18,021 research outputs found

    A distributional approach to fragmentation equations

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    We consider a linear integro-di®erential equation that models multiple fragmentation with inherent mass-loss. A systematic procedure is presented for constructing a space of generalised functions Z0 in which initial-value problems involving singular initial conditions such as the Dirac delta distribution can be analysed. The procedure makes use of results on sun dual semigroups and quasi-equicontinuous semigroups on locally convex spaces. The existence and uniqueness of a distributional solution to an abstract version of the initial-value problem are established for any given initial data u0 in Z0

    The Dynamics of School Attainment of Englands Ethnic Minorities

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    We exploit a universe dataset of state school students in England with linked test score records to document the evolution of attainment through school for different ethnic groups. The analysis yields a number of striking findings. First, we show that, controlling for personal characteristics, all minority groups make greater progress than white students over secondary schooling. Second, much of this improvement occurs in the high-stakes exams at the end of compulsory schooling. Third, we show that for most ethnic groups, this gain is pervasive, happening in almost all schools in which these students are found. We address some of the usual factors invoked to explain attainment gaps: poverty, language, school quality, and teacher influence. We conclude that our findings are more consistent with the importance of factors like aspirations and attitudes.Ethnic test score gap, school attainment, education

    The surface expression of the Arsia-Mangala Dike, Mars, is controlled by the "Sawtooth" profile of surface topography. : 42nd Lunar and Planetary Science Conference (2011)

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    Giant dike swarms are present on Venus, Earth, and Mars [1]. On Mars, sets of graben radiating from centres in the Tharsis volcanic region are taken as evidence for the presence of giant dike swarms [2]. The Mangala Fossa graben system and the related Mangala Valles flood valley probably have had their origins in crustal fracturing caused by the intrusion of one of these dikes [3, 4], which we call the Arsia-Mangala dike. The graben segments formed when the combination of regional extensional tectonic forces and local stresses due to dike injection caused surface subsidence along pairs of inward-facing faults [5]. In the longest graben segment, subsurface aquifer water exploited the graben faults to reach the surface, flood the graben interior, and overflow to erode the Mangala Valles flood channels [4]. Here we propose that 3 other groups of surface features are related to the emplacement of the Arsia-Mangala dike. Specifically, we infer that they are due to asymmetric changes in surface topography in the propagation direction, which the upper edge of the laterally propagating dike was unable to track vertically as the dike was being emplaced, thus leading to the dike top dynamically approaching unusually close to the surface

    Segregation and the Attainment of Minority Ethnic Pupils in England

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    In this paper we ask whether ethnic segregation in schools and in neighbourhoods has a causal effect on differential school attainment. We ask two related but different questions. First, we look at the test score gap between White and minority ethnic students, separately for Black Caribbean, Indian and Pakistani ethnic groups. Second, we consider the absolute performance of students in each of these minority ethnic groups across cities with varying levels of segregation. We show that, in strong contrast to similar studies in the US, the test score gap is largely unaffected by segregation for any of the three groups we study, and we find no evidence of a negative impact of ethnic segregation on absolute attainment levels.ethnic segregation, schools

    Fractional transformations of generalised functions

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    A distributional theory of fractional transformations is developed. A constructive approach, based on the eigenfunction expansion method pioneered by A. H. Zemanian, is used to produce an appropriate space of test functions and corresponding space of generalised functions. The fractional transformations that are defined are shown to form an equicontinuous group of operators on the space of test functions and a weak continuous group on the space of generalised functions. Integral representations for the fractional transformations are also obtained under certain conditions. The fractional Fourier transformation is considered as a particular case of our general theory

    Three-dimensional coating and rimming flow : a ring of fluid on a rotating horizontal cylinder

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    The steady three-dimensional flow of a thin, slowly varying ring of Newtonian fluid on either the outside or the inside of a uniformly rotating large horizontal cylinder is investigated. Specifically, we study “full-ring” solutions, corresponding to a ring of continuous, finite and non-zero thickness that extends all the way around the cylinder. In particular, it is found that there is a critical solution corresponding to either a critical load above which no full-ring solution exists (if the rotation speed is prescribed) or a critical rotation speed below which no full-ring solution exists (if the load is prescribed). We describe the behaviour of the critical solution and, in particular, show that the critical flux, the critical load, the critical semi-width and the critical ring profile are all increasing functions of the rotation speed. In the limit of small rotation speed, the critical flux is small and the critical ring is narrow and thin, leading to a small critical load. In the limit of large rotation speed, the critical flux is large and the critical ring is wide on the upper half of the cylinder and thick on the lower half of the cylinder, leading to a large critical load. We also describe the behaviour of the non-critical full-ring solution, and, in particular, show that the semi-width and the ring profile are increasing functions of the load but, in general, non-monotonic functions of the rotation speed. In the limit of large rotation speed, the ring approaches a limiting non-uniform shape, whereas in the limit of small load, the ring is narrow and thin with a uniform parabolic profile. Finally, we show that, while for most values of the rotation speed and the load the azimuthal velocity is in the same direction as the rotation of the cylinder, there is a region of parameter space close to the critical solution for sufficiently small rotation speed in which backflow occurs in a small region on the upward-moving side of the cylinder
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