THE EFFECTS OF PH, IONIC STRENGTH, AND IRON-FULVIC ACID INTERACTIONS ON THE KINETICS OF NON-PHOTOCHEMICAL IRON TRANSFORMATIONS. II. THE KINETICS OF THERMAL REDUCTION

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dc.contributor.author Pullin M.J.
dc.contributor.author Cabaniss S.E.
dc.date.accessioned 2021-12-30T03:20:43Z
dc.date.available 2021-12-30T03:20:43Z
dc.date.issued 2003
dc.identifier https://www.elibrary.ru/item.asp?id=5073900
dc.identifier.citation Geochimica et Cosmochimica Acta, 2003, 67, 21, 4079-4089
dc.identifier.issn 0016-7037
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/33932
dc.description.abstract A combination of flow-injection analysis and kinetic analysis was used to examine the speciation of iron(II) and iron(III) in fulvic acid solutions as a function of pH, ionic strength, and time. This methodology was used to follow a shift in iron speciation from faster to slower reacting species over a timescale of several days. This speciation data shows that both iron(II) and iron(III)-fulvic acid complexes are important iron species in humic-containing natural waters and that their amounts and their rates of transformation to colloidal iron are controlled primarily by the kinetics of thermal (dark) reduction and iron(II) oxidation. The kinetic analysis methodology also yielded the rate constants for the thermal reduction of iron by the fulvic acid. These rate constants decrease with increasing pH and are independent of ionic strength. While thermal reduction was found to be too slow to produce large amounts of steady state iron(II) at circumneutral pH, it does provide a mechanism for iron redox cycling in the absence of photochemical or biochemical processes.
dc.title THE EFFECTS OF PH, IONIC STRENGTH, AND IRON-FULVIC ACID INTERACTIONS ON THE KINETICS OF NON-PHOTOCHEMICAL IRON TRANSFORMATIONS. II. THE KINETICS OF THERMAL REDUCTION
dc.type Статья


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