1000 resultados para Resposta Auditiva de Estado Estável


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The use of glyphosate sub-lethal rates can be an alternative to reduce the plant height of sunn hemp, facilitating its mechanical harvest. However, little known on the other effects that its application can result in this culture. This work aimed to evaluate the influence of application times (10; 20 and 30 days after the emergence) and glyphosate sub-lethal rates (0; 30; 60; 90 and 120 g ha(-1)), on the vegetative and reproductive development of Crotalaria juncea cultivated in no-tillage system. The experiment was conducted between the january and june months of year 2010, in Selviria, Mato Grosso do Sul State, Brazil, on a clayey Rhodic Haplustox (20 degrees 20' S and 51 degrees 24' W). The experiment design was randomized blocks in factorial arrangement 3 x 5 (application times x glyphosate rates), with four replicates. Were measured agronomic characters and productivity and the results undergone to the test F, being the times averages compared by Tukey test (P<0.05) and of rates by regression analysis. The stem diameter, seeds number per pod and mass of one thousand seeds not were affected by glyphosate application. Despite the glyphosate have provided reduction in plant height and increase of the branches number in Crotalaria juncea, not recommended the sub-lethal rates application of product per of affect straightly the culture productivity.

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This thesis describes the general behavior of the northern shore of the State of Rio Grande do Norte relating beach profile morphology with hydrodynamic and sedimentological parameters. The Macau and Serra Oil Field are inserted on this area and are under accelerated coastal erosion. At these oil fields are installed oil wells from PETROBRAS, nowadays located directly in the shoreline, under constant attacks of coastal processes (e.g. waves, tides and currents), which promote an intense morphodynamic variability of this sandy coast. The area was monitored for 24 months in three different stations (P01, P02 and P03). The methodology applied involved current techniques of beach profiles, hydrodynamical processes, remote sensing and geophysics. A synthesis of results obtained through the use of different time scales (monthly, lunar cycle, seasonal, annual) from a coastal dynamics study is presented. The average wind direction corresponded to 77ºAz (NE). The steepness of the berm and of the shoreface, as well as coastal current direction, do not present major changes, with an average of 36º for the steepness of the berm, 15º for the shoreface and 15º for the coastal current direction. This data set allows us to infer that the months of larger coastal erosion were November/2000 and April/2001, because of the largest wave parameter during this time. The months of worse coastal erosion in this area are related with the increasing wavy energy. This in turn, seems to be related to seasonal climatic variations, with the wave energy and tide currents speed increasing during months of minor precipitations (June to January). The months of worse coastal erosion were September and November, when the largest wave parameters and speed currents are measured in the area. Since these months are included on the period of minor precipitations, we related the coastal erosion to seasonal climatic variations. The results obtained during these 24 months of monitoring confirms a situation of accentuated erosion, mainly in Profile 03 (Barra do Corta-Cachorro), where the wave height, period, and coastal current speed are always larger than the values found in Profile 02 (Macau5). Probably these values are more expressive in Profile 03, because it does not present any natural structure of protection against the wave impacts, as the barrier island located at Ponta do Tubarão, or the sand banks in front of Macau5. The transport of the sediments occurs from East to West, and the sand accumulation is more pronounced on Profile 03 intertidal zone, where there are embrionary dunes in dryer months. The tidal currents speed, on the other hand, is more accentuated in the Macau5 area (Profile 02). At Ponta do Tubarão, the tidal currents presented a preferential direction for NE, at times of flood, currents and for NW, at times of ebb current; at Barra do Corta-Cachorro the direction of the currents were predominantly for NW, independent of the tide phase, coinciding with the preferential direction of the longshore current. This currents inversion at Ponta do Tubarão is attributed to the presence of the Ponta do Tubarão island barrier and by the communication channel of the lagoon with the sea. The tide currents are better observed in protected areas, as in the Ponta do Tubarão, when they present inversion in their direction accordingly to the flood and ebb tide. In open areas, as in Barra do Corta-Cachorro, the tide currents are overprinted by the longshore currents. Sediment analysis does not show important modifications in grain size related to seasonality (dry- and rainy seasons). On the foreshore and backshore zones, the sediments vary from fine to medium sand, while in the shoreface they very from fine to very sands. The grains are mostly spheres, varying from sub rounded to sub angled. Quartz is the main component alongside Feldspat and heavy minerals as accessory components. Biogenic content is also present and mainly represented by mollusks fragments. The calculated sediment transport show values around 100 m3/day. The morphodynamic studies indicated that this is a reflexive area from October to April, and intermediate from May to September. The Relative Tide Range-RTR for this area is 4 < RTR < 15, and so classified in the mixed wave-tide group. Having this exposed we can affirm that the more active natural factors in this area are the currents, followed by the tides and the winds. The anthropic factors are exclusively local and punctual (Macau and Serra Oil Field). Taking in account the economic importance of the area, as well as the intensity of coastal processes acting on this shore, it is important a continuity of the monthly environmental monitoring looking for variations on longer-period cycles. These data have been stored on the geo-referenced database of the projects MARPETRO and PETRORISCO (REDE 05), aiming to model the coastal and sea environment, susceptible to oil spills and their derivatives

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Geological and geophysical studies (resistivity, self potential and VLF) were undertaken in the Tararaca and Santa Rita farms, respectively close to the Santo Antônio and Santa Cruz villages, eastern Rio Grande do Norte State, NE Brazil. Their aim was to characterize water acummulation structures in crystalline rocks. Based on geological and geophysical data, two models were characterized, the fracture-stream and the eluvio-alluvial through, in part already described in the literature. In the Tararaca Farm, a water well was located in a NW-trending streamlet; surrounding outcrops display fractures with the same orientation. Apparent resistivity sections, accross the stream channel, confirm fracturing at depth. The VLF profiles systematically display an alignment of equivalent current density anomalies, coinciding with the stream. Based on such data, the classical fracture-stream model seems to be well characterized at this place. In the Santa Rita Farm, a NE-trending stream display a metric-thick eluvioregolith-alluvial cover. The outcropping bedrock do not present fractures paralell to the stream direction, although the latter coincides with the trend of the gneiss foliation, which dips to the south. Geophysical data confirm the absence of a fracture zone at this place, but delineate the borders of a through-shaped structure filled with sediments (alluvium and regolith). The southern border of this structure dips steeper compared to the northern one. This water acummulation structure corresponds to an alternative model as regards to the classical fracture-stream, being named as the eluvio-alluvial trough. Its local controls are the drainage and relief, coupled with the bedrock weathering preferentially following foliation planes, generating the asymmetry of the through

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OBJETIVO: Analisar o consumo de medicamentos e os principais grupos terapêuticos consumidos por pessoas com deficiências físicas, auditivas ou visuais. MÉTODOS: Estudo transversal em que foram analisados dados do Inquérito Multicêntrico de Saúde no Estado de São Paulo (ISA-SP) em 2002 e do Inquérito de Saúde no Município de São Paulo (ISA-Capital), realizado em 2003. Os entrevistados que referiram deficiências foram estudados segundo as variáveis que compõem o banco de dados: área, sexo, renda, faixa etária, raça, consumo de medicamentos e tipos de medicamentos consumidos. RESULTADOS: A percentagem de consumo entre as pessoas com deficiência foi de: 62,8% entre os visuais; 60,2% entre os auditivos e 70,1% entre os físicos. As pessoas com deficiência física consumiram 20% mais medicamentos que os não-deficientes. Entre as pessoas com deficiência visual, os medicamentos mais consumidos foram os diuréticos, agentes do sistema renina-angiotensina e analgésicos. Pessoas com deficiência auditiva utilizaram mais analgésicos e agentes do sistema renina-angiotensina. Entre indivíduos com deficiência física, analgésicos, antitrombóticos e agentes do sistema renina-angiotensina foram os medicamentos mais consumidos. CONCLUSÕES: Houve maior consumo de medicamentos entre as pessoas com deficiências quando comparados com os não-deficientes, sendo os indivíduos com deficiência física os que mais consumiram fármacos, seguidos de deficientes visuais e auditivos.

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Com o objetivo de avaliar o efeito da enxertia e do enriquecimento da água de irrigação com dióxido de carbono sobre o teor de N, P, K, Ca, Mg, S, Mn e Zn na parte aérea de plantas de pepino tipo japonês cultivados em ambiente protegido, foram conduzidos experimentos em duas épocas do ano. O delineamento experimental foi em blocos ao acaso com quatro tratamentos e quatro repetições. Os tratamentos foram plantas de pepino enxertadas e não enxertadas, irrigadas com água comum ou enriquecida com CO2, em uma concentração de 1 no primeiro semestre e 0,25 no segundo semestre. No final do ciclo da cultura, o CO2, influenciou unicamente no primeiro semestre os teores de K, Ca, Mg, S e Zn; enquanto o teor de N só alterou no segundo semestre. Não houve padrão de resposta consistente da enxertia sobre os teores de N, P, Mg e Zn; porém, plantas enxertadas apresentam maior teor de K e menor teor de Mg, S e Ca na sua parte aérea, ao final do ciclo da cultura, podendo estar relacionado com os sintomas de deficiências nutricionais observados em plantas de pepino enxertadas.

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Foram estudadas as respostas plásticas em plântulas e plantas jovens de duas espécies arbóreas nativas, Adelia membranifolia (Müll. Arg.) Pax & K. Hoffm. (Euphorbiaceae) e Peltophorum dubium (Spreng.) Taub. (Leguminosae-Caesalpinoidae), submetidas ao alagamento do substrado associado ao déficit nutricional. Avaliou-se o acréscimo em superfície no módulo de expressão, definido como a região do eixo da plântula que, sob condições de estresse, sofre rediferenciação sendo considerada a hipertrofia lenticelar como a expressão morfogenética mais comum. em A. membranifolia a associação do estresse nutricional e alagamento do substrato foi a condição mais restritiva tanto para o crescimento em altura e diâmetro do colo quanto para as expressões morfogenéticas. Já em P. dubium o estado nutricional foi mais restritivo que o alagamento para o crescimento do colo. em geral, para ambas as espécies, plantas nutridas mantidas alagadas restabeleceram seu ritmo de crescimento a partir do terceiro mês de tratamento, além de expressarem respostas plásticas como a hipertrofia lenticelar e a formação de raízes adventícias. Quanto ao aumento em superfície, nos lotes desnutridos, verificou-se que em A. membranifolia de um total de 38% de superfície expressa, 12% corresponderam à hipertrofia lenticelar. em P. dubium verificou-se as maiores variações de aumento em superfície expressa por hipertrofia lenticelar, elevando de 5% para 13%. em geral a superfície modular nos lotes tratados foi o dobro em relação ao controle. É possível que o aumento em superfície, para algumas espécies, seja significativo como tendência ao aumento da estabilidade no desenvolvimento a partir de interações fisiológicas.

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