83 research outputs found
Quantum integrability and nonintegrability in the spin-boson model
We study the spectral properties of a spin-boson Hamiltonian that depends on
two continuous parameters (interaction strength) and
(integrability switch). In the classical limit this
system has two distinct integrable regimes, and . For
each integrable regime we can express the quantum Hamiltonian as a function of
two action operators. Their eigenvalues (multiples of ) are the natural
quantum numbers for the complete level spectrum. This functional dependence
cannot be extended into the nonintegrable regime . Here level
crossings are prohibited and the level spectrum is naturally described by a
single (energy sorting) quantum number. In consequence, the tracking of
individual eigenstates along closed paths through both regimes leads to
conflicting assignments of quantum numbers. This effect is a useful and
reliable indicator of quantum chaos -- a diagnostic tool that is independent of
any level-statistical analysis
Entanglement, fidelity, and quantum-classical correlations with an atom walking in a quantized cavity field
Stability and instability of quantum evolution are studied in the interaction
between a two-level atom with photon recoil and a quantized field mode in an
ideal cavity, the basic model of cavity quantum electrodynamics (QED). It is
shown that the Jaynes-Cummings dynamics can be unstable in the regime of
chaotic walking of the atomic center-of-mass in the quantized field of a
standing wave in the absence of any kind of interaction with environment. This
kind of quantum instability manifests itself in strong variations of reduced
quantum purity and entropy, correlating with the respective classical Lyapunov
exponent, and in exponential sensitivity of fidelity of quantum states to small
variations in the atom-field detuning. The connection between quantum
entanglement and fidelity and the center-of-mass motion is clarified
analytically and numerically for a few regimes of that motion. The results are
illustrated with two specific initial field states: the Fock and coherent ones.
Numerical experiments demonstrate various manifestations of the
quantum-classical correspondence, including dynamical chaos and fractals, which
can be, in principle, observed in real experiments with atoms and photons in
high finesse cavities
Dipolar ground state of planar spins on triangular lattices
An infinite triangular lattice of classical dipolar spins is usually
considered to have a ferromagnetic ground state. We examine the validity of
this statement for finite lattices and in the limit of large lattices. We find
that the ground state of rectangular arrays is strongly dependent on size and
aspect ratio. Three results emerge that are significant for understanding the
ground state properties: i) formation of domain walls is energetically favored
for aspect ratios below a critical valu e; ii) the vortex state is always
energetically favored in the thermodynamic limit of an infinite number of
spins, but nevertheless such a configuration may not be observed even in very
large lattices if the aspect ratio is large; iii) finite range approximations
to actual dipole sums may not provide the correct ground sta te configuration
because the ferromagnetic state is linearly unstable and the domain wall energy
is negative for any finite range cutoff.Comment: Several short parts have been rewritten. Accepted for publication as
a Rapid Communication in Phys. Rev.
Spin melting and refreezing driven by uniaxial compression on a dipolar hexagonal plate
We investigate freezing characteristics of a finite dipolar hexagonal plate
by the Monte Carlo simulation. The hexagonal plate is cut out from a piled
triangular lattice of three layers with FCC-like (ABCABC) stacking structure.
In the present study an annealing simulation is performed for the dipolar plate
uniaxially compressed in the direction of layer-piling. We find spin melting
and refreezing driven by the uniaxial compression. Each of the melting and
refreezing corresponds one-to-one with a change of the ground states induced by
compression. The freezing temperatures of the ground-state orders differ
significantly from each other, which gives rise to the spin melting and
refreezing of the present interest. We argue that these phenomena are
originated by a finite size effect combined with peculiar anisotropic nature of
the dipole-dipole interaction.Comment: Proceedings of the Highly Frustrated Magnetism (HFM2006) conference.
To appear in a special issue of J. Phys. Condens. Matte
Synchronization and bistability of qubit coupled to a driven dissipative oscillator
We study numerically the behavior of qubit coupled to a quantum dissipative
driven oscillator (resonator). Above a critical coupling strength the qubit
rotations become synchronized with the oscillator phase. In the synchronized
regime, at certain parameters, the qubit exhibits tunneling between two
orientations with a macroscopic change of number of photons in the resonator.
The life times in these metastable states can be enormously large. The
synchronization leads to a drastic change of qubit radiation spectrum with
appearance of narrow lines corresponding to recently observed single
artificial-atom lasing [O. Astafiev {\it et al.} Nature {\bf 449}, 588 (2007)].Comment: revtex 4 pages, 6 figs, research at http://www.quantware.ups-tlse.fr
Peculiar from-Edge-to-Interior Spin Freezing in a Magnetic Dipolar Cube
By molecular dynamics simulation, we have investigated classical Heisenberg
spins, which are arrayed on a finite simple cubic lattice and interact with
each other only by the dipole-dipole interaction, and have found its peculiar
it from-Edge-to-interior freezing process. As the temperature is decreased,
spins on each edge predominantly start to freeze in a ferromagnetic alignment
parallel to the edge around the corresponding bulk transition temperature, then
from each edges grow domains with short-range orders similar to the
corresponding bulk orders, and the system ends up with a unique multi-domain
ground state at the lowest temperature. We interpret this freezing
characteristics is attributed to the anisotropic and long-range nature of the
dipole-dipole interaction combined with a finite-size effect.Comment: 11 pages 5 figure
The transition to classical chaos in a coupled quantum system through continuous measurement
Continuous observation of a quantum system yields a measurement record that
faithfully reproduces the classically predicted trajectory provided that the
measurement is sufficiently strong to localize the state in phase space but
weak enough that quantum backaction noise is negligible. We investigate the
conditions under which classical dynamics emerges, via continuous position
measurement, for a particle moving in a harmonic well with its position coupled
to internal spin. As a consequence of this coupling we find that classical
dynamics emerges only when the position and spin actions are both large
compared to . These conditions are quantified by placing bounds on the
size of the covariance matrix which describes the delocalized quantum coherence
over extended regions of phase space. From this result it follows that a mixed
quantum-classical regime (where one subsystem can be treated classically and
the other not) does not exist for a continuously observed spin 1/2 particle.
When the conditions for classicallity are satisfied (in the large-spin limit),
the quantum trajectories reproduce both the classical periodic orbits as well
as the classically chaotic phase space regions. As a quantitative test of this
convergence we compute the largest Lyapunov exponent directly from the measured
quantum trajectories and show that it agrees with the classical value.Comment: 8 pages, 5 figure
Magnetic Properties of 2-Dimensional Dipolar Squares: Boundary Geometry Dependence
By means of the molecular dynamics simulation on gradual cooling processes,
we investigate magnetic properties of classical spin systems only with the
magnetic dipole-dipole interaction, which we call dipolar systems. Focusing on
their finite-size effect, particularly their boundary geometry dependence, we
study two finite dipolar squares cut out from a square lattice with
and , where is an angle between the direction of the lattice axis
and that of the square boundary. Distinctly different results are obtained in
the two dipolar squares. In the square, the ``from-edge-to-interior
freezing'' of spins is observed. Its ground state has a multi-domain structure
whose domains consist of the two among infinitely (continuously) degenerated
Luttinger-Tisza (LT) ground-state orders on a bulk square lattice, i.e., the
two antiferromagnetically aligned ferromagnetic chains (af-FMC) orders directed
in parallel to the two lattice axes. In the square, on the other
hand, the freezing starts from the interior of the square, and its ground state
is nearly in a single domain with one of the two af-FMC orders. These geometry
effects are argued to originate from the anisotropic nature of the
dipole-dipole interaction which depends on the relative direction of sites in a
real space of the interacting spins.Comment: 21 pages, 13 figures, submitted to Journal of Physical Society Japa
Restoration of the structure and soil protection role of no-till in chernozems and chestnuts soils of the Stavropol Territory
The results of research on the example of southern chernozem and chestnut soil are presented. Long-term use of plowing with rotation of the soil layer and the use of fallows leads to a critical state of the soil in terms of the content of aggregates measuring >10 mm and >1 mm. The introduction of notill on old arable soils leads to a general increase in the mean weighted diameter of aggregates (MWD). The intensity of restoration of the structural state of the soil during no-till in southern chernozem occurs more intensively than in chestnut soil, and the main changes are recorded in the fractions of agronomically valuable aggregates. In southern chernozem there is an increase in diameter from 6.0 mm to 9.5 mm, while in chestnut soil the MWD increases only to 7 mm. The content of erosion-susceptible aggregates <1 mm and their change depending on the intensity of agricultural cultivation in southern chernozem and chestnut soil indicates a tendency to restore the structure in the no-till variant. In southern chernozem, the content of particles of 1â0.5 mm size decreased by 1.2%, and in chestnut soil â by 6.2%. Refusal of mechanical tillage showed that, in contrast to dry aggregates, the influence of no-till on the water stability of the structure of the arable horizon is more significant and is presented in the form of fractions rearrangement. The use of no-till technology results in a reduction in the content of erosion-susceptible aggregates and increases the water stability of the structure of the arable horizon, which, together with the influence of crop residues on the soil surface, provides an anti-erosion effect. The restoration of the structural state of the soil during notill in southern chernozem proceeds more intensively than in chestnut soil. The main changes in the form of rearrangement occur in fractions of agronomically valuable aggregates
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