58,868 research outputs found

    Homogeneous SPC/E water nucleation in large molecular dynamics simulations

    Get PDF
    We perform direct large molecular dynamics simulations of homogeneous SPC/E water nucleation, using up to 4106\sim 4\cdot 10^6 molecules. Our large system sizes allow us to measure extremely low and accurate nucleation rates, down to 1019cm3s1\sim 10^{19}\,\textrm{cm}^{-3}\textrm{s}^{-1}, helping close the gap between experimentally measured rates 1017cm3s1\sim 10^{17}\,\textrm{cm}^{-3}\textrm{s}^{-1}. We are also able to precisely measure size distributions, sticking efficiencies, cluster temperatures, and cluster internal densities. We introduce a new functional form to implement the Yasuoka-Matsumoto nucleation rate measurement technique (threshold method). Comparison to nucleation models shows that classical nucleation theory over-estimates nucleation rates by a few orders of magnitude. The semi-phenomenological nucleation model does better, under-predicting rates by at worst, a factor of 24. Unlike what has been observed in Lennard-Jones simulations, post-critical clusters have temperatures consistent with the run average temperature. Also, we observe that post-critical clusters have densities very slightly higher, 5%\sim 5\%, than bulk liquid. We re-calibrate a Hale-type JJ vs. SS scaling relation using both experimental and simulation data, finding remarkable consistency in over 3030 orders of magnitude in the nucleation rate range, and 180180\,K in the temperature range.Comment: Accepted for publication in the Journal of Chemical Physic

    Synchrotron X-ray emission from old pulsars

    Full text link
    We study the synchrotron radiation as the observed non-thermal X-ray emission from old pulsars (110\gtrsim1-10Myr) to investigate the particle acceleration in their magnetospheres. We assume that the power-law component of the observed X-ray spectra is caused by the synchrotron radiation from electrons and positrons in the magnetosphere. We consider two pair production mechanisms of X-ray emitting particles, the magnetic and the photon-photon pair productions. High-energy photons, which ignite the pair production, are emitted via the curvature radiation of the accelerated particles. We use the analytical description for the radiative transfer and estimate the luminosity of the synchrotron radiation. We find that for pulsars with the spin-down luminosity Lsd1033L_{\rm sd}\lesssim10^{33} erg s1^{-1}, the locations of the particle acceleration and the non-thermal X-ray emission are within 107\lesssim10^7cm from the centre of the neutron star, where the magnetic pair production occurs. For pulsars with the spin-down luminosity Lsd1031L_{\rm sd}\lesssim10^{31} erg s1^{-1} such as J0108-1431, the synchrotron radiation is difficult to explain the observed non-thermal component even if we consider the existence of the strong and small-scale surface magnetic field structures.Comment: 25 pages, 7 figures, 2 tables, accepted for publication in MNRA

    Loopy belief propagation and probabilistic image processing

    Get PDF
    Estimation of hyperparameters by maximization of the marginal likelihood in probabilistic image processing is investigated by using the cluster variation method. The algorithms are substantially equivalent to generalized loopy belief propagation

    Absorption spectrum of (H2O)-O-18 in the range 12 400-14 520 cm(-1)

    Get PDF
    Fourier transform spectra recorded using (a) natural abundance water vapor, (b) (H2O)-O-18-enriched water vapor, and (c) (H2O)-O-17-enriched water vapor are analyzed. The ratio of intensities in three spectra is used to identify 927 lines due to absorption by (H2O)-O-18. Intensities and self-broadening parameters are derived for these lines. Using theoretical linelists, comparisons with previously assigned (H2O)-O-16 spectra, and automatic searches for combination differences, 747 lines are assigned. These lines belong to 14 vibrational states in the 3nu + delta and 4nu polyads. Newly determined (H2O)-O-18 vibrational band origins include 4nu(1) at 13 793.09 cm(-1), 3nu(1) + nu(3) at 13 795.40 cm(-1), 2nu(1) + 2nu(3) at 14 188.82 cm(-1), nu(1) + 3nu(3) at 14 276.34 cm(-1), and 2nu(2) + 2nu(2) + nu(3) at 13 612.71 cm(-1). These results are compared with data in HITRAN. (C) 2002 Elsevier Science (USA)
    corecore