Evaluation of organ-specific peripheral doses after 2-dimensional, 3-dimensional and hybrid intensity modulated radiation therapy for breast cancer based on Monte Carlo and convolution/superposition algorithms: implications for secondary cancer risk assessment.

To make a comprehensive evaluation of organ-specific out-of-field doses using Monte Carlo (MC) simulations for different breast cancer irradiation techniques and to compare results with a commercial treatment planning system (TPS). Three breast radiotherapy techniques using 6MV tangential photon beams were compared: (a) 2DRT (open rectangular fields), (b) 3DCRT (conformal wedged fields), and (c) hybrid IMRT (open conformal+modulated fields). Over 35 organs were contoured in a whole-body CT scan and organ-specific dose distributions were determined with MC and the TPS. Large differences in out-of-field doses were observed between MC and TPS calculations, even for organs close to the target volume such as the heart, the lungs and the contralateral breast (up to 70% difference). MC simulations showed that a large fraction of the out-of-field dose comes from the out-of-field head scatter fluence (>40%) which is not adequately modeled by the TPS. Based on MC simulations, the 3DCRT technique using external wedges yielded significantly higher doses (up to a factor 4-5 in the pelvis) than the 2DRT and the hybrid IMRT techniques which yielded similar out-of-field doses. In sharp contrast to popular belief, the IMRT technique investigated here does not increase the out-of-field dose compared to conventional techniques and may offer the most optimal plan. The 3DCRT technique with external wedges yields the largest out-of-field doses. For accurate out-of-field dose assessment, a commercial TPS should not be used, even for organs near the target volume (contralateral breast, lungs, heart).

Monte Carlo simulations of metasomatic enrichment in the lithosphere and implications for the source of alkaline basalts

One hypothesis for the origin of alkaline lavas erupted on oceanic islands and in intracontinental settings is that they represent the melts of amphibole-rich veins in the lithosphere (or melts of their dehydrated equivalents if metasomatized lithosphere is recycled into the convecting mantle). Amphibole-rich veins are interpreted as cumulates produced by crystallization of low-degree melts of the underlying asthenosphere as they ascend through the lithosphere. We present the results of trace-element modelling of the formation and melting of veins formed in this way with the goal of testing this hypothesis and for predicting how variability in the formation and subsequent melting of such cumulates (and adjacent cryptically and modally metasomatized lithospheric peridotite) would be manifested in magmas generated by such a process. Because the high-pressure phase equilibria of hydrous near-solidus melts of garnet lherzolite are poorly constrained and given the likely high variability of the hypothesized accumulation and remelting processes, we used Monte Carlo techniques to estimate how uncertainties in the model parameters (e.g. the compositions of the asthenospheric sources, their trace-element contents, and their degree of melting; the modal proportions of crystallizing phases, including accessory phases, as the asthenospheric partial melts ascend and crystallize in the lithosphere; the amount of metasomatism of the peridotitic country rock; the degree of melting of the cumulates and the amount of melt derived from the metasomatized country rock) propagate through the process and manifest themselves as variability in the trace-element contents and radiogenic isotopic ratios of model vein compositions and erupted alkaline magma compositions. We then compare the results of the models with amphibole observed in lithospheric veins and with oceanic and continental alkaline magmas. While the trace-element patterns of the near-solidus peridotite melts, the initial anhydrous cumulate assemblage (clinopyroxene +/- garnet +/- olivine +/- orthopyroxene), and the modelled coexisting liquids do not match the patterns observed in alkaline lavas, our calculations show that with further crystallization and the appearance of amphibole (and accessory minerals such as rutile, ilmenite, apatite, etc.) the calculated cumulate assemblages have trace-element patterns that closely match those observed in the veins and lavas. These calculated hydrous cumulate assemblages are highly enriched in incompatible trace elements and share many similarities with the trace-element patterns of alkaline basalts observed in oceanic or continental setting such as positive Nb/La, negative Ce/Pb, and similiar slopes of the rare earth elements. By varying the proportions of trapped liquid and thus simulating the cryptic and modal metasomatism observed in peridotite that surrounds these veins, we can model the variations in Ba/Nb, Ce/Pb, and Nb/U ratios that are observed in alkaline basalts. If the isotopic compositions of the initial low-degree peridotite melts are similar to the range observed in mid-ocean ridge basalt, our model calculations produce cumulates that would have isotopic compositions similar to those observed in most alkaline ocean island basalt (OIB) and continental magmas after similar to 0 center dot 15 Gyr. However, to produce alkaline basalts with HIMU isotopic compositions requires much longer residence times (i.e. 1-2 Gyr), consistent with subduction and recycling of metasomatized lithosphere through the mantle. such as a heterogeneous asthenosphere. These modelling results support the interpretation proposed by various researchers that amphibole-bearing veins represent cumulates formed during the differentiation of a volatile-bearing low-degree peridotite melt and that these cumulates are significant components of the sources of alkaline OIB and continental magmas. The results of the forward models provide the potential for detailed tests of this class of hypotheses for the origin of alkaline magmas worldwide and for interpreting major and minor aspects of the geochemical variability of these magmas.

Debris flow hazard modelling on medium scale: Valtellina di Tirano, Italy

Debris flow hazard modelling at medium (regional) scale has been subject of various studies in recent years. In this study, hazard zonation was carried out, incorporating information about debris flow initiation probability (spatial and temporal), and the delimitation of the potential runout areas. Debris flow hazard zonation was carried out in the area of the Consortium of Mountain Municipalities of Valtellina di Tirano (Central Alps, Italy). The complexity of the phenomenon, the scale of the study, the variability of local conditioning factors, and the lacking data limited the use of process-based models for the runout zone delimitation. Firstly, a map of hazard initiation probabilities was prepared for the study area, based on the available susceptibility zoning information, and the analysis of two sets of aerial photographs for the temporal probability estimation. Afterwards, the hazard initiation map was used as one of the inputs for an empirical GIS-based model (Flow-R), developed at the University of Lausanne (Switzerland). An estimation of the debris flow magnitude was neglected as the main aim of the analysis was to prepare a debris flow hazard map at medium scale. A digital elevation model, with a 10 m resolution, was used together with landuse, geology and debris flow hazard initiation maps as inputs of the Flow-R model to restrict potential areas within each hazard initiation probability class to locations where debris flows are most likely to initiate. Afterwards, runout areas were calculated using multiple flow direction and energy based algorithms. Maximum probable runout zones were calibrated using documented past events and aerial photographs. Finally, two debris flow hazard maps were prepared. The first simply delimits five hazard zones, while the second incorporates the information about debris flow spreading direction probabilities, showing areas more likely to be affected by future debris flows. Limitations of the modelling arise mainly from the models applied and analysis scale, which are neglecting local controlling factors of debris flow hazard. The presented approach of debris flow hazard analysis, associating automatic detection of the source areas and a simple assessment of the debris flow spreading, provided results for consequent hazard and risk studies. However, for the validation and transferability of the parameters and results to other study areas, more testing is needed.

«Meraviglioso diletto». La traduzione poetica del Cinquecento e le «Metamorfosi di Ovidio» di Giovanni Andrea dellʼAnguilllara

A partire dagli anni Trenta del Cinquecento la traduzione dei poeti classici in lingua volgare comincia a imporsi come un fenomeno di vasta portata nel mercato editoriale italiano. Omero, Virgilio, Stazio, ma soprattutto l'enciclopedico e lascivo Ovidio vengono liberamente riscritti e adattati per il diletto di un pubblico medio, desideroso di ritrovare i poemi antichi nel metro dell'Orlando furioso. Se molte di queste traduzioni non riuscirono a sopravvivere ai mutamenti del gusto, alcune di esse entrarono stabilmente nel canone delle versioni poetiche italiane. È il caso delle Metamorfosi ovidiane riscritte in ottava rima attorno alla metà del secolo da Giovanni Andrea dell'Anguillara, poeta della cerchia farnesiana destinato a vita tormentata ed errabonda. Digressivo, artificioso, magniloquente, l'Ovidio dell'Anguillara (cui è dedicato in gran parte questo volume) otterrà per almeno due secoli un incontrastato successo presso letterati, pittori e musicisti, da Marino a Tiepolo.

L' "altro sé" : rappresentazioni letterarie d'opposizione nel Novecento italiano

Nel secolo scorso è emersa in Italia un'originale modalité di rappresentazione letteraria che trasfigura i caratteri dell'identità per costruire una particolare forma di alterità, un "altro sé". Infatti, a causa di uno stato di crisi identitaria dello scrittore, in Silo ne e in Carlo Levi si assiste alla costruzione di figure di alterità (il "cafone", i contadini del Sud), rappresentazioni letterarie di quei soggetti socialmente subalterni che questi scrittori volevano riscattare ed emancipare. La tematizzazione dell'autorappresentazione che si riscontra in Brancati e in Pasolini va invece in un'altra direzione, diventa il progetto di una scoperta: la formalizzazione retorica di un'identità "altra" all'interno della propria individualità, letterariamente oggettivata e formalizzata. Brancati, cosi riletto e rivalutato, mostra la crisi dell'autorappresentazione, cioè del posizionamento d'autore nel momento del passaggio dal fascismo all'antifascismo, e quindi il processo di costruzione di un'identità "altra", più forte, che renda possibile la scrittura. Il brancatismo, cioè quel fenomeno culturale legato alia fortuna della narrativa brancatiana, ha anestetizzato questa dimensione critica della scrittura brancatiana riconducendo le sue figure e le sue trame narrative all'interno del discorso dell'alterità, iunzionale a una normalizzazione e borghesizzazione della società italiana del dopoguerra.La tesi propone quindi una teoria della rappresentazione italiana nel Novecento che, prendendo le mosse dalla critica postcoloniale, individua un'originale modalità di rappresentazione per cui gli elementi di "identità" vengono letterariamente trasfigurati in un'"alterità". Individuata questa esperienza, spiccano con inedita intensità le proposte di Carlo Levi per una nuova Italia, che incorporasse il sostrato "primitivo" nell'Italia contemporanea e futura; la progettualità delle esperienze artistiche di Pasolini dagli anni '50 alia sua scomparsa; e il percorso di Sciascia dall'acuta e innovativa riflessione sul pirandellismo degli esordi al ripiegamento sulla "sicilitudine" degli anni '80.

Come curare l'obesità nei bambini: revisione Cochrane per il medico di famiglia.

Cet article présente les résultats de la revue systématique: Oude Luttikhuis H, Baur L, Jansen H, et al. Interventions for treating obesity in children. Cochrane Database of Systematic Reviews 2009, Issue 1. Art. No.: CD001872. DOI: 10.1002/14651858.CD001872.pub2. PMID: 19160202.