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Experimental Column Setup for Studying Anaerobic Biogeochemical Interactions Between Iron OxyHydroxides, Trace Elements, and Bacteria
Published on: December 19, 2017
Arsenic removal in a sulfidogenic fixed-bed column bioreactor
Muslum Altun1, Erkan Sahinkaya2, Ilknur Durukan1
1Hacettepe University, Department of Chemistry, Beytepe, Ankara, Turkey.
Iron supplementation and optimized ethanol levels significantly enhance arsenic bioremoval from wastewater. Sulfate-reducing bacteria precipitate arsenic as sulfides and co-precipitate it with iron sulfides, achieving up to 96% removal.
Area of Science:
- Environmental Science
- Environmental Engineering
- Biotechnology
Background:
- Acidic wastewater often contains toxic heavy metals like arsenic.
- Arsenic contamination poses significant risks to ecosystems and human health.
- Bioremediation offers a sustainable approach for removing arsenic from industrial effluents.
Purpose of the Study:
- To investigate the bioremoval of arsenate (As(5+)) from synthetic acidic wastewater.
- To evaluate the impact of ferrous iron (Fe(2+)) and chemical oxygen demand (COD) on arsenic removal efficiency.
- To identify the mechanisms of arsenic precipitation mediated by sulfate-reducing bacteria (SRB).
Main Methods:
- Utilized an anaerobic up-flow fixed bed column bioreactor fed with ethanol.
- Varied concentrations of arsenate, ferrous iron, and chemical oxygen demand.
- Analyzed precipitate composition using X-ray diffraction (XRD), X-ray fluorescence (XRF), scanning electron microscopy (SEM), and energy dispersive X-ray spectroscopy (EDS).
Main Results:
- Arsenic removal was minimal (8%) without iron supplementation.
- Adding 100 mg/L Fe(2+) increased removal to 63%; 200 mg/L Fe(2+) improved it to 85%.
- Optimizing COD and maintaining 200 mg/L Fe(2+) and 20 mg/L As(5+) achieved 96% arsenic removal.
Conclusions:
- Ferrous iron addition is crucial for efficient arsenic bioremoval.
- Optimized substrate (ethanol) and iron concentrations maximize arsenic removal by SRB.
- Arsenic removal occurs primarily through the precipitation of arsenic sulfides and co-precipitation with iron sulfides.
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