The readsorption of ferrous ions produced by the abiotic and microbially-mediated reductive dissolution of iron oxy-hydroxides drives a series of transformations of the host minerals. To further understand the mechanisms by which these transformations occur and their kinetics within a microporous flow environment, flow-through experiments were conducted in which capillary tubes packed with ferrihydrite-coated glass spheres were injected with inorganic Fe(II) solutions under circumneutral pH conditions at 25 C. Synchrotron X-ray diffraction was used to identify the secondary phase(s) formed and to provide data for quantitative kinetic analysis. At concentrations at and above 1.8 mM Fe(II) in the injection solution, magnetite was the only sec...
Mineralogical transformations of 2-line ferrihydrite were studied under oxic and Fe3+-reducing condi...
The replacement of magnetite by hematite was studied through a series of experiments under mild hydr...
International audienceThis laboratory study describes the abiotic mineralogical transformation of fe...
Aqueous ferrous iron (Fe(II)) accelerates the transformation of ferrihydrite into secondary, more c...
Interaction with aqueous Fe(II) accelerates the transformation of the Fe(III) oxyhydroxide ferrihydr...
Iron cycling and the associated changes in solid phase have dramatic implications for trace element ...
The transformation of 2-line ferrihydrite to goethite from supersaturated solutions at alkaline pH ≥...
Owing to its high surface area and intrinsic reactivity, ferrihydrite serves as a dominant sink for ...
Electron transfer to ferric iron in (oxyhydr-)oxides (hereafter iron oxides) is a critical step in ...
Ferrihydrite is a common Fe mineral in soils and sediments that rapidly transforms to secondary mine...
There is growing awareness of the complexity of potential reaction pathways and the associated soli...
There is growing awareness of the complexity of potential reaction pathways and the associated solid...
Complex interactions between redox-driven element cycles in soils influence iron mineral transformat...
Aqueous Fe(II) (Fe(II)(aq))-catalyzed recrystallization of iron (hydr)oxides is the important chemic...
In redox-affected soil environments, electron transfer between aqueous Fe(II) and solid-phase Fe(III...
Mineralogical transformations of 2-line ferrihydrite were studied under oxic and Fe3+-reducing condi...
The replacement of magnetite by hematite was studied through a series of experiments under mild hydr...
International audienceThis laboratory study describes the abiotic mineralogical transformation of fe...
Aqueous ferrous iron (Fe(II)) accelerates the transformation of ferrihydrite into secondary, more c...
Interaction with aqueous Fe(II) accelerates the transformation of the Fe(III) oxyhydroxide ferrihydr...
Iron cycling and the associated changes in solid phase have dramatic implications for trace element ...
The transformation of 2-line ferrihydrite to goethite from supersaturated solutions at alkaline pH ≥...
Owing to its high surface area and intrinsic reactivity, ferrihydrite serves as a dominant sink for ...
Electron transfer to ferric iron in (oxyhydr-)oxides (hereafter iron oxides) is a critical step in ...
Ferrihydrite is a common Fe mineral in soils and sediments that rapidly transforms to secondary mine...
There is growing awareness of the complexity of potential reaction pathways and the associated soli...
There is growing awareness of the complexity of potential reaction pathways and the associated solid...
Complex interactions between redox-driven element cycles in soils influence iron mineral transformat...
Aqueous Fe(II) (Fe(II)(aq))-catalyzed recrystallization of iron (hydr)oxides is the important chemic...
In redox-affected soil environments, electron transfer between aqueous Fe(II) and solid-phase Fe(III...
Mineralogical transformations of 2-line ferrihydrite were studied under oxic and Fe3+-reducing condi...
The replacement of magnetite by hematite was studied through a series of experiments under mild hydr...
International audienceThis laboratory study describes the abiotic mineralogical transformation of fe...