988 resultados para Salina, Monte dei Porri, Stratigrafia, Petrografia, Geochimica


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ic first-order transition line ending in a critical point. This critical point is responsible for the existence of large premartensitic fluctuations which manifest as broad peaks in the specific heat, not always associated with a true phase transition. The main conclusion is that premartensitic effects result from the interplay between the softness of the anomalous phonon driving the modulation and the magnetoelastic coupling. In particular, the premartensitic transition occurs when such coupling is strong enough to freeze the involved mode phonon. The implication of the results in relation to the available experimental data is discussed.

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Ordering in a binary alloy is studied by means of a molecular-dynamics (MD) algorithm which allows to reach the domain growth regime. Results are compared with Monte Carlo simulations using a realistic vacancy-atom (MC-VA) mechanism. At low temperatures fast growth with a dynamical exponent x>1/2 is found for MD and MC-VA. The study of a nonequilibrium ordering process with the two methods shows the importance of the nonhomogeneity of the excitations in the system for determining its macroscopic kinetics.

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A Monte Carlo procedure to simulate the penetration and energy loss of low¿energy electron beams through solids is presented. Elastic collisions are described by using the method of partial waves for the screened Coulomb field of the nucleus. The atomic charge density is approximated by an analytical expression with parameters determined from the Dirac¿Hartree¿Fock¿Slater self¿consistent density obtained under Wigner¿Seitz boundary conditions in order to account for solid¿state effects; exchange effects are also accounted for by an energy¿dependent local correction. Elastic differential cross sections are then easily computed by combining the WKB and Born approximations to evaluate the phase shifts. Inelastic collisions are treated on the basis of a generalized oscillator strength model which gives inelastic mean free paths and stopping powers in good agreement with experimental data. This scattering model is accurate in the energy range from a few hundred eV up to about 50 keV. The reliability of the simulation method is analyzed by comparing simulation results and experimental data from backscattering and transmission measurements.

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Monte Carlo calculations of the isothermal elastic constants of the beta-CuxZn1-x alloy system as a function of the composition have been carried out. We assume the atoms interact via a two-body Morse potential function and use numerical values for the potential parameters evaluated taking into account experimental data. We find a quite good agreement between our results and the expected experimental behavior.

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O uso de água salina na irrigação torna-se importante alternativa diante daescassez de água de boa qualidade em todo o mundo. O pinhão-manso (Jatropha curcas L.) possui baixa exigência hídrica, sobrevive e apresenta produção satisfatória em solos de baixa fertilidade. No entanto, a sua produção é maior em cultivos irrigados, o que reforça a necessidade de desenvolvimento de pesquisas para uso de água salina. Este trabalho objetivou avaliar o efeito de diferentes níveis de salinidade da água de irrigação nas características morfofisiológicas de mudas de pinhão-manso. Para isso, foi conduzido experimento em casa de vegetação com interceptação de 50 % da radiação solar, localizada na Universidade Estadual de Goiás, Ipameri, Goiás. O experimento foi conduzido em vasos com capacidade de 4 L de solo, utilizando-se o delineamento inteiramente casualizado, com quatro tratamentos e cinco repetições. As plantas foram irrigadas diariamente com 150 mL de água não salina, durante os 30 primeiros dias após a germinação das sementes. Do 31º ao 50º dia, as plantas foram submetidas a quatro tratamentos: plantas diariamente irrigadas com água de condutividade elétrica igual a 0,5; 8; 16 e 24 dS m-1. Aos 50 dias após a germinação, analisaram-se as seguintes características nas mudas de pinhão-manso: número de folhas; altura de planta; diâmetro de ramo; teor relativo de água; área foliar; clorofila total; razões de massa radicular, massa caulinar, massa foliar e parte aérea/sistema radicular; e biomassa total. Os resultados evidenciaram que as mudas de pinhão-manso irrigadas com água de condutividade elétrica 8 dS m-1 não apresentaram redução do crescimento vegetativo. Todavia, a água de irrigação com condutividade elétrica 16 dS m-1 causou redução no crescimento vegetativo e elevou a senescência e abscisão foliar. Água com condutividade elétrica elétrica de pinhão-manso na fase de mudas.

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The Monte San Giorgio (Southern Alps, Ticino, Switzerland) is the most important locality in the world for vertebrates dating back to the Middle Triassic. For this reason it was registered in 2003 as a UNESCO World Heritage Site. One of the objectives of this doctoral thesis was to fill some of the cognitive gaps regarding the Ladinian succession, including in particular the San Giorgio Dolomite and the Meride Limestone. In order to achieve this, the entire succession, more than 600 metres thick, was measured and sampled. Biostratigraphic research based on new finds of fossil invertebrates and microfossils and on the palynological analysis of the entire section was integrated with single-zircon U-Pb dating of volcanic ash layers intercalated in the carbonate succession. This enabled a redefinition of the bio-chronostratigraphic and geochronologic framework of the succession, which encompasses a significantly shorter time interval than previously held. The Ladinian section extends from the E. curionii Ammonoid Zone (Early Fassanian) to the P. archelaus Ammonoid Zone (Early Longobardian). The age of the classic fossiliferous levels of the Meride Limestone, rich in organic matter and containing vertebrate fossils which are known all over the world, was defined in both biostratigraphic and geochronologic terms. The presumed stratigraphie significance of the pachypleurosaurid reptiles found in such levels is called into question by new finds. These fossiliferous horizons were found to correspond to the main volcanoclastic intervals of the Buchenstein Formation (Middle and Upper Pietra Verde). Thus, a correlation with the Bagolino Section (Italy) containing the GSSP for the base of the Ladinian was proposed. Bulk sedimentation rates in the studied succession average 200 m/Myr and therefore prove to be 20 times higher than those of the South-Alpine pelagic basins. These values express high carbonate productivity from the surrounding platforms on one hand, and on the other a marked subsidence of the basin. Only in the intervals consisting of laminated limestones did the sedimentation rates drop to average values of around 30 m/Myr. The distribution of organic and inorganic facies appears to be the consequence of relative variations in sea-level. The laminated and organic-matter- rich intervals of the Meride Limestone are linked to a relative sea-level drop which favoured dysoxic to anoxic bottom-water conditions, coupled with an increase in runoff, perhaps due to recurrent explosive volcanic activity. The transient development under dysoxic conditions of monospecific benthic meio-/macrofaunas was documented. Organic matter suggests a predominant origin due to benthic bacterial activity, as can be witnessed in alveolar structures typical of exopolymeric substances secreted by bacteria within microbial mats. A microbial contribution to the carbonate (peloidal) precipitation was documented. The protective effect exerted by these microbial mats is also indicated as the main taphonomic factor contributing to the excellent preservation of vertebrate fossils. A radiolarian assemblage discovered in the lower part of the section (earliest Ladinian, E. curionii Zone) suggests the transient existence of open-marine but not deep-water connections with the tethyan pelagic basins. It shows marked similarities to the faunas typical of the late Anisian, suggesting therefore a low resolution power provided by radiolarian biostratigraphy in recognizing the Anisian/Ladinian boundary. The present thesis describes a new species of conifer (Elatocladus cassinae), a new species of insect (Dasyleptus triassicus) and seven new species of radiolarians (Eptingium danieli, Eptingium neriae, Parentactinosphaera eoladinica, Sepsagon ticinensis, Sepsagon? valporinae, Novamuria wirzi and Pessagnollum? hexaspinosum). In addition, following revision of the type material of already existent taxa, four new genera of radiolarians are introduced: Bernoulliella, Eohexastylus, Ticinosphaera and Lahmosphaera.

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We study the analytical solution of the Monte Carlo dynamics in the spherical Sherrington-Kirkpatrick model using the technique of the generating function. Explicit solutions for one-time observables (like the energy) and two-time observables (like the correlation and response function) are obtained. We show that the crucial quantity which governs the dynamics is the acceptance rate. At zero temperature, an adiabatic approximation reveals that the relaxational behavior of the model corresponds to that of a single harmonic oscillator with an effective renormalized mass.

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CoFe-Ag-Cu granular films, prepared by rf sputtering, displayed magnetic domain microstructures for ferromagnetic concentrations above about 32% at, and below the percolation threshold. All samples have a fcc structure with an (111) texture perpendicular to the film plane. Magnetic force microscopy (MFM) showed a variety of magnetic domain microstructures, extremely sensitive to the magnetic history of the sample, which arise from the balance of the ferromagnetic exchange, the dipolar interactions and perpendicular magnetocrystalline anisotropy, MFM images indicate that in virgin samples, magnetic bubble domains with an out-of-plane component of the magnetization are surrounded by a quasicontinuous background of opposite magnetization domains. The application of a magnetic field in different geometries drastically modifies the microstructure of the system in the remanent state: i) for an in-plane field, the MFM images show that most of the magnetic moments are aligned along the film plane, ii) for an out-of-plane field, the MFM signal increases about one order of magnitude, and out-of-plane striped domains with alternating up and down magnetization are stabilized. Numerical simulations show that a variety of metastable domain structures (similar to those observed experimentally) can be reached, depending on magnetic history, in systems with competing perpendicular anisotropy, exchange and dipolar interactions.

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A general scheme for devising efficient cluster dynamics proposed in a previous paper [Phys. Rev. Lett. 72, 1541 (1994)] is extensively discussed. In particular, the strong connection among equilibrium properties of clusters and dynamic properties as the correlation time for magnetization is emphasized. The general scheme is applied to a number of frustrated spin models and the results discussed.

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Atribution as a function of the time are analyzed and this study leads to a deeper knowledge of the microscopic processes involved in the magnetic relaxation

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Monte Carlo simulations of a model for gamma-Fe2O3 (maghemite) single particle of spherical shape are presented aiming at the elucidation of the specific role played by the finite size and the surface on the anomalous magnetic behavior observed in small particle systems at low temperature. The influence of the finite-size effects on the equilibrium properties of extensive magnitudes, field coolings, and hysteresis loops is studied and compared to the results for periodic boundaries. It is shown that for the smallest sizes the thermal demagnetization of the surface completely dominates the magnetization while the behavior of the core is similar to that of the periodic boundary case, independently of D. The change in shape of the hysteresis loops with D demonstrates that the reversal mode is strongly influenced by the presence of broken links and disorder at the surface

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Résumé II lavoro verte sui volgarizzamenti quattro-cinquecenteschi di Luciano di Samosata, importante capitolo nella fortuna dell'autore greco, che diede l'avvio a quel vasto fenomeno chiamato "lucianesimo", esteso in Europa fino al XIX sec. In particolare fornisco l'edizione critica e commentata delle Storie vere volgarizzate, contenute nella prima, assai ampia (41 opuscoli), e per molto tempo unica, silloge lucianea in volgare, che ho datato a poco prima del 1480. Essa ci è giunta tramite un unico manoscritto, il Vaticano Chigiano L.VI.215, confezionato a Ferrara per Ercole I d'Este, nonché in almeno otto edizioni veneziane apparse fra il 1525 e il 1551. La princeps, da cui dipendono in vario modo tutte le edizioni successive, è pubblicata da Niccolò Zoppino. I1 ms. e le prime due edizioni (1525; 1527 Bindoni e Pasini) tacciono il nome del traduttore, che compare solo nell'edizione del 1529 (Zoppino): Niccolò Leoniceno (1428-1524), medico umanista e valente grecista, attivo a Ferrara dal 1464 al 1524, studioso e traduttore di Ippocrate e Galeno, editore di Aristotele e volgarizzatore di storici per Ercole d'Este. L'edizione ha richiesto uno studio preliminare sulle numerose traduzioni in latino e in volgare di Luciano, per valutare meglio le modalità della sua fortuna umanistica. Confrontando ms. e stampe, per le Storie vere si hanno due volgarizzamenti totalmente diversi, fin dal titolo: La vera historia nel ms., Le vere narrazioni nelle cinquecentine. Ma per l'ultimo quarto di testo, ms. e stampe in sostanza coincidono. La collazione ha coinvolto anche il testo greco (con gli apparati delle edizioni critiche) e la versione latina dell'umanista umbro Lilio Tifernate (1417/18-1486) risalente al 1439-43 ca., intitolata De veris narrationibus, di cui si hanno almeno tre redazioni d'autore; una quarta è invece dovuta probabilmente a Benedetto Bordon, che la inserì nella sua silloge latina di Luciano del 1494. Ho cosa stabilito che il volgarizzamento del ms. Chigiano, La vera historia, è stato eseguito direttamente dal greco, fatto eccezionale nel panorama delle traduzioni umanistiche, mentre quello a stampa, Le vere narrazioni, deriva dalla redazione Bordon del De veris narrationibus. La diversità dei titoli dipende dalle varianti dei codici greci utilizzati dai traduttori: il Vat. gr. 1323, o una sua copia, è utilizzato sia dal volgarizzatore del Chigiano, sia da Bordon, indipendentemente l'uno dall'altro; il Marc. gr. 434, o una sua copia, dal Tifernate. Il titolo latino mantenuto da Bordon risale al Tifernate. Per quanto riguarda l'attribuzione dei due volgarizzamenti, come già per altri due testi della silloge da me studiati (Lucio 01 Asino e Timone), anche per La vera historia del Chigiano è accettabile il nome di Niccolò Leoniceno, poiché: 1) essa è tradotta direttamente dal greco, correttamente e con buona resa in volgare, 2) Paolo Giovio -che conobbe di persona il Leoniceno -, negli Elogia veris clarorum virorum imaginibus apposita ricorda che i volgarizzamenti di Luciano e di Dione eseguiti dal Leoniceno piacquero molto ad Ercole d'Este, 3) nessuno nella prima metà del sec. XVI rivendica, per sé o per un suo maestro, il volgarizzamento di Luciano. Le vere narrazioni a stampa, tradotte dal latino del Bordon, dopo il 1494 e prima del 1525, per la parte che diverge dalla Vera historia rimangono invece anonime. Dato che si tratta di due volgarizzamenti distinti, ho allestito l'edizione a fronte dei due testi fin dove essi divergono, seguendo per l'uno il ms., per l'altro la princeps; per la parte finale, in cui confluiscono, mi baso invece sul manoscritto e relego in apparato le varianti più vistose della princeps (non è emerso un chiaro rapporto di dipendenza fra i due testimoni). Oltre all'apparato critico con le lezioni rifiutate, fornisco un commento con la giustificazione delle scelte e il confronto con i corrispondenti passi greci e latini.