947 resultados para Extreme waves
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The present thesis focuses on elastic waves behaviour in ordinary structures as well as in acousto-elastic metamaterials via numerical and experimental applications. After a brief introduction on the behaviour of elastic guided waves in the framework of non-destructive evaluation (NDE) and structural health monitoring (SHM) and on the study of elastic waves propagation in acousto-elastic metamaterials, dispersion curves for thin-walled beams and arbitrary cross-section waveguides are extracted via Semi-Analytical Finite Element (SAFE) methods. Thus, a novel strategy tackling signal dispersion to locate defects in irregular waveguides is proposed and numerically validated. Finally, a time-reversal and laser-vibrometry based procedure for impact location is numerically and experimentally tested. In the second part, an introduction and a brief review of the basic definitions necessary to describe acousto-elastic metamaterials is provided. A numerical approach to extract dispersion properties in such structures is highlighted. Afterwards, solid-solid and solid-fluid phononic systems are discussed via numerical applications. In particular, band structures and transmission power spectra are predicted for 1P-2D, 2P-2D and 2P-3D phononic systems. In addition, attenuation bands in the ultrasonic as well as in the sonic frequency regimes are experimentally investigated. In the experimental validation, PZTs in a pitch-catch configuration and laser vibrometric measurements are performed on a PVC phononic plate in the ultrasonic frequency range and sound insulation index is computed for a 2P-3D phononic barrier in the sonic frequency range. In both cases the numerical-experimental results comparison confirms the existence of the numerical predicted band-gaps. Finally, the feasibility of an innovative passive isolation strategy based on giant elastic metamaterials is numerically proved to be practical for civil structures. In particular, attenuation of seismic waves is demonstrated via finite elements analyses. Further, a parametric study shows that depending on the soil properties, such an earthquake-proof barrier could lead to significant reduction of the superstructure displacement.
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In dieser Arbeit wird eine Methode entwickelt, die Rossbywellenzüge automatisch identifiziert und und deren Eigenschaften quantifiziert. Mit dieser Methode wird der Wellenzug als eine Einheit in Raum und Zeit interpretiert. Einheit im Raum heißt, dass nicht die einzelnen Tröge und Rücken eines Wellenzugs betrachtet werden, sondern deren Einhüllende. Einheit in der Zeit bedeutet, dass der Wellenzug nicht nur zu einem Zeitpunkt betrachtet wird, sondern über seine gesamte Lebensdauer hinweg. Um den Wellenzug als räumliche und zeitliche Einheit zu erhalten, werden die Einhüllenden der Wellenzüge in Längengrad-Zeit Diagrammen, sogenannten Hovmöllerdiagrammen, betrachtet. Dort werden zusammenhängende Regionen als Objekte, die jeweils einen Wellenzug repräsentieren, identifiziert. Deren Eigenschaften werden dann automatisch berechnet. Diese Eigenschaften können nun direkt dem zugrunde liegenden Rossbywellenzug zugeordnet werden.rnDie neue Methode wird in zwei verschiedenen Szenarien angewendet: erstens zur Beurteilung der Vorhersagequalität eines einzelnen Rossbywellenzugs und zweitens für die klimatologische Betrachtung von Rossbywellenzügen im ERA-40 Reanalysedatensatz. Sie wurde weiterhin mit bisher verwendeten Methoden zur Identifikation und Quantifizierung von Rossbywellenzügen verglichen.rnDie Untersuchung der Vorhersagequalität ergab, dass in dem betrachteten Fall die Übereinstimmung der Vorhersage mit der Analyse des Wellenzugs gering war, sofern das Modell initialisiert wurde, bevor der Rossbywellenzug eingesetzt hatte. Im Gegensatz dazu nahm die Vorhersagequalität deutlich zu, wenn der Wellenzug bereits in den Vorhersagedaten enthalten war. Dies deutet darauf hin, dass es in dem vorliegenden Fall problematisch ist, mit dem Modell den Auslösemechanismus korrekt voherzusagen. Für die weitere Untersuchung der Vorhersagequalität wurde eine spezielle Art der Darstellung der Daten verwendet, mit deren Hilfe deutlich wurde, dass das verwendete Modell in der Lage ist, diesen Wellenzug ungefähr sechs Tage im Voraus vorherzusagen. Diese Zeitspanne ist deutlich kürzer als die Lebensdauer des Wellenzugs, die etwa 10 Tage beträgt.rnIm Rahmen der klimatologischen Studie ergab sich eine positive Korrelation zwischen der Lebensdauer eines Rossbywellenzugs und des Bereichs den dieser Wellenzug während seiner gesamten Existenz in zonaler Richtung überstreicht. Für Wellenzüge mit einer kurzen Lebensdauer ergab sich eine ebenfalls positive Korrelation zwischen der mittleren Amplitude und der Dauer des Wellenzugs. Für eine längere Lebensdauer geht diese Korrelation aber in eine Sättigung über und die mittlere Amplitude steigt nicht mehr weiter an. Als eine mögliche Erklärung für dieses Verhalten wird angeführt, dass eine gewisse Stärke der Amplitude benötigt wird um stromabwärtige Entwicklung zu erhalten aber zu große Amplituden im Allgemeinen zum Brechen der Welle führen. Das Brechen leitet den letzten Abschnitt im Lebenszyklus eines Rossbywellenzuges ein, welcher im Anschluss meist zerfällt. Ein weiteres Ergebnis der klimatologischen Untersuchung ist das Auffinden bevorzugter Regionen der Entstehung und des Abklingens von Rossbywellenzügen. Diese Regionen unterscheiden sich erheblich für Rossbywellenzüge unterschiedlicher minimaler Lebensdauer. Langlebige Rossbywellenzüge entstehen demnach hauptsächlich über Ostasien und dem Westpazifik und vergehen dann über Europa.rnSchließlich wurde die entwickelte Methode in einen systematischen Vergleich anderer Methoden zur Identifikation und Quantifizierung von Rossbywellenzügen eingereiht. Die betrachteten Methoden beinhalten verschiedene Trog-und-Rücken Hovmöllerdiagramme des Meridionalwindes, Methoden die Rossbywellenzüge als eine Einheit identifizieren und Methoden die den Beitrag verschiedener physikalischer Aspekte zu der Entwicklung von Rossbywellenenzügen quantifizieren. Der Vergleich macht deutlich, dass jede Methode ihre individuellen Stärken und Schwächen hat. Dies bedeutet insbesondere, dass die Eignung der Methode von dem Stadium des Lebenszyklus, in dem sich der Rossbywellenzug befindet und dem Fokus, den man bei der Betrachtung hat, abhängt. Ideal ist eine Kombination mehrerer Methoden, da dies ein vollständigeres Bild eines Rossbywellenzuges ergibt als einzelne Methoden es zu liefern vermögen. Obwohl alle Methoden für die Anwendungen, für die sie jeweils konzipiert wurden, geeignet sind, ergeben sich bei der Diagnose der Rossbywellenzüge beträchtliche Unterschiede. Letztendlich stellt sich heraus, dass sogar die Defintion eines Rossbywellenzugs bis zu einem gewissen Grad von der zu seiner Identifizierung verwendeten Methode abhängt.
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One of the most important challenges in chemistry and material science is the connection between the contents of a compound and its chemical and physical properties. In solids, these are greatly influenced by the crystal structure.rnrnThe prediction of hitherto unknown crystal structures with regard to external conditions like pressure and temperature is therefore one of the most important goals to achieve in theoretical chemistry. The stable structure of a compound is the global minimum of the potential energy surface, which is the high dimensional representation of the enthalpy of the investigated system with respect to its structural parameters. The fact that the complexity of the problem grows exponentially with the system size is the reason why it can only be solved via heuristic strategies.rnrnImprovements to the artificial bee colony method, where the local exploration of the potential energy surface is done by a high number of independent walkers, are developed and implemented. This results in an improved communication scheme between these walkers. This directs the search towards the most promising areas of the potential energy surface.rnrnThe minima hopping method uses short molecular dynamics simulations at elevated temperatures to direct the structure search from one local minimum of the potential energy surface to the next. A modification, where the local information around each minimum is extracted and used in an optimization of the search direction, is developed and implemented. Our method uses this local information to increase the probability of finding new, lower local minima. This leads to an enhanced performance in the global optimization algorithm.rnrnHydrogen is a highly relevant system, due to the possibility of finding a metallic phase and even superconductor with a high critical temperature. An application of a structure prediction method on SiH12 finds stable crystal structures in this material. Additionally, it becomes metallic at relatively low pressures.
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Recent studies found that soil-atmosphere coupling features, through soil moisture, have been crucial to simulate well heat waves amplitude, duration and intensity. Moreover, it was found that soil moisture depletion both in Winter and Spring anticipates strong heat waves during the Summer. Irrigation in geophysical studies can be intended as an anthropogenic forcing to the soil-moisture, besides changes in land proprieties. In this study, the irrigation was add to a LAM hydrostatic model (BOLAM) and coupled with the soil. The response of the model to irrigation perturbation is analyzed during a dry Summer season. To identify a dry Summer, with overall positive temperature anomalies, an extensive climatological characterization of 2015 was done. The method included a statistical validation on the reference period distribution used to calculate the anomalies. Drought conditions were observed during Summer 2015 and previous seasons, both on the analyzed region and the Alps. Moreover July was characterized as an extreme event for the referred distribution. The numerical simulation consisted on the summer season of 2015 and two run: a control run (CTR), with the soil coupling and a perturbed run (IPR). The perturbation consists on a mask of land use created from the Cropland FAO dataset, where an irrigation water flux of 3 mm/day was applied from 6 A.M. to 9 A.M. every day. The results show that differences between CTR and IPR has a strong daily cycle. The main modifications are on the air masses proprieties, not on to the dynamics. However, changes in the circulation at the boundaries of the Po Valley are observed, and a diagnostic spatial correlation of variable differences shows that soil moisture perturbation explains well the variation observed in the 2 meters height temperature and in the latent heat fluxes.On the other hand, does not explain the spatial shift up and downslope observed during different periods of the day. Given the results, irrigation process affects the atmospheric proprieties on a larger scale than the irrigation, therefore it is important in daily forecast, particularly during hot and dry periods.
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The aim of this study was to determine if extracorporeal shock wave therapy (ESWT) in vivo affects the structural integrity of articular cartilage. A single bout of ESWT (1500 shock waves of 0.5 mJ/mm(2)) was applied to femoral heads of 18 adult Sprague-Dawley rats. Two sham-treated animals served as controls. Cartilage of each femoral head was harvested at 1, 4, or 10 weeks after ESWT (n = 6 per treatment group) and scored on safranin-O-stained sections. Expression of tenascin-C and chitinase 3-like protein 1 (Chi3L1) was analyzed by immunohistochemistry. Quantitative real-time polymerase chain reaction (PCR) was used to examine collagen (II)alpha(1) (COL2A1) expression and chondrocyte morphology was investigated by transmission electron microscopy no changes in Mankin scores were observed after ESWT. Positive immunostaining for tenascin-C and Chi3L1 was found up to 10 weeks after ESWT in experimental but not in control cartilage. COL2A1 mRNA was increased in samples 1 and 4 weeks after ESWT. Alterations found on the ultrastructural level showed expansion of the rough-surfaced endoplasmatic reticulum, detachment of the cell membrane and necrotic chondrocytes. Extracorporeal shock waves caused alterations of hyaline cartilage on a molecular and ultrastructural level that were distinctly different from control. Similar changes were described before in the very early phase of osteoarthritis (OA). High-energy ESWT might therefore cause degenerative changes in hyaline cartilage as they are found in initial OA.
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Bucknell University's instructional technology division of Library and IT partnered with Professor Carmen Gillespie for an innovative course called "Extreme Creativity".
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The lack of effective tools have hampered our ability to assess the size, growth and ages of clonal plants. With Serenoa repens (saw palmetto) as a model, we introduce a novel analytical framework that integrates DNA fingerprinting and mathematical modelling to simulate growth and estimate ages of clonal plants. We also demonstrate the application of such life-history information of clonal plants to provide insight into management plans. Serenoa is an ecologically important foundation species in many Southeastern United States ecosystems; yet, many land managers consider Serenoa a troublesome invasive plant. Accordingly, management plans have been developed to reduce or eliminate Serenoa with little understanding of its life history. Using Amplified Fragment Length Polymorphisms, we genotyped 263 Serenoa and 134 Sabal etonia (a sympatric non-clonal palmetto) samples collected from a 20 X 20 m study plot in Florida scrub. Sabal samples were used to assign small field-unidentifiable palmettos to Serenoa or Sabal and also as a negative control for clone detection. We then mathematically modelled clonal networks to estimate genet ages. Our results suggest that Serenoa predominantly propagate via vegetative sprouts and 10000-year-old genets may be common, while showing no evidence of clone formation by Sabal. The results of this and our previous studies suggest that: (i) Serenoa has been part of scrub associations for thousands of years, (ii) Serenoa invasion are unlikely and (ii) once Serenoa is eliminated from local communities, its restoration will be difficult. Reevaluation of the current management tools and plans is an urgent task.
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We present an analysis of daily extreme precipitation events for the extended winter season (October–March) at 20 Mediterranean coastal sites covering the period 1950–2006. The heavy tailed behaviour of precipitation extremes and estimated return levels, including associated uncertainties, are derived applying a procedure based on the Generalized Pareto Distribution, in combination with recently developed methods. Precipitation extremes have an important contribution to make seasonal totals (approximately 60% for all series). Three stations (one in the western Mediterranean and the others in the eastern basin) have a 5-year return level above 100 mm, while the lowest value (estimated for two Italian series) is equal to 58 mm. As for the 50-year return level, an Italian station (Genoa) has the highest value of 264 mm, while the other values range from 82 to 200 mm. Furthermore, six series (from stations located in France, Italy, Greece, and Cyprus) show a significant negative tendency in the probability of observing an extreme event. The relationship between extreme precipitation events and the large scale atmospheric circulation at the upper, mid and low troposphere is investigated by using NCEP/NCAR reanalysis data. A 2-step classification procedure identifies three significant anomaly patterns both for the western-central and eastern part of the Mediterranean basin. In the western Mediterranean, the anomalous southwesterly surface to mid-tropospheric flow is connected with enhanced moisture transport from the Atlantic. During ≥5-year return level events, the subtropical jet stream axis is aligned with the African coastline and interacts with the eddy-driven jet stream. This is connected with enhanced large scale ascending motions, instability and leads to the development of severe precipitation events. For the eastern Mediterranean extreme precipitation events, the identified anomaly patterns suggest warm air advection connected with anomalous ascent motions and an increase of the low- to mid-tropospheric moisture. Furthermore, the jet stream position (during ≥5-year return level events) supports the eastern basin being in a divergence area, where ascent motions are favoured. Our results contribute to an improved understanding of daily precipitation extremes in the cold season and associated large scale atmospheric features.
Resumo:
The lack of effective tools has hampered our ability to assess the size, growth and ages of clonal plants. With Serenoa repens (saw palmetto) as a model, we introduce a novel analytical frame work that integrates DNA fingerprinting and mathematical modelling to simulate growth and estimate ages of clonal plants. We also demonstrate the application of such life-history information of clonal plants to provide insight into management plans. Serenoa is an ecologically important foundation species in many Southeastern United States ecosystems; yet, many land managers consider Serenoa a troublesome invasive plant. Accordingly, management plans have been developed to reduce or eliminate Serenoa with little understanding of its life history. Using Amplified Fragment Length Polymorphisms, we genotyped 263 Serenoa and 134 Sabal etonia (a sympatric non-clonal palmetto) samples collected from a 20 x 20 m study plot in Florida scrub. Sabal samples were used to assign small field-unidentifiable palmettos to Serenoa or Sabal and also as a negative control for clone detection. We then mathematically modelled clonal networks to estimate genet ages. Our results suggest that Serenoa predominantly propagate via vegetative sprouts and 10000-year-old genets maybe common, while showing no evidence of clone formation by Sabal. The results of this and our previous studies suggest that: (i) Serenoa has been part of scrub associations for thousands of years, (ii) Serenoa invasions are unlikely and (ii) once Serenoa is eliminated from local communities, its restoration will be difficult. Reevaluation of the current management tools and plans is an urgent task.
Resumo:
High levels of HIV-1 replication during the chronic phase of infection usually correlate with rapid progression to severe immunodeficiency. However, a minority of highly viremic individuals remains asymptomatic and maintains high CD4⁺ T cell counts. This tolerant profile is poorly understood and reminiscent of the widely studied nonprogressive disease model of SIV infection in natural hosts. Here, we identify transcriptome differences between rapid progressors (RPs) and viremic nonprogressors (VNPs) and highlight several genes relevant for the understanding of HIV-1-induced immunosuppression. RPs were characterized by a specific transcriptome profile of CD4⁺ and CD8⁺ T cells similar to that observed in pathogenic SIV-infected rhesus macaques. In contrast, VNPs exhibited lower expression of interferon-stimulated genes and shared a common gene regulation profile with nonpathogenic SIV-infected sooty mangabeys. A short list of genes associated with VNP, including CASP1, CD38, LAG3, TNFSF13B, SOCS1, and EEF1D, showed significant correlation with time to disease progression when evaluated in an independent set of CD4⁺ T cell expression data. This work characterizes 2 minimally studied clinical patterns of progression to AIDS, whose analysis may inform our understanding of HIV pathogenesis.