976 resultados para Rienzo, Cola di, d. 1354
Resumo:
The wheel - rail contact analysis plays a fundamental role in the multibody modeling of railway vehicles. A good contact model must provide an accurate description of the global contact phenomena (contact forces and torques, number and position of the contact points) and of the local contact phenomena (position and shape of the contact patch, stresses and displacements). The model has also to assure high numerical efficiency (in order to be implemented directly online within multibody models) and a good compatibility with commercial multibody software (Simpack Rail, Adams Rail). The wheel - rail contact problem has been discussed by several authors and many models can be found in the literature. The contact models can be subdivided into two different categories: the global models and the local (or differential) models. Currently, as regards the global models, the main approaches to the problem are the so - called rigid contact formulation and the semi – elastic contact description. The rigid approach considers the wheel and the rail as rigid bodies. The contact is imposed by means of constraint equations and the contact points are detected during the dynamic simulation by solving the nonlinear algebraic differential equations associated to the constrained multibody system. Indentation between the bodies is not permitted and the normal contact forces are calculated through the Lagrange multipliers. Finally the Hertz’s and the Kalker’s theories allow to evaluate the shape of the contact patch and the tangential forces respectively. Also the semi - elastic approach considers the wheel and the rail as rigid bodies. However in this case no kinematic constraints are imposed and the indentation between the bodies is permitted. The contact points are detected by means of approximated procedures (based on look - up tables and simplifying hypotheses on the problem geometry). The normal contact forces are calculated as a function of the indentation while, as in the rigid approach, the Hertz’s and the Kalker’s theories allow to evaluate the shape of the contact patch and the tangential forces. Both the described multibody approaches are computationally very efficient but their generality and accuracy turn out to be often insufficient because the physical hypotheses behind these theories are too restrictive and, in many circumstances, unverified. In order to obtain a complete description of the contact phenomena, local (or differential) contact models are needed. In other words wheel and rail have to be considered elastic bodies governed by the Navier’s equations and the contact has to be described by suitable analytical contact conditions. The contact between elastic bodies has been widely studied in literature both in the general case and in the rolling case. Many procedures based on variational inequalities, FEM techniques and convex optimization have been developed. This kind of approach assures high generality and accuracy but still needs very large computational costs and memory consumption. Due to the high computational load and memory consumption, referring to the current state of the art, the integration between multibody and differential modeling is almost absent in literature especially in the railway field. However this integration is very important because only the differential modeling allows an accurate analysis of the contact problem (in terms of contact forces and torques, position and shape of the contact patch, stresses and displacements) while the multibody modeling is the standard in the study of the railway dynamics. In this thesis some innovative wheel – rail contact models developed during the Ph. D. activity will be described. Concerning the global models, two new models belonging to the semi – elastic approach will be presented; the models satisfy the following specifics: 1) the models have to be 3D and to consider all the six relative degrees of freedom between wheel and rail 2) the models have to consider generic railway tracks and generic wheel and rail profiles 3) the models have to assure a general and accurate handling of the multiple contact without simplifying hypotheses on the problem geometry; in particular the models have to evaluate the number and the position of the contact points and, for each point, the contact forces and torques 4) the models have to be implementable directly online within the multibody models without look - up tables 5) the models have to assure computation times comparable with those of commercial multibody software (Simpack Rail, Adams Rail) and compatible with RT and HIL applications 6) the models have to be compatible with commercial multibody software (Simpack Rail, Adams Rail). The most innovative aspect of the new global contact models regards the detection of the contact points. In particular both the models aim to reduce the algebraic problem dimension by means of suitable analytical techniques. This kind of reduction allows to obtain an high numerical efficiency that makes possible the online implementation of the new procedure and the achievement of performance comparable with those of commercial multibody software. At the same time the analytical approach assures high accuracy and generality. Concerning the local (or differential) contact models, one new model satisfying the following specifics will be presented: 1) the model has to be 3D and to consider all the six relative degrees of freedom between wheel and rail 2) the model has to consider generic railway tracks and generic wheel and rail profiles 3) the model has to assure a general and accurate handling of the multiple contact without simplifying hypotheses on the problem geometry; in particular the model has to able to calculate both the global contact variables (contact forces and torques) and the local contact variables (position and shape of the contact patch, stresses and displacements) 4) the model has to be implementable directly online within the multibody models 5) the model has to assure high numerical efficiency and a reduced memory consumption in order to achieve a good integration between multibody and differential modeling (the base for the local contact models) 6) the model has to be compatible with commercial multibody software (Simpack Rail, Adams Rail). In this case the most innovative aspects of the new local contact model regard the contact modeling (by means of suitable analytical conditions) and the implementation of the numerical algorithms needed to solve the discrete problem arising from the discretization of the original continuum problem. Moreover, during the development of the local model, the achievement of a good compromise between accuracy and efficiency turned out to be very important to obtain a good integration between multibody and differential modeling. At this point the contact models has been inserted within a 3D multibody model of a railway vehicle to obtain a complete model of the wagon. The railway vehicle chosen as benchmark is the Manchester Wagon the physical and geometrical characteristics of which are easily available in the literature. The model of the whole railway vehicle (multibody model and contact model) has been implemented in the Matlab/Simulink environment. The multibody model has been implemented in SimMechanics, a Matlab toolbox specifically designed for multibody dynamics, while, as regards the contact models, the CS – functions have been used; this particular Matlab architecture allows to efficiently connect the Matlab/Simulink and the C/C++ environment. The 3D multibody model of the same vehicle (this time equipped with a standard contact model based on the semi - elastic approach) has been then implemented also in Simpack Rail, a commercial multibody software for railway vehicles widely tested and validated. Finally numerical simulations of the vehicle dynamics have been carried out on many different railway tracks with the aim of evaluating the performances of the whole model. The comparison between the results obtained by the Matlab/ Simulink model and those obtained by the Simpack Rail model has allowed an accurate and reliable validation of the new contact models. In conclusion to this brief introduction to my Ph. D. thesis, we would like to thank Trenitalia and the Regione Toscana for the support provided during all the Ph. D. activity. Moreover we would also like to thank the INTEC GmbH, the society the develops the software Simpack Rail, with which we are currently working together to develop innovative toolboxes specifically designed for the wheel rail contact analysis.
Resumo:
La tesi può intendersi schematicamente suddivisibile in quattro macrosettori: il primo concerne un excursus storico-giuridico sulla nascita ed evoluzione dei Monti di Pietà , nonché delle Casse di Risparmio; il secondo macrosettore si riferisce peculiarmente alla profonda trasformazione e riorganizzazione delle Banche Pubbliche in Società per Azioni e alla conseguente nascita delle Fondazioni Bancarie, con l'approfondimento delle problematiche attinenti alla loro natura giuridica, e con il richiamo alle sentenze nn. 300 e 301/2003 della Corte Costituzionale; il terzo prende in esame il ruolo delle Fondazioni nella prospettiva della operatività del principio di sussidiarietà orizzontale; infine, nell'ambito del quarto macrosettore ci si è soffermati sulla struttura organizzativa delle Fondazioni, sul loro regime fiscale e sul tema dell'attività d'impresa delle stesse.
Resumo:
Il cervello è una rete di cellule nervose connesse da assoni e le cellule stesse sono reti di molecole connesse da reazioni biochimiche. Anche le società sono reti di persone collegate da rapporti di amicizia, parentela e legami professionali. Su più larga scala, catene alimentari ed ecosistemi possono essere rappresentati come reti di specie viventi. E le reti pervadono la tecnologia: Internet, reti elettriche e sistemi di trasporto non sono che pochi degli esempi possibili. Anche il linguaggio che si sta usando in questo momento per veicolare questi ragionamenti a chi legge è una rete, fatta di parole connesse da relazioni sintattiche. A dispetto dell'importanza e della pervasività delle reti, gli scienziati hanno sempre avuto poca comprensione delle loro strutture e proprietà . In che modo le interazioni di alcuni nodi non funzionanti in una complessa rete genetica possono generare il cancro? Come può avvenire così rapidamente la diffusione in taluni sistemi sociali e di comunicazioni, portando ad epidemie di malattie e a virus informatici? Come possono alcune reti continuare a funzionare anche dopo che la maggioranza dei loro nodi ha, invece, smesso di farlo? [...] Le reti reali sono realmente casuali?
Resumo:
Un livello di sicurezza che prevede l’autenticazione e autorizzazione di un utente e che permette di tenere traccia di tutte le operazioni effettuate, non esclude una rete dall’essere soggetta a incidenti informatici, che possono derivare da tentativi di accesso agli host tramite innalzamento illecito di privilegi o dai classici programmi malevoli come virus, trojan e worm. Un rimedio per identificare eventuali minacce prevede l’utilizzo di un dispositivo IDS (Intrusion Detection System) con il compito di analizzare il traffico e confrontarlo con una serie d’impronte che fanno riferimento a scenari d’intrusioni conosciute. Anche con elevate capacità di elaborazione dell’hardware, le risorse potrebbero non essere sufficienti a garantire un corretto funzionamento del servizio sull’intero traffico che attraversa una rete. L'obiettivo di questa tesi consiste nella creazione di un’applicazione con lo scopo di eseguire un’analisi preventiva, in modo da alleggerire la mole di dati da sottoporre all’IDS nella fase di scansione vera e propria del traffico. Per fare questo vengono sfruttate le statistiche calcolate su dei dati forniti direttamente dagli apparati di rete, cercando di identificare del traffico che utilizza dei protocolli noti e quindi giudicabile non pericoloso con una buona probabilità .
Resumo:
La frenetica evoluzione sociale e culturale, data dal crescente e continuo bisogno di conoscenza dell’uomo, ha portato oggi a navigare in un oceano sconfinato di dati e informazioni. Esse assumono una propria peculiare importanza, un valore sia dal punto di vista del singolo individuo, sia all’interno di un contesto sociale e di un settore di riferimento specifico e concreto. La conseguente mutazione dell’interazione e della comunicazione a livello economico della società , ha portato a parlare oggi di economia dell’informazione. In un contesto in cui l’informazione rappresenta la risorsa principale per l’attività di crescita e sviluppo economico, è fondamentale possedere la più adeguata strategia organizzativa per la gestione dei dati grezzi. Questo per permetterne un’efficiente memorizzazione, recupero e manipolazione in grado di aumentare il valore dell’organizzazione che ne fa uso. Un’informazione incompleta o non accurata può portare a valutazioni errate o non ottimali. Ecco quindi la necessità di gestire i dati secondo specifici criteri al fine di creare un proprio vantaggio competitivo. La presente rassegna ha lo scopo di analizzare le tecniche di ottimizzazione di accesso alle basi di dati. La loro efficiente implementazione è di fondamentale importanza per il supporto e il corretto funzionamento delle applicazioni che ne fanno uso: devono garantire un comportamento performante in termini di velocità , precisione e accuratezza delle informazioni elaborate. L’attenzione si focalizzerà sulle strutture d’indicizzazione di tipo gerarchico: gli alberi di ricerca. Verranno descritti sia gli alberi su dati ad una dimensione, sia quelli utilizzati nel contesto di ricerche multi dimensionali (come, ad esempio, punti in uno spazio). L’ingente sforzo per implementare strutture di questo tipo ha portato gli sviluppatori a sfruttare i principi di ereditarietà e astrazione della programmazione ad oggetti al fine di ideare un albero generalizzato che inglobasse in sé tutte le principali caratteristiche e funzioni di una struttura di indicizzazione gerarchica, così da aumentarne la riusabilità per i più particolari utilizzi. Da qui la presentazione della struttura GiST: Generalized Search Tree. Concluderà una valutazione dei metodi d’accesso esposti nella dissertazione con un riepilogo dei principali dati relativi ai costi computazionali, vantaggi e svantaggi.
Resumo:
Progetto di riqualificazione urbana di un'area industriale attraverso il riordino del verde. Inserimento di laboratori di ricerca e incubatori d'impresa e coworking e riorganizzazione degli impianti sportivi preesistenti.
Resumo:
Tesi riguardo la fase preliminare di una campagna sperimentale su elementi rinforzati a flessione e taglio con fibra di basalto e malta e successivamente testati al fuoco. Comprende una parte relativa al comportamento dei comositi allle alte temperature e una sul problema della delaminazione alle alte temperature. Sono inoltre condotte simulazione numeriche relativamente al problema dell trasmissione del calore all'interno della sezione, con particolare attenzione alla modellazione dell'intuemescente. Sono stati eseguite prove di pull-out sui rinforzi e una serie di prove a compressione a caldo sulla malta d'incollaggio.
Resumo:
The Thrace Basin is the largest and thickest Tertiary sedimentary basin of the eastern Balkans region and constitutes an important hydrocarbon province. It is located between the Rhodope-Strandja Massif to the north and west, the Marmara Sea and Biga Peninsula to the south, and the Black Sea to the est. It consists of a complex system of depocenters and uplifts with very articulate paleotopography indicated by abrupt lateral facies variations. Its southeastern margin is widely deformed by the Ganos Fault, a segment of the North Anatolian strike-slip fault system . Most of the Thrace Basin fill ranges from the Eocene to the Late Oligocene. Maximum total thickness, including the Neogene-Quaternary succession, reaches 9.000 meters in a few narrow depocenters. This sedimentary succession consists mainly of basin plain turbiditic deposits with a significant volcaniclastic component which evolves upwards to shelf deposits and continental facies, with deltaic bodies prograding towards the basin center in the Oligocene. This work deals with the provenance of Eocene-Oligocene clastic sediments of the southern and western part of Thrace Basin in Turkey and Greece. Sandstone compositional data (78 gross composition analyses and 40 heavy minerals analyses) were used to understand the change in detrital modes which reflects the provenance and geodinamic evolution of the basin. Samples were collected at six localities, which are from west to est: Gökçeada, Gallipoli and South-Ganos (south of Ganos Fault), Alexandroupolis, Korudağ and North-Ganos (north of Ganos Fault). Petrologic (framework composition and heavy-mineral analyses) and stratigraphic-sedimentologic data, (analysis of sedimentologic facies associations along representative stratigraphic sections, paleocurrents) allowed discrimination of six petrofacies; for each petrofacies the sediment dispersal system was delineated. The Thrace Basin fill is made mainly of lithic arkoses and arkosic litharenites with variable amount of low-grade metamorphic lithics (also ophiolitic), neovolcanic lithics, and carbonate grains (mainly extrabasinal). Picotite is the most widespread heavy mineral in all petrofacies. Petrological data on analyzed successions show a complex sediment dispersal pattern and evolution of the basin, indicating one principal detrital input from a source area located to the south, along both the İzmir-Ankara and Intra-Pontide suture lines, and a possible secondary source area, represented by the Rhodope Massif to the west. A significant portion of the Thrace Basin sediments in the study area were derived from ophiolitic source rocks and from their oceanic cover, whereas epimetamorphic detrital components came from a low-grade crystalline basement. An important penecontemporaneous volcanic component is widespread in late Eocene-Oligocene times, indicating widespread post-collisional (collapse?) volcanism following the closure of the Vardar ocean. Large-scale sediment mass wasting from south to north along the southern margin of the Thrace Basin is indicated (i) in late Eocene time by large olistoliths of ophiolites and penecontemporaneous carbonates, and (ii) in the mid-Oligocene by large volcaniclastic olistoliths. The late Oligocene paleogeographic scenario was characterized by large deltaic bodies prograding northward (Osmancik Formation). This clearly indicates that the southern margin of the basin acted as a major sediment source area throughout its Eocene-Oligocene history. Another major sediment source area is represented by the Rhodope Massif, in particolar the Circum-Rhodopic belt, especially for plutonic and metamorphic rocks. Considering preexisting data on the petrologic composition of Thrace Basin, silicilastic sediments in Greece and Bulgaria (Caracciolo, 2009), a Rhodopian provenance could be considered mostly for areas of the Thrace Basin outside our study area, particularly in the northern-central portions of the basin. In summary, the most important source area for the sediment of Thrace Basin in the study area was represented by the exhumed subduction-accretion complex along the southern margin of the basin (Biga Peninsula and western-central Marmara Sea region). Most measured paleocurrent indicators show an eastward paleoflow but this is most likely the result of gravity flow deflection. This is possible considered a strong control due to the east-west-trending synsedimentary transcurrent faults which cuts the Thrace Basin, generating a series of depocenters and uplifts which deeply influenced sediment dispersal and the areal distribution of paleoenvironments. The Thrace Basin was long interpreted as a forearc basin between a magmatic arc to the north and a subduction-accretion complex to the south, developed in a context of northward subduction. This interpretation was challenged by more recent data emphasizing the lack of a coeval magmatic arc in the north and the interpretation of the chaotic deposit which outcrop south of Ganos Fault as olistoliths and large submarine slumps, derived from the erosion and sedimentary reworking of an older mélange unit located to the south (not as tectonic mélange formed in an accretionary prism). The present study corroborates instead the hypothesis of a post-collisional origin of the Thrace Basin, due to a phase of orogenic collapse, which generated a series of mid-Eocene depocenters all along the İzmir-Ankara suture (following closure of the Vardar-İzmir-Ankara ocean and the ensuing collision); then the slab roll-back of the remnant Pindos ocean played an important role in enhancing subsidence and creating additional accommodation space for sediment deposition.