La città e i consumi. Consumi e trasformazioni urbane a Bologna tra anni '50 e '70

Il primo capitolo di questo lavoro è dedicato all’opera svolta dagli amministratori locali e da un ente governativo come la Camera di commercio per arrivare a decifrare le effettive caratteristiche del quadro locale dal punto di vista economico, sociale, della percezione e del significato che assumono i consumi e gli spazi urbani ad essi dedicati. La caratteristica più originale rilevata dagli amministratori (che contano tra le proprie fila studiosi come Ardigò, Zangheri e Bellettini) è quella di una notevole omogeneità politica e culturale del quadro sociale. E questo, nonostante le massicce immigrazioni che sono, in proporzione, seconde solo quelle di Milano, ma per la stragrande maggioranza provenienti dalla stessa provincia o, al massimo, dalla regione e da analoghi percorsi di socializzazione e di formazione. Fondando essenzialmente su questa omogeneità (capitolo secondo), gli enti bolognesi cercarono di governare la trasformazione della città e anche l’espansione dei consumi che appariva colpita da eccessi e distorsioni. Facendo leva sulle pesanti crisi del 1963-1965 e del 1973-1977, gli amministratori locali puntarono ad ottenere la propria legittimazione fondandola proprio sui consumi, sulla base di una precisa cognizione del nuovo che arrivava, ma schierandosi decisamente a contenerne gli effetti dirompenti sul tessuto locale e indirizzando gli sforzi acquisitivi dei bolognesi sulla base di una temperante razionalizzazione nutrita di pianificazione urbanistica. Ritardi, spinte dal basso, ostacoli burocratici e legislativi resero questi percorsi difficili, o comunque assai poco lineari; fino a che l’ingresso negli anni Ottanta non ne modificò sensibilmente il corso. Ma questo, allo stato attuale delle conoscenze, è già tema per nuova ricerca. Il terzo capitolo è dedicato alla visualizzazione cartografica (GIS) dell’espansione degli spazi commerciali urbani durante le fasi più significative del miracolo.

Il Senato come camera di rappresentanza territoriale

La riforma del bicameralismo rappresenta nell’ordinamento italiano una delle tematiche più dibattute sin dalla “concessione” dello Statuto Albertino. In Assemblea Costituente, infatti, l’opzione tra monocamerali e bicameralismo - prima - e il dibattito su che tipo di bicameralismo si sarebbe dovuto adottare - poi - hanno dato vita ad una parte organizzativa particolarmente debole e in gran parte antiquata rispetto alle esigenze della prima parte della Costituzione che, al contrario, ha rappresentato il precipitato di una profonda consonanza di ideali. La tesi si propone dunque l’obiettivo di dimostrare che l’esigenza di procedere ad una riforma del sistema bicamerale in Italia sia oggi quanto mai attuale e necessaria. Da un lato, infatti, essa favorirebbe il superamento delle inefficienze del sistema parlamentare e potrebbe rappresentare uno strumento per ovviare alla debole razionalizzazione della forma di governo che, da sempre, ha determinato la strutturale instabilità degli esecutivi. Dall’altro lato, la riforma servirebbe soprattutto a realizzare quella connessione organica tra Stato e regioni necessaria per completare il disegno regionalistico che si ricava dalla Costituzione stessa. Esigenza questa che, peraltro, si è notevolmente rafforzata con la riforma del titolo V della Costituzione, la cui portata innovativa è stata sostanzialmente svuotata di contenuto a causa delle difficoltà che si sono incontrate nella sua attuazione.

Numerical simulations of magma chamber dynamics at Campi Flegrei, and associated seismicity, deformation and gravity changes

Understanding the complex relationships between quantities measured by volcanic monitoring network and shallow magma processes is a crucial headway for the comprehension of volcanic processes and a more realistic evaluation of the associated hazard. This question is very relevant at Campi Flegrei, a volcanic quiescent caldera immediately north-west of Napoli (Italy). The system activity shows a high fumarole release and periodic ground slow movement (bradyseism) with high seismicity. This activity, with the high people density and the presence of military and industrial buildings, makes Campi Flegrei one of the areas with higher volcanic hazard in the world. In such a context my thesis has been focused on magma dynamics due to the refilling of shallow magma chambers, and on the geophysical signals detectable by seismic, deformative and gravimetric monitoring networks that are associated with this phenomenologies. Indeed, the refilling of magma chambers is a process frequently occurring just before a volcanic eruption; therefore, the faculty of identifying this dynamics by means of recorded signal analysis is important to evaluate the short term volcanic hazard. The space-time evolution of dynamics due to injection of new magma in the magma chamber has been studied performing numerical simulations with, and implementing additional features in, the code GALES (Longo et al., 2006), recently developed and still on the upgrade at the Istituto Nazionale di Geofisica e Vulcanologia in Pisa (Italy). GALES is a finite element code based on a physico-mathematical two dimensional, transient model able to treat fluids as multiphase homogeneous mixtures, compressible to incompressible. The fundamental equations of mass, momentum and energy balance are discretised both in time and space using the Galerkin Least-Squares and discontinuity-capturing stabilisation technique. The physical properties of the mixture are computed as a function of local conditions of magma composition, pressure and temperature.The model features enable to study a broad range of phenomenologies characterizing pre and sin-eruptive magma dynamics in a wide domain from the volcanic crater to deep magma feeding zones. The study of displacement field associated with the simulated fluid dynamics has been carried out with a numerical code developed by the Geophysical group at the University College Dublin (O’Brien and Bean, 2004b), with whom we started a very profitable collaboration. In this code, the seismic wave propagation in heterogeneous media with free surface (e.g. the Earth’s surface) is simulated using a discrete elastic lattice where particle interactions are controlled by the Hooke’s law. This method allows to consider medium heterogeneities and complex topography. The initial and boundary conditions for the simulations have been defined within a coordinate project (INGV-DPC 2004-06 V3_2 “Research on active volcanoes, precursors, scenarios, hazard and risk - Campi Flegrei”), to which this thesis contributes, and many researchers experienced on Campi Flegrei in volcanological, seismic, petrological, geochemical fields, etc. collaborate. Numerical simulations of magma and rock dynamis have been coupled as described in the thesis. The first part of the thesis consists of a parametric study aimed at understanding the eect of the presence in magma of carbon dioxide in magma in the convection dynamics. Indeed, the presence of this volatile was relevant in many Campi Flegrei eruptions, including some eruptions commonly considered as reference for a future activity of this volcano. A set of simulations considering an elliptical magma chamber, compositionally uniform, refilled from below by a magma with volatile content equal or dierent from that of the resident magma has been performed. To do this, a multicomponent non-ideal magma saturation model (Papale et al., 2006) that considers the simultaneous presence of CO2 and H2O, has been implemented in GALES. Results show that the presence of CO2 in the incoming magma increases its buoyancy force promoting convection ad mixing. The simulated dynamics produce pressure transients with frequency and amplitude in the sensitivity range of modern geophysical monitoring networks such as the one installed at Campi Flegrei . In the second part, simulations more related with the Campi Flegrei volcanic system have been performed. The simulated system has been defined on the basis of conditions consistent with the bulk of knowledge of Campi Flegrei and in particular of the Agnano-Monte Spina eruption (4100 B.P.), commonly considered as reference for a future high intensity eruption in this area. The magmatic system has been modelled as a long dyke refilling a small shallow magma chamber; magmas with trachytic and phonolitic composition and variable volatile content of H2O and CO2 have been considered. The simulations have been carried out changing the condition of magma injection, the system configuration (magma chamber geometry, dyke size) and the resident and refilling magma composition and volatile content, in order to study the influence of these factors on the simulated dynamics. Simulation results allow to follow each step of the gas-rich magma ascent in the denser magma, highlighting the details of magma convection and mixing. In particular, the presence of more CO2 in the deep magma results in more ecient and faster dynamics. Through this simulations the variation of the gravimetric field has been determined. Afterward, the space-time distribution of stress resulting from numerical simulations have been used as boundary conditions for the simulations of the displacement field imposed by the magmatic dynamics on rocks. The properties of the simulated domain (rock density, P and S wave velocities) have been based on data from literature on active and passive tomographic experiments, obtained through a collaboration with A. Zollo at the Dept. of Physics of the Federici II Univeristy in Napoli. The elasto-dynamics simulations allow to determine the variations of the space-time distribution of deformation and the seismic signal associated with the studied magmatic dynamics. In particular, results show that these dynamics induce deformations similar to those measured at Campi Flegrei and seismic signals with energies concentrated on the typical frequency bands observed in volcanic areas. The present work shows that an approach based on the solution of equations describing the physics of processes within a magmatic fluid and the surrounding rock system is able to recognise and describe the relationships between geophysical signals detectable on the surface and deep magma dynamics. Therefore, the results suggest that the combined study of geophysical data and informations from numerical simulations can allow in a near future a more ecient evaluation of the short term volcanic hazard.