1000 resultados para lâminas permanentes


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Available on demand as hard copy or computer file from Cornell University Library.

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Imprint varies: v.2, D. Juan Oliveres.

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A presente pesquisa tem como objetivo avaliar cefalometricamente, o espaço e po-sicionamento das coroas dos segundos e terceiros molares superiores permanentes não erupcionados na região da tuberosidade maxilar durante a distalização dos pri-meiros molares superiores, além de verificar a correlação entre estas duas variáveis. A amostra foi constituída de 38 telerradiografias em norma lateral direita, obtidas de 19 pacientes, jovens brasileiros, leucodermas e melanodermas, sendo 6 do sexo masculino e 13 do sexo feminino, com idade média de 9 anos 5 meses 13 dias. A metodologia constou inicialmente da divisão dos tempos (T1) inicial, e após a distali-zação do primeiro molar superior permanente em (T2) por um período médio de 10 meses e 23 dias. Para avaliação do espaço e angulação das coroas existente utili-zou-se uma Linha referencial intracraniana (Linha M) sendo esta demarcada, a partir de dois pontos, o ponto SE localizado na sutura esfenoetmoidal, e o ponto Pt locali-zado na parte anterior da fossa pterigopalatina. Esta linha referencial foi transferida até o ponto F, (Linha M ) ponto este localizado na região mais posterio-inferior da tuberosidade maxilar. O espaço avaliado compreendeu entre a Linha M , até a face distal do primeiro molar superior permanente. Na análise estatística usou-se o teste t (Teste t Student) , e na correlação entre espaço e angulação foi utilizado o coefi-ciente de correlação de Pearson. Concluímos que o espaço correspondente entre a distal dos primeiros molares superiores permanentes e extremidade da tuberosidade maxilar, na fase inicial e após a movimentação distal, não é suficiente para a erup-ção dos segundos e terceiros molares superiores permanentes. A angulação das coroas na fase inicial e após a movimentação distal posicionam-se com angulações mais para distal. Quanto à correlação das angulações das coroas dos segundos e terceiros molares superiores permanentes e o espaço para erupção verificamos que quanto maior a angulação das coroas para distal, menor os espaços oferecidos para a erupção.(AU)

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The understanding of the occurrence and flow of groundwater in the subsurface is of fundamental importance in the exploitation of water, just like knowledge of all associated hydrogeological context. These factors are primarily controlled by geometry of a certain pore system, given the nature of sedimentary aquifers. Thus, the microstructural characterization, as the interconnectivity of the system, it is essential to know the macro properties porosity and permeability of reservoir rock, in which can be done on a statistical characterization by twodimensional analysis. The latter is being held on a computing platform, using image thin sections of reservoir rock, allowing the prediction of the properties effective porosity and hydraulic conductivity. For Barreiras Aquifer to obtain such parameters derived primarily from the interpretation of tests of aquifers, a practice that usually involves a fairly complex logistics in terms of equipment and personnel required in addition to high cost of operation. Thus, the analysis and digital image processing is presented as an alternative tool for the characterization of hydraulic parameters, showing up as a practical and inexpensive method. This methodology is based on a flowchart work involving sampling, preparation of thin sections and their respective images, segmentation and geometric characterization, three-dimensional reconstruction and flow simulation. In this research, computational image analysis of thin sections of rocks has shown that aquifer storage coefficients ranging from 0,035 to 0,12 with an average of 0,076, while its hydrogeological substrate (associated with the top of the carbonate sequence outcropping not region) presents effective porosities of the order of 2%. For the transport regime, it is evidenced that the methodology presents results below of those found in the bibliographic data relating to hydraulic conductivity, mean values of 1,04 x10-6 m/s, with fluctuations between 2,94 x10-6 m/s and 3,61x10-8 m/s, probably due to the larger scale study and the heterogeneity of the medium studied.

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Cactus pear is an important forage for livestock in semi-arid region of Brazil, due to its adaptation to climate conditions in this region, high productivity and nutritional value. The yield of this cactus has positively responded to techniques such as planting density, fertilization and cutting managements, however, in Rio Grande do Norte State, only certain areas have favorable climate conditions to the development of this crop. Drip irrigation, with a small amount of water, has proven to be an alternative to the viability of cactus pear cultivation in these areas. The research aimed to evaluate the effects of different levels of saline water and manure organic fertilization on the morphological characteristics and production of fresh and dry matter of the prickly-pear cactus cv. Miúda (Nopalea cochenillifera Salm Dick) in a dense planting system. The experiment was conducted at the Experimental Station of Terras Secas (EMPARN), Pedro Avelino, latitude 5°31'21" South and longitude 36°23'14" West. The soil was classified as Typical Cambisol Haplicum Carbonate and the water used in irrigation, C4S1T3 (5,25 dS.m-1), with planting spacing of 2.0 x 0.25 m (20,000 plants ha-1). A completely randomized design in a split plot was used, where water levels (0, 7.5, 15.0 and 30.0 mm month-1) with 10 days intervals, were the main plots and organic fertilization (0 , 25 and 50 Mg ha-1 yr-1) the subplots, with four replicates. The measured morphological characteristics were number of cladodes, height and volume of the plant; length, width, perimeter, thickness, area and cladodes area index, fresh and dry matter production, dry matter content, water use efficiency (WUE) and damage promoted by cochineal pest (Diaspis echinocacti) and soft rot (Erwinia carotovora). There was no influence (P>0.05) of organic fertilization on most variables, particularly in relation to the production of fresh and dry matter. The water levels had a significant influence (P<0.05) on most variables, promoting higher height and volume of the plants, larger and thicker cladodes, and increase on fresh and dry matter production (13.55 Mg DM ha-1 yr-1). The absence of irrigation caused a significant expansion in plant damage caused by the cochineal pest and when irrigated with different water levels there was an increase in damage and stand loss, caused by soft rot, been more intense at the higher water level.