Bioreduction rates of iron (Fe) oxides are a key variable for predicting the fate and transport
of Fe and contaminants in subsurface environments. Such rates, however, vary significantly …

Purpose Dissimilatory iron-reducing bacteria have been described by both culture-
dependent and-independent methods in various environments, including freshwater, marine …

Abstract Vivianite (Fe 3 (PO 4) 2· 8H 2 O) is a common hydrous ferrous phosphate mineral
which often occurs in reductive conditions, especially anoxic non-sulfide environment …

Of all the terminal electron acceptors, Fe (III) is the most naturally abundant in many
subsurface environments. Fe (III)-reducing microorganisms are phylogenetically diverse and …

Few electroactive bacteria have shown the capacity of exchanging electrons with electrode
in both directions, and the mechanisms of such bidirectional electron transfer remain …

Aim: The application of iron‐reducing bacteria (IRB) to phosphate removal from returned
liquor (liquid fraction after activated sludge digestion and anaerobic sludge dewatering) of …

The current understanding of dissimilatory metal reduction is based primarily on isolates
from the proteobacterial genera Geobacter and Shewanella. However, environments …

The stimulation of subsurface microbial metabolism often associated with engineered
bioremediation of groundwater contaminants presents subsurface microorganisms, which …

Iron-reducing bacteria (FeRB) play key roles in anaerobic metal and carbon cycling and
carry out biogeochemical transformations that can be harnessed for environmental …

Iron is a redox-sensitive element. It forms poorly soluble iron oxyhydroxides in the presence
of O2, poorly soluble iron sulfides in the presence of dissolved sulfide, but soluble Fe (II) …