Quantum
effects melt the spin ice: the spontaneous Hall effect and the time-reversal
symmetry breaking without magnetic dipole order
Our recent research in
collaboration with University of Tokyo group uncovers the time-reversal symmetry
breaking without magnetic dipole order in the frustrated magnet Pr2Ir2O7 [1],
suggesting a chiral spin liquid as a result of a melting of spin ice. There
have also been accumulated evidences supporting the melting of spin ice
accompanied by the quantum nature. How does the spin ice melt? A theoretical
scenario has been proposed [2].
References:
1.
Yo Machida, Satoru Nakatsuji, Shigeki Onoda, Takashi Tayama, &
Toshiro Sakakibara,
乬Time-reversal
symmetry breaking and spontaneous Hall effect without magnetic dipole order乭,
Nature
advanced online publication, 9 December 2009.
2.
Shigeki Onoda & Yoichi Tanaka,
乬Quantum melting
of spin ice into spin smectic with cooperative quadrupole and chirality乭,
preprint (ArXiv:0907.2536).
A novel chiral spin state spontaneously breaking the time-reversal
symmetry but not forming any magnetic order has been discovered in a metallic
magnet through the emergence of the Hall resistivity at zero magnetic field.
The solid state is dominantly determined by the
behaviors of a macroscopic number of electrons. Usually, the electronic state
in the thermal equilibrium has the time-reversal symmetry. Namely, the state obtained by reversing the
motion of all the electrons shows exactly the same physical properties as the
original. However, it is known that in some cases, this time-reversal symmetry is broken spontaneously. The typical examples
include ferromagnets, where the electronic spin angular momentum
and/or orbital angular momentum is imbalanced, producing the magnetization
characteristic of the permanent magnet. In principle, the time-reversal
symmetry breaking is not restricted to such cases where a magnetic order appears. Even without the observable macroscopic
magnetization, the broken time-reversal symmetry on a macroscopic scale could be probed, if the
spin chirality, which distinguishes the handedness in which
the spins change their directions in space, appears on a macroscopic scale.
Cooling a metallic magnetic oxcide containing the praseodymium and the iridium
down to extremely low temperatures, we have discovered through the Hall
resistivity measurement at zero applied magnetic field a novel thermodynamic
phase of matter that shows the spontaneously broken time-reversal symmetry in the absence of magnetic order. This research result is
published in Nature Advanced Online Publication on 9 December 2009.
Possible scenarios of
the spontaneous breaking of the time-reversal
symmetry
without magnetic order have been
investigated intensively and extensively from both theoretical and experimental
viewpoints, mainly in the studies of the mechanism and the background of high-temperature cuprate
superconductivity.
An exotic possibility has been proposed that main roles in forming an order are
played by not the spins themselves but the spin chirality of electrons because
of strong quantum fluctuations of a macroscopic
number of interacting electrons. However, its
emergence has not been established yet from both theoretical and experimental
viewpoints.
One of the most important probes of the broken time-reversal symmetry on a macroscopic scale is provided through the
anomalous Hall effect. In metals and semiconductors, the application of
electric current I in the
perpendicular direction to the applied magnetic field B produces a voltage drop VH
in the direction perpendicular to both the applied magnetic field and electric
current. This is the so-called Hall effect, one of the most fundamental
electron transport phenomena in solids, and also has significant importance in
application. On the other hand, in metallic ferromagnets, a macroscopic magnetization appears through
an alignment of electronic spin and/or orbital angular momentum. This
magnetization plays a role of the time-reversal symmetry-breaking field as the
applied magnetic field does: it breaks the time-reversal symmetry on a macroscopic scale, producing the Hall
resistivity (Fig.1A). This is a phenomenon called the anomalous Hall effect. (A recent comprehensive review
article on the anomalous Hall effect from both theoretical and experimental
viewpoints is being published in a US journal 乬Reviews of Modern Physics乭). A similar phenomenon is
also caused by the spin chirality. However, the source of the previously
reported Hall effect is restricted to the applied magnetic field and/or a
macroscopic magnetization associated with magnetic order. Namely, the spontaneously broken time-reversal symmetry on a macroscopic scale in magnets has been
observed only when a certain magnetic order appears with the associated macroscopic
magnetization.
We have discovered for the first time in the
world a novel state which spontaneously produces the Hall effect at zero
magnetic field without any alignment order of electronic spins (Fig.1 B). It
has been found in a compound Pr2Ir2O7, which
is categorized into magnets having a geometrical frustration, or so-called frustrated magnets. This
material contains the praseodymium (Pr) element which plays dominant roles in
the nontrivial magnetism of the material. Because of the geometrical frustration, the magnetic moments of Pr3+ ions
do not form a conventional order even at low temperatures. Instead, it shows a
freezing behavior into a glass state at absolute temperature Tf = 0.3 K (Kelvin乯. Through detailed measurements of the Hall
resistivity and the magnetization, we have detected the spontaneous emergence
of the finite Hall conductivity in the temperature range below TH = 1.5 K above the
freezing temperature Tf =
0.3 K where the Pr magnetic moments do not show either magnetic order or
freezing behavior (Fig.2).
Fig.侾 A) The anomalous Hall effect in ferromagnets. The spontaneous magnetization bears a
fictitious internal magnetic field b through the relativistic spin-orbit
interaction, bending the electronic motion in the direction perpendicular to
the applied electric current. B) The Hall effect without magnetic order. Even at zero magnetic field (B = 0), certain states that do not have
the spontaneous spin magnetization can show the Hall effect spontaneously. In
this case, the fictitious internal magnetic field b, which is a source of bending the electron motion, can be
produced by the order of the spin chirality. Since the Hall effect has appeared in
our observation spontaneously without both applied magnetic field and
spontaneous spin magnetization, the ordering of the spin chirality is naturally considered as a candidate
to the origin of the spontaneous Hall effect.
Fig.2丂The
remnant anomalous Hall conductivity and magnetization measured at zero applied
magnetic field as functions of temperature, after the magnetization process up
to 7 T (tesla). The remnant
anomalous Hall conductivity emerges below an onset temperature TH ~ 1.5 K well above the spin-freezing temperature Tf ~ 0.3 K. The finite remnant magnetization appears
below Tf where the
spins look partially frozen.
Then a question arises. Why does such 乬time-reversal symmetry breaking without magnetic order乭 emerge? In our recent work described in a preprint, we have made the following key observations
common in pyrochlore-lattice magnets Pr2M2O7 (M
= Ir, Sn, Zr), derived their effective quantum model, and carried out
theoretical analyses. Then, it is found that geometrical frustration of magnetic interactions, which has an analogy
in a freezing phenomenon of a water to form an ice, and the quantum nature of
electrons play crucial roles.
In an ice into which the water
comprising H2O molecules crystallizes, H+ ions are
displaced from the vertices of the pyrochlore lattice structure (Fig.3A).
Because of hydrogen bonding, the displacements are allowed only in either
direction of the O2- ions located at the centers of the two
tetrahedrons sharing this vertex. Namely, if one looks at one tetrahedron, two
of the four H+ ions are displaced inwards, while the other two are
displaced outwards (Fig.3B). Thus, for each O2-
ion, there exist six different ways of choosing two H+ ions to form
the hydrogen bonding. In the crystal consisting of a macroscopic number of
ions, this leaves a macroscopic number of ways.
The geometrical frustration as found
in the water ice has also been observed in pyrochlore-lattice magnets R2Ti2O7 (R =Dy, Ho), which has been called a spin ice.
Fig.3: A) Pyrochlore-lattice structure. Red
symbols on the vertices of the tetrahedral network represent the basic
positions of H+ ions in a water ice and the positions of Pr3+ ions in
Pr2M2O7.
B) 乬2-in, 2-out乭 tetrahedral
configurations. Two H+ ions in the case of a water ice and the magnetic moments (spins) of two
Pr ions in the case of spin ice point inwards to the center of the tetrahedron,
while the other two point outwards.
A series of pyrochlore-lattice magnets
containing Pr3+ ions, Pr2M2O7 (M
=Ir, Sn, Zr), can be understood as a sort of spin-ice systems but having
appreciable quantum fluctuations of magnetic moments. As in classical spin-ice
systems R2Ti2O7
(R = Dy, Ho), the directions of
magnetic moments of Pr3+ ions are severely restricted and they can
point either inwards (乬in乭) to or outwards (乬out乭) from the center of the tetrahedron
(non-Kramers magnetic doublet), which can be described in terms of the
so-called Ising spins. In particular, experiments on single crystalline samples
of Pr2Ir2O7 show a metamagnetic transition at
low temperatures under the applied magnetic field along the [111] direction
(Fig.4). This phenomenon should be observed if and only if 乬2-in, 2-out乭 tetrahedral configuration is
favored at low magnetic field. In this case, one of the four spins always
points to the unfavorable direction under the magnetic field applied along the
[111] direction. It is flipped to form a 乬3-in,
1-out乭 or 乬1-in,
3-out乭 configuration when the
magnetic field strength exceeds a threshold value comparable to the effective
coupling between the spins. This indicates that each tetrahedron is mainly in a
乬2-in,
2-out乭
configuration (Fig.3B), and that this spin-ice rule is satisfied in a certain
length/time scale. From the value of the magnetic field where the metamagnetic
transition has been observed, an effective ferromagnetic coupling has been
estimated to be 1.4 K (~ 1.6 meV). These materials do not show a diverging
behavior of the magnetic susceptibility unlike the classical spin-ice systems.
Because the magnitude of the Pr3+ magnetic moment is 1/4 ~ 1/3 of that of the Dy moment, the magnetic dipole-dipole interaction,
which is a driving source of the spin-ice behaviors, is of the order of 0.1 K,
an order of magnitude smaller. Therefore, a quantum-mechanical superexchange
interaction is anticipated to be a dominant interaction between the moments. Actually, neutron-scattering
experiments on Pr2Sn2O7 have reported that
there appears no magnetic Bragg peak even at the lowest temperature and that
the inelastic scattering spectra have a rather broad peak up to 0.2 meV,
which is comparable to the effective coupling mentioned above, in an otherwise
classical spin-ice behavior. This indicates much stronger quantum fluctuations of the magnetic
moments than in the classical spin ice. It suggests an intriguing possibility
that the geometrical
frustration and the quantum
fluctuation cooperatively suppress an conventional magnetic order, and realize a chiral spin liquid where the time-reversal symmetry is
broken on a macroscopic scale by the order in the spin chirality, a higher degrees of
freedom associated with the spins. Then, we demonstrate theoretically that
under the constraints of the spin-ice rule and the zero spin magnetization, it
is possible to make a chiral spin structure that produces a finite Hall effect
at zero applied magnetic field.
Fig.4 A) The scalar spin chirality kijk = Si丒Sj亊Sk is defined using three nearby spins in a
noncoplanar configuration. B) Crystal structure of Pr2Ir2O7.
Both of Pr (red) and Ir (green) atoms form the pyrochlore lattice. Each Pr3+
magnetic moment can be described as an Ising spin which points either inwards
to or outwards from the center of the tetrahedron. It is most likely that blue
arrows indicate the spin directions stable at zero magnetic field, forming 乬2-in, 2-out乭 spin-ice configurations
together with the red arrows at the other Pr3+ sites, and that they
are flipped to the red arrows at a metamagnetic transition under the applied
magnetic field along the [111] direction. Under the applied field along the
[100] and [110] directions, a metamagnetic transition was not observed.
Now we have recognized theoretically that
this state to which the spin ice quantum-mechanically melts shows an analogy to
liquid crystals. There are various categories of liquid crystals depending on
the way of directional and positional alignments of nonpolar molecules. In
particular, that forming a directional order is referred to as a nematic liquid
crystal. A prototype of nematic liquid crystals that are optically active
because of the helical directional alignments is called a cholesteric liquid
crystal. A nematic liquid crystal also showing the positional order is called a
smectic liquid crystal. Our recent theoretical studies have uncovered that the
spin ice quantum-mechanically melts to a spin analog of the smectic liquid
crystal.
Fig.5 The figures show how the sum of the
four magnetic moments (spins) in each tetrahedron is inclined to align each
other for nearby tetrahedron pairs.
Red and blue regions represent those favorable and unfavorable
directions for the sum of the four spins to point. The favorable direction
depends on the spatial direction of the two tetrahedrons, but on average, all
the spins have a favorable direction of the +z and –z. This results in a
compression of the crystal in the z direction.
It has also been found that the quantum state of each tetrahedral unit can be labeled by the left-handed or right-handed chirality. Then, in the quantum melted spin-ice state, the chirality of a tetrahedron is inclined to have an opposite sign between the two tetrahedrons shown in Fig.5. Here, the geometrical frustration found in the freezing behavior of the water appears for the chirality degrees of freedom. This raises a further exotic scenario: a chirality ice which breaks the time-reversal symmetry on a macroscopic scale might be realized as the freezing of the chirality.
The research achievements described here have been produced in Japan. Further theoretical and experimental studies are currently being performed and planned, aiming at a full understanding on the spin liquid with the spontaneously broken time-reversal symmetry and in the quest to a novel state of matter.
The content of this
article has been done in
collaboration with Y. Machida (Tokyo
Institute of Technology, Research Associate), S. Nakatsuji (Institute for Solid State Physics, Univ. of
Tokyo, Associate Professor), T. Tayama (Univ.
Toyama, Associate Professor), T. Sakakibara (Institute for Solid State Physics, Univ. of Tokyo, Professor), and
Y. Tanaka (Condensed Matter Theory Lab., RIKEN, Research Fellow).
This is one of the most fundamental symmetry in
physics under the equilibrium, satisfied if a quantum state shows exactly the
same physical properties under the time-reversal operation that also reverse
all the motions of particles and waves of interest and thus inverts their
wavevectors and angular momenta.
Magnet is a substance that
contains a macroscopic number of microscopic magnetic moments associated with
the spin angular momentum, i.e, rotational motion, of electrons. Usually, these
electronic spins form a magnetic order in a certain spatial pattern. They are
classified into several subclasses; ferromagents (like iron, cobalt, and
nickel) having a macroscopic magnetization, antiferromagents where the
magnetization is cancelled out within the material, paramagnets that do not
show any magnetic order, and so on.
Three nearby electronic spins,
each of which has a directional degree of freedom, may form a noncoplanar
structure in materials. Then, the solid angle subtended by these three spins,
with the positive or negative sign, depending on whether they form a
left-handed or right-handed, is referred to as the spin chirality (Fig.2A).
This distinguishes the handedness in the spin space, irrespective of that in
the crystal structure.
When the electronic spin
located at each vertex of a triangle can point either upwards or downwards and
any pair of neighboring spins is forced to align antiferromagnetically, namely,
in an anti-parallel configuration (乬up, down乭), there is no way to achieve these constraints
at the same time; one of three pairs has a ferromagnetic configuration (乬up, up乭 or 乬down, down乭). Then, the spins feel 乬frustration乭 that originates from the geometry of the
lattice structure.
The
superconductivity accompanied by the zero-resistive state occurs, when charge
carriers are chemically doped into mother antiferromagnetic compounds of
cuprate ceramics. It is significantly important on scientific grounds as a
superconductivity realized in a vicinity of an insulating state. It has also been
utilized for application because of its high transition temperature. (The
highest transition temperature
under pressure amounts to -140
degree in
Celsius.)
In the classical Newtonian physics, the
physical observable quantities are always determined at the same time. However,
in quantum mechanics describing microscopic physical phenomena, there exist
collections of observables that can never be determined simultaneously and
completely. For instance, three components of the angular momentum, jx, jy, and jz,
are not to be determined at the same time. Then, even upon cooling to the
absolute zero temperature, mutually interacting macroscopic number of electrons
have directions of their angular momenta fluctuate among various quantum
states. In magnets, it is sometimes also called quantum magnetic fluctuations.
The spin liquid is a system
where each electronic spin confined to the magnetic ion site does not have a fixed
direction to point and fluctuates both spatially and dynamically. In
particular, the spin liquid with the broken time-reversal symmetry on a
macroscopic scale is referred to as a chiral spin liquid.
Related article in Nakatsuji Group, Institute for Solid State
Physics, University of Tokyo