2,377 research outputs found

    Studies of charmed baryons at LHCb

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    We report a search for the doubly charmed baryon Ξcc+\Xi_{cc}^{+} through the decay Ξcc+→Λc+K−π+\Xi_{cc}^{+} \to \Lambda_{c}^{+} K^{-} \pi^{+}, using a data sample corresponding to an integrated luminosity of 0.65 pb−10.65~\mathrm{pb^{-1}} of pppp collisions at s=7 TeV\mathrm{\sqrt{s}} = 7~\mathrm{TeV}. In the mass range 3300-3800 MeV/c2~\mathrm{MeV}/c^{2} no significant signal is observed. Upper limits at 95%95\% confidence level are set on RR, the ratio of the production cross section of the Ξcc+\Xi_{cc}^{+} times the relevant branching fraction over the Λc+\Lambda_{c}^{+} cross section, as a function of the Ξcc+\Xi_{cc}^{+} mass and lifetime. The largest upper limits on RR over the investigated mass range are R<1.5×10−2R<1.5\times10^{-2} for a lifetime of 100 fs100~\mathrm{fs} and R<3.9×10−4R<3.9\times10^{-4} for a lifetime of 400 fs400~\mathrm{fs}.Comment: Article to appear in the proceedings of The 6th International Workshop on Charm Physics (CHARM 2013

    Characterising sand and gravel deposits using electrical resistivity tomography (ERT) : case histories from England and Wales

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    Electrical Resistivity Tomography (ERT) is a rapidly developing geophysical imaging technique that is now widely used to visualise subsurface geological structure, groundwater and lithological variations. It is being increasingly used in environmental and engineering site investigations, but despite its suitability and potential benefits, ERT has yet to be routinely applied by the minerals industry to sand and gravel deposit assessment and quarry planning. The principal advantages of ERT for this application are that it is a cost-effective non-invasive method, which can provide 2D or 3D spatial models of the subsurface throughout the full region of interest. This complements intrusive sampling methods, which typically provide information only at discrete locations. Provided that suitable resistivity contrasts are present, ERT has the potential to reveal mineral and overburden thickness and quality variations within the body of the deposit. Here we present a number of case studies from the UK illustrating the use of 2D and 3D ERT for sand and gravel deposit investigation in a variety of geological settings. We use these case studies to evaluate the performance of ERT, and to illustrate good practice in the application of ERT to deposit investigation. We propose an integrated approach to site investigation and quarry planning incorporating both conventional intrusive methods and ERT

    Seismic topographic scattering in the context of GW detector site selection

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    In this paper, we present a calculation of seismic scattering from irregular surface topography in the Born approximation. Based on US-wide topographic data, we investigate topographic scattering at specific sites to demonstrate its impact on Newtonian-noise estimation and subtraction for future gravitational-wave detectors. We find that topographic scattering at a comparatively flat site in Oregon would not pose any problems, whereas scattering at a second site in Montana leads to significant broadening of wave amplitudes in wavenumber space that would make Newtonian-noise subtraction very challenging. Therefore, it is shown that topographic scattering should be included as criterion in the site-selection process of future low-frequency gravitational-wave detectors.Comment: 16 pages, 7 figure

    Fourier, Gauss, Fraunhofer, Porod and the Shape from Moments Problem

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    We show how the Fourier transform of a shape in any number of dimensions can be simplified using Gauss's law and evaluated explicitly for polygons in two dimensions, polyhedra three dimensions, etc. We also show how this combination of Fourier and Gauss can be related to numerous classical problems in physics and mathematics. Examples include Fraunhofer diffraction patterns, Porods law, Hopfs Umlaufsatz, the isoperimetric inequality and Didos problem. We also use this approach to provide an alternative derivation of Davis's extension of the Motzkin-Schoenberg formula to polygons in the complex plane.Comment: 21 pages, no figure
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