Ferric iron geometry and coordination during hydrolysis and ferrihydrite precipitation
dc.contributor.author | Collins, RN | en_AU |
dc.contributor.author | Rose, AL | en_AU |
dc.contributor.author | Glover, CJ | en_AU |
dc.contributor.author | Boland, DD | en_AU |
dc.contributor.author | Payne, TE | en_AU |
dc.contributor.author | Waite, TD | en_AU |
dc.date.accessioned | 2020-06-03T08:38:52Z | en_AU |
dc.date.available | 2020-06-03T08:38:52Z | en_AU |
dc.date.issued | 2011-10-01 | en_AU |
dc.date.statistics | 2020-05-14 | en_AU |
dc.description.abstract | Definitive structural characterisation of ferrihydrite has challenged scientists primarily due to its nanosized particles and inherent long-range structural disorder which challenges analytical methodology (and modelling) typically employed to determine the structure of minerals. Here we report on the application of a synchrotron quick-scanning X-ray absorption spectroscopy (XAS) approach, which allows the collection of Extended X-ray Absorption Fine Structure (EXAFS) spectral data to k = 15 Å-1 in < 1 minute, to obtain unparalleled iron Kedge data on the hydrolysis of FeIII(H2O)6 and ferrihydrite precipitation. Modelling of the pre-edge and EXAFS data: 1) supports theoretical studies which have suggested the existence of a monomeric penta-coordinated FeIII hydrolysis species and; 2) corroborates recently proposed structural models of ferrihydrite that contain tetrahedral FeIII. Modelling results indicate that ferrihydrite consists of 15 to 25 % tetrahedral FeIII and suggest that this geometry must be included in any comprehensive structural model of ferrihydrite and, furthermore, should be considered when evaluating the reactivity, stability and other structure-property relationships of this mineral. © 2011 The Authors. | en_AU |
dc.identifier.citation | Collins, R. N., Rose, A. L., Glover, C. J., Boland, D. D., Payne. T. E., & Waite, T. D. (2011). Ferric iron geometry and coordination during hydrolysis and ferrihydrite precipitation. Abstract presented to Goldschmidt 2011, Prague, Czech Republic, 14 August 2011 - 19 August 2011. | en_AU |
dc.identifier.conferenceenddate | 19 August 2011 | en_AU |
dc.identifier.conferencename | Goldschmidt 2011 | en_AU |
dc.identifier.conferenceplace | Prague, Czech Republic | en_AU |
dc.identifier.conferencestartdate | 14 August 2011 | en_AU |
dc.identifier.govdoc | 9482 | en_AU |
dc.identifier.uri | https://www.goldschmidtabstracts.info/abstracts/abstractView?id=2011003059#pills-pdf | en_AU |
dc.identifier.uri | http://apo.ansto.gov.au/dspace/handle/10238/9499 | en_AU |
dc.language.iso | en | en_AU |
dc.publisher | Mineralogical Society of Great Britain & Ireland | en_AU |
dc.subject | Iron compounds | en_AU |
dc.subject | Ferrites | en_AU |
dc.subject | Geometry | en_AU |
dc.subject | Precipitation | en_AU |
dc.subject | Nanostructures | en_AU |
dc.subject | Minerals | en_AU |
dc.subject | Absorption spectroscopy | en_AU |
dc.subject | Simulation | en_AU |
dc.title | Ferric iron geometry and coordination during hydrolysis and ferrihydrite precipitation | en_AU |
dc.type | Conference Abstract | en_AU |