『Abstract
The present research reproduces the chemical and microbiological
reactions that occur naturally when a metal sulfide is discharged
onto a natural soil, with special emphasis on iron cycle. The
role of indigenous microbiota from an extremely acidic site on
both weathering and attenuation processes related to the iron
mobilization has been studied and the iron cycle has been reproduced
at laboratory scale. In the first stage, the weathering phase,
a residual sulfide mineral was bioleached using a mixed culture
of iron-oxidizing bacteria isolated from the own substrate. The
acid liquor obtained (pH 2), with a high metal concentration (160
mM in total iron), was filtered and neutralized. solids obtained
from the two sources (from the weathering process and after the
neutralization stage) were characterized by X-ray and scanning
electron microscopy/energy dispersive X-ray spectroscopy, resulting
ferric iron precipitates such as jarosites, goethites, and ferrihydrites
with different crystalline properties. The contribution of ferric
iron-reducing bacteria on the attenuation of high-content iron
effluents was also studied. Mixed cultures of ferric iron-reducing
bacteria, isolated from those acidic substrates, were active in
reducing soluble ferric iron (60 mM in concentration), and a 66%
of bioreduction was reached after 15 days. Dissimilatory ferric
iron reduction has been achieved with adapted cultures at pH values
from 7 to 4.
Keywords: Weathering; Natural attenuation; Iron cycle; Iron oxidizers;
Dissimilatory iron reducers』
1. Introduction
2. Materials and methods
2.1. The model
2.2. Samples
2.3. Chemical and mineralogical characterization of samples
2.4. Isolation and culture of bacteria
2.4.1. Ferrous iron oxidizers
2.4.2. Ferric iron reducers
2.5. Weathering tests
2.6. Dissimilatory Fe(III) reduction kinetic
3. Results and discussion
3.1. Chemical and mineralogical characterization of the original
samples
3.2. Microbiology
3.3. Weathering tests
3.4. Kinetics of ferric iron-reducing bacteria
3.5. Biogenic solids
4. Final remarks
Acknowledgments
References