975 resultados para Blow up along a submanifold


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Using recent results on the compactness of the space of solutions of the Yamabe problem, we show that in conformal classes of metrics near the class of a nondegenerate solution which is unique (up to scaling) the Yamabe problem has a unique solution as well. This provides examples of a local extension, in the space of conformal classes, of a well-known uniqueness criterion due to Obata.

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We prove that asymptotically (as n -> infinity) almost all graphs with n vertices and C(d)n(2-1/2d) log(1/d) n edges are universal with respect to the family of all graphs with maximum degree bounded by d. Moreover, we provide an efficient deterministic embedding algorithm for finding copies of bounded degree graphs in graphs satisfying certain pseudorandom properties. We also prove a counterpart result for random bipartite graphs, where the threshold number of edges is even smaller but the embedding is randomized.

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Questa tesi si prefigge lo scopo di dimostrare il teorema di Igusa. Inizia introducendo algebricamente i numeri p-adici e ne dà una rappresentazione grafica. Sviluppa poi un integrale definito dalla misura di Haar, invariante per traslazione e computa alcuni esempi. Utilizza il blow up come strumento per la risoluzione di alcuni integrali ed enuncia un'applicazione del teorema di Hironaka sulla risolubilità delle singolarità. Infine usa questi risultati per dimostrare il teorema di Igusa.

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In questa tesi viene presentato il modello di Keller-Segel per la chemiotassi, un sistema di tipo parabolico-ellittico che appare nella descrizione di molti fenomeni in ambito biologico e medico. Viene mostrata l'esistenza globale della soluzione debole del modello, per dati iniziali sufficientemente piccoli in dimensione N>2. La scelta di dati iniziali abbastanza grandi invece può causare il blow-up della soluzione e viene mostrato sotto quali condizioni questo si verifica. Infine il modello della chemiotassi è stato applicato per descrivere una fase della malattia di Alzheimer ed è stata effettuata un'analisi di stabilità del sistema.

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A field study of thermal circulation over very gentle slope is described for a specific day characterised by weak synoptic conditions. The emphasis was on morning and evening transitions, but measurements cover the entire day; therefore a brief analysis is performed to represent the general thermal circulation pattern. Both transition periods are characterised by complex dynamic behaviours. During evening transition, the upslope flow has got through a stagnation condition characterised by wind velocity U<0:5 m=s. Only when the stagnating air has become negative buoyant, the flow is allowed to pour downslope like a slab. Some features of front formation has been found during the transition development, such as delay time of downslope flow start up along the slope, and the presence of positive turbulent kinetic energy at the onset of the motion. Eventually the observed evening transition has followed a mixed mechanisms, with features from different models. Therefore the Rayleigh number seems not to be a good criterion by which parametrise evening transition itself. Morning transition is characterised by destruction of nocturnal temperature inversion and the onset of upslope flow. Inversion destruction can be described in terms of CBL growth at surface and inversion decent from the top of the layer. KH has found to be a good indicator of inversion breakup, if used as parameter to study the inversion breakup in terms of temperature reversal. After the inversion breakup, buoyancy and mechanical productions supply the flow with the necessary energy to start the upslope wind. More quantitative analysis are provided by the study of stability parameters and turbulent kinetic energy budgets. Gradient Richardson number has been used in this terms, finding that a mixed SBL-CBL behaviour dominates the most of the observed layers. Tke budget has shown high turbulent behaviour during morning transition while the evening transition has developed entirely in laminar condition, apart from short intermittent turbulent events.

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In the West Bank city of Hebron the Israeli-Palestinian conflict still overshadows all activities. Despite the tension, friction, and violence that have become integral to the city’s everyday life, the Jewish Community of Hebron is expanding in numbers and geographical extent. Since the Six Day War, the community has attracted some of the most militant groups among the settlers in the West Bank, responsible for severe violence against Palestinians, including harassment, car bombs, and attempts to blow up the Dome of the Rock mosque itself. Why do the members of the Jewish Community of Hebron wish to live and raise their children in such a violent setting? Using a series of interviews with members of the Jewish Community of Hebron and related settler communities in the period 2000–05, the article examines the ways the Jewish Community legitimizes its disputed presence. It reveals a deep religious belief, blended with intense distrust of and hatred toward the Palestinian population.

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This paper is about young migrants without chance of being granted legal residence status in the Schengen zone. Previous observations suggest that some migrants, whose country of origin leaves them with low chances of receiving asylum or in fact any type of residence permit, exhibit a highly complex migration pattern that is characterised by 1) durable “transit” across Europe, which is a multi-linear movement according to opportunities that open up along the journey; 2) a high degree of flexibility, as they have to respond to suddenly changing conditions, such as work opportunities, rejection of asylum claims, detention or deportation, and 3) switching between different legal statuses, such as asylum seeker, sans papiers or detainee. The experiences of these young adults thus show a deep ambivalence between a sense of autonomy, on the one hand, and of profound hope and powerlessness, on the other. The Dublin Convention intends to limit such a hypermobility of migrants but seems to fail in many cases. Simultaneously it provokes some of the movements by sending asylum seekers and irregular migrants back to their first country of arrivals. Given the fact that little is known about these fragmented journeys inside of the Schengen area, this ethnographic study produces novel data on a highly pertinent migration pattern, the impact of the European migration management on individual migrants as well as the inter-relatedness of the asylum regime and irregular migration in Europe. At the same time these fragmented journeys are an excellent example to discuss mobility as a resource on the one hand (since it enables this specific migrant group to extend their presence in Europe) and as a handicap on the other (since it impedes the building of stable social networks, the planning of the future, etc.).

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Las Universidades públicas en América Latina se enfrentan a nuevos dilemas y problemas en un escenario de globalización académica, tendencias a la transnacionalización y privatización de la educación universitaria y a la descapitalización del sistema público. El tiempo presente invita a explorar lo que Francois Duber denominó como el proceso de declive de las instituciones modernas. En tanto ese declive se vincula con la sobrevivencia precaria proponemos explorar el caso de la Universidad de Buenos Aires. Nuestro objetivo es indagar en qué período histórico quedó localizado el programa institucional y cuáles de sus improntas permanecen hoy, deteniéndonos en el ciclo que la historiografía sobre la Universidad argentina identifica como de renovación y modernización universitaria (1955-1966). Para ello exploraremos la obra escrita y la trayectoria de Risieri Frondizi, una figura de notorio prestigio, a la vez olvidada pero omnipresente en toda reflexión sobre la Universidad.

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Igneous rocks recovered from Ocean Drilling Program (ODP) Leg 134 Sites 827, 829, and 830 at the toe of the forearc slope of New Hebrides Island Arc were investigated, using petrography, mineral chemistry, major and trace element, and Sr, Nd, and Pb isotopic analyses. Basaltic and andesitic clasts, together with detrital crystals of plagioclase, pyroxenes, and amphiboles embedded in sed-lithic conglomerate or volcanic siltstone and sandstone of Pleistocene age, were recovered from Sites 827 and 830. Petrological features of these lava clasts suggest a provenance from the Western Belt of New Hebrides Island Arc; igneous constituents were incorporated into breccias and sandstones, which were in turn reworked into a second generation breccia. Drilling at Site 829 recovered a variety of igneous rocks including basalts and probably comagmatic dolerites and gabbros, plus rare ultramafic rocks. Geochemical features, including Pb isotopic ratios, of the mafic rocks are intermediate between midocean ridge basalts and island arc tholeiites, and these rocks are interpreted to be backarc basin basalts. No correlates of these mafic rocks are known from Espiritu Santo and Malakula islands, nor do they occur in the Pleistocene volcanic breccias at Sites 827 and 830. However, basalts with very similar trace element and isotopic compositions have been recovered from the northern flank of North d'Entrecasteaux Ridge at Site 828. It is proposed that igneous rocks drilled at Site 829 represent material from the North d'Entrecasteaux Ridge accreted onto the over-riding Pacific Plate during collision. An original depleted mantle harzburgitic composition is inferred for a serpentinite clast recovered at 407 meters below seafloor (mbsf) in Hole 829A. Its provenance is a matter of speculation. It could have been brought up along a deep thrust fault affecting the Pacific Plate at the colliding margin, or analogous to the Site 829 basaltic lavas, it may represent material accreted from the North d'Entrecasteaux Ridge.

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Las Universidades públicas en América Latina se enfrentan a nuevos dilemas y problemas en un escenario de globalización académica, tendencias a la transnacionalización y privatización de la educación universitaria y a la descapitalización del sistema público. El tiempo presente invita a explorar lo que Francois Duber denominó como el proceso de declive de las instituciones modernas. En tanto ese declive se vincula con la sobrevivencia precaria proponemos explorar el caso de la Universidad de Buenos Aires. Nuestro objetivo es indagar en qué período histórico quedó localizado el programa institucional y cuáles de sus improntas permanecen hoy, deteniéndonos en el ciclo que la historiografía sobre la Universidad argentina identifica como de renovación y modernización universitaria (1955-1966). Para ello exploraremos la obra escrita y la trayectoria de Risieri Frondizi, una figura de notorio prestigio, a la vez olvidada pero omnipresente en toda reflexión sobre la Universidad.

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Las Universidades públicas en América Latina se enfrentan a nuevos dilemas y problemas en un escenario de globalización académica, tendencias a la transnacionalización y privatización de la educación universitaria y a la descapitalización del sistema público. El tiempo presente invita a explorar lo que Francois Duber denominó como el proceso de declive de las instituciones modernas. En tanto ese declive se vincula con la sobrevivencia precaria proponemos explorar el caso de la Universidad de Buenos Aires. Nuestro objetivo es indagar en qué período histórico quedó localizado el programa institucional y cuáles de sus improntas permanecen hoy, deteniéndonos en el ciclo que la historiografía sobre la Universidad argentina identifica como de renovación y modernización universitaria (1955-1966). Para ello exploraremos la obra escrita y la trayectoria de Risieri Frondizi, una figura de notorio prestigio, a la vez olvidada pero omnipresente en toda reflexión sobre la Universidad.

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The influence of atmospheric dust on climate and biogeochemical cycles in the oceans is well understood but poorly quantified. Glacial atmospheric dust loads were generally greater than those during the Holocene, as shown, for example, by the covariation of dust fluxes in the Equatorial Pacific and Antarctic ice cores. Nevertheless, it remains unclear whether these increases in dust flux were associated with changes in sources of dust, which would in turn suggest variations in wind patterns, climate or paleo-environment. Such questions can be answered using radiogenic isotope tracers of dust provenance. Here, we present a 160-kyr high-precision lead isotope time-series of dust input to the Eastern Equatorial Pacific (EEP) from core ODP Leg 138, Site 849 (0°11.59' N, 110°31.18' W). The Pb isotope record, combined with Nd isotope data, rules out contributions from Northern Hemisphere dust sources, north of the Intertropical Convergence Zone, such as Asia or North Africa/Sahara; similarly, eolian sources in Australia, Central America, the Northern Andes and Patagonia appear insignificant based upon the radiogenic isotope data. Fluctuations in Pb isotope ratios throughout the last 160 kyr show, instead, that South America remained the prevailing source of dusts to the EEP. There are two distinct South American Pb isotope end-members, constrained to be located in the south Central Volcanic Zone (CVZ, 22° S - 27.5° S) and the South Volcanic Zone (SVZ, 33° S - 43° S), with the former most likely originating in the Atacama Desert. Dust availability in the SVZ appears to be related to the weathering of volcanic deposits and the development of ash-derived Andosols, and influenced by local factors that might include vegetation cover. Variations in the dust fluxes from the two sources are in phase with both the dust flux and temperature records from Antarctican ice cores. We show that the forcing of dust provenance over time in the EEP overall is influenced by high-southerly-latitude climate conditions, leading to changes in the latitudinal position and strength of the South Westerlies as well as the coastal winds that blow northward along the Chilean margin. The net result is a modulation of dust emission from the Atacama Desert and the SVZ via a northward migration of the South Westerlies during cold periods and southward retreat during glacial terminations.

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Studies of the annual pollen and spore deposition in different areas of the Lena Delta were undertaken for the first time in the Asian sector of the Arctic during the Russian-German ''LENA 98'' and ''LENA 99'' expeditions in the framework of the International ''Laptev Sea System-2000'' Project. To achieve this objective, three spore-pollen traps were set up along the meridional delta profile in accordance with the European Pollen Monitoring Programme for the period July 1998 to August 1999. A comparison between the results of spore-pollen analysis of the contents of traps and the surrounding vegetation was performed. The results confirmed the current spore-pollen spectra are comprised both of pollen and spores of the local plants and of long-distance pollen and spores. The dependence of the long-distance pollen deposition on the character of the wind regime of the region was established. The prevailing southerly and southeasterly wind direction determines the main pollen influx of tree species from the areas of their growth south of the delta. The features of the morphological structure and fossilization of pollen and the features of the productive capability and plant growing conditions are of large significance in the pollen transfer and deposition.

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Recently a new type of cosmological singularity has been postulated for infinite barotropic index w in the equation of state p = wρ of the cosmological fluid, but vanishing pressure and density at the singular event. Apparently the barotropic index w would be the only physical quantity to blow up at the singularity. In this talk we would like to discuss the strength of such singularities and compare them with other types. We show that they are weak singularities