APS March Meeting 2011
Volume 56, Number 1
Monday–Friday, March 21–25, 2011;
Dallas, Texas
Session Q17: Focus Session: Bulk Properties of Complex Oxides - Ruthenates
11:15 AM–2:15 PM,
Wednesday, March 23, 2011
Room: D174
Sponsoring
Units:
DMP GMAG
Chair: Ward Plummer, Louisiana State University
Abstract ID: BAPS.2011.MAR.Q17.1
Abstract: Q17.00001 : High-pressure Synthesis and Magnetic Properties of 4d and 5d Transition-metal Oxides*
11:15 AM–11:51 AM
Preview Abstract
Abstract
Author:
J.-G. Cheng
(University of Texas at Austin)
The pressure effect on synthesis of oxides with perovskite
ABO$_{3}$ and
perovskite-related structures has become more clear in recent
years. The
geometric tolerance factor t $\equiv $ (A-O)/$\surd $2(B-O)
measures the
structural stability. High-pressure synthesis enlarges the range
of the t
factor where the perovskite structure can be stabilized. For the
ABO$_{3}$
compounds with t $>$ 1, high pressure reduces the t factor since
the A-O
bond is more compressible than the B-O bond. Therefore,
perovskite would be
the high-pressure phase for ambient-pressure polytype structures.
However,
the bonding compressibility argument is no longer valid for the
ABO$_{3}$
with t $<$ 1. A dt/dP $>$ 0 is normally obtained for t less than
but very
close to 1$, i.e.$ the orthorhombic distortion becomes smaller
under pressure. For
those highly distorted perovskites with t factor far less than
one, pressure
enlarges further the orthorhombic distortion and eventually leads
to a phase
transition to the post-perovskite phase. As for PbRuO$_{3}$, high
pressure
prefers the small-volume perovskite phase relative to a competitive
pyrochlore phase Pb$_{2}$Ru$_{2}$O$_{7}$. Understanding the
pressure effect
and the new capacity provided by a Walker-type multianvil press
enabled us
to expand the perovskite family and to obtain new phases of 4d
and 5d
oxides. Studies of these new 4d and 5d oxides allow us not only
to address
long-standing problems, but also to explore exotic physical
properties. (1)
In the perovskite ARuO$_{3}$ (A= alkaline earth), we have
completed the
phase diagram from A= Ca to Sr and to Ba and also accounted for
the A-cation
size-variance effect. A systematic study of the Curie temperature
T$_{c}$
and the critical behavior as a function of the average A-site
size and the
size variance as well as external high pressures reveals
explicitly the
crucial role of the lattice strain on the ferromagnetism. The
mean-field
critical behaviour near T$_{c}$ found previously in SrRuO$_{3}$
is not
typical of these perovskite ruthenates. T$_{c}$ is completely
suppressed by
Pb doping in Sr$_{1-x}$Pb$_{x}$RuO$_{3}$ not due to the steric
effect, but
to the orbital hybridization between Pb$^{2+}$ 6s and Ru$^{4+}$
4d. As the
end member, metallic PbRuO$_{3}$ undergoes a first-order phase
transition to
a metallic \textit{Imma} phase at T$_{t} \approx $ 90 K. (2) A
new polytype phase
5H has been synthesized under a narrow pressure range, which fits
the
structural sequence along with other polytypes 9R, 6H and 3C of
BaIrO$_{3}$.
The ground states of these BaIrO$_{3}$ polytypes evolve from a
ferromagnetic
insulator with T$_{c }\approx $ 180 K in the 9R phase to a
ferromagnetic
metal with T$_{c }\approx $ 50 K in the 5H phase, and finally to an
exchange-enhanced paramagnetic metal in the 6H phase, which may
be close to
a quantum critical point. (3) In the Ca$_{1-x}$Sr$_{x}$IrO$_{3}$
system,
high pressure stabilizes the post-perovskite structure on the Ca
side (x $<$
0.3), but favors the perovskite structure on the Sr side (x $>$
0.6). Refs.
J.-G. Cheng, \textit{et al.} PRB \textbf{80}, 104430(2009);
\textbf{80}, 174426 (2009);
\textbf{81}, 134412(2010); JACS \textbf{131}, 7461(2009).
*Supported by NSF-DMR-0904282. Work under the supervision of Profs. J.-S. Zhou and J. B. Goodenough.
To cite this abstract, use the following reference: http://meetings.aps.org/link/BAPS.2011.MAR.Q17.1