242 research outputs found
Charging Spectrum of a Small Wigner Crystal Island
Charging of a clean two-dimensional island is studied in the regime of small
concentration of electrons when they form the Wigner crystal. The number of
electrons in the island is assumed to be not too big (N < 100). It is shown
that the total energy of the island as a function of N has a quasi-periodic
component of a universal shape, that is independent of the form of
electron-electron interactions. These oscillations are caused by the
combination of the geometric effects associated with packing of the triangular
lattice into the circular island. These effects are: the shell effect,
associated with starting a new crystalline row, and the so-called confinement
polaronic effect. In the presence of close metallic gates, which eliminate the
long-range part of the electron-electron interactions, the oscillations of the
energy bring about simultaneous entering of the dot by a few electrons.Comment: 8 pages, Latex, 8 Postscript pages are include
Segmentation of the Izu-Bonin and Mariana slabs based on the analysis of the Benioff seismicity distribution and regional tomography results
We present a new model of P and S velocity anomalies in the mantle down to a depth of 1300 km beneath the Izu-Bonin and Mariana (IBM) arcs. This model is derived based on tomographic inversion of global travel time data from the revised ISC catalogue. The results of inversion are thoroughly verified using a series of different tests. The obtained model is generally consistent with previous studies by different authors. We also present the distribution of relocated deep events projected to the vertical surface along the IBM arc system. Unexpectedly, the seismicity forms elongated vertical clusters instead of horizontal zones indicating phase transitions in the slab. We propose that these vertical seismicity zones mark zones of intense deformation and boundaries between semi-autonomous segments of the subducting plate. The P and S seismic tomography models consistently display the slab as prominent high-velocity anomalies coinciding with the distribution of deep seismicity. We can distinguish at least four segments which subduct differently. The northernmost segment of the Izu-Bonin arc has the gentlest angle of dipping which is explained by backward displacement of the trench. In the second segment, the trench stayed at the same location, and we observe the accumulation of the slab material in the transition zone and its further descending to the lower mantle. In the third segment, the trench is moving forward causing the steepening of the slab. Finally, for the Mariana segment, despite the backward displacement of the arc, the subducting slab is nearly vertical. Between the Izu-Bonin and Mariana arcs we clearly observe a gap which can be traced down to about 400 km in depth. Based on joint consideration of the tomography results and the seismicity distribution, we propose two different scenarios of the subduction evolution in the IBM zone during the recent time, depending on the reference frame of plate displacements. In the first case, we consider the movements in respect to the Philippine Plate, and explain the different styles of the subduction by the relative backward and forward migrations of the trench. In the second case, all the elements of the subduction system move westward in respect to the stable Asia. Different subduction styles are explained by the "anchoring" of selected segments of the slab, different physical properties of the subducting plate and the existence of buoyant rigid blocks related to sea mount and igneous provinces
Statistics of the Charging Spectrum of a Two-Dimensional Coulomb Glass Island
The fluctuations of capacitance of a two-dimensional island are studied in
the regime of low electron concentration and strong disorder, when electrons
can be considered classical particles. The universal capacitance distribution
is found, with the dispersion being of the order of the average. This
distribution is shown to be closely related to the shape of the Coulomb gap in
the one-electron density of states of the island. Behavior of the the
capacitance fluctuations near the metal - insulator transition is discussed.Comment: 4 pages, LaTex, 4 Postscript figures are included Discussion of the
situation with screening by metallic gate is adde
Quantum orientational melting of mesoscopic clusters
By path integral Monte Carlo simulations we study the phase diagram of two -
dimensional mesoscopic clusters formed by electrons in a semiconductor quantum
dot or by indirect magnetoexcitons in double quantum dots. At zero (or
sufficiently small) temperature, as quantum fluctuations of particles increase,
two types of quantum disordering phenomena take place: first, at small values
of quantum de Boer parameter q < 0.01 one can observe a transition from a
completely ordered state to that in which different shells of the cluster,
being internally ordered, are orientationally disordered relative to each
other. At much greater strengths of quantum fluctuations, at q=0.1, the
transition to a disordered (superfluid for the boson system) state takes place.Comment: 4 pages, 6 Postscript figure
Interaction-induced oscillations of the tunneling density of states in a non-quantizing magnetic field
We study tunneling into interacting disordered two-dimensional electron gas
in a non-quantizing magnetic field, which does not cause the standard de Haas--
van Alphen oscillations. Interaction induces a new type of oscillations in the
tunneling density of states with the characteristic period of cyclotron
quantum.Comment: 4 pages, 1 .eps figure, submitted to Phys. Rev. Let
Two-dimensional electron liquid with disorder in a weak magnetic field
We present the effective theory for low energy dynamics of a two-dimensional
interacting electrons in the presence of a weak short-range disorder and a weak
perpendicular magnetic field, the filling factor . We investigate
the exchange enhancement of the -factor, the effective mass and the decay
rate of the simplest spin wave excitations at . We obtain the
enhancement of the field-induced gap in the tunneling density of states and
dependence of the tunneling conductivity on the applied bias.Comment: 17 pages, no figure
Mean-field Phase Diagram of Two-Dimensional Electrons with Disorder in a Weak Magnetic Field
We study two-dimensional interacting electrons in a weak perpendicular
magnetic field with the filling factor and in the presence of a
quenched disorder. In the framework of the Hartree-Fock approximation, we
obtain the mean-field phase diagram for the partially filled highest Landau
level. We find that the CDW state can exist if the Landau level broadening
does not exceed the critical value .
Our analysis of weak crystallization corrections to the mean-field results
shows that these corrections are of the order of and
therefore can be neglected
Conductivity tensor of striped quantum Hall phases
We study the transport properties of pinned striped quantum Hall phases. We
show that under quite general assumptions, the macroscopic conductivity tensor
satisfies a semicircle law. In particular, this result is valid for both
smectic and nematic stripe phases, independent of the presence of topological
defects such as dislocations and grain boundaries. As a special case, our
results explain the experimental validity of a product rule for the dissipative
part of the resistivity tensor, which was previously derived by MacDonald and
Fisher for a perfect stripe structure.Comment: 5 pages, 2 figure
Joint Inversion of Active and Passive Seismic Data in Central Java
Seismic and volcanic activities in Central Java, Indonesia, the area of interest of this study, are directly or indirectly related to the subduction of the Indo-Australian plate. In the framework of the MERapi AMphibious EXperiments (MERAMEX), a network consisting of about 130
seismographic stations was installed onshore and offshore in Central Java and operated for more than 150 days. In addition, 3-D active seismic experiments were carried out offshore. In this paper, we present the results of processing combined active and passive seismic data,
which contain traveltimes from 292 local earthquakes and additional airgun shots along three offshore profiles. The inversion was performed using the updated LOTOS-06 code that allows processing for active and passive source data. The joint inversion of the active and passive data
set considerably improves the resolution of the upper crust, especially in the offshore area in comparison to only passive data. The inversion results are verified using a series of synthetic tests. The resulting images showan exceptionally strong low-velocity anomaly (−30 per cent) in
the backarc crust northward of the active volcanoes. In the upper mantle beneath the volcanoes, we observe a low-velocity anomaly inclined towards the slab, which probably reflects the paths of fluids and partially melted materials in the mantle wedge. The crust in the forearc appears to be strongly heterogeneous. The onshore part consists of two high-velocity blocks separated by a narrow low-velocity anomaly, which can be interpreted as a weakened contact zone between two rigid crustal bodies. The recent Java Mw = 6.3 earthquake (2006/05/26-UTC) occurred at
the lower edge of this zone. Its focal strike slip mechanism is consistent with the orientation of this contact
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