13,383 research outputs found

    From Point Defects in Graphene to Two-Dimensional Amorphous Carbon

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    While crystalline two-dimensional materials have become an experimental reality during the past few years, an amorphous 2-D material has not been reported before. Here, using electron irradiation we create an sp2-hybridized one-atom-thick flat carbon membrane with a random arrangement of polygons, including four-membered carbon rings. We show how the transformation occurs step-by-step by nucleation and growth of low-energy multi-vacancy structures constructed of rotated hexagons and other polygons. Our observations, along with first-principles calculations, provide new insights to the bonding behavior of carbon and dynamics of defects in graphene. The created domains possess a band gap, which may open new possibilities for engineering graphene-based electronic devices.Comment: 10 pages, 10 figures including supplementary informatio

    The X-ray Fundamental Plane and LX−TL_X-T Relation of Clusters of Galaxies

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    We analyze the relations among central gas density, core radius, and temperature of X-ray clusters by plotting the observational data in the three-dimensional (log⁡ρ0\log \rho_0, log⁡R\log R, and log⁡T\log T) space and find that the data lie on a 'fundamental plane'. Its existence implies that the clusters form a two-parameter family. The data on the plane still has a correlation and form a band on the plane. The observed relation LX∝T3L_{\rm X} \propto T^3 turns out to be the cross section of the band perpendicular to the major axis, while the major axis is found to describe the virial density. We discuss implications of this two-parameter family nature of X-ray clusters.Comment: 7 pages, 2 figures. To be published in ApJ Letter

    Continuous-flow IRMS technique for determining the 17O excess of CO2 using complete oxygen isotope exchange with cerium oxide

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    This paper presents an analytical system for analysis of all single substituted isotopologues (<sup>12</sup>C<sup>16</sup>O<sup>17</sup>O, <sup>12</sup>C<sup>16</sup>O<sup>18</sup>O, <sup>13</sup>C<sup>16</sup>O<sup>16</sup>O) in nanomolar quantities of CO<sub>2</sub> extracted from stratospheric air samples. CO<sub>2</sub> is separated from bulk air by gas chromatography and CO<sub>2</sub> isotope ratio measurements (ion masses 45 / 44 and 46 / 44) are performed using isotope ratio mass spectrometry (IRMS). The <sup>17</sup>O excess (Δ<sup>17</sup>O) is derived from isotope measurements on two different CO<sub>2</sub> aliquots: unmodified CO<sub>2</sub> and CO<sub>2</sub> after complete oxygen isotope exchange with cerium oxide (CeO<sub>2</sub>) at 700 °C. Thus, a single measurement of Δ<sup>17</sup>O requires two injections of 1 mL of air with a CO<sub>2</sub> mole fraction of 390 μmol mol<sup>−1</sup> at 293 K and 1 bar pressure (corresponding to 16 nmol CO<sub>2</sub> each). The required sample size (including flushing) is 2.7 mL of air. A single analysis (one pair of injections) takes 15 minutes. The analytical system is fully automated for unattended measurements over several days. The standard deviation of the <sup>17</sup>O excess analysis is 1.7&permil;. Multiple measurements on an air sample reduce the measurement uncertainty, as expected for the statistical standard error. Thus, the uncertainty for a group of 10 measurements is 0.58&permil; for &Delta; <sup>17</sup>O in 2.5 h of analysis. 100 repeat analyses of one air sample decrease the standard error to 0.20&permil;. The instrument performance was demonstrated by measuring CO<sub>2</sub> on stratospheric air samples obtained during the EU project RECONCILE with the high-altitude aircraft Geophysica. The precision for RECONCILE data is 0.03&permil; (1&sigma;) for δ<sup>13</sup>C, 0.07&permil; (1&sigma;) for δ<sup>18</sup>O and 0.55&permil; (1&sigma;) for &delta;<sup>17</sup>O for a sample of 10 measurements. This is sufficient to examine stratospheric enrichments, which at altitude 33 km go up to 12&permil; for &delta;<sup>17</sup>O and up to 8&permil; for δ<sup>18</sup>O with respect to tropospheric CO<sub>2</sub> : &delta;<sup>17</sup>O ~ 21&permil; Vienna Standard Mean Ocean Water (VSMOW), δ<sup>18</sup>O ~ 41&permil; VSMOW (Lämmerzahl et al., 2002). The samples measured with our analytical technique agree with available data for stratospheric CO<sub>2</sub>

    Direct measurements of the polarization of terrestrial kilometric radiation from Voyagers 1 and 2

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    Terrestrial radiation measurements obtained with planetary radio astronomy experiments on Voyager-1 and 2 during the early portions of each flight show the signals to be predominantly left-hand circularly polarized. Since these emissions were most probably generated above the Northern Hemisphere auroral zone, it is concluded that the radiation is emitted primarily in the extraordinary mode

    Feasibility of Experimental Realization of Entangled Bose-Einstein Condensation

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    We examine the practical feasibility of the experimental realization of the so-called entangled Bose-Einstein condensation (BEC), occurring in an entangled state of two atoms of different species. We demonstrate that if the energy gap remains vanishing, the entangled BEC persists as the ground state of the concerned model in a wide parameter regime. We establish the experimental accessibility of the isotropic point of the effective parameters, in which the entangled BEC is the exact ground state, as well as the consistency with the generalized Gross-Pitaevskii equations. The transition temperature is estimated. Possible experimental implementations are discussed in detail.Comment: 6 pages, published versio

    Probing Dark Energy with Baryonic Acoustic Oscillations from Future Large Galaxy Redshift Surveys

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    We show that the measurement of the baryonic acoustic oscillations in large high redshift galaxy surveys offers a precision route to the measurement of dark energy. The cosmic microwave background provides the scale of the oscillations as a standard ruler that can be measured in the clustering of galaxies, thereby yielding the Hubble parameter and angular diameter distance as a function of redshift. This, in turn, enables one to probe dark energy. We use a Fisher matrix formalism to study the statistical errors for redshift surveys up to z=3 and report errors on cosmography while marginalizing over a large number of cosmological parameters including a time-dependent equation of state. With redshifts surveys combined with cosmic microwave background satellite data, we achieve errors of 0.037 on Omega_x, 0.10 on w(z=0.8), and 0.28 on dw(z)/dz for cosmological constant model. Models with less negative w(z) permit tighter constraints. We test and discuss the dependence of performance on redshift, survey conditions, and fiducial model. We find results that are competitive with the performance of future supernovae Ia surveys. We conclude that redshift surveys offer a promising independent route to the measurement of dark energy.Comment: submitted to ApJ, 24 pages, LaTe
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