Geological and Structural evolution of the Eurasia Africa plate boundary in the Gulf of Cadiz Central Eastern Atlantic Sea.

Iberia Africa plate boundary, cross, roughly W-E, connecting the eastern Atlantic Ocean from Azores triple junction to the Continental margin of Morocco. Relative movement between the two plate change along the boundary, from transtensive near the Azores archipelago, through trascurrent movement in the middle at the Gloria Fracture Zone, to transpressive in the Gulf of Cadiz area. This study presents the results of geophysical and geological analysis on the plate boundary area offshore Gibraltar. The main topic is to clarify the geodynamic evolution of this area from Oligocene to Quaternary. Recent studies have shown that the new plate boundary is represented by a 600 km long set of aligned, dextral trascurrent faults (the SWIM lineaments) connecting the Gloria fault to the Riff orogene. The western termination of these lineaments crosscuts the Gibraltar accretionary prism and seems to reach the Moroccan continental shelf. In the past two years newly acquired bathymetric data collected in the Moroccan offshore permit to enlighten the present position of the eastern portion of the plate boundary, previously thought to be a diffuse plate boundary. The plate boundary evolution, from the onset of compression in the Oligocene to the Late Pliocene activation of trascurrent structures, is not yet well constrained. The review of available seismics lines, gravity and bathymetric data, together with the analysis of new acquired bathymetric and high resolution seismic data offshore Morocco, allows to understand how the deformation acted at lithospheric scale under the compressive regime. Lithospheric folding in the area is suggested, and a new conceptual model is proposed for the propagation of the deformation acting in the brittle crust during this process. Our results show that lithospheric folding, both in oceanic and thinned continental crust, produced large wavelength synclines bounded by short wavelength, top thrust, anticlines. Two of these anticlines are located in the Gulf of Cadiz, and are represented by the Gorringe Ridge and Coral Patch seamounts. Lithospheric folding probably interacted with the Monchique – Madeira hotspot during the 72 Ma to Recent, NNE – SSW transit. Plume related volcanism is for the first time described on top of the Coral Patch seamount, where nine volcanoes are found by means of bathymetric data. 40Ar-39Ar age of 31.4±1.98 Ma are measured from one rock sample of one of these volcanoes. Analysis on biogenic samples show how the Coral Patch act as a starved offshore seamount since the Chattian. We proposed that compression stress formed lithospheric scale structures playing as a reserved lane for the upwelling of mantle material during the hotspot transit. The interaction between lithospheric folding and the hotspot emplacement can be also responsible for the irregularly spacing, and anomalous alignments, of individual islands and seamounts belonging to the Monchique - Madeira hotspot.

Analisi del profilo tossicologico e cancerogeno del particolato atmosferico e identificazione dei rischi per la salute umana correlati all'esposizione

Gli impianti di incenerimento di rifiuti solidi suscitano preoccupazione nella popolazione per i possibili effetti avversi associati all’esposizione. Gli effetti delle polveri sottili (PM2.5), generate dai processi di combustione, sulla salute umana includono l’insorgenza di patologie a carico del sistema respiratorio e cardiovascolare e l’aumento della mortalità per malattie polmonari e probabilmente cancro al polmone. Lo scopo della tesi è quello di valutare il profilo tossicologico e cancerogeno del particolato atmosferico in prossimità dell’inceneritore di Bologna rispetto alle aree adiacenti mediante l’utilizzo di test alternativi alle metodologie in vivo, come il test di trasformazione cellulare e approcci di tossicogenomica (soprattutto trascrittomica) oltre alla valutazione della variazione del rischio cancerogeno indotto dall’esposizione di PM2.5 in diversi siti (massima ricaduta, controllo, fondo urbano e fondo rurale) e in differenti periodi di campionamento (estate 2008 e inverno 2009). Gli estratti di PM2.5 relativi alla stagione invernale sono risultati più tossici rispetto ai campioni estivi, che inducono tossicità soprattutto alle alte dosi. Per i campioni invernali il numero medio di colonie di cellule BALB/c 3T3 A31-1-1 risulta ridotto in modo significativo anche per le dosi più basse saggiate indipendentemente dal sito di provenienza. Tutti i campioni analizzati sono risultati negativi nel test di trasformazione cellulare in vitro. L’analisi dell’espressione genica delle cellule BALB/c 3T3 A31-1-1, in seguito all’esposizione agli estratti di PM2.5, ha mostrato un effetto stagionale evidente. Relativamente ai campioni invernali è stato evidenziato un maggior effetto tossico da parte del sito di controllo rispetto alla massima ricaduta, poiché nel sito di controllo risultano attivati marcatori di morte cellulare per apoptosi. La valutazione del rischio cancerogeno in tutti i siti valutati non mostra situazioni preoccupanti legate alla predizione di eccessi di rischio di tumori imputabili all’attività dell’inceneritore in quanto le stime di rischio non eccedono mai il valore limite riportato in letteratura.

Classical limit of the Nelson model

Since the development of quantum mechanics it has been natural to analyze the connection between classical and quantum mechanical descriptions of physical systems. In particular one should expect that in some sense when quantum mechanical effects becomes negligible the system will behave like it is dictated by classical mechanics. One famous relation between classical and quantum theory is due to Ehrenfest. This result was later developed and put on firm mathematical foundations by Hepp. He proved that matrix elements of bounded functions of quantum observables between suitable coherents states (that depend on Planck's constant h) converge to classical values evolving according to the expected classical equations when h goes to zero. His results were later generalized by Ginibre and Velo to bosonic systems with infinite degrees of freedom and scattering theory. In this thesis we study the classical limit of Nelson model, that describes non relativistic particles, whose evolution is dictated by Schrödinger equation, interacting with a scalar relativistic field, whose evolution is dictated by Klein-Gordon equation, by means of a Yukawa-type potential. The classical limit is a mean field and weak coupling limit. We proved that the transition amplitude of a creation or annihilation operator, between suitable coherent states, converges in the classical limit to the solution of the system of differential equations that describes the classical evolution of the theory. The quantum evolution operator converges to the evolution operator of fluctuations around the classical solution. Transition amplitudes of normal ordered products of creation and annihilation operators between coherent states converge to suitable products of the classical solutions. Transition amplitudes of normal ordered products of creation and annihilation operators between fixed particle states converge to an average of products of classical solutions, corresponding to different initial conditions.