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Free keywords:
schwertmannite
ferrihydrite
goethite
hematite
sulfate
time-resolved
energy-dispersive X-ray diffraction
acid-mine-drainage
synthetic schwertmannite
ferrihydrite
iron
sulfate
phosphate
adsorption
waters
crystallization
lepidocrocite
Geochemistry & Geophysics
Mineralogy
Abstract:
The transformation of schwertmannite to goethite and/or hematite in high pH solutions was studied between 60 and 240 degrees C using synchrotron-based, in-situ energy-dispersive X-ray diffraction (EDXRD). Powder diffraction and electron microscopy indicate that the crystallization of hematite and goethite Occurred via intermediate ferrihydrite. At temperatures <= 80 degrees C goethite was the only crystallization product, while at temperatures >80 degrees C goethite and hematite crystallized almost simultaneously. At temperatures <= 150 degrees C a secondary crystallization stage was obsened in which goethite transformed to hematite. The activation energies of nucleation for goethite and hematite are 27 I and 25 I kJ/mol, respectively, while the activation energies of crystallization are 33 I and 28 I kJ/mol. Most of the sulfate was released from the schwertmannite during the early stages of crystallization with <5% of the sulfate remaining associated with the solid phase after crystallization was complete. Sulfate from the initial schwertmannite retarded the dissolution of ferrihydrite, which inhibited the nucleation and the early stages of goethite formation, but did not significantly affect the later stages of goethite crystallization. At high temperatures the presence of sulfate favored the crystallization of hematite over goethite. The activation energy of crystallization for the secondary transformation of goethite to hematite is 103 +/- 3 kJ/mol.
