Estudo retrospectivo de ferimentos cardíacos ocorridos em Manaus/AM

OBJETIVO: Avaliar as formas de tratamento empregadas e os principais aspectos relacionados à morbidade e à mortalidade dos ferimentos cardíacos.. MÉTODOS: Estudo retrospectivo de 102 doentes com lesão cardíaca, atendidos nos dois prontos socorros de Manaus (Pronto Socorro Municipal 28 de Agosto e Hospital Pronto Socorro Dr. João Lúcio P. Machado) no período de janeiro de 1998 a junho de 2006. RESULTADOS: Dos 102 doentes, 95,1% eram homens; a média de idade foi 27 anos; ferimentos por arma branca representaram 81,4% dos casos, contra 18,6% por arma de fogo; cardiorrafia foi realizada em 98,1% dos casos. As câmaras cardíacas atingidas foram: VD: 43,9% (36,2% isoladamente e 7,7% associada a outras câmaras); VE: 37,2%; AD: 8,5% e AE: 10,4%, com mortalidades específicas de 21%, 23%, 22% e 45%, respectivamente. Lesões de duas câmaras associadas alcançaram mortalidade de 37,5%, sendo 20% para VD+AD, 100% para VD+VE e zero para VD+AE. O pulmão correspondeu a 33,7% de 89 lesões associadas. Os tempos médios de cirurgia e de internação foram de 121 minutos e 8,2 dias, respectivamente. Cerca de 22,5% complicaram representando 41 complicações. A mortalidade foi 28,4%. Lesões grau IV e V corresponderam a 55% e 41% dos casos, com mortalidade específica de 26% e 15%, respectivamente. Todos os doentes com lesão grau VI morreram. CONCLUSÃO: O ferimentos cardíacos por arma branca estiveram associados a menor mortalidade, as lesões cardíacas grau IV estiveram associadas à maior mortalidade e um menor tempo operatório esteve associado à maior gravidade e mortalidade.

Dynamics of the cold surface layer of polythermal Storglaciären, Sweden

Polythermal glaciers, i.e. glaciers with a combination of ice at and below the freezing point, are widespread in arctic and subarctic environments. The polythermal structure has major implications for glacier hydrology, ice flow and glacial erosion. However, the interplay of factors governing its spatial and temporal variations such as net mass balance, ice advection and water content in the ice is poorly investigated and as yet not fully understood. This study deals with a thorough investigation of the polythermal regime on Storglaciären, northern Sweden, a small valley glacier with a cold surface layer in the ablation area. Extensive field work was performed including mapping of the cold surface layer using ground-penetrating radar, ice temperature measurements, mass balance and ice velocity measurements. Analyses of these data combined with numerical modelling were used specifically to investigate the spatial and temporal variability of the cold surface layer, the spatial distribution of the water content just below the cold surface layer transition, the effect of radar frequency on the detection of the surface layer, and the sensitivity of the cold surface layer to changes in forcing. A comparison between direct temperature measurements in boreholes and ground-penetrating surveys shows that the radar-inferred cold-temperate transition depth is within ±1 m from the melting point of ice at frequencies above ~300 MHz. At frequencies below ~155 MHz, the accuracy degrades because of reduced scattering efficiency that occurs when the scatterers become much smaller compared to the wavelength. The mapped spatial pattern of the englacial cold-temperate transition boundary is complex. This pattern reflects the observed spatial variation in net loss of ice at the surface by ablation and vertical advection of ice, which is suggested to provide the predominant forcing of the cold surface layer thickness pattern. This is further supported by thermomechanical modeling of the cold surface layer, which indicates high sensitivity of the cold surface layer thickness to changes in vertical advection rates. The water content is the least investigated quantity that is relevant for the thermal regime of glaciers, but also the most difficult to assess. Spatial variability of absolute water content in the temperate ice immediately below the cold surface layer on Storglaciären was determined by combining relative estimates of water content from ground-penetrating radar data with absolute determination from temperature measurements and the thermal boundary condition at the freezing front. These measurements indicate large-scale spatial variability in the water content, which seems to arise from variations in entrapment of water at the firn-ice transition. However, this variability cannot alone explain the spatial pattern in the thermal regime on Storglaciären. Repeated surveys of the cold surface layer show a 22% average thinning of the cold surface layer on Storglaciären between 1989 and 2001. Transient thermomechanical modeling results suggest that the cold surface layer adapts to new equilibrium conditions in only a few decades after a perturbation in the forcing is introduced. An increased winter air temperature since mid-1980s seems to be the cause of the observed thinning of the cold surface layer. Over the last decades, mass balance measurements indicate that the glacier has been close to a steady state. The quasi-steady state situation is also reflected in the vertical advection, which shows no significant changes during the last decades. Increased winter temperatures at the ice surface would result in a slow-down of the formation of cold ice at the base of the cold surface layer and lead to a larger imbalance between net loss of ice at the surface and freezing of temperate ice at the cold-temperate transition.

Applicazione ed integrazione di metodi di prospezione geofisica: studio idrogeofisico della Zona Insatura in condizioni idriche controllate

Il lavoro è incentrato sull’applicazione ed integrazione di differenti tecniche di indagine geofisica in campo ambientale e ingegneristico/archeologico. Alcuni esempi sono stati descritti al fine di dimostrare l’utilità delle metodologie geofisiche nella risoluzione di svariate problematiche. Nello specifico l’attenzione è stata rivolta all’utilizzo delle tecniche del Ground Penetrating Radar e del Time Domain Reflectometry in misure condotte su un corpo sabbioso simulante una Zona Insatura. L’esperimento è stato realizzato all’interno di un’area test costruita presso l’azienda agricola dell’Università La Tuscia di Viterbo. Hanno partecipato al progetto le Università di Roma Tre, Roma La Sapienza, La Tuscia, con il supporto tecnico della Sensore&Software. Nello studio è stato condotto un approccio definito idrogeofisico al fine di ottenere informazioni da misure dei parametri fisici relativi alla Zona Insatura simulata nell’area test. Il confronto e l’integrazione delle due differenti tecniche di indagine ha offerto la possibilità di estendere la profondità di indagine all’interno del corpo sabbioso e di verificare l’utilità della tecnica GPR nello studio degli effetti legati alle variazioni del contenuto d’acqua nel suolo, oltre a determinare la posizione della superficie piezometrica per i differenti scenari di saturazione. Uno specifico studio è stato realizzato sul segnale radar al fine di stabilire i fattori di influenza sulla sua propagazione all’interno del suolo. Il comportamento dei parametri dielettrici nelle condizioni di drenaggio e di imbibizione del corpo sabbioso è stato riprodotto attraverso una modellizzazione delle proprietà dielettriche ed idrologiche sulla base della dimensione, forma e distribuzione dei granuli di roccia e pori, nonché sulla base della storia relativa alla distribuzione dei fluidi di saturazione all’interno del mezzo. La modellizzazione è stata operata sulle basi concettuali del Differential Effective Medium Approximation.

Untersuchungen zum infektiösen Aufnahmeweg des humanen Papillomvirus HPV33

Nicht-umhüllte humane Papillomviren binden an Heparansulfatproteoglykane (HSPG) der Zelloberfläche und werden durch Endocytose in Zielzellen aufgenommen. Um eine effiziente Infektion zu etablieren, muss die virale DNA in den Zellkern transportiert werden. Auf welche Art und Weise hierbei die Endosomenmembran überwunden wird, war bislang völlig unklar. Die Suche nach potentiellen membrandestabilisierenden Eigenschaften der Kapsidproteine L1 und L2 von HPV führte im Vorfeld der vorliegenden Dissertation zur Identifizierung eines carboxyterminalen Peptids des minoren L2-Proteins, welches als sehr mikrobizid und fungizid beschrieben werden konnte. Es ist gekennzeichnet durch einen Bereich basischer und einen Bereich hydrophober Aminosäuren. Da das minore L2-Protein für den Infektionsprozess von Papillomviren essentiell ist, wurde im Rahmen dieser Arbeit die Rolle des C-terminalen Peptids für den Transport des infektiösen Materials durch die zelluläre Membranbarriere genauer untersucht. Es konnte gezeigt werden, dass das carboxyterminale L2-Peptid von HPV33 nach externer Zugabe eine cytotoxische Wirkung auf höhere eukaryotische Zellen hat. Es lokalisiert an zellulären Membranen und induziert eine pH-abhängige Reduktion des ATP-Gehalts von Säugerzellen. Weiter wurde nachgewiesen, dass das Peptid die Cytoplasmamembran permeabilisieren und für kleine, hydrophile Substanzen wie Propidiumjodid durchlässig machen kann. Mutationen innerhalb des Peptids verdeutlichten die Notwendigkeit beider Bereiche, basischer und hydrophober Aminosäuren, für den membrandestabilisierenden Effekt. Im Folgenden wurde die intrazelluläre Aktivität des L2-Peptids mit Hilfe von GFP2-Peptid-Fusionen analysiert. Das Peptid ist in der Lage, eine Integration des globulären GFP-Dimers in Membranen zu vermitteln, was bei einem hohen Prozentsatz der exprimierenden Zellen zum Absterben führt. Auch wt 33L2 weist im Gegensatz zu C-terminalen Deletions- und Punktmutanten die Fähigkeit zur Membranassoziation auf. Abschließend wurde der Effekt von Mutationen innerhalb dieses L2-Peptids auf die Infektiösität von L1/L2-Pseudovirionen beschrieben. Die Mutationen haben keinen Einfluss auf den Einbau des L2-Proteins in die Pseudovirionen und auf die DNA-Verpackung. Die Virusmorphogenese ist somit nicht negativ beeinträchtigt. Die Infektiösität der HPV33- wie auch von HPV16-Pseudovirionen mit C-terminal mutiertem L2-Protein ist jedoch auf das Niveau von solchen reduziert, die nur aus dem majoren L1 bestehen und geht gegen Null. Zusammenfassend kann man festhalten, dass das minore Kapsidprotein L2 von HPV am Carboxyterminus eine membrandestabilisierende Aktivität besitzt, welche unter Papillomviren konserviert und für eine effektive Infektion essentiell ist.

Electron identification and reconstruction with the OPERA ECC bricks and search for muon neutrino to electron neutrino oscillations

The procedure for event location in OPERA ECC has been optimazed for penetrating particles while is less efficient for electrons. For this reason new procedure has been defined in order to recover event with an electromagnetic shower in its final state not located with the standard one. The new procedure include the standard procedure during which several electromagnetic shower hint has been defined by means of the available data. In case the event is not located, the presence of an electromagnetic shower hint trigger a dedicated procedure. The old and new location procedure has been then simulated in order to obtain the standard location efficiency and the possible gain due to the new one for the events with electromagnetic shower. Finally a Data-MC comparison has been performed for the 2008 and 2009 runs for what concern the NC in order to validate the Monte Carlo. Then the expected electron neutrino interactions for the 2008 and 2009 runs has been evaluated and compared with the available data.

Aktivierung von Hämocyanin zur Tyrosinase

Ziel der Arbeit war die enzymatische Aktivierung von Cheliceraten-Hämocyanin zur Erforschung ihrer Phenoloxidase-Aktivität. Hierzu wurden zwei Hämocyanine in vergleichenden Untersuchungen herangezogen: Das bekannte 24-mer aus der Spinne Eurypelma californicum und das ebenfalls 24-mere Hämocyanin des Skorpions Pandinus imperator, dessen Struktur hier aufgeklärt wurde. Elektronenmikroskopisch und in der dynamischer Lichtstreuung sind sich beide Hämocyanine sehr ähnlich und sedimentieren bei analytischer Ultrazentrifugation ebenfalls in gleicher Weise (Sedimentationskoeffizient von 37 S (S20, W)). Durch Dissoziation im alkalischen Milieu gewinnt man bis zu zwölf Untereinheiten, von denen sich neun immunologisch unterscheiden lassen. Das absorptionsspektroskopische Verhalten von P. imperator- und E. californicum-Hämocyanin sowie Sekundärstrukturanalyse mittels CD-Spektroskopie ist nahezu identisch. Die Stabilität des Hämocyanins gegenüber Temperatur und Denaturierungsmitteln wurde mit Circulardichroismus- und Fluoreszenzspektroskopie sowie durch die enzymatische Aktivität untersucht. Erstmals konnten die Hämocyanine von P. imperator und E. californicum nicht nur zu einer stabilen Diphenoloxidase umgewandelt werden, sondern auch eine Monophenolhydroxylase-Aktivität induziert und reguliert werden. Für letztere Aktivität ist dabei die Präsenz von Tris- oder Hepes-Puffer wesentlich. Während sich die Monophenolhydroxylase-Aktivität nur auf Ebene der oligomeren Zustände beobachten lässt, erkennt man bei den isolierten Untereinheiten-Typen lediglich eine Diphenoloxidase-Aktivität. Bei dem Spinnen-Hämocyanin zeigen die Untereinheiten bc die stärkste katalytische Aktivität auf, bei P. imperator-Hämocyanin findet man drei bis vier Untereinheiten, die enzymatisch aktiv sind. Die Aktivierung mit SDS liefert den Hinweis, dass die Quartärstruktur in eine andere Konformation gebracht und nicht durch SDS denaturiert wird. Zugabe von Mg2+ reguliert die Phenoloxidase-Aktivität und verschiebt bei P. imperator-Hämocyanin die enzymatische Aktivität zugunsten der Diphenoloxidase. Mit keiner der zur Verfügung stehenden Methoden konnte jedoch ein Konformationsübergang eindeutig nachgewiesen werden. Die Stabilität scheint durch die niedrigen SDS-Konzentrationen nicht beeinträchtigt zu werden. Die sehr lange “Verzögerungsphase“ bei der Monophenolhydroxylase-Aktivität konnte durch Zugabe von katalytischem Diphenol drastisch verkürzt werden, was ein Hinweis auf die echte Tyrosinase-Aktivität des aktivierten Hämocyanins ist. Ein in vivo-Aktivator konnte bis jetzt noch nicht gefunden werden. Trotzdem scheinen die Hämocyanine in der Immunologie von Cheliceraten eine bedeutende Rolle zu spielen, indem sie die Rolle der Tyrosinasen / Phenoloxidasen beziehungsweise Catecholoxidasen übernehmen, die bei Cheliceraten nicht vorkommen. Weitere Möglichkeiten des Cheliceraten-Immunsystems, eindringende Fremdorganismen abzuwehren, wurden untersucht. Das Fehlen einer ´echten` Phenoloxidase-Aktivität bei den Cheliceraten, mit der Fähigkeit, sowohl mono- als auch diphenolische Substrate umzusetzen, stützt die Hypothese, dass aktiviertes Hämocyanin in vivo an die Stelle der Phenoloxidase tritt.

Transport properties of YBa 2 Cu 3 O 7, PrBa 2 Cu 3 O 7-superlattices

The understanding of the coupling between superconducting YBa2Cu3O7 (YBCO) layers decoupled by non superconducting PrBa2Cu3O7 (PBCO) layers in c-axis oriented superlattices was the aim of this thesis. For this purpose two conceptually different kind of transport experiments have been performed. rnrnIn the first type of transport experiments the current is flowing parallel to the layers. Here the coupling is probed indirectly using magnetic vortex lines, which are penetrating the superlattice. Movement of the vortex segments in neighbouring YBCO layers is more or less coherent depending on the thickness of both the superconducting and non superconducting layers. This in-plane transport was measured either by sending an external current through bridges patterned in the superlattice or by an induced internal current. rnThe vortex-creep activation energy U was determined by analysis of the in-plane resistive transition in an external magnetic field B oriented along the c-axis. The activation energies for two series of superlattices were investigated. In one series the thickness of the YBCO layers was constant (nY=4 unit cells) and the number of the PBCO unit cells was varied, while in the other the number of PBCO layers was constant (nP=4) and nY varied. The correlation length of the vortex system was determined to be 80 nm along the c-axis direction. It was found that even a single PBCO unit cell in a superlattice effectively cuts the flux lines into shorter weakly coupled segments, and the coupling of the vortex systems in neighbouring layers is negligible already for a thickness of four unit cells of the PBCO layers. A characteristic variation of the activation energy for the two series of superlattices was found, where U0 is proportional to the YBCO thickness. A change in the variation of U0 with the current I in the specimen was observed, which can be explained in terms of a crossover in the vortex creep process, generated by the transport current. At low I values the dislocations mediated (plastic) vortex creep leads to thermally assisted flux-flow behaviour, whereas at high current the dc transport measurements are dominated by elastic (collective) creep.rnThe analysis of standard dc magnetization relaxation data obtained for a series superlattices revealed the occurrence of a crossover from elastic (collective) vortex creep at low temperature to plastic vortex creep at high T. The crossover is generated by the T dependent macroscopic currents induced in the sample. The existence of this creep crossover suggests that, compared with the well known Maley technique, the use of the normalized vortex creep activation energy is a better solution for the determination of vortex creep parameters.rnrnThe second type of transport experiments was to measure directly a possible Josephson coupling between superconducting CuO2 double planes in the superlattices by investigation of the transport properties perpendicular to the superconducting planes. Here three different experiments have been performed. The first one was to pattern mesa structures photolithographically as in previous works. The second used three-dimensional nanostructures cut by a focused ion beam. For the these two experiments insufficient patterning capabilities prevented an observation of the Josephson effect in the current voltage curves. rnA third experiment used a-axis and (110) oriented YBCO films, where in-plane patterning can in principle be sufficient to measure transport perpendicular to the superconducting planes. Therefore the deposition of films with this unusual growth orientation was optimized and investigated. The structural and microstructural evolution of c-axis to a-axis orientation was monitored using x-ray diffraction, scanning electron microscopy and magnetization measurements. Films with full a-axis alignment parallel to the substrate normal could be achieved on (100)SrTiO3. Due to the symmetry of the substrate the c-axis direction in-plane is twofold. Transferring the deposition conditions to films grown on (110)SrTiO3 allowed the growth of (110) oriented YBCO films with a unique in-plane c-axis orientation. While these films were of high quality by crystallographic and macroscopic visual inspection, electron microscopy revealed a coherent crack pattern on a nanoscale. Therefore the actual current path in the sample was not determined by the macroscopic patterning which prohibited investigations of the in-plane anisotropy in this case.rn

Frost heave testing of norwegian materials for road infrastructure

In areas of seasonal frost, frost susceptibility composed by frost heaving during the winter and thaw softening during the spring is one of the most dangerous phenomenon for transportation, road and railway infrastructure. Therefore, the need for frost protection layer becomes imperative. The purpose of frost protection layer is to prevent frost from penetrating down through the pavement and into the sub-soils. Frost susceptible soils under the road can be cause damages on the roads or other structures due to frost heave or reduced capacity characteristics thaw period. "Frost heave" is the term given to the upwards displacement of the ground surface caused by the formation of ice within soils or aggregates (Rempel et al., 2004). Nowadays in Scandinavia the most common material used in frost protection layer in the pavement structure of roads and in the ballast of the railway tracks are coarse-grain crushed rocks aggregates. Based on the capillary rise, the mechanics of frost heave phenomenon is based on the interaction between aggregates and water, as suggested by Konrad and Lemieux in 2005 that said that the fraction of material below the 0.063 mm sieve for coarse-grained soils must be controlled so as to reduce the sensitivity to frost heave. The study conducted in this thesis project is divided in two parts: - the analysis of the coarse grained aggregates used in frost protection layer in Norway; - the analysis of the frost heave phenomenon in the laboratory under known boundary conditions, through the use of the most widely used method, the frost heave test, in” closed system” (without access of water).

E-ToF-Messungen mit kalorimetrischen Tieftemperatur-Detektoren zur Bestimmung spezischer Energieverluste und zur Massenidentifikation niederenergetischer Schwerionen

Kalorimetrische Tieftemperatur-Detektoren (Calorimetric Low Temperature Detectors, CLTDs) wurden erstmals in Messungen zur Bestimmung des spezifischen Energieverlustes (dE/dx) niederenergetischer Schwerionen beim Durchgang durch Materie eingesetzt. Die Messungen wurden im Energiebereich unterhalb des Bragg-Peaks, mit 0.1 - 1.4 MeV/u 238U-Ionen in Kohlenstoff und Gold sowie mit 0.05 - 1.0 MeV/u 131Xe-Ionen in Kohlenstoff, Nickel und Gold, durchgeführt. Die Kombination der CLTDs mit einem Flugzeitdetektor ermöglichte dabei, kontinuierliche dE/dx-Kurven über größere Energiebereiche hinweg simultan zu bestimmen. Im Vergleich zu herkömmlichen Meßsystemen, die Ionisationsdetektoren zur Energiemessung verwenden, erlaubten die höhere Energieauflösung und -linearität der CLTDs eine Verringerung der Kalibrierungsfehler sowie eine Erweiterung des zugänglichen Energiebereiches der dE/dx-Messungen in Richtung niedriger Energien. Die gewonnen Daten können zur Anpassung theoretischer und semi-empirischer Modelle und somit zu einer Erhöhung der Präzision bei der Vorhersage spezifischer Energieverluste schwerer Ionen beitragen. Neben der experimentellen Bestimmung neuer Daten wurden das alternative Detektionsprinzip der CLTDs, die Vorteile dieser Detektoren bezüglich Energieauflösung und -linearität sowie der modulare Aufbau des CLTD-Arrays aus mehreren Einzeldetektoren genutzt, um diese Art von Messung auf potentielle systematische Unsicherheiten zu untersuchen. Unter anderem wurden hierbei unerwartete Channeling-Effekte beim Durchgang der Ionen durch dünne polykristalline Absorberfolien beobachtet. Die koinzidenten Energie- und Flugzeitmessungen (E-ToF) wurden weiterhin genutzt, um das Auflösungsvermögen des Detektor-Systems bei der direkten in-flight Massenbestimmung langsamer und sehr schwerer Ionen zu bestimmen. Durch die exzellente Energieauflösung der CLTDs konnten hierbei Massenauflösungen von Delta-m(FWHM) = 1.3 - 2.5 u für 0.1 - 0.6 MeV/u 238U-Ionen erreicht werden. In einer E-ToF-Messung mit Ionisationsdetektoren sind solche Werte in diesem Energie- und Massenbereich aufgrund der Limitierung der Energieauflösung durch statistische Schwankungen von Verlustprozessen beim Teilchennachweis nicht erreichbar.

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.

Observations and modeling of the Marginal Ice Zone

Global climate change in recent decades has strongly influenced the Arctic generating pronounced warming accompanied by significant reduction of sea ice in seasonally ice-covered seas and a dramatic increase of open water regions exposed to wind [Stephenson et al., 2011]. By strongly scattering the wave energy, thick multiyear ice prevents swell from penetrating deeply into the Arctic pack ice. However, with the recent changes affecting Arctic sea ice, waves gain more energy from the extended fetch and can therefore penetrate further into the pack ice. Arctic sea ice also appears weaker during melt season, extending the transition zone between thick multi-year ice and the open ocean. This region is called the Marginal Ice Zone (MIZ). In the Arctic, the MIZ is mainly encountered in the marginal seas, such as the Nordic Seas, the Barents Sea, the Beaufort Sea and the Labrador Sea. Formed by numerous blocks of sea ice of various diameters (floes) the MIZ, under certain conditions, allows maritime transportation stimulating dreams of industrial and touristic exploitation of these regions and possibly allowing, in the next future, a maritime connection between the Atlantic and the Pacific. With the increasing human presence in the Arctic, waves pose security and safety issues. As marginal seas are targeted for oil and gas exploitation, understanding and predicting ocean waves and their effects on sea ice become crucial for structure design and for real time safety of operations. The juxtaposition of waves and sea ice represents a risk for personnel and equipment deployed on ice, and may complicate critical operations such as platform evacuations. The risk is difficult to evaluate because there are no long-term observations of waves in ice, swell events are difficult to predict from local conditions, ice breakup can occur on very short time-scales and wave-ice interactions are beyond the scope of current forecasting models [Liu and Mollo-Christensen, 1988,Marko, 2003]. In this thesis, a newly developed Waves in Ice Model (WIM) [Williams et al., 2013a,Williams et al., 2013b] and its related Ocean and Sea Ice model (OSIM) will be used to study the MIZ and the improvements of wave modeling in ice infested waters. The following work has been conducted in collaboration with the Nansen Environmental and Remote Sensing Center and within the SWARP project which aims to extend operational services supporting human activity in the Arctic by including forecast of waves in ice-covered seas, forecast of sea-ice in the presence of waves and remote sensing of both waves and sea ice conditions. The WIM will be included in the downstream forecasting services provided by Copernicus marine environment monitoring service.

Multidetector CT (MD-CT) in the diagnosis of uncertain open globe injuries

To evaluate the significance of multislice CT for the diagnosis of uncertain penetrating globe injuries.

Suicidal knife wound to the heart: challenges in reconstructing wound channels with post mortem CT and CT-angiography

We present a case of an individual who stabbed himself through the heart with a large knife. Post mortem computed tomography (CT) and CT-angiography were used to assess the stab channel and to reconstruct the sequence of events. After penetrating injuries to the chest, both the intra-thoracic organs and the injury causing instrument may shift (e.g. from pnemothorax) and render forensic reconstructions more challenging. This case report illustrates the potentials and the pitfalls of CT for the reconstruction of penetrating injures to the chest.

Geophysical Analysis of Seasonal Montandon Gravel Ridge Water Table Fluctuation and Moisture Gradient Variation due to Storm Events

The purpose of this research project is to continue exploring the Montandon Long-Term Hydrologic Research Site(LTHR) by using multiple geophysical methods to obtain more accurate and precise information regarding subsurface hydrologic properties of a local gravel ridge,which are important to both the health of surrounding ecosystems and local agriculture. Through using non-invasive geophysical methods such as seismic refraction, Direct Current resistivity and ground penetrating radar (GPR) instead of invasive methods such as boreholedrilling which displace sediment and may alter water flow, data collection is less likely to bias the data itself. In addition to imaging the gravel ridge subsurface, another important researchpurpose is to observe how both water table elevation and the moisture gradient (moisture content of the unsaturated zone) change over a seasonal time period and directly after storm events. The combination of three types of data collection allows the strengths of each method combine together and provide a relatively strongly supported conclusions compared to previous research. Precipitation and geophysical data suggest that an overall increase in precipitation during the summer months causes a sharp decrease in subsurface resistivity within the unsaturated zone. GPR velocity data indicate significant immediate increase in moisture content within the shallow vadose zone (< 1m), suggesting that rain water was infiltrating into the shallow subsurface. Furthermore, the combination of resistivity and GPR results suggest that the decreased resistivity within the shallow layers is due to increased ion content within groundwater. This is unexpected as rainwater is assumed to have a DC resistivity value of 3.33*105 ohm-m. These results may suggest that ions within the sediment must beincorporated into the infiltrating water.

INVESTIGATION OF INTRAOCULAR PRESSURE AS A PREDICTOR OF TRAUMATIC EYE INJURIES

Eye injuries are a large societal problem in both the military and civilian sectors. Eye injury rates are increasing in recent military conflicts, and there are over 1.9 million eye injuries in the United States civilian sector annually. In order to develop a better understanding of eye injury risk, several previous studies have developed eye injury criteria based on projectile characteristics. While these injury criteria have been used to estimate eye injury potential of impact scenarios, they require that the mass, size and velocity of the projectile are known. It is desirable to develop a method to assess the severity of an eye impact in environments where it would be difficult or impossible to determine these projectile characteristics. The current study presents a measurement technique for monitoring intraocular pressure of the eye under impactloading. Through experimental tests with a custom pressure chamber, a subminiature pressure transducer was validated to be thermally stable and suitable for testing in an impact environment.Once validated, the transducer was utilized intraocularly, inserted through the optic nerve, to measure the pressure of the eye during blunt-projectile impacts. A total of 150 impact tests were performed using projectiles ranging from 3.2 mm to 17.5 mm in diameter. Investigation of the relationship between projectile energy and intraocular pressure lead to the identification of at least two distinct trends. Intraocular pressure and normalized energy measurements indicated a different response for penetrating-type globe rupture injuries with smaller diameter (d < 1 cm)projectiles, and blunt-type globe rupture injuries with larger diameter (d > 1 cm) projectiles. Furthermore, regression analysis indicates that relationships exist between intraocular pressureand projectile energy that may allow quantification of eye injury risk based on pressure data, and also that intraocular pressure measurements of impact may lead to a better understanding of thetransition between penetrating and blunt globe rupture injury mechanisms.