Energetics of stable and metastable low temperature iron oxides and oxyhydroxides
Abstract
Iron oxides and oxyhydroxides are widespread in nature. Understanding the thermodynamic properties of the transformation in the iron oxide/hydroxide system permits the characterization of numerous geochemical processes including weathering, soil chemistry, and diagenesis in continental and oceanic environments. The aim of this study is to measure the energetics of a series of metastable oxides and oxyhydroxides in order to determine the effects of polymorphism, of oxidation state and of hydration. High temperature solution calorimetry using sodium molybdate as a solvent and transposed temperature drop calorimetry at 979 K were used. Enthalpies of formation from the elements of the metastable iron oxides and oxyhydroxides were calculated from the measured values of the enthalpies of drop solution. The experiments allow an estimate of the enthalpy of formation from the elements of {gamma}Fe{sub 2}O{sub 3} ({minus}817.4 {+-} 1.2 kJ/mol for sample with tetragonal symmetry and {minus}816.9 {+-} 1.2 kJ/mol for sample with cubic symmetry) and {beta}-FeOOH ({minus}561.3 {+-} 3.1 kJ/mol) which are currently unavailable in the literature. The stability of the structure depends mostly on the degree of hydration and on the average oxidation state of iron. It depends less strongly on the topology of the structure itself and of the tunnel anion.
- Authors:
-
- Univ. of California, Davis, CA (United States). Dept. of Chemical Engineering and Materials Science
- Publication Date:
- Sponsoring Org.:
- National Science Foundation, Washington, DC (United States)
- OSTI Identifier:
- 323458
- Report Number(s):
- CONF-971201-
Journal ID: ISSN 0272-9172; TRN: IM9911%%71
- Resource Type:
- Book
- Resource Relation:
- Conference: 1997 fall meeting of the Materials Research Society, Boston, MA (United States), 1-5 Dec 1997; Other Information: PBD: 1998; Related Information: Is Part Of Phase transformations and systems driven far from equilibrium; Ma, E. [ed.] [Louisiana State Univ., Baton Rouge, LA (United States)]; Atzmon, M. [ed.] [Univ. of Michigan, Ann Arbor, MI (United States)]; Bellon, P. [ed.] [Univ. of Illinois, Urbana, IL (United States)]; Trivedi, R. [ed.] [Ames Lab., IA (United States)]|[Iowa State Univ., Ames, IA (United States)]; PB: 703 p.; Materials Research Society symposium proceedings, Volume 481
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 36 MATERIALS SCIENCE; ENTHALPY; IRON OXIDES; IRON HYDROXIDES; CRYSTAL STRUCTURE; CALORIMETRY; OXIDATION; HYDRATION; EXPERIMENTAL DATA
Citation Formats
Laberty, C, and Navrotsky, A. Energetics of stable and metastable low temperature iron oxides and oxyhydroxides. United States: N. p., 1998.
Web.
Laberty, C, & Navrotsky, A. Energetics of stable and metastable low temperature iron oxides and oxyhydroxides. United States.
Laberty, C, and Navrotsky, A. 1998.
"Energetics of stable and metastable low temperature iron oxides and oxyhydroxides". United States.
@article{osti_323458,
title = {Energetics of stable and metastable low temperature iron oxides and oxyhydroxides},
author = {Laberty, C and Navrotsky, A},
abstractNote = {Iron oxides and oxyhydroxides are widespread in nature. Understanding the thermodynamic properties of the transformation in the iron oxide/hydroxide system permits the characterization of numerous geochemical processes including weathering, soil chemistry, and diagenesis in continental and oceanic environments. The aim of this study is to measure the energetics of a series of metastable oxides and oxyhydroxides in order to determine the effects of polymorphism, of oxidation state and of hydration. High temperature solution calorimetry using sodium molybdate as a solvent and transposed temperature drop calorimetry at 979 K were used. Enthalpies of formation from the elements of the metastable iron oxides and oxyhydroxides were calculated from the measured values of the enthalpies of drop solution. The experiments allow an estimate of the enthalpy of formation from the elements of {gamma}Fe{sub 2}O{sub 3} ({minus}817.4 {+-} 1.2 kJ/mol for sample with tetragonal symmetry and {minus}816.9 {+-} 1.2 kJ/mol for sample with cubic symmetry) and {beta}-FeOOH ({minus}561.3 {+-} 3.1 kJ/mol) which are currently unavailable in the literature. The stability of the structure depends mostly on the degree of hydration and on the average oxidation state of iron. It depends less strongly on the topology of the structure itself and of the tunnel anion.},
doi = {},
url = {https://www.osti.gov/biblio/323458},
journal = {},
issn = {0272-9172},
number = ,
volume = ,
place = {United States},
year = {Thu Dec 31 00:00:00 EST 1998},
month = {Thu Dec 31 00:00:00 EST 1998}
}