2,006 research outputs found

    Non Singular Origin of the Universe and its Present Vacuum Energy Density

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    We consider a non singular origin for the Universe starting from an Einstein static Universe, the so called "emergent universe" scenario, in the framework of a theory which uses two volume elements −gd4x\sqrt{-{g}}d^{4}x and Φd4x\Phi d^{4}x, where Φ\Phi is a metric independent density, used as an additional measure of integration. Also curvature, curvature square terms and for scale invariance a dilaton field ϕ\phi are considered in the action. The first order formalism is applied. The integration of the equations of motion associated with the new measure gives rise to the spontaneous symmetry breaking (S.S.B) of scale invariance (S.I.). After S.S.B. of S.I., it is found that a non trivial potential for the dilaton is generated. In the Einstein frame we also add a cosmological term that parametrizes the zero point fluctuations. The resulting effective potential for the dilaton contains two flat regions, for ϕ→∞\phi \rightarrow \infty relevant for the non singular origin of the Universe, followed by an inflationary phase and ϕ→−∞\phi \rightarrow -\infty, describing our present Universe. The dynamics of the scalar field becomes non linear and these non linearities are instrumental in the stability of some of the emergent universe solutions, which exists for a parameter range of values of the vacuum energy in ϕ→−∞\phi \rightarrow -\infty, which must be positive but not very big, avoiding the extreme fine tuning required to keep the vacuum energy density of the present universe small. Zero vacuum energy density for the present universe defines the threshold for the creation of the universe.Comment: 28 pages, short version of this paper awarded an honorable mention by the Gravity Research Foundation, 2011, accepted for publication in International Journal of Modern Physics

    Sensor electroquímic de clor per a aigües potables

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    El lleixiu, amb el clor que conté, és necessari per a desinfectar l'aigua que prenem, però en dosis elevades podria intoxicar-nos. Per això, és important que les eines que detecten la quantitat de clor en l'aigua siguin fiables. Investigadors del Centre Nacional de Microelectrónica han creat un xip que permet verificar amb exactitud i de manera continuada la quantitat de clor en l'aigua

    Micropatterning of bioactive glass nanoparticles on chitosan membranes for spatial controlled biomineralization

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    [Excerpt] Objectives: Chitosan membranes were patterned with bioactive glass nanoparticles (BG-NPs) capable of bone regeneration by a Microcontact Printing technique, in order to spatially control biomineralization and also cell adhesion and proliferation. [...

    Caminando por sistemas productivos rentables

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    En la presente comunicación se analizan diferentes aspectos del suelo, sus características, la relación con el clima y las estrategias de producción agrícola para un mejor uso de los recursos.Trabajo galardonado con el Premio "Ing. Agr. Antonio J. Prego",Academia Nacional de Agronomía y Veterinaria (ANAV

    Caminando por sistemas productivos rentables

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    En la presente comunicación se analizan diferentes aspectos del suelo, sus características, la relación con el clima y las estrategias de producción agrícola para un mejor uso de los recursos.Trabajo galardonado con el Premio "Ing. Agr. Antonio J. Prego",Academia Nacional de Agronomía y Veterinaria (ANAV

    Shortcuts to adiabaticity in a time-dependent box

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    A method is proposed to drive an ultrafast non-adiabatic dynamics of an ultracold gas trapped in a box potential. The resulting state is free from spurious excitations associated with the breakdown of adiabaticity, and preserves the quantum correlations of the initial state up to a scaling factor. The process relies on the existence of an adiabatic invariant and the inversion of the dynamical self-similar scaling law dictated by it. Its physical implementation generally requires the use of an auxiliary expulsive potential analogous to those used in soliton control. The method is extended to a broad family of many-body systems. As illustrative examples we consider the ultrafast expansion of a Tonks-Girardeau gas and of Bose-Einstein condensates in different dimensions, where the method exhibits an excellent robustness against different regimes of interactions and the features of an experimentally realizable box potential.Comment: 6 pp, 4 figures, typo in Eq. (6) fixe

    Emerging Universe from Scale Invariance

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    We consider a scale invariant model which includes a R2R^{2} term in action and show that a stable "emerging universe" scenario is possible. The model belongs to the general class of theories, where an integration measure independent of the metric is introduced. To implement scale invariance (S.I.), a dilaton field is introduced. The integration of the equations of motion associated with the new measure gives rise to the spontaneous symmetry breaking (S.S.B) of S.I. After S.S.B. of S.I. in the model with the R2R^{2} term (and first order formalism applied), it is found that a non trivial potential for the dilaton is generated. The dynamics of the scalar field becomes non linear and these non linearities are instrumental in the stability of some of the emerging universe solutions, which exists for a parameter range of the theory.Comment: 21 pages, 4 figures. Accepted for publication in JCA

    SEM and TEM evidence of mixed-layer illite-smectite formed by dissolutioncrystallization processes in continental Paleogene sequences in northwestern Argentina

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    In the northernmost Calchaquí Valley (Salta, Argentina), the Paleogene continental sediments show a transition from smectite, at the top, to R3 I-S (>90% illite) through R1 I-S (65–80% illite), in contrast to the remaining sectors, containing smectite up to the bottom. Samples at the base of the succession were characterized by high-quality step-scan X-ray diffraction (XRD), scanning electron microscopy (SEM) and analytical high-resolution transmission electron microscopy (HRTEM). Analysis by SEM demonstrated dissolution of primary phases (feldspars, micas and quartz) and crystallization of illite, I-S and kaolinite. As this alteration is not pervasive, an intermediate fluid/rock ratio could be inferred. The lattice-fringe images of the samples from upper parts of the sequence show abundant I1-rich areas, whereas in the lower parts of the sequence, illite packets and I3 I-S coexist and compositions evolve towards muscovite (tetrahedral-charge increase, principally compensated by Mgby-Al substitution in octahedral sites and by a slight decrease in Ca in interlayer sites). As burial temperatures were probably similar in all the samples, depth was not responsible for the illite formation at the bottom. The TEM textures suggest that illitization proceeded mainly by dissolution-crystallization. The active faults close to the northern Calchaquí Valley probably promoted the circulation of hot, deep fluids, favouring illitization
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