“…solid-humic-metal, revealed that the additivity rule cannot be simply applied (46)(47)(48). As a matter of fact, a large number of authors has clearly shown that slow sorption kinetic, fractionation phenomena and solid phase dissolution were implied (9,12,(61)(62)(63)(64)(65)(66). Thus, a reliable thermodynamic modelling of these systems is difficult to assess without prior assessment of an actual equilibrium state.…”
The influence of addition order and contact time in the system hematite (α-Fe 2 O 3 ) -humic acid (HA) -thorium (IV) was studied in batch experiments. Thorium (IV) is considered here as a chemical analogue of other actinides (IV). The sorption isotherms were acquired varying pH in the range 2-10, and HA concentration in the range 1-100 mg/L. As already observed by numerous authors, thorium (IV) retention was hindered when HA and hematite were equilibrated beforehand during 24 hours. As it has been observed in a previous study, this 2 effect was drastic when the ratio between humic and surface (iron oxide) sites exceeds a critical value. However, when HA were added after a 24 hours equilibration of the hematitethorium (IV) system, thorium (IV) was barely desorbed from the iron oxide surface.Furthermore, no drastic effect of the ratio between humic and surface sites could be evidenced, as the increase of HA concentration only results in a slight monotonic decrease in Th(IV) retention. Increasing contact time between components of the systems only indicated slight Th(IV) retention variation. This was interpreted as a consequence of slow kinetic controls of both the Th(IV)-HA complexation and HA-hematite sorption.
“…solid-humic-metal, revealed that the additivity rule cannot be simply applied (46)(47)(48). As a matter of fact, a large number of authors has clearly shown that slow sorption kinetic, fractionation phenomena and solid phase dissolution were implied (9,12,(61)(62)(63)(64)(65)(66). Thus, a reliable thermodynamic modelling of these systems is difficult to assess without prior assessment of an actual equilibrium state.…”
The influence of addition order and contact time in the system hematite (α-Fe 2 O 3 ) -humic acid (HA) -thorium (IV) was studied in batch experiments. Thorium (IV) is considered here as a chemical analogue of other actinides (IV). The sorption isotherms were acquired varying pH in the range 2-10, and HA concentration in the range 1-100 mg/L. As already observed by numerous authors, thorium (IV) retention was hindered when HA and hematite were equilibrated beforehand during 24 hours. As it has been observed in a previous study, this 2 effect was drastic when the ratio between humic and surface (iron oxide) sites exceeds a critical value. However, when HA were added after a 24 hours equilibration of the hematitethorium (IV) system, thorium (IV) was barely desorbed from the iron oxide surface.Furthermore, no drastic effect of the ratio between humic and surface sites could be evidenced, as the increase of HA concentration only results in a slight monotonic decrease in Th(IV) retention. Increasing contact time between components of the systems only indicated slight Th(IV) retention variation. This was interpreted as a consequence of slow kinetic controls of both the Th(IV)-HA complexation and HA-hematite sorption.
“…Adsorbed fulvic acids are able to slow down the rate at which ferrihydrite transforms to more stable (oxyhydr)oxides by blocking dissolution sites or hindering the nucleation of the more stable phases (Jones et al, 2009). Might the retardation effects on transformation (Vilge-Ritter et al, 1999) be less efficient with discontinuous coatings or with coprecipitated organic matter? A more mineralogical-based approach to the filterable Fe fraction in seawater should be high on everyone's wish list.…”
Section: Si-2 Filterable Iron and Complexed Iron In Seawatermentioning
“…Concerning the mechanism of flocculation, there is some controversy about whether organic compounds are scavenged by adsorption onto precipitated iron hydroxide colloids (Ying et al, 1988;Tseng et al, 1989) or the organic colloids are precipitated as a consequence of charge compensation by dissolved Fe (Schmitt et al, 1996;Vilgé-Ritter et al, 1999;Cheng, 2002;Jung et al, 2005). In fact, precipitates of humic acid and colloidal iron hydroxide look very similar.…”
Section: Flocculation Of Humic Acid On Addition Of Fementioning
confidence: 99%
“…In flocculated Fe/HA precipitates, the presence of iron oligomers could be detected by X-ray spectroscopy (Vilgé-Ritter et al, 1999;Jung et al, 2005).…”
Section: Characteristics Of Fe-ha Interactionmentioning
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