1997
DOI: 10.1021/es950654l
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Arsenate and Chromate Retention Mechanisms on Goethite. 2. Kinetic Evaluation Using a Pressure-Jump Relaxation Technique

Abstract: The kinetics of arsenate and chromate adsorption/ desorption on goethite (R-FeOOH) were investigated using a pressure-jump (p-jump) relaxation technique. Information provided by this technique was used to elucidate the fate of arsenate and chromate in natural environments. Chemical relaxations resulting from rapidly induced pressure changes were monitored via conductivity detection. The adsorption/desorption of these oxyanions on goethite involved a double relaxation event. The proposed mechanism for the adsor… Show more

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Cited by 336 publications
(229 citation statements)
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“…These results were in accordance with previous studies, suggesting that high-chemisorbed water molecules prevented the bidentate complexes from forming, as noted for the complexation of chromium with ferrihydrite [48]. A similar substitution of water molecules by HCrO 4 − anions could take place at a higher chromium concentration, even at hydration equilibrium, explaining the formation of bidentate surface species when there is a high surface coverage, observed for the adsorption of Cr (VI) or a similar anion on ferrihydrite [29]. It should be noted that the C 10 ≡ > S(HCrO 4 )H 0 complex could also be expressed as an outer-sphere > SOH + 2 − HCrO − 4 species, since we could not distinguish between the different complexes' formulations or structures, based on one H 2 O molecule.…”
Section: Surface Complexes and Effect Of Ph And Contact Time On H 3 Osupporting
confidence: 91%
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“…These results were in accordance with previous studies, suggesting that high-chemisorbed water molecules prevented the bidentate complexes from forming, as noted for the complexation of chromium with ferrihydrite [48]. A similar substitution of water molecules by HCrO 4 − anions could take place at a higher chromium concentration, even at hydration equilibrium, explaining the formation of bidentate surface species when there is a high surface coverage, observed for the adsorption of Cr (VI) or a similar anion on ferrihydrite [29]. It should be noted that the C 10 ≡ > S(HCrO 4 )H 0 complex could also be expressed as an outer-sphere > SOH + 2 − HCrO − 4 species, since we could not distinguish between the different complexes' formulations or structures, based on one H 2 O molecule.…”
Section: Surface Complexes and Effect Of Ph And Contact Time On H 3 Osupporting
confidence: 91%
“…The variation in the extraction efficiency with the solution's pH could be related to the protonation/deprotonating of both surface groups, and to the acidity of H 2 CrO 4 (pK a1 = 0.2 and pK a2 = 6.5) [27][28][29]. According to the chromium speciation pH-diagram, the chromium (VI) was adsorbed as hydrogen chromate (HCrO 4 − ) at pH ≤ 5.0 (≥95%), as chromate (CrO 4 2− ) at pH ≥ 7.6 (≥95%), and as a mixture of these species between pH 5.0 and 7.6.…”
Section: Effect Of Ph On Chromium Adsorptionmentioning
confidence: 99%
“…49,50 Some of these surface hydroxyls are exchangeable, and oxyanions, such as chromate, can form both monodentate surface complexes and biatomic-bidentate surface complexes where an oxygen is shared between the oxyanion and a surface iron atom. [51][52][53] The net surface charge of a hydoxylated iron surface is pH dependant (protons readily exchange with the surface groups to produce OH 2 + , OH, or O -depending on pH. 50 For most iron-containing minerals, the solution pH value that results in no net charge on the surface (i.e.…”
Section: Sem Analysis Of Cr-reacted Zvi Couponsmentioning
confidence: 99%
“…According to literature data, two mechanisms of arsenic binding on the surface of iron oxi-hydroxide are: the mechanism of surface precipitation and the mechanism of surface complexation. Surface complexation mechanism can be monodentate, dominant at a low surface coverage of modified zeolite, or bidendate at higher surface coverage when iron forms complexes with arsenic [42][43][44]. …”
mentioning
confidence: 99%