0000000000951578

AUTHOR

L. Mattioni

showing 2 related works from this author

Long Range Bond-Bond Correlations in Dense Polymer Solutions

2004

The scaling of the bond-bond correlation function $C(s)$ along linear polymer chains is investigated with respect to the curvilinear distance, $s$, along the flexible chain and the monomer density, $\rho$, via Monte Carlo and molecular dynamics simulations. % Surprisingly, the correlations in dense three dimensional solutions are found to decay with a power law $C(s) \sim s^{-\omega}$ with $\omega=3/2$ and the exponential behavior commonly assumed is clearly ruled out for long chains. % In semidilute solutions, the density dependent scaling of $C(s) \approx g^{-\omega_0} (s/g)^{-\omega}$ with $\omega_0=2-2\nu=0.824$ ($\nu=0.588$ being Flory's exponent) is set by the number of monomers $g(\r…

chemistry.chemical_classificationPhysicsLinear polymerGeneral Physics and AstronomyFOS: Physical sciences02 engineering and technologyPolymerCondensed Matter - Soft Condensed Matter010402 general chemistry021001 nanoscience & nanotechnology01 natural sciencesPower lawOmega0104 chemical sciencesChemical bondchemistryDensity dependentExponentSoft Condensed Matter (cond-mat.soft)Statistical physicsAtomic physics0210 nano-technologyScaling[PHYS.COND.CM-SCM]Physics [physics]/Condensed Matter [cond-mat]/Soft Condensed Matter [cond-mat.soft]61.25.Hq 05.10.Ln 05.40.Fb
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The Argille Varicolori Unit of Lucania (Italy): a record offscraping and gravity sliding in the Mesozoic-Tertiary Lagonegro Basin, southern Apennines

2006

Detailed geological mapping and new stratigraphic and structural data collected in the Lucania area of the southern Apennines allowed us to assess the deformation history of 11 Monte-Corleto Perticara zone, in the High Agri Valley (Lucanian Apennines, southern Italy) where red and green shales (known as Argille Varicolori or Argille scagliose) crop out. Our observations suggest that: (1) 'chaotic' facies within the Argille Varicolori may be attributed to a broken formation generated by overthrusting of Apenninic Platform units onto already deformed Lagonegro basin strata; (2) gravity sliding phenomena at the thrust front enhanced the development of debris flow and the emplacement of olistos…

Gravity (chemistry)BELTCONSTRAINTSGeologyOcean EngineeringStructural basinEVOLUTIONUnit (housing)MECHANISMSTectonicsPaleontologyMesozoicGeologySeismologyWater Science and Technology
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