917 resultados para Elementary and high schools


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This partial translation of a longer article describes the phenomenon of ”Blasensand”. Blasensand is formed when sedimentation of dried out sand is suddenly flooded from above. A more detailed explanation of Blasensand is given in this translated part of the paper.

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The quasicontinuum (QC) method was introduced to coarse-grain crystalline atomic ensembles in order to bridge the scales from individual atoms to the micro- and mesoscales. Though many QC formulations have been proposed with varying characteristics and capabilities, a crucial cornerstone of all QC techniques is the concept of summation rules, which attempt to efficiently approximate the total Hamiltonian of a crystalline atomic ensemble by a weighted sum over a small subset of atoms. In this work we propose a novel, fully-nonlocal, energy-based formulation of the QC method with support for legacy and new summation rules through a general energy-sampling scheme. Our formulation does not conceptually differentiate between atomistic and coarse-grained regions and thus allows for seamless bridging without domain-coupling interfaces. Within this structure, we introduce a new class of summation rules which leverage the affine kinematics of this QC formulation to most accurately integrate thermodynamic quantities of interest. By comparing this new class of summation rules to commonly-employed rules through analysis of energy and spurious force errors, we find that the new rules produce no residual or spurious force artifacts in the large-element limit under arbitrary affine deformation, while allowing us to seamlessly bridge to full atomistics. We verify that the new summation rules exhibit significantly smaller force artifacts and energy approximation errors than all comparable previous summation rules through a comprehensive suite of examples with spatially non-uniform QC discretizations in two and three dimensions. Due to the unique structure of these summation rules, we also use the new formulation to study scenarios with large regions of free surface, a class of problems previously out of reach of the QC method. Lastly, we present the key components of a high-performance, distributed-memory realization of the new method, including a novel algorithm for supporting unparalleled levels of deformation. Overall, this new formulation and implementation allows us to efficiently perform simulations containing an unprecedented number of degrees of freedom with low approximation error.

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A single-longitudinal-mode (SLM) laser-diode pumped Nd: YAG laser with adjustable pulse width is developed by using the techniques of pre-lasing and changing polarization of birefingent crystal. The Q-switching voltage is triggered by the peak of the pre-lasing pulse to achieve the higher stability of output pulse energy. The output energy of more than 1 mJ is obtained with output energy stability of 3% (rms) at 100 Hz. The pulse-width can be adjusted from 30 ns to 300 ns by changing the Q-switching voltage. The probability of putting out single-longitudinal-mode pulses is almost 100%. The laser can be run over four hours continually without mode hopping.

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Based on the well known sea ice phase diagram, equations are derived for determining the brine and gas content of sea Ice for high temperatures (range 0 to -2 °C) and low salinities. The presently widely used equations of Cox and Weeks (1982) are valid only for temperatures below -2°C. Fresh-water ice is used as a boundary condition for the equations. The relative salt concentrations in brine are_assumed to be the same as in normal (or standard) seawater. Two sets of equations are presented: 1) accurate formulae based on UNESCO standard sea water equations, and 2) approximate formulae based on general properties of weak solutions. The approximate formulae are not essentially different from the classical system which basically assumes the freezing point to be a linear function of fractional salt content. The agreement between the two approaches is excellent and the approximate system is good enough for most applications.

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A new method was used to prepare erbium-doped high silica (SiO2% > 96%) glasses by sintering nanoporous glasses. The concentration of erbium ions in high silica glasses can be considerably more than that in silica glasses prepared by using conventional methods. The fluorescence of 1532 nm has an FWHM (Full Wave at Half Maximum) of 50 nm, wider than 35 nm of EDSFA (erbium-doped silica fiber amplifer), and hence the glass possesses potential application in broadband fiber amplifiers. The Judd-Ofelt theoretical analysis reflects that the quantum efficiency of this erbium-doped glass is about 0.78, although the erbium concentration in this glass (6 x 103) is about twenty times higher than that in silica glass. These excellent characteristics of Er-doped high silica glass will be conducive to its usage in optical amplifiers and microchip lasers.

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A disponibilidade gratuita na Internet de imagens de satélite e SIG somada à facilidade dos alunos no manuseio de multimídia através dos seus smartphones criam possibilidades para trabalhar com geotecnologias e recursos de multimídia no ensino de Cartografia. Nesta pesquisa foram avaliadas as contribuições, os limites e as possibilidades da inserção da tecnologia espacial, geoprocessamento e recursos de multimídia nas aulas de Geografia do sétimo ano da rede pública municipal de São Gonçalo/RJ; foi desenvolvida uma metodologia em meio digital, por meio da Internet, denominada Mapeando Meu Rio (MMR) cuja temática abordada foi a Percepção Socioambiental do Rio Alcântara. Observaram-se o interesse e o envolvimento dos alunos no decorrer das atividades propostas, por meio do uso de recursos de multimídia e geotecnologias como materiais de apoio à Educação Ambiental. Os resultados da avaliação do MMR mostraram que os alunos chegaram ao final do sétimo ano com dificuldades em relação à alfabetização cartográfica; isso foi constatado tanto na produção dos mapas mentais como também pela utilização do GPS, Google Earth e do ArcGIS Online. Os alunos tiveram dificuldades em utilizar os conhecimentos básicos da Cartografia para elaborar uma representação espacial, mais especificamente, legenda, coordenadas geográficas e orientação espacial. A alfabetização cartográfica não deve ser considerada como conteúdo que se restringe ao 6 ano, mas uma linguagem de comunicação para o entendimento da dinâmica espacial no decorrer do Ensino Fundamental e do Ensino Médio. As atividades geográficas deve permitir ao aluno melhorar a compreensão do espaço geográfico de uma maneira mais significativa para construir abstrações a partir da própria realidade, ou seja, do espaço vivido.