894 resultados para Calculus of variations
Resumo:
There is an increasing tendency of turning the current power grid, essentially unaware of variations in electricity demand and scattered energy sources, into something capable of bringing a degree of intelligence by using tools strongly related to information and communication technologies, thus turning into the so-called Smart Grid. In fact, it could be considered that the Smart Grid is an extensive smart system that spreads throughout any area where power is required, providing a significant optimization in energy generation, storage and consumption. However, the information that must be treated to accomplish these tasks is challenging both in terms of complexity (semantic features, distributed systems, suitable hardware) and quantity (consumption data, generation data, forecasting functionalities, service reporting), since the different energy beneficiaries are prone to be heterogeneous, as the nature of their own activities is. This paper presents a proposal on how to deal with these issues by using a semantic middleware architecture that integrates different components focused on specific tasks, and how it is used to handle information at every level and satisfy end user requests.
Resumo:
A expansão rápida da maxila assistida cirurgicamente (ERMAC) é um dos procedimentos de escolha para correção da deficiência transversal em pacientes adultos. Este estudo avaliou as alterações produzidas nos arcos dentais superiores e inferiores de 18 pacientes, sendo seis do sexo masculino e 12 do sexo feminino, com média de idade de 23,3 anos submetidos à ERMAC. Para cada paciente foram preparados três modelos de gesso, que foram digitalizados por meio do Scanner 3D, obtidos em diferentes fases: inicial, antes do procedimento operatório (T1); três meses pós-expansão (T2); seis meses pós-expansão (T3). Foram avaliadas as distâncias transversais do arcos dentários superior e inferior, a inclinação dentária dos dentes posteriores superiores, a altura da coroa clínica dos dentes posteriores do arco superior e foi observado se havia correlação entre a quantidade de inclinação dentária com o desenvolvimento de recessões gengivais. Para análise dos resultados foram utilizados a análise de Variância, o Teste de Tukey e o Teste de Correlação de Pearson, sendo que para a análise do erro sistemático intra-examinador foi utilizado o teste t pareado e para determinação do erro casual utilizou-se o cálculo do erro de Dahlberg. Com base na metodologia utilizada e nos resultados obtidos, pode-se concluir que: 1. com relação as alterações produzidas no sentido transversal do arco superior, obteve-se um aumento em todas as variáveis de T1 para T2 e uma manutenção dos valores em todas as variáveis de T2 para T3 demonstrando efetividade e estabilidade do procedimento; 2. no arco inferior não houve alterações transversais estatisticamente significantes, com exceção dos primeiros molares; 3. com relação às inclinações dentárias, observou-se um aumento desta de T1 para T2 em todos os dentes, porém, com significância estatística apenas para segundo molar e primeiro e segundo pré-molar do lado direito e primeiro molar e segundo pré-molar do lado esquerdo.; 4. a ERMAC não acarretou o desenvolvimento de recessões gengivais em nenhum dos tempos; 5. não houve correlação entre a quantidade de inclinação dentária e o desenvolvimento de recessões gengivais.(AU)
Resumo:
A expansão rápida da maxila assistida cirurgicamente (ERMAC) é um dos procedimentos de escolha para correção da deficiência transversal em pacientes adultos. Este estudo avaliou as alterações produzidas nos arcos dentais superiores e inferiores de 18 pacientes, sendo seis do sexo masculino e 12 do sexo feminino, com média de idade de 23,3 anos submetidos à ERMAC. Para cada paciente foram preparados três modelos de gesso, que foram digitalizados por meio do Scanner 3D, obtidos em diferentes fases: inicial, antes do procedimento operatório (T1); três meses pós-expansão (T2); seis meses pós-expansão (T3). Foram avaliadas as distâncias transversais do arcos dentários superior e inferior, a inclinação dentária dos dentes posteriores superiores, a altura da coroa clínica dos dentes posteriores do arco superior e foi observado se havia correlação entre a quantidade de inclinação dentária com o desenvolvimento de recessões gengivais. Para análise dos resultados foram utilizados a análise de Variância, o Teste de Tukey e o Teste de Correlação de Pearson, sendo que para a análise do erro sistemático intra-examinador foi utilizado o teste t pareado e para determinação do erro casual utilizou-se o cálculo do erro de Dahlberg. Com base na metodologia utilizada e nos resultados obtidos, pode-se concluir que: 1. com relação as alterações produzidas no sentido transversal do arco superior, obteve-se um aumento em todas as variáveis de T1 para T2 e uma manutenção dos valores em todas as variáveis de T2 para T3 demonstrando efetividade e estabilidade do procedimento; 2. no arco inferior não houve alterações transversais estatisticamente significantes, com exceção dos primeiros molares; 3. com relação às inclinações dentárias, observou-se um aumento desta de T1 para T2 em todos os dentes, porém, com significância estatística apenas para segundo molar e primeiro e segundo pré-molar do lado direito e primeiro molar e segundo pré-molar do lado esquerdo.; 4. a ERMAC não acarretou o desenvolvimento de recessões gengivais em nenhum dos tempos; 5. não houve correlação entre a quantidade de inclinação dentária e o desenvolvimento de recessões gengivais.(AU)
Resumo:
The human β2-adrenergic receptor gene has multiple single-nucleotide polymorphisms (SNPs), but the relevance of chromosomally phased SNPs (haplotypes) is not known. The phylogeny and the in vitro and in vivo consequences of variations in the 5′ upstream and ORF were delineated in a multiethnic reference population and an asthmatic cohort. Thirteen SNPs were found organized into 12 haplotypes out of the theoretically possible 8,192 combinations. Deep divergence in the distribution of some haplotypes was noted in Caucasian, African-American, Asian, and Hispanic-Latino ethnic groups with >20-fold differences among the frequencies of the four major haplotypes. The relevance of the five most common β2-adrenergic receptor haplotype pairs was determined in vivo by assessing the bronchodilator response to β agonist in asthmatics. Mean responses by haplotype pair varied by >2-fold, and response was significantly related to the haplotype pair (P = 0.007) but not to individual SNPs. Expression vectors representing two of the haplotypes differing at eight of the SNP loci and associated with divergent in vivo responsiveness to agonist were used to transfect HEK293 cells. β2-adrenergic receptor mRNA levels and receptor density in cells transfected with the haplotype associated with the greater physiologic response were ≈50% greater than those transfected with the lower response haplotype. The results indicate that the unique interactions of multiple SNPs within a haplotype ultimately can affect biologic and therapeutic phenotype and that individual SNPs may have poor predictive power as pharmacogenetic loci.
Resumo:
Because of variations in tRNA sequences in evolution, tRNA synthetases either do not acylate their cognate tRNAs from other organisms or execute misacylations which can be deleterious in vivo. We report here the cloning and primary sequence of a 958-aa Saccharomyces cerevisiae alanyl-tRNA synthetase. The enzyme is a close homologue of the human and Escherichia coli enzymes, particularly in the region of the primary structure needed for aminoacylation of RNA duplex substrates based on alanine tRNA acceptor stems with a G3.U70 base pair. An ala1 disrupted allele demonstrated that the gene is essential and that, therefore, ALA1 encodes an enzyme required for cytoplasmic protein synthesis. Growth of cells harboring the ala1 disrupted allele was restored by a cDNA clone encoding human alanyl-tRNA synthetase, which is a serum antigen for many polymyositis-afflicted individuals. The human enzyme in extracts from rescued yeast was detected with autoimmune antibodies from a polymyositis patient. We conclude that, in spite of substantial differences between human and yeast tRNA sequences in evolution, strong conservation of the G3.U70 system of recognition is sufficient to yield accurate aminoacylation in vivo across wide species distances.
Resumo:
A irrigação quando bem manejada, pode minimizar os riscos econômicos da atividade sucroalcooleira, particularmente em safras com presença de instabilidade climática onde a restrição hídrica, promovida pela diminuição no volume de chuvas, pode reduzir a produtividade dos canaviais. Dentre as ferramentas disponíveis para a gestão eficiente da água na agricultura irrigada, a técnica de irrigação sob déficit pode se tornar uma escolha acertada para a cana-de-açúcar, desde que sejam identificadas as fases fenológicas e épocas de cultivo onde a limitação da oferta de água não implique em reduções antieconômicas no rendimento da cultura. Diante disso, a hipótese que norteia essa pesquisa, é a de que existe uma estratégia de irrigação sob déficit, que associada a uma variedade com características específicas, possibilite a expressão de indicadores de produtividade tão satisfatórios quanto os obtidos em condições de irrigação plena. Nessa linha, os objetivos da pesquisa envolveram o estudo da dinâmica foliar, acúmulo e particionamento de biomassa e ainda, índices de produtividade da água para biomassa, açúcar e etanol de 1ª e 2ª geração de oito variedade de cana-de-açúcar, submetidas a diferentes condições de disponibilidade hídrica no solo em dois ciclos de cultivo (cana-planta e cana-soca). A pesquisa foi realizada na Escola Superior de Agricultura \"Luiz de Queiroz\", em Piracicaba/SP, onde foram estudados os dois primeiros ciclos de cultivo da cana-de-açúcar, sendo estes abordados nesta tese como Experimento 1 (cana-planta) e Experimento 2 (cana-soca). O delineamento experimental adotado para ambos os ciclos foi o de blocos casualizados, com três blocos completos. Os tratamentos foram compostos por três fatores em esquema de parcelas sub-subdivididas. Estas parcelas foram formadas por duas plantas (touceiras) alocadas em um vaso com aproximadamente 330 litros de solo. No Experimento 1, foram estudados três fatores, sendo o primeiro e segundo com quatro níveis e o terceiro com oito (4x4x8), totalizando assim 128 tratamentos, sendo eles: quatro níveis de irrigação ao longo do ciclo (125, 100, 75 e 50% da ETc); oito variedades comerciais de cana-de-açúcar e quatro procedimentos de maturação, impostos por meio de variações na intensidade do déficit hídrico aplicado. Para o Experimento 2, substitui-se o fator Maturação por Épocas de Corte, o qual consistiu em colheitas de um quarto do experimento a cada 90 dias. Os resultados encontrados apontaram que a área foliar responde positivamente a maior disponibilidade hídrica no solo, tendo sido verificado uma relação proporcional entre estes. Quanto ao acúmulo de biomassa, verificou-se que para as oito variedades estudadas houve incremento de biomassa a medida em que se aumentou o volume de água disponibilizado às variedades. No tocante ao particionamento, as folhas foram os drenos principais de fotoassimilados da planta até os 100 dias de cultivo, sendo que após este período, os colmos ocuparam o lugar de dreno preferencial. Os indicadores de produtividade da água apresentaram diferenças significativas para o fator lâmina, o que indica a existência de cultivares de cana-de-açúcar mais eficientes no uso da água. Por fim, observou-se que a produtividade da água para etanol total apresentou valores expressivos, com média para essa variável igual a 1,81 L m-3, o que denota o potencial de rendimento de etanol (1G + 2G) a partir da cana-de-açúcar quando é adotado o aproveitamento integral das plantas.
Resumo:
The moisture content and its spatial distribution has a great influence on the durability properties of concrete structures. Several non-destructive techniques have been used for the determination of the total water content, but moisture distribution is difficult to determine. In this paper impedance spectroscopy is used to study the water distribution in concrete samples with controlled and homogeneously distributed moisture contents. The technique is suitable for the determination of water distribution inside the sample, using the appropriate equivalent circuits. It is shown that using the selected drying procedures there is no change in the solid phase of the samples, although the technique can only be used for the qualitative study of variations in the solid phase when samples are too thick. The results of this work show that for a wide range of concrete percentages of saturation, from full to 18 % saturation, practically all the pores keep at least a thin layer of electrolyte covering their walls, since the capacitance measurement results are practically independent of the saturation degree.
Resumo:
The frequency of large-scale heavy precipitation events in the European Alps is expected to undergo substantial changes with current climate change. Hence, knowledge about the past natural variability of floods caused by heavy precipitation constitutes important input for climate projections. We present a comprehensive Holocene (10,000 years) reconstruction of the flood frequency in the Central European Alps combining 15 lacustrine sediment records. These records provide an extensive catalog of flood deposits, which were generated by flood-induced underflows delivering terrestrial material to the lake floors. The multi-archive approach allows suppressing local weather patterns, such as thunderstorms, from the obtained climate signal. We reconstructed mainly late spring to fall events since ice cover and precipitation in form of snow in winter at high-altitude study sites do inhibit the generation of flood layers. We found that flood frequency was higher during cool periods, coinciding with lows in solar activity. In addition, flood occurrence shows periodicities that are also observed in reconstructions of solar activity from 14C and 10Be records (2500-3000, 900-1200, as well as of about 710, 500, 350, 208 (Suess cycle), 150, 104 and 87 (Gleissberg cycle) years). As atmospheric mechanism, we propose an expansion/shrinking of the Hadley cell with increasing/decreasing air temperature, causing dry/wet conditions in Central Europe during phases of high/low solar activity. Furthermore, differences between the flood patterns from the Northern Alps and the Southern Alps indicate changes in North Atlantic circulation. Enhanced flood occurrence in the South compared to the North suggests a pronounced southward position of the Westerlies and/or blocking over the northern North Atlantic, hence resembling a negative NAO state (most distinct from 4.2 to 2.4 kyr BP and during the Little Ice Age). South-Alpine flood activity therefore provides a qualitative record of variations in a paleo-NAO pattern during the Holocene. Additionally, increased South Alpine flood activity contrasts to low precipitation in tropical Central America (Cariaco Basin) on the Holocene and centennial time scale. This observation is consistent with a Holocene southward migration of the Atlantic circulation system, and hence of the ITCZ, driven by decreasing summer insolation in the Northern hemisphere, as well as with shorter-term fluctuations probably driven by solar activity.
Resumo:
Mg/Ca, Sr/Ca, and stable isotope measurements have been performed on tests from the planktonic foraminifers Globigerinoides ruber (white), Globigerina bulloides, and Neogloboquadrina pachyderma (right coiling) in samples from Ocean Drilling Program site 977A in the Alboran Sea (Western Mediterranean). The evolution of different water masses between 250 and 150 ka is described. Warm substages were characterized by strong seasonality and thermal stratification of the water column. By contrast, less pronounced seasonality and basin stratification seem to prevail during cold substages. Several periods of stratification due to the low salinity of the upper water mass occurred during the formation of organic-rich layers and also during a possible Heinrich-like event at 220 ka. The three foraminifer species studied show a common and large shell Sr/Ca variability in short timescales, suggesting changes in the global ocean Sr/Ca ratio as one of the main causes of variations in shell composition.
Resumo:
ODP Site 798 on the Oki Ridge in the Southern Japan Sea yielded the first continuous and well-preserved record of Pleistocene planktonic foraminifers in the Northwestern Pacific Ocean region. Quantitative analysis of planktonic foraminifers completed for 122 samples from the 200-m-thick Pleistocene section cored at ODP Site 798 provides a proxy record of variations in sea-surface temperature, productivity, and circulation during the past 1.6 m.y. in an area beneath the track of the Tsushima Current. Faunal census data allow recognition of five distinct assemblages: (1) type A assemblages dominated by sinistrally coiling forms of Neogloboquadrina pachyderma representing polar-subpolar surface temperatures, (2) type B assemblages dominated by Globigerina bulloides and thought to represent periods of increased surface productivity and upwelling, (3) type C assemblages marked by significant abundances of dextrally coiling forms of N. pachyderma thought to represent the warm transitional waters of the Tsushima Current, (4) type D assemblages distinguished by relatively high percentages of dextral N. pachyderma and Globorotalia inflata that also represent warmer surface temperatures and increased flow of the Tsushima Current, and (5) type E assemblages marked by relatively large numbers of the delicate species Globigerina quinqueloba and Globigerinita spp., indicative of exceptional preservation conditions and/or episodic high production of these taxa. Early and middle Pleistocene coiling patterns of Neogloboquadrina pachyderma at Site 798 can be correlated with Pleistocene coiling trends and planktonic foraminiferal datums established in the onshore Oga Peninsula sequence of Northern Honshu and open-ocean N. pachyderma coiling dominance shifts in the North Pacific region. A sustained early Pleistocene warm period recognized in both the Oga Peninsula sequence and the Northern Pacific can clearly be recognized at Site 798. In addition, the late Pleistocene planktonic foraminiferal record at Site 798 shows good correlation with glaciation/deglaciation events for the Northern Hemisphere as delineated by oxygen isotopes and represents the first detailed analysis of Pleistocene sea-surface temperature changes in the Northwestern Pacific Ocean region.
Resumo:
A high-resolution (10-20 kyr) record of variations in CaCO3 content and dissolution was established for latest Cretaceous (last 0.7 Myr) deep-sea sediments from the South Atlantic Ocean (DSDP Site 516 from the Rio Grande Rise, and sites 525 and 527 from the Walvis Ridge). The degree of fragmentation of planktonic foraminifera (DFP) was used as a measure of calcite dissolution. High negative correlations between DFP and other independent measures of carbonate dissolution (percentage of sand fraction, absolute abundance of planktonic foraminifera, and planktonic/benthic foraminiferal ratio) validate its use as a sensitive index of calcite dissolution in upper Maastrichtian deep-sea sediments. Very high DFP and a significant negative correlation between DFP and CaCO 3 content suggest that Site 516 was located below the foraminiferal lysocline during the entire interval studied. Such a shallow position of the lysocline (paleodepth of Site 516 was 1.2 km) may be explained by "upwelling" of corrosive deep waters along the southern margin of the Rio Grande Rise. Sites 525 and 527 were located above the foraminiferal lysocline; however, three short periods of enhanced dissolution were recognised at Site 525 (paleodepth 1 km) and one interval of strong dissolution was identified at Site 527 (paleodepth 2.7 km). The lack of correspondence between the dissolution regimes at sites from the Walvis Ridge suggests limited deep-water communication across this physiographic barrier. Two of the dissolution maxima recognised at Site 525 correspond to carbonate maxima at Site 527. Variations in "upwelling" intensity along the Walvis Ridge, resulting in fluctuations in primary productivity in this area, may be the proximal cause of both carbonate cycles at Site 527 and dissolution cycles at Site 525. We suggest that development of the bottom Ekman layer between a hypothetical westward geostrophic current and the topographical height of the Rio Grande Rise-Walvis Ridge system may be a plausible hydrodynamical explanation for the proposed "'upwelling" along the southern margin of this topographical structure.
Resumo:
A mathematical model for long-term, three-dimensional shoreline evolution is developed. The combined effects of variations of sea level; wave refraction and diffraction; loss of sand by density currents during storms, by rip currents, and by wind; bluff erosion and berm accretion; effects of manmade structures such as long groin or navigational structures; and beach nourishment are all taken into account. A computer program is developed with various subroutines which permit modification as the state-of-the-art progresses. The program is applied to a test case at Holland Harbor, Michigan. (Author).
Resumo:
"April 23, 1962."
Resumo:
Available on demand as hard copy or computer file from Cornell University Library.
Resumo:
Available on demand as hard copy or computer file from Cornell University Library.