904 resultados para emissions trading


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[EN] The main types of submarine geological emissions are classified as cold seeps (hydrocarbons and brines) and hot vents. These processes result in the emission of geological fluids: brine, gases (mainly hydro-carbons), sediments and rocks. Submarine emissions are associated with an intensive geological, geo-chemical, thermal and biological activity (Judd and Hovland, 2007), and constitute a key process in the dynamics of the global cycles of the planet Earth.

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[EN]A three-dimensional finite element model for the pollutant dispersion is presented. In these environmental processes over a complex terrain, a mesh generator capable of adapting itself to the topographic characteristics is essential. The first stage of the model consists on the construction of an adaptive tetrahedral mesh of a rectangular region bounded in its lower part by the terrain and in its upper part by a horizontal plane. Once the mesh is constructed, an adaptive local refinement of tetrahedra is used in order to capture the plume rise. Wind measurements are used to compute an interpolated wind field, that is modified by using a mass-consistent model and perturbing its vertical component to introduce the plume rise effect...

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[EN]A three-dimensional air pollution model for the short-term simulation of emission, transport and reaction of pollutants is presented. In the finite element simulation of these environmental processes over a complex terrain, a mesh generator capable of adapting itself to the topographic characteristics is essential, A local refinement of tetrahedra is used in order to capture the plume rise. Then a wind field is computed by using a mass-consistent model and perturbing its vertical component to introduce the plume rise effect. Finally, an Eulerian convection-diffusionreaction model is used to simulate the pollutant dispersion…

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[EN]In this paper we propose a finite element method approach for modelling the air quality in a local scale over complex terrain. The area of interest is up to tens of kilometres and it includes pollutant sources. The proposed methodology involves the generation of an adaptive tetrahedral mesh, the computation of an ambient wind field, the inclusion of the plume rise effect in the wind field, and the simulation of transport and reaction of pollutants. The methodology is used to simulate a fictitious pollution episode in La Palma island (Canary Island, Spain)…

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Congresos y conferencias

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Doctorado en la Insularidad : Turismo, interculturalidad y desarrollo sostenible

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Il problema che si cerca di risolvere attraverso la gestione quantitativa del portafoglio è la riduzione del rischio tramite strategie che non dipendano dalla diversificazione dei titoli che compongono il portafoglio. Nel momento in cui si decide di applicare un trading system su un determinato gruppo di asset, il capitale non viene allocato automaticamente su tutti i titoli e si deve affrontare invece un continuo investimento tramite l’apertura dinamica di posizioni sul mercato.Questo significa che la diversificazione non è più una misura adeguata del rischio sostenuto poiché i rendimenti attesi dell’investimento non dipendono più dalle proprietà stesse degli strumenti scelti, ma dalla profittabilità dei segnali generati dalla logica del trading system su questi. Bisogna testare in questo caso le performance del sistema a livello statistico e prevedere anche, per esempio, che l’algoritmo possa generare dei segnali errati che portano a delle posizioni in perdita. Il portafoglio a livello quantitativo deve essere gestito tramite dei trading system che abbiano la possibilità di valutare aspetti globali, come il profitto totale di tutte le posizioni attualmente aperte, o l’intero rischio sostenuto dal capitale gestito. Le decisioni non vengono prese dall’analisi delle prestazioni individuali che la strategia ottiene operando sui singoli titoli. Per affrontare una possibile soluzione a questa problematica si sono quindi selezionati due trading system le cui prestazioni fossero robuste su un intero portafoglio e non solo su determinati titoli. In un successivo momento vengono analizzate le prestazioni del portafoglio aggiungendo ai test due ulteriori strategie di uscita: lo stoploss di portafoglio e il target di portafoglio. Nonostante esse ricalchino idee ampiamente utilizzate per la gestione delle singole posizioni su un titolo, per i test si è deciso di modificarle implementando la gestione globale del capitale all’interno del trading system di portafoglio.

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Le pagine che seguono sono il racconto dello studio e della ricerca della soluzione ecommerce ideale per Trading Library, casa editrice rivolta al mondo del Trading. L’elaborato è diviso in tre parti: • INTRODUZIONE:Analisiestudiodelpassato,delpresenteedelfuturo dell’ecommerce e studio del settore editoriale. • LE FASI: Analisi del progetto Trading Library, pianificazione dell’attivi- tà, descrizione delle fasi cognitiva, progettuale e divulgativa. • CONCLUSIONE: Considerazioni,previsioni per il futuro ed autocritica sul lavoro svolto. Nella presentazione di ogni capitolo si sono riassunte le argomentazioni trattate, mano a mano che si scende nelle sottosezioni le informazioni riguardo allo studio svolto diventano più tecniche e dettagliate.

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This dissertation focuses on characterizing the emissions of volatile organic compounds (VOCs) from grasses and young trees, and the burning of biomass mainly from Africa and Indonesia. The measurements were performed with a proton-transfer-reaction mass spectrometer (PTR-MS). The biogenic emissions of tropical savanna vegetation were studied in Calabozo (Venezuela). Two field campaigns were carried out, the first during the wet season (1999) and the second during the dry season (2000). Three grass species were studied: T. plumosus, H. rufa and A. canescens, and the tree species B. crassifolia, C. americana and C. vitifolium. The emission rates were determined with a dynamic plant enclosure system. In general, the emissions increased exponentially with increasing temperature and solar radiation. Therefore, the emission rates showed high variability. Consequently, the data were normalized to a standard temperature of 30°C, and standard emission rates thus determined allowed for interspecific and seasonal comparisons. The range of average daytime (10:00-16:00) emission rates of total VOCs measured from green (mature and young) grasses was between 510-960 ngC/g/h. Methanol was the primary emission (140-360 ngC/g/h), followed by acetaldehyde, butene and butanol and acetone with emission rates between 70-200 ngC/g/h. The emissions of propene and methyl ethyl ketone (MEK) were <80 ngC/g/h, and those of isoprene and C5-alcohols were between 10-130 ngC/g/h. The oxygenated species represented 70-75% of the total. The emission of VOCs was found to vary by up to a factor of three between plants of the same species, and by up to a factor of two between the different species. The annual source of methanol from savanna grasses worldwide estimated in this work was 3 to 4.4 TgC, which could represent up to 12% of the current estimated global emission from terrestrial vegetation. Two of the studied tree species, were isoprene emitters, and isoprene was also their primary emission (which accounted for 70-94% of the total carbon emitted) followed by methanol and butene + butanol. The daytime average emission rate of isoprene measured in the wet season was 27 mgC/g/h for B. crassifolia, and 123 mgC/g/h for C. vitifolium. The daytime emissions of methanol and butene + butanol were between 0.3 and 2 mgC/g/h. The total sum of VOCs emission measured during the day in the wet season was between 30 and 130 mgC/g/h. In the dry season, in contrast, the methanol emissions from C. vitifolium saplings –whose leaves were still developing– were an order of magnitude higher than in the wet season (15 mgC/g/h). The isoprene emission from B. crassifolia in the dry season was comparable to the emission in the wet season, whereas isoprene emission from C. vitifolium was about a factor of three lower (~43 mgC/g/h). Biogenic emission inventories show that isoprenoids are the most prominent and best-studied compounds. The standard emission rates of isoprene and monoterpenes of the measured savanna trees were in the lower end of the range found in the literature. The emission of other biogenic VOCs has been sparsely investigated, but in general, the standard emissions from trees studied here were within the range observed in previous investigations. The biomass burning study comprised the measurement of VOCs and other trace-gas emissions of 44 fires from 15 different fuel types, primarily from Africa and Indonesia, in a combustion laboratory. The average sum of emissions (excluding CO2, CO and NO) from African fuels was ~18 g(VOC)/kg. Six of the ten most important emissions were oxygenated VOCs. Acetic acid was the major emission, followed by methanol and formaldehyde. The emission of methane was of the same order as the methanol emission (~5 g/kg), and that of nitrogen-containing compounds was ~1 g/kg. An estimate of the VOC source from biomass burning of savannas and grasslands worldwide suggests that the sum of emissions is about 56 Tg/yr, of which 34 Tg correspond to oxygenated VOCs, 14 Tg to unsaturated and aromatic compounds, 5 Tg to methane and 3 Tg to N-compounds. The estimated emissions of CO, CO2 and NO are 216, 5117 and 9.4 Tg/yr, respectively. The emission factors reported here for Indonesian fuels are the first results of laboratory fires using Indonesian fuels. Acetic acid was the highest organic emission, followed by acetol, a compound not previously reported in smoke, methane, mass 97 (tentatively identified as furfural, dimethylfuran and ethylfuran), and methanol. The sum of total emissions of Indonesian fuels was 91 g/kg, which is 5 times higher than the emissions from African fuels. The results of this study reinforces the importance of oxygenated compounds. Due to the vast area covered by tropical savannas worldwide, the biogenic and biomass burning emission of methanol and other oxygenated compounds may be important for the regional and even global tropospheric chemistry.