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Magnetite the Enigma of the Verwey transition finally solved or Magnetite it never ceases to surpris

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9/4/09. Compres 2006. Magnetite; the Enigma of the Verwey transition finally solved! ... (4-fold) Fe3 Fe3 Fe3 Fe2 The enigma started with this experiment. ... – PowerPoint PPT presentation

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Title: Magnetite the Enigma of the Verwey transition finally solved or Magnetite it never ceases to surpris


1
Magnetite the Enigma of the Verwey transition
finally solved!orMagnetite it never ceases
to surprise
together with Weiming Xu and Gregory Rozenberg
(TAU)R. D. Taylor (LANL), and R. Jeanloz (UCB)
2
Magnetite (Fe3O4), a cubic inverse spinel
Fe3
B-site (6-fold)
Fe3
Fe3
  • Mixed-valence oxide.
  • Fe3 is in a A-site (inverse spinel) and
    Fe2 Fe3 in a B - site.
  • Fe3/Fe2 2/1
  • Ferrimagnet (TN 850K)with Ms4µB
  • A good conductor at RT.

Fe2
A-site (4-fold)
Normal Spinel Structure of Magnetite(?)
3
The enigma started with this experiment..
4
and then came Mott.
T lt TV
  • Mott adopted Verweys concept and proposed that
    the electron assembly in magnetite above TV is a
    Wigner glass and the electron assembly in the
    coordinated sites is subject to long range order
  • At T TV the Wigner glass transforms
    discontinuously into a Wigner crystal and the
    electrons are locked.
  • N F. Mott, Festkörperproblem 19, 331 (1979)

5
An unfortunate consequence of a Dogma

6
The Verwey transition, known experimental facts
  • At T TV a discontinuous increase in
    resistance, by 3 4 orders of magnitude.
  • A structural phase transition of the first-order
    at T lt TV.
  • TV 121 1 K for highly stoichiometric Fe3O4

7
Experimental evidences for mixed Fe valence
within B-sites at T gt TV
  • Mössbauer Spectroscopy
  • No evidence for explicit Fe3 and Fe2 in
    B-sites. Proposed scheme Fe3 (Fe3 e-) or
    Fe2.5 Fe2.5 with possible electron hopping
    with time scale lt 10-11 s.
  • Resonant Fe x-ray scattering and 57Fe NMR
  • B-site iron atoms are electronically equivalent
    in a time scale lt 10-16s.

?
B-site
8
Experimental search for "d" localization!
70s today XRD Transport 57Fe NMR 57Fe
Mössbauer Spectroscopy Raman Neutrons Absorption
Fe K-edge spectroscopy Etc., etc.
9
Contradictory results (1)
10
Contradictory results (2)
2001
11
Contradictory results (3)
12
Contradictory results (4 and 5)
13
EXPERIMENTAL
  • Sample
  • Fe2O3 Fe ? Fe3O4 solid-solid reaction of
    stoichiometric amounts of Fe and Fe2O3 enriched
    with 25 57Fe in an evacuated quartz tube at
    900C.
  • Diamond-Anvils Cell
  • Mössbauer Spectroscopy, XRD (ESRF)

14
57Fe Mössbauer Effect
The Mössbauer signature of the Verwey
transition at ambient pressure
T gt TV 2-components
  • The best probe for detecting charge order (TltTV)
    or disorder (TgtTV) in magnetite

2-components spectrum
3-components spectrum
T lt TV 2-components?
15
a serendipitous discovery...
Magnetite at 10 GPa, 200 K is metallic. The MS
spectrum should show the T gt TV spectral
features! Whats going on?
  • Spinel structure of magnetite extends to 30
    GPa. It undergoes a 1st order phase transition to
    a CaTi2O4-type structure (Bbmm) accompanied by a
    large volume shrinkage in which Fe2 becomes
    8-fold coordinated (according to Fei et al.)
  • We were interested in studying the spin-state of
    Fe2 and transport properties of the new HP phase
    (P gt 30 GPa)
  • But Weiming insisted in investigating the HP
    properties of the spinel magnetite (P lt 30 GPa).

Localization signature?
16
Pressure-induced coordination crossover,
transition from inverse to normal spinel
(Fe3)A(Fe2.5,Fe2.5)B ? (Fe2)A(Fe3,Fe3)B
P
Spectrum of a normal spinel !!!
Fe3A
Fe2A
Typical spectrum for T lt TV
Fe2A Fe3Fe3B. Fe2A / Fe3Fe3B 1/2
Intermediate spinel
Typical spectrum for T gt TV at ambient pressure.
Fe3A Fe2.5Fe2.5B.
Fe3A / Fe2.5Fe2.5B 1/2
Fe3A
Fe2.5A
17
inverse?normal spinel transformation reversible
with temperature and pressure
Normal
Inverse
18
(No Transcript)
19
The Progressive transformation of inverse ?
normal spinel
20
Are there any other (experimental) evidences for
the inverse?normal conversion?YES!
INVERSE
NORMAL
INVERSE
NORMAL
21
Are there any other (experimental) evidences for
the inverse?normal conversion?YES!
50
Magnetic moment of the ferrimagnetic Inverse
Spinel (5/22)µB - (5/2)µB 2µB
B-site
A-site
Magnetic moment of the ferrimagnetic Normal
Spinel (5/25/2)µB - (2)µB 3µB
B-site
A-site
HPNP-2 (Cologne 2004)
a 50 enhancement
22
P-T phase diagram of magnetite
23
and finally
24
The origin of the Verwey transition
charge-ordering at the B-sites?
it's due to the Orthorhombic Distortion (OD)
  • TV(P) scales with OD(P) Probable Cause of MI
    transition
  • Opening of a p-p gap within the orthorhombic
    phase

º cubic
º orthorhombic
25
EPILOGUE
  • Beware of false knowledge it is more dangerous
    than ignorance things
  • George Bernard Shaw
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