Abstract
Scorodite is an arsenic mineral with the chemical formula FeAsO4·2H2O. It is the most common natural arsenate associated with arsenic-bearing ore deposits. In the present study we show that the thermoacidophilic iron-oxidizing archaeon Acidianus sulfidivorans is able to precipitate scorodite in the absence of any primary minerals or seed crystals, when grown on 0.7 g L-1 ferrous iron (Fe2+) at 80 °C and pH 1 in the presence of 1.9 g L-1 arsenate (H3AsO4). The simultaneous biologically induced crystallization of ferric iron (Fe3+) and arsenic to scorodite prevented accumulation of ferric iron. As a result, crystal growth was favored over primary nucleation which resulted in the formation of highly crystalline biogenic scorodite very similar to the mineral scorodite. Because mineral scorodite has a low water solubility and high chemical stability, scorodite crystallization may form the basis for a novel method for immobilization of arsenic from contaminated waters with high arsenic concentrations
| Original language | English |
|---|---|
| Pages (from-to) | 675-680 |
| Journal | Environmental Science and Technology |
| Volume | 44 |
| Issue number | 2 |
| DOIs | |
| Publication status | Published - 2010 |
Keywords
- atmospheric-pressure conditions
- center-dot 2h(2)o
- ferric arsenate
- sulfate-solutions
- solubility
- stability
- precipitation
- feaso4.2h2o
- mine
- ferrihydrite
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