Climate impact studies of sediment transport on the Adriatic coastal zone

The study of the impact of climate change on the environment has been based, until very recently, on an global approach, whose interest from a local point of view is very limited. This thesis, on the contrary, has treated the study of the impact of climate change in the Adriatic Sea basin following a twofold strategy of regionalization and integration of numerical models in order to reproduce the present and future scenarios of the system through a more and more realistic and solid approach. In particular the focus of the study was on the impact on the physical environment and on the sediment transport in the basin. This latter is a very new and original issue, to our knowledge still uninvestigated. The study case of the coastal area of Montenegro was particularly studied, since it is characterized by an important supply of sediment through the Buna/Bojana river, second most important in the Adriatic basin in terms of flow. To do this, a methodology to introduce the tidal processes in a baroclinic primitive equations Ocean General Circulation Model was applied and tidal processes were successfully reproduced in the Adriatic Sea, analyzing also the impacts they have on the mean general circulation, on salt and heat transport and on mixing and stratification of the water column in the different seasons of the year. The new hydrodynamical model has been further coupled with a wave model and with a river and sea sediment transport model, showing good results in the reproduction of sediment transport processes. Finally this complex coupled platform was integrated in the period 2001-2030 under the A1B scenario of IPCC, and the impact of climate change on the physical system and on sediment transport was preliminarily evaluated.

Structure of the Southern Tyrrhenian subduction system: insights from seismological analysis of anisotropy and attenuation

The Southern Tyrrhenian subduction system shows a complex interaction among asthenospheric flow, subducting slab and overriding plate. To shed light on the deformations and mechanical properties of the slab and surrounding mantle, I investigated seismic anisotropy and attenuation properties through the subduction region. I used both teleseisms and slab earthquakes, analyzing shear-wave splitting on SKS and S phases, respectively. The fast polarization directions φ, and the delay time, δt, were retrieved using the method of Silver and Chan [1991. SKS and S φ reveal a complex anisotropy pattern across the subduction zone. SKS-rays sample primarily the sub-slab region showing rotation of fast directions following the curved shape of the slab and very strong anisotropy. S-rays sample mainly the slab, showing variable φ and a smaller δt. SKS and S splitting reveals a well developed toroidal flow at SW edge of the slab, while at its NE edge the pattern is not very clear. This suggests that the anisotropy is controlled by the slab rollback, responsible for about 100 km slab parallel φ in the sub-slab mantle. The slab is weakly anisotropic, suggesting the asthenosphere as main source of anisotropy. To investigate the physical properties of the slab and surrounding regions, I analyzed the seismic P and S wave attenuation. By inverting high-quality S-waves t* from slab earthquakes, 3D attenuation models down to 300 km were obtained. Attenuation results image the slab as low-attenuation body, but with heterogeneous QS and QP structure showing spot of high attenuation , between 100-200 km depth, which could be due dehydration associated to the slab metamorphism. A low QS anomaly is present in the mantle wedge beneath the Aeolian volcanic arc and could indicate mantle melting and slab dehydration.

Theoretical studies of microfluidics: "walking" drops and "melting" snowflakes.

The present PhD thesis summarizes two examples of research in microfluidics. Both times water was the subject of interest, once in the liquid state (droplets adsorbed on chemically functionalized surfaces), the other time in the solid state (ice snowflakes and their fractal behaviour). The first problem deals with a slipping nano-droplet of water adsorbed on a surface with photo-switchable wettability characteristics. Main focus was on identifying the underlying driving forces and mechanical principles at the molecular level of detail. Molecular Dynamics simulation was employed as investigative tool owing to its record of successfully describing the microscopic behaviour of liquids at interfaces. To reproduce the specialized surface on which a water droplet can effectively “walk”, a new implicit surface potential was developed. Applying this new method the experimentally observed droplet slippage could be reproduced successfully. Next the movement of the droplet was analyzed at various conditions emphasizing on the behaviour of the water molecules in contact with the surface. The main objective was to identify driving forces and molecular mechanisms underlying the slippage process. The second part of this thesis is concerned with theoretical studies of snowflake melting. In the present work snowflakes are represented by filled von Koch-like fractals of mesoscopic beads. A new algorithm has been developed from scratch to simulate the thermal collapse of fractal structures based on Monte Carlo and Random Walk Simulations (MCRWS). The developed method was applied and compared to Molecular Dynamics simulations regarding the melting of ice snowflake crystals and new parameters were derived from this comparison. Bigger snow-fractals were then studied looking at the time evolution at different temperatures again making use of the developed MCRWS method. This was accompanied by an in-depth analysis of fractal properties (border length and gyration radius) in order to shed light on the dynamics of the melting process.

Le Zone Franche Urbane: Mercato europeo e Ordinamenti tributari

Lo studio delle Zone Franche Urbane all’interno del Diritto tributario europeo non ha potuto prescindere da una introduttiva delimitazione del lavoro, capace di distinguere le diverse tipologie di zone franche esistenti nei Paesi intra/extra Ue. Attraversando i casi-studio di Madeira, delle Azzorre, fino alla istituenda Zona Franca di Bruxelles, Zone d’Economie Urbaine stimulée (ZEUS), si è giunti alla constatazione dell’assenza di una definizione di Zona Franca Urbana: analizzando le esperienze normative vissute in Francia e in Italia, si è potuto tratteggiare il profilo territoriale, soggettivo e oggettivo del sistema agevolativo rivolto al recupero delle aree urbane degradate. La funzione strumentale della fiscalità, esplicitata per mezzo delle ZFU, ha condotto ad una verifica di diritto interno per controllare la legittimità delle scelte nazionali in ragione dei principi costituzionali nazionali, come anche una di diritto europeo per evitare che le scelte nazionali, anche se legittime sul piano interno, possano per gli stessi effetti incentivanti alle attività d'impresa presentarsi come una forma territoriale di aiuti di Stato fiscali. Evidenziando il rapporto tra le ZFU e il Mercato europeo si è voluto, da un lato, effettuare una ricostruzione sistemica necessaria per un’interpretazione delle ZFU che metta in luce le componenti di tale strumento orientate al perseguimento di un interesse socioeconomico, che in prima battuta generi una contraddizione, una deroga ai principi costituzionali e comunitari, per poi “sciogliersi” in una coerente applicazione degli stessi; dall’altro, tentare di elevare le ZFU a misura sistemica dell’Ordinamento europeo. Si è svolto, infine, un ragionamento in termini di federalismo fiscale con riferimento alle ZFU, trovando una adeguata collocazione nel percorso di devoluzione intrapreso dal legislatore nazionale, avendo quali interlocutori privilegiati le Regioni a Statuto Speciale.