Integration of MFA and LCA methodologies: the anthropogenic aluminium cycle in Italy

MFA and LCA methodologies were applied to analyse the anthropogenic aluminium cycle in Italy with focus on historical evolution of stocks and flows of the metal, embodied GHG emissions, and potentials from recycling to provide key features to Italy for prioritizing industrial policy toward low-carbon technologies and materials. Historical trend series were collected from 1947 to 2009 and balanced with data from production, manufacturing and waste management of aluminium-containing products, using a ‘top-down’ approach to quantify the contemporary in-use stock of the metal, and helping to identify ‘applications where aluminium is not yet being recycled to its full potential and to identify present and future recycling flows’. The MFA results were used as a basis for the LCA aimed at evaluating the carbon footprint evolution, from primary and electrical energy, the smelting process and the transportation, embodied in the Italian aluminium. A discussion about how the main factors, according to the Kaya Identity equation, they did influence the Italian GHG emissions pattern over time, and which are the levers to mitigate it, it has been also reported. The contemporary anthropogenic reservoirs of aluminium was estimated at about 320 kg per capita, mainly embedded within the transportation and building and construction sectors. Cumulative in-use stock represents approximately 11 years of supply at current usage rates (about 20 Mt versus 1.7 Mt/year), and it would imply a potential of about 160 Mt of CO2eq emissions savings. A discussion of criticality related to aluminium waste recovery from the transportation and the containers and packaging sectors was also included in the study, providing an example for how MFA and LCA may support decision-making at sectorial or regional level. The research constitutes the first attempt of an integrated approach between MFA and LCA applied to the aluminium cycle in Italy.

Uno studio sulla responsabilita' da reato degli enti

Il lavoro è suddiviso in due sezioni, che si compongono rispettivamente di tre e due capitoli. La prima sezione è dedicata all'esame dei principi fondamentali e della "parte generale" della disciplina della responsabilità amministrativa degli enti: il primo capitolo si concentra sull'evoluzione storica del principio Societas delinquere non potest nell'ordinamento giuridico italiano, prodromica all'analisi della natura della responsabilità amministrativa dipendente da reato degli enti. svolta nel secondo capitolo. Nel terzo capitolo della prima sezione si affronta la disciplina di "parte generale" del decreto 231, evidenziando, in particolare. i principi fondamentali che caratterizzano questo paradigma di illecito. La seconda sezione affronta invece due degli aspetti maggiormente problematici della "parte speciale" del decreto, ovvero la responsabilità degli enti per i delitti di omicidio e lesioni colpose (ai quali è dedicato il primo capitolo) e quella derivante dalla commissione di reati associativi (ai quali è dedicato il secondo capitolo).

La prova penale nelle indagini difensive. Analisi comparata degli strumenti processuali concessi alla difesa nei sistemi italiano e statunitense.

L’elaborato si occupa di fare il punto in materia di indagini difensive a tre lustri dall’entrata in vigore della legge n. 397/2000, epilogo di un lungo processo evolutivo che ha visto da un lato, una gestazione faticosa e travagliata, dall’altro, un prodotto normativo accolto dagli operatori in un contesto di scetticismo generale. In un panorama normativo e giurisprudenziale in continua evoluzione, i paradigmi dettati dagli artt. 24 e 111 della Costituzione, in tema di diritto alla difesa e di formazione della prova penale secondo il principio del contraddittorio tra le parti, in condizioni di parità, richiedono che il sistema giustizia offra sia all’indagato che all’imputato sufficienti strumenti difensivi. Tenuto conto delle diversità che caratterizzano naturalmente i ruoli dell’accusa e della difesa che impongono asimmetrie genetiche inevitabili, l’obiettivo della ricerca consiste nella disamina degli strumenti idonei a garantire il diritto alla prova della difesa in ogni stato e grado del procedimento, nel tentativo di realizzare compiutamente il principio di parità accusa - difesa nel processo penale. La ricerca si dipana attraverso tre direttrici: l’analisi dello statuto sulle investigazioni difensive nella sua evoluzione storica sino ai giorni nostri, lo studio della prova penale nel sistema americano e, infine, in alcune considerazioni finali espresse in chiave comparatistica. Le suggestioni proposte sono caratterizzate da un denominatore comune, ovvero dal presupposto che per contraddire è necessario conoscere e che solo per tale via sia possibile, finalmente, riconoscere il diritto di difendersi indagando.

La reducción de las donaciones inoficiosas en el Derecho español. Una contribución al estudio de la sucesión necesaria.

La llamada sucesión necesaria plantea una serie de problemas que atienden a la tutela del legitimario, en cuyo ámbito la reducción de las disposiciones inoficiosas y, en particular la que atiende a los actos inter vivos del causante, adquiere una gran importancia. Importancia que es particularmente relevante en el ordenamiento jurídico español, en el que la acción de reducción, si bien prevista por el Derecho positivo, no está completamente regulada en la norma, subsistiendo, por ello, múltiples cuestiones sin resolver. La presente investigación busca profundizar en el régimen jurídico de la donación inoficiosa tal y como lo recoge el Código civil español, enriqueciéndolo con las aportaciones de la doctrina italiana, cuya solidez interpretativa puede servir de referencia para una eventual reforma del Derecho castellano. Con este objetivo, la presente investigación se centra, entre otros puntos, sobre la configuración histórica de la acción de reducción; el concepto de donación inoficiosa; las operaciones de cálculo de la legítima; la naturaleza jurídica de la acción de reducción y la valoración del bien donado a los efectos de reducción. Finalmente, estudia la validez de las “cláusulas de reducción in valorem”, por medio del as cuales el donante puede autorizar al donatario para que conserve el bien objeto de la donación, entregando al legitimario una cantidad de dinero. En conclusión, la presente tesis permite individuar las características del acto impugnable mediante la acción de reducción de donaciones y las líneas esenciales de la reducción como categoría de ineficacia, lo que a su vez favorecer la resolución de algunos problemas de aplicación de la reducción de donaciones que se encuentran en el ordenamiento español. La investigación, además, permite formular algunas propuestas “de lege ferenda” a fin de agilizar la práctica de la reducción y reducir la litigiosidad, salvaguardando los intereses de legitimario y donatario.

Petrology and geochemistry of Lipari Island (Aeolian archipelago): constraints on magma genesis and evolution

A full set of geochemical and Sr, Nd and Pb isotope data both on bulk-rock and mineral samples is provided for volcanic rocks representative of the whole stratigraphic succession of Lipari Island in the Aeolian archipelago. These data, together with petrographic observations and melt/fluid inclusion investigations from the literature, give outlines on the petrogenesis and evolution of magmas through the magmatic and eruptive history of Lipari. This is the result of nine successive Eruptive Epochs developing between 271 ka and historical times, as derived from recentmost volcanological and stratigraphic studies, combined with available radiometric ages and correlation of tephra layers and marine terrace deposits. These Eruptive Epochs are characterized by distinctive vents partly overlapping in space and time, mostly under control of the main regional tectonic trends (NNW-SSE, N-S and minor E-W). A large variety of lava flows, scoriaceous deposits, lava domes, coulees and pyroclastics are emplaced, ranging in composition through time from calcalkaline (CA) and high-K (HKCA) basaltic andesites to rhyolites. CA and HKCA basaltic andesitic to dacitic magmas were erupted between 271 and 81 ka (Eruptive Epochs 1-6) from volcanic edifices located along the western coast of the island (and subordinately the eastern Monterosa) and the M.Chirica and M.S.Angelo stratocones. These mafic to intermediate magmas mainly evolved through AFC and RAFC processes, involving fractionation of mafic phases, assimilation of wall rocks and mixing with newly injected mafic magmas. Following a 40 ka-long period of volcanic quiescence, the rhyolitic magmas were lately erupted from eruptive vents located in the southern and north-eastern sectors of Lipari between 40 ka and historical times (Eruptive Epochs 7-9). They are suggested to derive from the previous mafic to intermediate melts through AFC processes. During the early phases of rhyolitic magmatism (Eruptive Epochs 7-8), enclaves-rich rocks and banded pumices, ranging in composition from HKCA dacites to low-SiO2 rhyolites were erupted, representing the products of magma mixing between fresh mafic magmas and the fractionated rhyolitic melts. The interaction of mantle-derived magmas with the crust represents an essential process during the whole magmatic hystory of Lipari, and is responsible for the wide range of observed geochemical and isotopic variations. The crustal contribution was particularly important during the intermediate phases of activity of Lipari when the cordierite-bearing lavas were erupted from the M. S.Angelo volcano (Eruptive Epoch 5, 105 ka). These lavas are interpreted as the result of mixing and subsequent hybridization of mantle-derived magmas, akin to the ones characterizing the older phases of activity of Lipari (Eruptive Epochs 1-4), and crustal anatectic melts derived from dehydration-melting reactions of metapelites in the lower crust. A comparison between the adjacent islands of Lipari and Vulcano outlines that their mafic to intermediate magmas seem to be genetically connected and derive from a similar mantle source affected by different degrees of partial melting (and variable extent of crustal assimilation) producing either the CA magmas of Lipari (higher degrees) or the HKCA to SHO magmas of Vulcano (lower degrees). On a regional scale, the most primitive rocks (SiO2<56%, MgO>3.5%) of Lipari, Vulcano, Salina and Filicudi are suggested to derive from a similar MORB-like source, variably metasomatized by aqueous fluids coming from the slab and subordinately by the additions of sediments.