1,632 research outputs found

    Nuclear Structure Functions at Low-xx in a Holographic Approach

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    Nuclear effects in deep inelastic scattering at low−x-x are phenomenologically described changing the typical dynamical and/or kinematical scales characterizing the free nucleon case. In a holographic approach, this rescaling is an analytical property of the computed structure function F2(x,Q2)F_2(x,Q^2). This function is given by the sum of a conformal term and of a contribution due to quark confinement, depending on IR hard-wall parameter z0z_0 and on the mean square distances, related to a parameter Q′Q^\prime, among quarks and gluons in the target. The holographic structure function per nucleon in a nucleus AA is evaluated showing that a rescaling of the typical nucleon size, z0z_0 and Q′Q^\prime, due to nuclear binding, can be reabsorbed in a Q2Q^2-rescaling scheme. The difference between neutron and proton structure functions and the effects of the longitudinal structure functions can also be taken into account. The obtained theoretical results favourably compare with the experimental data.Comment: 10 pages, 10 figure

    The Vector and Axial-Vector Charmonium-like States

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    After constructing all the tetraquark interpolating currents with JPC=1−+,1−−,1++J^{PC}=1^{-+}, 1^{--}, 1^{++} and 1+−1^{+-} in a systematic way, we investigate the two-point correlation functions to extract the masses of the charmonium-like states with QCD sum rule. For the 1−−1^{--} qcqˉcˉqc\bar q\bar c charmonium-like state, mX=4.6∼4.7m_X=4.6\sim4.7 GeV, which implies a possible tetraquark interpretation for the state Y(4660). The masses for both the 1++1^{++} qcqˉcˉqc\bar q\bar c and scsˉcˉsc\bar s\bar c charmonium-like states are around 4.0∼4.24.0\sim 4.2 GeV, which are slightly above the mass of X(3872). For the 1−+1^{-+} qcqˉcˉqc\bar q\bar c charmonium-like state, the extracted mass is 4.5∼4.74.5\sim 4.7 GeV. We also discuss the possible decay modes and experimental search of the 1−+1^{-+} charmonium-like states.Comment: 18 pages, 6 figures and 6 table

    Quarkonium dissociation in a far-from-equilibrium holographic setup

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    The real-time dissociation of the heavy quarkonium in a strongly coupled boost-invariant non-Abelian plasma relaxing towards equilibrium is analyzed in a holographic framework. The effects driving the plasma out of equilibrium are described by boundary quenching, impulsive variations of the boundary metric. Quarkonium is represented by a classical string with endpoints kept close to the boundary. The evolution of the string profile is computed in the time-dependent geometry, and the dissociation time is evaluated for different configurations with respect to the direction of the plasma expansion. Dissociation occurs fastly for the quarkonium placed in the transverse plane.Comment: 14 pages, 8 figures. References added. Matches the published versio

    Vertical dipoles to detect self potential signals in a seismic area of southern Italy: Tito station

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    International audienceSince 2000 the Institute of Methodologies for the Environmental Analysis (National Council of Research, Tito, Italy) installed a geophysical monitoring network able to detect geoelectric, geochemic and seismometric parameters in seismic areas of southern Italy. During this period a very large data-base of geophysical time series has been organized and it is actually available to assess robust statistical methodologies to identify geophysical anomalous patterns linked with local seismicity. To better understand the influence of rain and cultural noise on geoelectrical signals (Self Potential), during May 2004 we drilled in Tito station a 20 m-depth hole to measure the SP vertical component. The array is characterized by five Pb-PbCl2 electrodes put at different depths. The common electrode is fixed at 20 m. In this work we present some electrical anomalies probably correlated with local seismic activity on vertical dipoles recorded in Tito station

    Multifractal variability in geoelectrical signals and correlations with seismicity: a study case in southern Italy

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    International audienceMultifractal fluctuations in the time dynamics of geoelectrical data, recorded in a seismic area of southern Italy, have been revealed using the Multifractal Detrended Fluctuation Analysis (MF-DFA), which allows to detect multifractality in nonstationary signals. Our findings show that the geoelectrical time series, recorded in the seismic area of southern Apennine Chain (Italy), is multifractal. The time evolution of the multifractality suggests that the multifractal degree increases prior the occurrence of earthquakes. This study aims to propose another approach to investigate the complex dynamics of earthquake-related geoelectrical signals

    Strong Interactions at Low Energy

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    The lectures review some of the basic concepts relevant for an understanding of the low energy properties of the strong interactions: chiral symmetry, spontaneous symmetry breakdown, Goldstone bosons, quark condensate. The effective field theory used to analyze the low energy structure is briefly sketched. As an illustration, I discuss the implications of the recent data on the decay K→ππeνK\to \pi\pi e\nu for the magnitude of the quark condensate.Comment: Lectures given at the school of physics "Understanding the structure of hadrons", Prague, July 2001, 20 p
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