorbed
ferrihydrite, ferrihydrite-PGA (polygalacturonic acid), and ferrihydrite-HA
(humic acid) complexes to two typical Fe(III)- and As(V)-reducing
bacteria, and followed the fate of Fe and As in the solid and aqueous
phases. Results show that PGA and HA promoted the reductive dissolution
of Fh, resulting in 0.7–1.6 and 0.8–1.9 times more As
release than in the OM-free Fh, respectively. This was achieved by
higher cell numbers in the presence of PGA, and through Fe-reduction
via electron-shuttling facilitated by HA. Arsenic-XAS results showed
that the solid-phase arsenite fraction in Fh-PGA and Fh-HA was 15–19%
and 27–28% higher than in pure Fh, respectively. The solid-associated
arsenite fraction likely increased because PGA promoted cell growth
and As(V) reduction, while HA provided electron shuttling compounds
for direct microbial As(V)-reduction. Collectively, our findings demonstrate
that As speciation and partitioning during microbial reduction of
Fh-organic associations are strongly influenced by PGA and HA, as
well as the strains’ abilities to utilize electron-shuttling
compounds.