3,568 research outputs found

    Multifractal properties of critical eigenstates in two-dimensional systems with symplectic symmetry

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    The multifractal properties of electronic eigenstates at the metal-insulator transition of a two-dimensional disordered tight-binding model with spin-orbit interaction are investigated numerically. The correlation dimensions of the spectral measure D~2\widetilde{D}_{2} and of the fractal eigenstate D2D_{2} are calculated and shown to be related by D2=2D~2D_{2}=2\widetilde{D}_{2}. The exponent η=0.35±0.05\eta=0.35\pm 0.05 describing the energy correlations of the critical eigenstates is found to satisfy the relation η=2D2\eta=2-D_{2}.Comment: 6 pages RevTeX; 3 uuencoded, gzipped ps-figures to appear in J. Phys. Condensed Matte

    Geometrical structure effect on localization length of carbon nanotubes

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    The localization length and density of states of carbon nanotubes are evaluated within the tight-binding approximation. By comparison with the corresponding results for the square lattice tubes, it is found that the hexagonal structure affects strongly the behaviors of the density of states and localization lengths of carbon nanotubes.Comment: 7 pages, 4 figures, revised version to appear in Chin. Phys. Lett. The title is changed. Some arguments are adde

    Localization Transition in Multilayered Disordered Systems

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    The Anderson delocalization-localization transition is studied in multilayered systems with randomly placed interlayer bonds of density pp and strength tt. In the absence of diagonal disorder (W=0), following an appropriate perturbation expansion, we estimate the mean free paths in the main directions and verify by scaling of the conductance that the states remain extended for any finite pp, despite the interlayer disorder. In the presence of additional diagonal disorder (W>0W > 0) we obtain an Anderson transition with critical disorder WcW_c and localization length exponent ν\nu independently of the direction. The critical conductance distribution Pc(g)P_{c}(g) varies, however, for the parallel and the perpendicular directions. The results are discussed in connection to disordered anisotropic materials.Comment: 10 pages, Revtex file, 8 postscript files, minor change

    The Anderson transition: time reversal symmetry and universality

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    We report a finite size scaling study of the Anderson transition. Different scaling functions and different values for the critical exponent have been found, consistent with the existence of the orthogonal and unitary universality classes which occur in the field theory description of the transition. The critical conductance distribution at the Anderson transition has also been investigated and different distributions for the orthogonal and unitary classes obtained.Comment: To appear in Physical Review Letters. Latex 4 pages with 4 figure

    The Anderson Transition in Two-Dimensional Systems with Spin-Orbit Coupling

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    We report a numerical investigation of the Anderson transition in two-dimensional systems with spin-orbit coupling. An accurate estimate of the critical exponent ν\nu for the divergence of the localization length in this universality class has to our knowledge not been reported in the literature. Here we analyse the SU(2) model. We find that for this model corrections to scaling due to irrelevant scaling variables may be neglected permitting an accurate estimate of the exponent ν=2.73±0.02\nu=2.73 \pm 0.02

    Relation between Energy Level Statistics and Phase Transition and its Application to the Anderson Model

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    A general method to describe a second-order phase transition is discussed. It starts from the energy level statistics and uses of finite-size scaling. It is applied to the metal-insulator transition (MIT) in the Anderson model of localization, evaluating the cumulative level-spacing distribution as well as the Dyson-Metha statistics. The critical disorder Wc=16.5W_{c}=16.5 and the critical exponent ν=1.34\nu=1.34 are computed.Comment: 9 pages, Latex, 6 PostScript figures in uuencoded compressed tar file are appende

    Stereoscopic electron spectroscopy of solar hard X-ray flares with a single spacecraft

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    Hard X-ray (HXR) spectroscopy is the most direct method of diagnosing energetic electrons in solar flares. Here we present a technique which allows us to use a single HXR spectrum to determine an effectively stereoscopic electron energy distribution. Considering the Sun's surface to act as a 'Compton mirror' allows us to look at emitting electrons also from behind the source, providing vital information on downward-propagating particles. Using this technique we determine simultaneously the electron spectra of downward and upward directed electrons for two solar flares observed by the Ramaty High Energy Solar Spectroscopic Imager (RHESSI). The results reveal surprisingly near-isotropic electron distributions, which contrast strongly with the expectations from the standard model which invokes strong downward beaming, including collisional thick-target model.Comment: 7 pages, 3 figures, accepted to Astrophysical Journal Letter

    Insulator-Metal Transition in the One and Two-Dimensional Hubbard Models

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    We use Quantum Monte Carlo methods to determine T=0T=0 Green functions, G(r,ω)G(\vec{r}, \omega), on lattices up to 16×1616 \times 16 for the 2D Hubbard model at U/t=4U/t =4. For chemical potentials, μ\mu, within the Hubbard gap, μ<μc |\mu | < \mu_c, and at {\it long} distances, r\vec{r}, G(r,ω=μ)er/ξlG(\vec{r}, \omega = \mu) \sim e^{ -|\vec{r}|/\xi_l} with critical behavior: ξlμμcν\xi_l \sim | \mu - \mu_c |^{-\nu}, ν=0.26±0.05 \nu = 0.26 \pm 0.05. This result stands in agreement with the assumption of hyperscaling with correlation exponent ν=1/4\nu = 1/4 and dynamical exponent z=4z = 4. In contrast, the generic band insulator as well as the metal-insulator transition in the 1D Hubbard model are characterized by ν=1/2\nu = 1/2 and z=2z = 2.Comment: 9 pages (latex) and 5 postscript figures. Submitted for publication in Phys. Rev. Let

    Scaling of the conductance distribution near the Anderson transition

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    The single parameter scaling hypothesis is the foundation of our understanding of the Anderson transition. However, the conductance of a disordered system is a fluctuating quantity which does not obey a one parameter scaling law. It is essential to investigate the scaling of the full conductance distribution to establish the scaling hypothesis. We present a clear cut numerical demonstration that the conductance distribution indeed obeys one parameter scaling near the Anderson transition

    Possible Jurassic age for part of Rakaia Terrane: implications for tectonic development of the Torlesse accretionary prism

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    Greywacke sandstone and argillite beds comprising Rakaia Terrane (Torlesse Complex) in mid Canterbury, South Island, New Zealand, are widely regarded as Late Triassic (Norian) in age based on the occurrence of Torlessia trace fossils, Monotis, and other taxa. This paleontological age assignment is tested using published 40Ar/39Ar mica and U-Pb zircon ages for these rocks and published and new zircon fission track (FT) ages. The youngest U-Pb zircon ages in the Rakaia Terrane rocks in mid Canterbury are Norian, whereas 10-20% of the 40Ar/39Ar muscovite ages are younger than Norian. Numerical modelling of these mica ages shows that they cannot have originated from partial thermal overprinting in the Torlesse prism if the thermal maximum was short-lived and early in the prism history (210-190 Ma), as commonly inferred for these rocks. The young component of mica ages could, however, be explained by extended residence (200-100 Ma) at 265-290deg.C in the prism. Early Jurassic (c. 189 Ma) zircon FT ages for sandstone beds from Arthur's Pass, the Rakaia valley, and the Hermitage (Mt Cook) are interpreted not to have experienced maximum temperatures above 210deg.C, and therefore cannot have been reduced as a result of partial annealing in the Torlesse prism. This is based on identification of a fossil Cretaceous, zircon FT, partial annealing zone in low-grade schists to the west, and the characteristics of the age data. The Early Jurassic zircon FT ages and the young component of 40Ar/39Ar mica ages are regarded therefore as detrital ages reflecting cooling in the source area, and constrain the maximum depositional age of parts of the Rakaia Terrane in mid Canterbury. The zircon FT data also show the initiation (c. 100 Ma) of marked and widespread Late Cretaceous cooling of Rakaia Terrane throughout Canterbury, which is attributed to uplift and erosion of inboard parts of the Torlesse prism due to continuing subduction accretion at its toe. The critical wedge concept is proposed as a new framework for investigating the development of the Torlesse Complex. The Rakaia Terrane may have formed the core of an accretionary wedge imbricated against the New Zealand margin during the Middle or Late Jurassic. Late Jurassic nonmarine sediments (e.g., Clent Hills Formation) accumulated upon the inner parts of the prism as it enlarged, emerged, and continued to be imbricated. Exhumation of Otago Schist from c. 135 Ma may mark the development of a balance (steady state) between sediments entering the prism at the toe and material exiting at the inboard margin. The enlargement of the area of exhumation to all of Canterbury from c. 100 Ma may reflect a dynamic response to widening of the prism through the accretion of Cretaceous sediments. The model of a dynamic critical wedge may help to explain the various expressions of the Rangitata Orogeny
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