19,550 research outputs found

    Two-component model for the chemical evolution of the Galactic disk

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    In the present paper, we introduce a two-component model of the Galactic disk to investigate its chemical evolution. The formation of the thick and thin disks occur in two main accretion episodes with both infall rates to be Gaussian. Both the pre-thin and post-thin scenarios for the formation of the Galactic disk are considered. The best-fitting is obtained through χ2\chi^2-test between the models and the new observed metallicity distribution function of G dwarfs in the solar neighbourhood (Hou et al 1998). Our results show that post-thin disk scenario for the formation of the Galactic disk should be preferred. Still, other comparison between model predictions and observations are given.Comment: 23 pages, 7 figure

    Momentum Distribution of Near-Zero-Energy Photoelectrons in the Strong-Field Tunneling Ionization in the Long Wavelength Limit

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    We investigate the ionization dynamics of Argon atoms irradiated by an ultrashort intense laser of a wavelength up to 3100 nm, addressing the momentum distribution of the photoelectrons with near-zero-energy. We find a surprising accumulation in the momentum distribution corresponding to meV energy and a \textquotedblleft V"-like structure at the slightly larger transverse momenta. Semiclassical simulations indicate the crucial role of the Coulomb attraction between the escaping electron and the remaining ion at extremely large distance. Tracing back classical trajectories, we find the tunneling electrons born in a certain window of the field phase and transverse velocity are responsible for the striking accumulation. Our theoretical results are consistent with recent meV-resolved high-precision measurements.Comment: 5 pages, 4 figure

    NMR Search for the Spin Nematic State in LaFeAsO Single Crystal

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    We report a 75-As single crystal NMR investigation of LaFeAsO, the parent phase of a pnictide high Tc superconductor. We demonstrate that spin dynamics develop a strong two-fold anisotropy within each orthorhombic domain below the tetragonal-orthorhombic structural phase transition at T[TO]~156 K. This intermediate state with a dynamical breaking of the rotational symmetry freezes progressively into a spin density wave (SDW) below T[SDW]~142 K. Our findings are consistent with the presence of a spin nematic state below T[TO] with an incipient magnetic order.Comment: Revised manuscript accepted for publication in Phys. Rev. Let

    Contributions of biomass/biofuel burning to organic aerosols and particulate matter in Tanzania, East Africa, based on analyses of ionic species, organic and elemental carbon, levoglucosan and mannosan

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    Atmospheric aerosol samples of PM<sub>2.5</sub> and PM<sub>10</sub> were collected at a rural site in Tanzania, East Africa, in 2011 during wet and dry seasons and were analysed for carbonaceous components, levoglucosan, mannosan and water-soluble inorganic ions. The contributions of biomass/biofuel burning to the organic carbon (OC) and particulate matter (PM) mass were estimated to be 46&ndash;52% and 87&ndash;13%, respectively. The mean mass concentrations of PM<sub>2.5</sub> and PM<sub>10</sub> were 28 ± 6 μg m<sup>−3</sup> and 47 ± 8 μg m<sup>−3</sup> in wet season, and 39 ± 10 μg m<sup>−3</sup> and 61 ± 19 μg m<sup>−3</sup> in dry season, respectively. Total carbon (TC) accounted for 16&ndash;19% of the PM<sub>2.5</sub> mass and 13&ndash;15% of the PM<sub>10</sub> mass. On average, 86 to 89% of TC in PM<sub>2.5</sub> and 87 to 90% of TC in PM<sub>10</sub> was OC, of which 67&ndash;72% and 63% was found to be water-soluble organic carbon (WSOC) in PM<sub>2.5</sub> and PM<sub>10</sub>, respectively. We found that concentrations of levoglucosan and mannosan (specific organic tracers of pyrolysis of cellulose) well correlated with non-sea-salt potassium (nss-K<sup>+</sup>) (<i>r</i><sup>2</sup> = 0.56&ndash;0.75), OC (<i>r</i><sup>2</sup> = 0.75&ndash;0.96) and WSOC (<i>r</i><sup>2</sup> = 0.52&ndash;0.78). The K<sup>+</sup> / OC ratios varied from 0.06 to 0.36 in PM<sub>2.5</sub> and from 0.03 to 0.36 in PM<sub>10</sub> with slightly higher ratios in dry season. Mean percent ratios of levoglucosan and mannosan to OC were found to be 3&ndash;4% for PM<sub>2.5</sub> and PM<sub>10</sub> in both seasons. We found lower levoglucosan / K<sup>+</sup> ratios and higher K<sup>+</sup> / EC (elemental carbon) ratios in the biomass-burning aerosols from Tanzania than those reported from other regions. This feature is consistent with the high levels of potassium reported in the soils of Morogoro, Tanzania, suggesting an importance of direct emission of potassium by soil resuspension although K<sup>+</sup> is present mostly in fine particles. It is also likely that biomass burning of vegetation of Tanzania emits high levels of potassium that may be enriched in plant tissues. The present study demonstrates that emissions from mixed biomass- and biofuel-burning activities largely influence the air quality in Tanzania
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