Modeling and simulation of severe slugging with mass transfer effects

A mathematical model and numerical simulations are presented to investigate the dynamics of gas, oil and water flow in a pipeline-riser system. The pipeline is modeled as a lumped parameter system and considers two switchable states: one in which the gas is able to penetrate into the riser and another in which there is a liquid accumulation front, preventing the gas from penetrating the riser. The riser model considers a distributed parameter system, in which movable nodes are used to evaluate local conditions along the subsystem. Mass transfer effects are modeled by using a black oil approximation. The model predicts the liquid penetration length in the pipeline and the liquid level in the riser, so it is possible to determine which type of severe slugging occurs in the system. The method of characteristics is used to simplify the differentiation of the resulting hyperbolic system of equations. The equations are discretized and integrated using an implicit method with a predictor-corrector scheme for the treatment of the nonlinearities. Simulations corresponding to severe slugging conditions are presented and compared to results obtained with OLGA computer code, showing a very good agreement. A description of the types of severe slugging for the three-phase flow of gas, oil and water in a pipeline-riser system with mass transfer effects are presented, as well as a stability map. (C) 2011 Elsevier Ltd. All rights reserved.

Enzyme Microheterogeneous Hydration and Stabilization in Supercritical Carbon Dioxide

Supercritical carbon dioxide is a promising green-chemistry solvent for many enzyme-catalyzed chemical reactions, yet the striking stability of some enzymes in such unconventional environments is not well understood. Here, we investigate the stabilization of the Candida antarctica Lipase B (CALB) in supercritical carbon dioxide-water biphasic systems using molecular dynamics simulations. The preservation of the enzyme structure and optimal activity depend on the presence of small amounts of water in the supercritical dispersing medium. When the protein is at least partially hydrated, water molecules bind to specific sites on the enzyme surface and prevent carbon dioxide from penetrating its catalytic core. Strikingly, water and supercritical carbon dioxide cover the protein surface quite heterogeneously. In the first solvation layer, the hydrophilic residues at the surface of the protein are able to pin down patches of water, whereas carbon dioxide solvates preferentially hydrophobic surface residues. In the outer solvation shells, water molecules tend to cluster predominantly on top of the larger water patches of the first solvation layer instead of spreading evenly around the remainder of the protein surface. For CALB, this exposes the substrate-binding region of the enzyme to carbon dioxide, possibly facilitating diffusion of nonpolar substrates into the catalytic funnel. Therefore, by means of microheterogeneous solvation, enhanced accessibility of hydrophobic substrates to the active site can be achieved, while preserving the functional structure of the enzyme. Our results provide a molecular picture on the nature of the stability of proteins in nonaqueous media.

Pachymetry-Guided Intrastromal Air Injection ("Pachy-Bubble") for Deep Anterior Lamellar Keratoplasty

To evaluate an innovative technique for intrastromal air injection to achieve deep anterior lamellar keratoplasty (DALK) with bare Descemet membrane (DM). Thirty-four eyes with anterior corneal pathology, including 27 with keratoconus, underwent DALK. After 400 mm trephination with a suction trephine, ultrasound pachymetry was performed 0.8 mm internally from the trephination groove in the 11 to 1 o'clock position. In this area, a 2-mm incision was created, parallel to the groove, with a micrometer diamond knife calibrated to 90% depth of the thinnest measurement. A cannula was inserted through the incision and 0.5 mL of air was injected to dissect the DM from the stroma. After peripheral paracentesis, anterior keratectomy was carried out to bare the DM. A 0.25-mm oversized graft was sutured in place. Overall, 94.1% of eyes achieved DALK. Bare DM was achieved in 30 eyes, and a pre-DM dissection was performed in 2 eyes. Air injection was successful in detaching the DM (achieving the big bubble) in 88.2% of the eyes. In keratoconus eyes, the rate was 88.9%. All cases but one required a single air injection to achieve DM detachment. Microperforations occurred in 5 cases: 3 during manual layer-by-layer dissection after air injection failed to detach the DM, 1 during removal of the residual stroma after big-bubble formation, and 1 during the diamond knife incision. Two cases (5.9%) were converted to penetrating keratoplasty because of macroperforations. The technique was reproducible, safe, and highly effective in promoting DALK with bare DM.

Upper Pleistocene to Holocene peatland evolution in Southern Brazilian highlands as depicted by radar stratigraphy, sedimentology and palynology

Paleoenvironmental interpretation of proxy data derived from peatlands is largely based upon an evolutionary model for ombrotrophic bogs, in which peat accumulates in still environments. Reports on proxies obtained from minerotrophic fens, where hydrologic inputs are variable, are less common. In this study, a highland peatland in southern Brazil is presented through ground penetrating radar (GPR) and sedimentological, palynological and geochronologic data. The radar stratigraphic interpretation suggests a relatively complex history of erosion and deposition at the site since the beginning of Marine Isotope Stage 3 (MIS 3) interstadial period. In spite of this, radar stratigraphic and palynologic interpretations converge. Electromagnetic reflections tend to group in clusters that show lateral coherence and correlate with different sediment types, while pollen grains abound and are well preserved. As a result, the study of minerotrophic fens provides a source of proxies. suggesting that ombrotrophic bogs are not the only reliable source of data in wetlands for palynological analysis. (C) 2012 University of Washington. Published by Elsevier Inc. All rights reserved.

Isolated right atrial appendage (RAA) rupture in blunt trauma – a case report and an anatomic study comparing RAA and right atrium (RA) wall thickness

Abstract Background Heart chambers rupture in blunt trauma is uncommon and is associated with a high mortality. The determinant factors, and the incidence of isolated heart chambers rupture remains undetermined. Isolated rupture of the right atrium appendage (RAA) is very rare, with 8 cases reported in the reviewed literature. The thin wall of the RAA has been presumed to render this chamber more prone to rupture in blunt trauma. Objective To report a case of isolated RAA rupture in blunt trauma, and to compare right atrium (RA) and RAA wall thickness in a necropsy study. Methods The thickness of RA and RAA wall of hearts from cadavers of fatal penetrating head trauma victims was measured. Our case of isolated RAA rupture is presented. The main findings of the 8 cases reported in the literature, and the findings of our case, were organized in a table. Result The comparison of the data showed that wall thickness of the RAA (0.53 ± 0.33 mm) was significantly thinner than that of RA (1.11 ± 0.42 mm) (p < 0.05). Comments In all these 9 cases of isolated RAA rupture, cardiac tamponade occurred, RAA rupture was diagnosed intraoperatively and sutured, and the patients survived. Main mechanisms hypothesized for heart chamber rupture include mechanical compression coincident with phases of cardiac cycle, leading to high hydrostatic pressure inside the chamber. Published series include numerous cases of RA rupture, and only a few cases of RAA rupture. Conclusion Thus, our data suggests that wall thickness is not a determinant factor for RA or RAA rupture in blunt trauma.

“Features of two proteins of Leptospira interrogans with potential role in host-pathogen interactions”

Abstract Background Leptospirosis is considered a re-emerging infectious disease caused by pathogenic spirochaetes of the genus Leptospira. Pathogenic leptospires have the ability to survive and disseminate to multiple organs after penetrating the host. Leptospires were shown to express surface proteins that interact with the extracellular matrix (ECM) and to plasminogen (PLG). This study examined the interaction of two putative leptospiral proteins with laminin, collagen Type I, collagen Type IV, cellular fibronectin, plasma fibronectin, PLG, factor H and C4bp. Results We show that two leptospiral proteins encoded by LIC11834 and LIC12253 genes interact with laminin in a dose - dependent and saturable mode, with dissociation equilibrium constants (KD) of 367.5 and 415.4 nM, respectively. These proteins were named Lsa33 and Lsa25 (Leptospiral surface adhesin) for LIC11834 and LIC12253, respectively. Metaperiodate - treated laminin reduced Lsa25 - laminin interaction, suggesting that sugar moieties of this ligand participate in this interaction. The Lsa33 is also PLG - binding receptor, with a KD of 23.53 nM, capable of generating plasmin in the presence of an activator. Although in a weak manner, both proteins interact with C4bp, a regulator of complement classical route. In silico analysis together with proteinase K and immunoflorescence data suggest that these proteins might be surface exposed. Moreover, the recombinant proteins partially inhibited leptospiral adherence to immobilized laminin and PLG. Conclusions We believe that these multifunctional proteins have the potential to participate in the interaction of leptospires to hosts by mediating adhesion and by helping the bacteria to escape the immune system and to overcome tissue barriers. To our knowledge, Lsa33 is the first leptospiral protein described to date with the capability of binding laminin, PLG and C4bp in vitro.

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.