Thermodynamics and crystal chemistry of the hematite–corundum solid solution and the FeAlO 3 phase
dc.contributor.author | Majzlan, J. | en_US |
dc.contributor.author | Navrotsky, Alexandra | en_US |
dc.contributor.author | Evans, B. J. | en_US |
dc.date.accessioned | 2006-09-08T19:57:50Z | |
dc.date.available | 2006-09-08T19:57:50Z | |
dc.date.issued | 2002-09 | en_US |
dc.identifier.citation | Majzlan, J.; Navrotsky, A.; Evans, B. J.; (2002). "Thermodynamics and crystal chemistry of the hematite–corundum solid solution and the FeAlO 3 phase." Physics and Chemistry of Minerals 29(8): 515-526. <http://hdl.handle.net/2027.42/42094> | en_US |
dc.identifier.issn | 0342-1791 | en_US |
dc.identifier.uri | https://hdl.handle.net/2027.42/42094 | |
dc.description.abstract | High-temperature oxide-melt calorimetry and Rietveld refinement of powder X-ray diffraction patterns were used to investigate the energetics and structure of the hematite–corundum solid solution and ternary phase FeAlO 3 (with FeGaO 3 structure). The mixing enthalpies in the solid solution can be described by a polynomial ΔH mix = WX hem (1− X hem ) with W =116 ± 10 kJ mol −1 . The excess mixing enthalpies are too positive to reproduce the experimental phase diagram, and excess entropies in the solid solution should be considered. The hematite–corundum solvus can be approximately reproduced by a symmetric, regular-like solution model with Δ G excess =( W H − TW S ) X hem X cor , where W H = 116 ± 10 kJ mol −1 and W S =32 ± 4 J mol −1 K −1 . In this model, short-range order (SRO) of Fe/Al is neglected because SRO probably becomes important only at intermediate compositions close to Fe:Al=1:1 but these compositions cannot be synthesized. The volume of mixing is positive for Al-hematite but almost ideal for Fe-corundum. Moreover, the degree of deviation from Vegard's law for Al-hematite depends on the history of the samples. Introduction of Al into the hematite structure causes varying distortion of the hexagonal network of oxygen ions while the position of the metal ions remains intact. Distortion of the hexagonal network of oxygen ions attains a minimum at the composition (Fe 0.95 Al 0.05 ) 2 O 3 . The enthalpy of formation of FeAlO 3 from oxides at 298 K is 27.9 ± 1.8 kJ mol −1 . Its estimated standard entropy (including configurational entropy due to disorder of Fe/Al) is 98.9 J mol −1 K −1 , giving the standard free energy of formation at 298 K from oxides and elements as +19.1 ± 1.8 and −1144.2 ± 2.0 kJ mol −1 , respectively. The heat capacity of FeAlO 3 is approximated as C p ( T in K)= 175.8 − 0.002472 T − (1.958 × 10 6 )/ T 2 − 917.3/ T 0.5 +(7.546 × 10 −6 ) T 2 between 298 and 1550 K, based on differential scanning calorimetric measurements. No ferrous iron was detected in FeAlO 3 by Mössbauer spectroscopy. The ternary phase is entropy stabilized and is predicted to be stable above about 1730 ± 70 K, in good agreement with the experiment. Static lattice calculations show that the LiNbO 3 -, FeGaO 3 -, FeTiO 3 -, and disordered corundum-like FeAlO 3 structures are less stable (in the order in which they are listed) than a mechanical mixture of corundum and hematite. At high temperatures, the FeGaO 3 -like structure is favored by its entropy, and its stability field appears on the phase diagram. | en_US |
dc.format.extent | 199970 bytes | |
dc.format.extent | 3115 bytes | |
dc.format.mimetype | application/pdf | |
dc.format.mimetype | text/plain | |
dc.language.iso | en_US | |
dc.publisher | Springer-Verlag; Springer-Verlag Berlin Heidelberg | en_US |
dc.subject.other | Solid Solution | en_US |
dc.subject.other | Thermodynamics | en_US |
dc.subject.other | Legacy | en_US |
dc.subject.other | FeAlO3 | en_US |
dc.subject.other | Keywords Hematite | en_US |
dc.subject.other | Corundum | en_US |
dc.title | Thermodynamics and crystal chemistry of the hematite–corundum solid solution and the FeAlO 3 phase | en_US |
dc.type | Article | en_US |
dc.subject.hlbsecondlevel | Geology and Earth Sciences | en_US |
dc.subject.hlbsecondlevel | Chemistry | en_US |
dc.subject.hlbtoplevel | Science | en_US |
dc.description.peerreviewed | Peer Reviewed | en_US |
dc.contributor.affiliationum | Department of Chemistry University of Michigan Ann Arbor Michigan 48109, USA, US | en_US |
dc.contributor.affiliationother | Thermochemistry Facility Department of Geology University of California at Davis Davis California 95616, USA e-mail: jmajzlan@ucdavis.edu Fax: +1-530-752-9307 Tel.: +1-530-754-2131, US | en_US |
dc.contributor.affiliationother | Thermochemistry Facility Department of Geology University of California at Davis Davis California 95616, USA e-mail: jmajzlan@ucdavis.edu Fax: +1-530-752-9307 Tel.: +1-530-754-2131, US | en_US |
dc.contributor.affiliationumcampus | Ann Arbor | en_US |
dc.description.bitstreamurl | http://deepblue.lib.umich.edu/bitstream/2027.42/42094/1/269-29-8-515_20290515.pdf | en_US |
dc.identifier.doi | http://dx.doi.org/10.1007/s00269-002-0261-7 | en_US |
dc.identifier.source | Physics and Chemistry of Minerals | en_US |
dc.owningcollname | Interdisciplinary and Peer-Reviewed |
Files in this item
Remediation of Harmful Language
The University of Michigan Library aims to describe library materials in a way that respects the people and communities who create, use, and are represented in our collections. Report harmful or offensive language in catalog records, finding aids, or elsewhere in our collections anonymously through our metadata feedback form. More information at Remediation of Harmful Language.
Accessibility
If you are unable to use this file in its current format, please select the Contact Us link and we can modify it to make it more accessible to you.