Evaluation of a multi variated analysis for the selection of t-tbar multijet events in the current CMS implemented environment at LHC

In the present study we are using multi variate analysis techniques to discriminate signal from background in the fully hadronic decay channel of ttbar events. We give a brief introduction to the role of the Top quark in the standard model and a general description of the CMS Experiment at LHC. We have used the CMS experiment computing and software infrastructure to generate and prepare the data samples used in this analysis. We tested the performance of three different classifiers applied to our data samples and used the selection obtained with the Multi Layer Perceptron classifier to give an estimation of the statistical and systematical uncertainty on the cross section measurement.

Reconstruction of CNGS neutrino events in the emulsions of the OPERA experiment

The OPERA experiment aims at the direct observation of ν_mu -> ν_tau oscillations in the CNGS (CERN Neutrinos to Gran Sasso) neutrino beam produced at CERN; since the ν_e contamination in the CNGS beam is low, OPERA will also be able to study the sub-dominant oscillation channel ν_mu -> ν_e. OPERA is a large scale hybrid apparatus divided in two supermodules, each equipped with electronic detectors, an iron spectrometer and a highly segmented ~0.7 kton target section made of Emulsion Cloud Chamber (ECC) units. During my research work in the Bologna Lab. I have taken part to the set-up of the automatic scanning microscopes studying and tuning the scanning system performances and efficiencies with emulsions exposed to a test beam at CERN in 2007. Once the triggered bricks were distributed to the collaboration laboratories, my work was centered on the procedure used for the localization and the reconstruction of neutrino events.

Slope stability analysis by multi-temporal DEMs and 3D modelling: The 2002 and 2007 Stromboli landslide events

Natural hazard related to the volcanic activity represents a potential risk factor, particularly in the vicinity of human settlements. Besides to the risk related to the explosive and effusive activity, the instability of volcanic edifices may develop into large landslides often catastrophically destructive, as shown by the collapse of the northern flank of Mount St. Helens in 1980. A combined approach was applied to analyse slope failures that occurred at Stromboli volcano. SdF slope stability was evaluated by using high-resolution multi-temporal DTMMs and performing limit equilibrium stability analyses. High-resolution topographical data collected with remote sensing techniques and three-dimensional slope stability analysis play a key role in understanding instability mechanism and the related risks. Analyses carried out on the 2002–2003 and 2007 Stromboli eruptions, starting from high-resolution data acquired through airborne remote sensing surveys, permitted the estimation of the lava volumes emplaced on the SdF slope and contributed to the investigation of the link between magma emission and slope instabilities. Limit Equilibrium analyses were performed on the 2001 and 2007 3D models, in order to simulate the slope behavior before 2002-2003 landslide event and after the 2007 eruption. Stability analyses were conducted to understand the mechanisms that controlled the slope deformations which occurred shortly after the 2007 eruption onset, involving the upper part of slope. Limit equilibrium analyses applied to both cases yielded results which are congruent with observations and monitoring data. The results presented in this work undoubtedly indicate that hazard assessment for the island of Stromboli should take into account the fact that a new magma intrusion could lead to further destabilisation of the slope, which may be more significant than the one recently observed because it will affect an already disarranged deposit and fractured and loosened crater area. The two-pronged approach based on the analysis of 3D multi-temporal mapping datasets and on the application of LE methods contributed to better understanding volcano flank behaviour and to be prepared to undertake actions aimed at risk mitigation.

Sviluppo e validazione sperimentale di strategie di previsione e controllo del fenomeno della preaccensione (Mega-Knock)

L’algoritmo per la previsione del Mega-Knock si inserisce all’interno di uno dei temi cardine dell’attuale ricerca nel campo motoristico: la minimizzazione del consumo di combustibile nei motori ad alto grado di sovralimentazione, sviluppati nell’ottica del downsizing. La possibilità di prevedere l’innescarsi del Mega-Knock consente di ottimizzare la definizione dell’obiettivo di titolo, evitando arricchimenti non necessari in un range di funzionamento del motore che frequentemente viene esplorato nella normale guida su strada. Si tratterà la possibilità di utilizzare una relazione empirica per cercare di arrivare alla previsione dell’insorgere della preaccensione, per poi ricorrere ad opportune strategie motore per evitare il verificarsi del fenomeno; il tutto tramite lo sviluppo di un algoritmo in ambiente MatLab-Simulink

Events Management: il caso FPA Worlds 2012

Un problema comune agli Ingegneri Gestionali è quello legato alla necessità di dover sempre spiegare in cosa consista veramente il proprio campo di studi. Amici, conoscenti e parenti non dimostrano mai, infatti, familiarità con il termine. Chi scrive è costretto addirittura ad ammettere di avere una madre che, a pochi giorni dalla discussione dalla Tesi Magistrale, continui ad affermare di non aver ancora capito quale lavoro andrà poi a fare il figlio. Medicina, Giurisprudenza ed Economia sono concetti facili da comprendere; “studiare con approccio quantitativo l'organizzazione e i processi produttivi delle imprese costruendo e applicando modelli per la soluzione dei loro problemi” in effetti lo è un po’ meno. Accade così che si debbano quindi aggiungere altri termini, spiegando l’ingegneria gestionale come insieme di altre discipline: produzione, logistica, marketing, economia aziendale, risorse umane, gestione, progetti... Si dà il caso che questo insieme di altre discipline coincida in larga parte con una branca ancora più oscura ai più: l’event management. Questo lavoro di Tesi è incentrato proprio sulla gestione di un evento: gli FPA Worlds 2012, i Mondiali di Frisbee Freestyle 2012 tenutisi a Riccione dal 2 al 5 agosto. L’autore, nell’ambito del suo percorso di Tirocinio, ne è stato l’event manager, ovvero il massimo responsabile e organizzatore, andando a far confluire esperienze, conoscenze e passioni personali con la coronazione degli studi universitari. L’intero progetto lo ha coinvolto dal luglio 2010 al settembre 2012, all’interno di un’azienda riminese con cui già collaborava dal 2009. La Tesi, di carattere prettamente sperimentale, va quindi ad esporre i processi gestionali “nascosti” dietro ad un evento che ha riscosso successo di pubblico e mediatico, affiancando in ognuno dei capitoli tematici modelli teorici e risultati pratici. La vastità di conoscenze, competenze e strumenti utilizzati ha reso quest’esperienza altamente stimolante, così come le numerose sfide che si sono succedute nel difficile percorso per organizzare il miglior Mondiale di Frisbee Freestyle di sempre.

Die Re-Definition der Wirklichkeit durch Motto-Events

Eine aktuelle Ausprägung der Veranstaltungslandschaft sind die so genannten Motto-Events, die die Inszenierung einer Anderswelt-Konstruktion einsetzen, um emotionale und kommunikatorische Ziele zu erreichen. Dabei werden themengebundene Entwürfe räumlich und inhaltlich in die lebensweltliche Wirklichkeit transportiert und auf diese Weise eine dynamische und integrative Scheinwelt erschaffen. In dieser konstruierten Welt können schließlich Abenteuer erlebt und heroische Taten begangen werden. Durch die reziproke Beeinflussung von Inszenierung und Handlung befinden sich die Akteure außerhalb der gesellschaftlichen Norm, sie erleben innerhalb der "gated community" der Motto-Veranstaltung eine re-definierte Wirklichkeit. Aus einer Kombination von aktiven und passiven Elementen werden homogene Klischees inszeniert, die durch ihren Bekanntheitsgrad eine hohe Anschlussfähigkeit der Teilnehmer garantieren. Die vorliegende Arbeit beschäftigt sich mit den Mechanismen, die diese re-definierte Wirklichkeit in Szene setzen. Dadurch wird es möglich, in einer zusammenfassenden Betrachtung die Rezeption verschiedener Event-Modelle zu beschreiben und Handlungsempfehlungen zu geben.

Conversione per il Semantic Web di dati Turistico-Culturali: il progetto QRPlaces - Semantic Events

Il progetto QRPlaces - Semantic Events, oggetto di questo lavoro, focalizza l’attenzione sull’analisi, la progettazione e l’implementazione di un sistema che sia in grado di modellare i dati, relativi a diversi eventi facenti parte del patrimonio turistico - culturale della Regione Emilia Romagna 1, rendendo evidenti i vantaggi associati ad una rappresentazione formale incentrata sulla Semantica. I dati turistico - culturali sono intesi in questo ambito sia come una rappresentazione di “qualcosa che accade in un certo punto ad un certo momento” (come ad esempio un concerto, una sagra, una raccolta fondi, una rappresentazione teatrale e quant’altro) sia come tradizioni e costumi che costituiscono il patrimonio turistico-culturale e a cui si fa spesso riferimento con il nome di “Cultural Heritage”. Essi hanno la caratteristica intrinseca di richiedere una conoscenza completa di diverse informa- zioni correlata, come informazioni di geo localizzazione relative al luogo fisico che ospita l’evento, dati biografici riferiti all’autore o al soggetto che è presente nell’evento piuttosto che riferirsi ad informazioni che descrivono nel dettaglio tutti gli oggetti, come teatri, cinema, compagnie teatrali che caratterizzano l’evento stesso. Una corretta rappresentazione della conoscenza ad essi legata richiede, pertanto, una modellazione in cui i dati possano essere interconnessi, rivelando un valore informativo che altrimenti resterebbe nascosto. Il lavoro svolto ha avuto lo scopo di realizzare un dataset rispondente alle caratteristiche tipiche del Semantic Web grazie al quale è stato possibile potenziare il circuito di comunicazione e informazione turistica QRPlaces 2. Nello specifico, attraverso la conversione ontologica di dati di vario genere relativi ad eventi dislocati nel territorio, e sfruttando i principi e le tecnologie del Linked Data, si è cercato di ottenere un modello informativo quanto più possibile correlato e arricchito da dati esterni. L’obiettivo finale è stato quello di ottenere una sorgente informativa di dati interconnessi non solo tra loro ma anche con quelli presenti in sorgenti esterne, dando vita ad un percorso di collegamenti in grado di evidenziare una ricchezza informativa utilizzabile per la creazione di valore aggiunto che altrimenti non sarebbe possibile ottenere. Questo aspetto è stato realizzato attraverso un’in- terfaccia di MashUp che utilizza come sorgente il dataset creato e tutti i collegamenti con la rete del Linked Data, in grado di reperire informazioni aggiuntive multi dominio.

Molekularbiologische Charakterisierung der beiden Untereinheiten des Mega-Hämocyanins der Schnecke Melanoides tuberculata

Bei dem 2010 von unserer Arbeitsgruppe entdeckten Mega-Hämocyanin handelt es sich um einen stark abgewandelten Typ des respiratorischen Proteins Hämocyanin, bestehend aus zwei flankierenden regulären Dekameren und einem zentralen Mega-Dekamer. Diese sind aus zwei immunologisch verschiedenen Untereinheiten mit ~400 bzw. ~550 kDa aufgebaut, die in unserer Arbeitsgruppe bereits proteinbiochemisch charakterisiert wurden. Im Zuge dieser Untersuchungen konnte zudem eine 3D-Rekonstruktion des Oligomers (13,5 MDa) mit einer Auflösung von 13Å erstellt werden. Das Ziel der vorliegenden Arbeit war die Aufklärung der Primärstruktur beider Polypeptide bei der Schnecke Melanoides tuberculata (MtH). Es gelang, die cDNAs der beiden Untereinheiten vollständig zu sequenzieren. Die zu typischen Dekameren assemblierende MtH400-Untereinheit umfasst 3445 Aminosäuren und besitzt eine theoretische Molekularmasse von 390 kDa. Nach dem Signalpeptid von 23 Aminosäuren Länge folgen die für Gastropoden-Hämocyanine typischen funktionellen Einheiten FU-a bis FU-h. Insgesamt verfügt die MtH400-Untereinheit über sechs potentielle N-Glykosylierungsstellen. Die MtH550-Untereinheit, welche mit 10 Kopien das Mega-Dekamer bildet, umfasst 4999 Aminosäuren und besitzt eine theoretische Molekularmasse von 567 kDa. Damit handelt es sich bei dieser Untereinheit um die zweitgrößte jemals bei einem Protein detektierte Polypeptidkette. Die MtH550-Untereinheit besteht aus einem Signalpeptid von 20 Aminosäuren Länge und den typischen Wand-FUs (FU-a bis FU-f). Daran anschließend folgen sechs weitere Varianten der FU-f (FU-f1 bis FU-f6). Die MtH550-Untereinheit verfügt über insgesamt zwölf potentielle N-Glykosylierungsstellen. Anhand der ermittelten Primärstrukturdaten wird klar, dass der auffällig vergrößerte Kragenbereich des Mega-Dekamers aus je 10 Kopien der FU-f1 bis FU-f6 besteht. Die ermittelten Sequenzdaten der beiden MtH-Untereinheiten weisen im Vergleich zu anderen Hämocyanin Sequenzen einige sehr charakteristische Indels sowie unübliche N-Glykosylierungsstellen auf. Es war zudem möglich, anhand einer molekularen Uhr den Entstehungszeitpunkt des Mega-Hämocyanins zu datieren (145 ± 35 MYA). Sowohl die Topologie als auch die berechneten Trennungszeitpunkte des an allen Verzweigungen gut unterstützten Stammbaums stimmen mit den bisher publizierten und auf Hämocyanindaten basierenden molekularen Uhren überein.

Inversion of low frequency seismo-volcanic events

The inversion of seismo-volcanic events is performed to retrieve the source geometry and to determine volumetric budgets of the source. Such observations have shown to be an important tool for the seismological monitoring of volcanoes. We developed a novel technique for the non-linear constrained inversion of low frequency seismo-volcanic events. Unconstrained linear inversion methods work well when a dense network of broadband seismometers is available. We propose a new constrained inversion technique, which has shown to be efficient also in a reduced network configuration and a low signal-noise ratio. The waveform inversion is performed in the frequency domain, constraining the source mechanism during the event to vary only in its magnitude. The eigenvectors orientation and the eigenvalue ratio are kept constant. This significantly reduces the number of parameters to invert, making the procedure more stable. The method has been tested over a synthetic dataset, reproducing realistic very-long-period (VLP) signals of Stromboli volcano. The information obtained by performing the synthetic tests is used to assess the reliability of the results obtained on a VLP dataset recorded on Stromboli volcano and on a low frequency events recorded at Vesuvius volcano.

Analysis of cerebral and autonomic response to respiratory events in patients with Sleep Apnea Syndrome

The arousal scoring in Obstructive Sleep Apnea Syndrome (OSAS) is important to clarify the impact of the disease on sleep but the currently applied American Academy of Sleep Medicine (AASM) definition may underestimate the subtle alterations of sleep. The aims of the present study were to evaluate the impact of respiratory events on cortical and autonomic arousal response and to quantify the additional value of cyclic alternating pattern (CAP) and pulse wave amplitude (PWA) for a more accurate detection of respiratory events and sleep alterations in OSAS patients. A retrospective revision of 19 polysomnographic recordings of OSAS patients was carried out. Analysis was focused on quantification of apneas (AP), hypopneas (H) and flow limitation (FL) events, and on investigation of cerebral and autonomic activity. Only 41.1% of FL events analyzed in non rapid eye movement met the AASM rules for the definition of respiratory event-related arousal (RERA), while 75.5% of FL events ended with a CAP A phase. The dual response (EEG-PWA) was the most frequent response for all subtypes of respiratory event with a progressive reduction from AP to H and FL. 87.7% of respiratory events with EEG activation showed also a PWA drop and 53,4% of the respiratory events without EEG activation presented a PWA drop. The relationship between the respiratory events and the arousal response is more complex than that suggested by the international classification. In the estimation of the response to respiratory events, the CAP scoring and PWA analysis can offer more extensive information compared to the AASM rules. Our data confirm also that the application of PWA scoring improves the detection of respiratory events and could reduce the underestimation of OSAS severity compared to AASM arousal.

Cascading events triggering industrial accidents: quantitative assessment of NaTech and domino scenarios

The so called cascading events, which lead to high-impact low-frequency scenarios are rising concern worldwide. A chain of events result in a major industrial accident with dreadful (and often unpredicted) consequences. Cascading events can be the result of the realization of an external threat, like a terrorist attack a natural disaster or of “domino effect”. During domino events the escalation of a primary accident is driven by the propagation of the primary event to nearby units, causing an overall increment of the accident severity and an increment of the risk associated to an industrial installation. Also natural disasters, like intense flooding, hurricanes, earthquake and lightning are found capable to enhance the risk of an industrial area, triggering loss of containment of hazardous materials and in major accidents. The scientific community usually refers to those accidents as “NaTechs”: natural events triggering industrial accidents. In this document, a state of the art of available approaches to the modelling, assessment, prevention and management of domino and NaTech events is described. On the other hand, the relevant work carried out during past studies still needs to be consolidated and completed, in order to be applicable in a real industrial framework. New methodologies, developed during my research activity, aimed at the quantitative assessment of domino and NaTech accidents are presented. The tools and methods provided within this very study had the aim to assist the progress toward a consolidated and universal methodology for the assessment and prevention of cascading events, contributing to enhance safety and sustainability of the chemical and process industry.

Holocene tsunami events in the Eastern Ionian Sea - Geoscientific evidence from Cefalonia and the western Peloponnese (Greece)

This study presents geo-scientific evidence for Holocene tsunami impact along the shores of the Eastern Ionian Sea. Cefalonia Island, the Gulf of Kyparissia and the Gialova Lagoon were subject of detailed geo-scientific investigations. It is well known that the coasts of the eastern Mediterranean were hit by the destructive influence of tsunamis in the past. The seismically highly active Hellenic Trench is considered as the most significant tsunami source in the Eastern Ionian Sea. This study focuses on the reconstruction and detection of sedimentary signatures of palaeotsunami events and their influence on the Holocene palaeogeographical evolution. The results of fine grained near coast geo-archives are discussed and interpreted in detail to differentiate between tsunami, storm and sea level highstands as sedimentation processes.rnA multi-method approach was applied using geomorphological, sedimentological, geochemical, geophysical and microfaunal analyses to detect Holocene tsunamigenic impact. Chronological data were based on radiocarbondatings and archaeological age estimations to reconstruct local geo-chronostratigraphies and to correlate them on supra-regional scales.rnDistinct sedimentary signatures of 5 generations of tsunami impact were found along the coasts of Cefalonia in the Livadi coastal plain. The results show that the overall coastal evolution was influenced by tsunamigenic impact that occured around 5700 cal BC (I), 4250 cal BC (II), at the beginning of the 2nd millennium cal BC (III), in the 1st millennium cal BC (IV) and posterior to 780 cal AD (V). Sea level reconstructions and the palaeogeographical evolution show that the local Holocene sea level has never been higher than at present.rnAt the former Mouria Lagoon along the Gulf of Kyparissia almost four allochtonous layers of tsunamigenic origin were identified. The stratigraphical record and palaeogeographical reconstructions show that major environmental coastal changes were linked to these extreme events. At the southern end of the Agoulenitsa Lagoon at modern Kato Samikon high-energy traces were found more than 2 km inland and upt ot 9 m above present sea level. The geo-chronological framework deciphered tsunami landfall for the 5th millennium cal BC (I), mid to late 2nd mill. BC (II), Roman times (1st cent. BC to early 4th cent. AD) (III) and most possible one of the historically well-known 365 AD or 521/551 AD tsunamis (IV).rnCoarse-grained allochthonous sediments of marine origin were found intersecting muddy deposits of the quisecent sediments of the Gialova Lagoon on the southwestern Peloponnese. Radiocarbondatings suggest 6 generations of major tsunami impact. Tsunami generations were dated to around 3300 cal BC (I), around the end of 4th and the beginning of 3rd millennium BC (II), after around 1100 cal BC (III), after the 4th to 2nd cent. BC (IV), between the 8th and early 15th cent. AD (V) and between the mid 14th to beginning of 15th cent. AD (VI). Palaeogeographical and morphological characteristics in the environs of the Gialova Lagoon were controlled by high-energy influence.rnSedimentary findings in all study areas are in good accordance to traces of tsunami events found all over the Ionian Sea. The correlation of geo-chronological data fits very well to coastal Akarnania, the western Peloponnese and finding along the coasts of southern Italy and the Aegean. Supra-regional influence of tsunamigenic impact significant for the investigated sites. The palaeogeographical evolution and palaeo-geomorphological setting of the each study area was strongly affected by tsunamigenic impact.rnThe selected geo-archives represent extraordinary sediment traps for the reconstruction of Holocene coastal evolution. Our result therefore give new insight to the exceptional high tsunami risk in the eastern Mediterranean and emphasize the underestimation of the overall tsunami hazard.

Ancient Greek harbours used as geo-archives for palaeotsunami research : case studies from Krane (Cefalonia), Lechaion (Gulf of Corinth) and Kyllini (Peloponnese)

Since historical times, coastal areas throughout the eastern Mediterranean are exposed to tsunami hazard. For many decades the knowledge about palaeotsunamis was solely based on historical accounts. However, results from timeline analyses reveal different characteristics affecting the quality of the dataset (i.e. distribution of data, temporal thinning backward of events, local periodization phenomena) that emphasize the fragmentary character of the historical data. As an increasing number of geo-scientific studies give convincing examples of well dated tsunami signatures not reported in catalogues, the non-existing record is a major problem to palaeotsunami research. While the compilation of historical data allows a first approach in the identification of areas vulnerable to tsunamis, it must not be regarded as reliable for hazard assessment. Considering the increasing economic significance of coastal regions (e.g. for mass tourism) and the constantly growing coastal population, our knowledge on the local, regional and supraregional tsunami hazard along Mediterranean coasts has to be improved. For setting up a reliable tsunami risk assessment and developing risk mitigation strategies, it is of major importance (i) to identify areas under risk and (ii) to estimate the intensity and frequency of potential events. This approach is most promising when based on the analysis of palaeotsunami research seeking to detect areas of high palaeotsunami hazard, to calculate recurrence intervals and to document palaeotsunami destructiveness in terms of wave run-up, inundation and long-term coastal change. Within the past few years, geo-scientific studies on palaeotsunami events provided convincing evidence that throughout the Mediterranean ancient harbours were subject to strong tsunami-related disturbance or destruction. Constructed to protect ships from storm and wave activity, harbours provide especially sheltered and quiescent environments and thus turned out to be valuable geo-archives for tsunamigenic high-energy impacts on coastal areas. Directly exposed to the Hellenic Trench and extensive local fault systems, coastal areas in the Ionian Sea and the Gulf of Corinth hold a considerably high risk for tsunami events, respectively.Geo-scientific and geoarcheaological studies carried out in the environs of the ancient harbours of Krane (Cefalonia Island), Lechaion (Corinth, Gulf of Corinth) and Kyllini (western Peloponnese) comprised on-shore and near-shore vibracoring and subsequent sedimentological, geochemical and microfossil analyses of the recovered sediments. Geophysical methods like electrical resistivity tomography and ground penetrating radar were applied in order to detect subsurface structures and to verify stratigraphical patterns derived from vibracores over long distances. The overall geochronological framework of each study area is based on radiocarbon dating of biogenic material and age determination of diagnostic ceramic fragments. Results presented within this study provide distinct evidence of multiple palaeotsunami landfalls for the investigated areas. Tsunami signatures encountered in the environs of Krane, Lechaion and Kyllini include (i) coarse-grained allochthonous marine sediments intersecting silt-dominated quiescent harbour deposits and/or shallow marine environments, (ii) disturbed microfaunal assemblages and/or (iii) distinct geochemical fingerprints as well as (iv) geo-archaeological destruction layers and (v) extensive units of beachrock-type calcarenitic tsunamites. For Krane, geochronological data yielded termini ad or post quem (maximum ages) for tsunami event generations dated to 4150 ± 60 cal BC, ~ 3200 ± 110 cal BC, ~ 650 ± 110 cal BC, and ~ 930 ± 40 cal AD, respectively. Results for Lechaion suggest that the harbour was hit by strong tsunami impacts in the 8th-6th century BC, the 1st-2nd century AD and in the 6th century AD. At Kyllini, the harbour site was affected by tsunami impact in between the late 7th and early 4th cent. BC and between the 4th and 6th cent. AD. In case of Lechaion and Kyllini, the final destruction of the harbour facilities also seems to be related to the tsunami impact. Comparing the tsunami signals obtained for each study areas with geo-scientific data from palaeotsunami events from other sites indicates that the investigated harbour sites represent excellent geo-archives for supra-regional mega-tsunamis.