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Commento agli articoli da 1188 a 1192 del codice civile in tema di destinatario del pagamento, pagamento al creditore apparente, pagamento al creditore incapace, pagamento eseguito da un incapace, pagamento eseguito con cose altrui. L'analisi, attenta al dato normativo interno e sovranazionale, all'elaborazione giurisprudenziale e alla riflessione dottrinale in materia, scrutina l'incidenza che specificità relative ai soggetti del rapporto obbligatorio hanno sulla vicenda attuativa dell'obbligazione.

The aim of the paper is to study the evolution of the language of the specific genre of white house press briefings across 18 years. Phraseologies will be taken into consideration in order to compare and contrast the language of the 'podium' during three different administrations: Clinton, Bush and Obama.

This chapter sets out to describe how different subcorpora were integrated to form the unified body of texts know as the CordDis corpus.

Introduction Kidney and liver transplants are the most frequent transplantation procedures carried out in Italy. We report the result of an epidemiological study on kidney transplanted patients resident in the Province of Messina (Italy). Methods Seventy-five patients were enrolled between June 2010 march 2011, interviewed and evaluated using an adapted Italian version short-form 36. Socio-economic characteristics, quality of life modifications and involvement in transplant-related charities were studied. The follow-up period was ranging between 52 and 356 months. All subjects gave written informed consent and all results were analysed by chi-square test. Results No statistically significant differences were found between sexes, social and interpersonal relationship modifications. Discussion The benefits obtained on quality of life after trans- plantation is the prerogative of a small percentage of patients and is related to medium and high socio-economic conditions. The possibility of avoiding the haemodialysis represents the primary benefit for the totality of patients., Journal of Preventive Medicine and Hygiene, Vol 54, No 4 (2013)

J. CHEM. PHYS.

A volcanoclastic ash-layer, 1 m thick, has been found interbedded in the Antognola Formation (Epiligurian successions, Oligo-Miocene) in the Sillaro riverbed (Bologna foothils, Northern Apennines). Five micropaleontological samples have provided a Chattian- Aquitanian age for the section comprehending the body. Even if volcanoclastic layers are rather frequent in the Oligocene and early Miocene of the Northern Apennines (particularly in the Antognola Formation), this finding is unusual because of the coarse grain size and the presence of medium scale cross-bedding. The deposit was investigated with an interdisciplinary approach using compositional, sedimentological and stratigraphic studies. The ash-layer is a crystal-tuff composed up to 50% of plagioclase crystals associated with secondary smectite, harmotome and heulandite. This mineralogy supports an origin from intermediate products of calc-alkaline volcanic suite. The secondary minerals suggest different stages of alteration, the first one producing smectite and harmotome from probably amorphous original materials and praecursor smectite. No other beds of the same composition occur throughout the 300 m thick section. The ash-layer consists of at least 3 depositional events related to high density turbidity current. The sequence below and above the ash-layer is constituted mostly of gravity emplaced, fine grained deposits, alternating with thin hemipelagic layers. Gravity flow deposits are represented by thin bedded turbidites (TBT), slump deposits, and debris flow deposits indicating a slope association. As to the possible volcanic sources, the known active volcanic provinces at the time of the deposition were: 1) Periadriatic magmatism (along the Insubric Line in the Alps); 2) Mortara volcanic body (buried under the Po Plain); 3) Pieve S. Stefano volcanic body (buried under the central part of the Northern Apennines); 4) Sardinia volcanic arc; 5) Provence volcanic district (south of France). The dynamics of emplacement of the ash layer and its grain size are incompatible with all of these known sources. We propose a closer location of the volcanic source, even in an intrabasin position (Epiligurian basins were located to the W-SW of the present location) This volcanic center can be related to a transversal transcurrent lineament (Sillaro line).

INT. J. BIOL. MACROMOL. (IN PRESS)

CHEM. PHYS. LETTERS