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Title: Structure-Controlled Oxygen Concentration in Fe2O3 and FeO2

Journal Article · · Inorganic Chemistry
ORCiD logo [1];  [2]; ORCiD logo [3];  [2];  [4];  [5];  [6];  [7]
  1. Univ. of Nevada, Las Vegas, NV (United States); Center for High Pressure Science and Technology Advanced Research (HPSTAR), Shanghai (China)
  2. Stanford Univ., CA (United States)
  3. Center for High Pressure Science and Technology Advanced Research (HPSTAR), Shanghai (China)
  4. Argonne National Lab. (ANL), Lemont, IL (United States)
  5. Univ. of Hawaii, Honolulu, HI (United States)
  6. Center for High Pressure Science and Technology Advanced Research (HPSTAR), Shanghai (China); Carnegie Inst. of Washington, Washington, DC (United States). Geophysical Lab.
  7. Univ. of Nevada, Las Vegas, NV (United States)

Solid-solid reaction, particularly in the Fe-O binary system, has been extensively studied in the past decades because of its various applications in chemistry and materials and earth sciences. The recently synthesized pyrite-FeO2 at high pressure suggested a novel oxygen-rich stoichiometry that extends the achievable O-Fe ratio in iron oxides by 33%. Although FeO2 was synthesized from Fe2O3 and O2, the underlying solid reaction mechanism remains unclear. Herein, combining in situ X-ray diffraction experiments and first-principles calculations, we identified that two competing phase transitions starting from Fe2O3: (1) without O2, perovskite-Fe2O3 transits to the post-perovskite structure above 50 GPa; (2) if free oxygen is present, O diffuses into the perovskite-type lattice of Fe2O3 leading to the pyritetype FeO2 phase. We found the O-O bonds in FeO2 are formed by the insertion of oxygen into the Pv lattice via the external stress and such O-O bonding is only kinetically stable under high pressure. This may provide a general mechanism of adding extra oxygen to previous known O saturated oxides to produce unconventional stoichiometries. Our results also shed light on how O is enriched in mantle minerals under pressure.

Research Organization:
Argonne National Lab. (ANL), Argonne, IL (United States)
Sponsoring Organization:
USDOE Office of Science (SC), Basic Energy Sciences (BES); USDOE National Nuclear Security Administration (NNSA); National Science Foundation (NSF)
Grant/Contract Number:
AC02-06CH11357; NA0001982; NA0001974; FG02-94ER14466; FG02-99ER45775; EAR-1661511; EAR-1345112; EAR-1722515; EAR-1447438
OSTI ID:
1530397
Journal Information:
Inorganic Chemistry, Vol. 58, Issue 9; ISSN 0020-1669
Publisher:
American Chemical Society (ACS)Copyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 7 works
Citation information provided by
Web of Science

References (35)

Preparation, Properties and Structure of Cadmium Peroxide journal August 1959
Oxygen‐Rich Lithium Oxide Phases Formed at High Pressure for Potential Lithium–Air Battery Electrode journal May 2017
Novel stable compounds in the Mg–O system under high pressure journal January 2013
Stable magnesium peroxide at high pressure journal September 2015
FeO2 and FeOOH under deep lower-mantle conditions and Earth’s oxygen–hydrogen cycles journal June 2016
Origin of Tunable Photocatalytic Selectivity of Well-Defined α-Fe 2 O 3 Nanocrystals journal September 2013
α-Fe2O3 Nanoflakes as an Anode Material for Li-Ion Batteries journal October 2007
Discovery of the recoverable high-pressure iron oxide Fe4O5 journal October 2011
Unraveling the complexity of iron oxides at high pressure and temperature: Synthesis of Fe5O6 journal June 2015
Structural complexity of simple Fe2O3 at high pressures and temperatures journal February 2016
Unexpected 3+ valence of iron in FeO2, a geologically important material lying “in between” oxides and peroxides journal October 2017
High-pressure phase transition of hematite, Fe2O3 journal August 2004
In situ x-ray observation of the phase transformation of Fe 2 O 3 journal January 2005
In situ X-ray observation of phase transformation in Fe2O3 at high pressures and high temperatures journal October 2005
CO2-induced destabilization of pyrite-structured FeO2Hx in the lower mantle journal March 2018
Novel high pressure monoclinic Fe 2 O 3 polymorph revealed by single-crystal synchrotron X-ray diffraction studies journal August 2013
Oxygen Activation and Dissociation on Transition Metal Free Perovskite Surfaces journal December 2015
Hydrogen-Bond Symmetrization Breakdown and Dehydrogenation Mechanism of FeO 2 H at High Pressure journal August 2017
Dehydrogenation of goethite in Earth’s deep lower mantle journal January 2017
Electronic and magnetic structures of the postperovskite-type Fe2O3 and implications for planetary magnetic records and deep interiors journal March 2009
Interstitial iron impurities at grain boundaries in silicon: A first-principles study journal January 2015
A generalized solid-state nudged elastic band method journal February 2012
Anisotropy of Earth's D″ layer and stacking faults in the MgSiO3 post-perovskite phase journal December 2005
Stochastic Surface Walking Method for Structure Prediction and Pathway Searching journal February 2013
Double-Ended Surface Walking Method for Pathway Building and Transition State Location of Complex Reactions journal November 2013
Variable cell nudged elastic band method for studying solid–solid structural phase transitions journal September 2013
Variable-Cell Double-Ended Surface Walking Method for Fast Transition State Location of Solid Phase Transitions journal September 2015
Possible structural polymorphism in Al-bearing magnesiumsilicate post-perovskite journal April 2008
Atomic Structure of Heterophase Junction from Theoretical Prediction journal May 2015
Hydrogen-bearing iron peroxide and the origin of ultralow-velocity zones journal November 2017
When water meets iron at Earth's core–mantle boundary journal September 2017
Perovskite in Earth’s deep interior journal November 2017
Discovery of a hexagonal ultradense hydrous phase in (Fe,Al)OOH journal March 2018
Valence and spin states of iron are invisible in Earth’s lower mantle journal March 2018
Prediction of new thermodynamically stable aluminum oxides journal April 2015

Cited By (2)

Dependency of f states in fluorite-type XO 2 (X = Ce, Th, U) on the stability and electronic state of doped transition metals journal January 2019
Iron oxides with a reverse spinel structure: impact of active sites on molecule adsorption journal January 2019

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