62 resultados para Water level


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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

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The influence of water level variation (flood pulse) on the biomass and chemical composition of the aquatic macrophyte Eichhornia azurea, was investigated in a tropical oxbow lake of the Rio Mogi-Guacu, State of São Paulo, Brazil. The flood pulse causes an increase in total nitrogen content from 0.67 to 1.35 mg/L and total phosphorus content from 10.5 to 101.0 mu g/L of the water. This fertilization, associated with other factors, determines a typical seasonal variation in the biomass and chemical composition of the macrophyte.

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The largest losses in mechanical harvesting of peanuts occur during the stage of digging, and its assessment is still incipient in Brazil. Therefore, the aim of this study was to evaluate the quantitative losses and the performance of the tractor-digger-inverter, according to soil water content and plant populations. The experiment was conducted in a completely randomized block design with a factorial scheme 2 x 3, in which the treatments consisted of two soil, water content (19.3 and 24.8%) and three populations of plants (86,111, 127,603 and 141,144 plants ha-1), with four replications. The quantitative digging losses and the set mechanized performance were evaluated. The largest amount of visible and total losses was found in the population of 141.144 plants ha-1 for the 19.3% soil water content. The harvested material flow and the tractor-digger-inverter performance were not influenced by soil water content and plant population. The water content in the pods was higher in 24.8% soil water content only for the population of 86,111 plants ha-1; the yield was higher in the populations of 141.144 and 127.603 plants ha-1, in the 19.3 e 24.8% soil water content, respectively.

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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

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Soil compaction may be defined as the pressing of soil to make it denser. Soil compaction makes the soil denser, decreases permeability of gas and water exchange as well as alterations in thermal relations, and increases mechanical strength of the soil. Compacted soil can restrict normal root development. Simulations of the root restricting layers in a greenhouse are necessary to develop a mechanism to alleviate soil compaction problems in these soils. The selection of three distinct bulk densities based on the standard proctor test is also an important factor to determine which bulk density restricts the root layer. This experiment aimed to assess peanut (Arachis hypogea) root volume and root dry matter as a function of bulk density and water stress. Three levels of soil density (1.2, 1.4, and 1.6g cm-3), and two levels of the soil water content (70 and 90% of field capacity) were used. Treatments were arranged as completely randomized design, with four replications in a 3×2 factorial scheme. The result showed that peanut yield generally responded favorably to subsurface compaction in the presence of high mechanical impedance. This clearly indicates the ability of this root to penetrate the hardpan with less stress. Root volume was not affected by increase in soil bulk density and this mechanical impedance increased root volume when roots penetrated the barrier with less energy. Root growth below the compacted layer (hardpan), was impaired by the imposed barrier. This stress made it impossible for roots to grow well even in the presence of optimum soil water content. Generally soil water content of 70% field capacity (P<0.0001) enhanced greater root proliferation. Nonetheless, soil water content of 90% field capacity in some occasions proved better for root growth. Some of the discrepancies observed were that mechanical impedance is not a good indicator for measuring root growth restriction in greenhouse. Future research can be done using more levels of water to determine the lowest soil water level, which can inhibit plant growth.

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In order to evaluate the bean yield under different water table levels as well as the moisture and nitrate distribution in the soil profile, a field experiment was carried out in the experimental area of the College of Agricultural Sciences - UNESP, Botucatu, SP, Brazil. Beans were grown in field lysimeters under five water table depths: 30; 40; 50; 60 and 70 cm. The moisture in the soil profile was determined gravimetrically using samples collected at 10; 20; 30; 40; 50; 60 and 70 cm deep. The water table depths of 30cm and 40cm showed the highest productivities (3,228.4kg.ha-1 and 3,422.1kg.ha-1, respectively), with no statistical differences between them. The highest productivity was related to the two highest water table levels (30 and 40cm), which provided the highest moisture average values on the basis of volume in the soil profile (33.3 e 31%) as well as the consumptive use of water (416 and 396mm). The nitrate content during the bean cycle at the extraction depth of 60cm was below the safe drinking limit of 10mg.1-1 for water table depths of 30; 40; 50 and 60cm, which shows the denitrification efficiency as a way of controlling nitrate pollution in water tables. The management of water table can lead to high levels of bean yield and to a better control of nitrate pollution in underground water.

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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

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Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

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The irrigation application is one of the most useful techniques in tropical environments, especially during dry seasons. In this study, CO2 efflux, temperature and soil moisture were studied in a field sampled with a grid having 48 points distributed in 35 x 25 m, under irrigation promoted by a sprinkler located at the center of the area, provoking different levels of water deposition, with maximum irrigation levels of 44.4 and 62.2 mm in points closer to the sprinkler. The results show that the emissions, temperature and moisture were strongly affected by the two irrigations events, having a total water level added of 106,6 mm for the points next to the sprinkler and zero for the most distant points from it. The maps of space variation of the variables, as well as the linear correlation between them, indicate that the emissions were positively related to the soil moisture and negative correlated to the soil temperature only after the irrigations events. The special variability models of soil CO2 emission changed from exponential to spherical after the irrigations events. Such results indicate that soil moisture is among possible controlling factors of the soil CO2 emission, because even with reductions in soil temperature provoked by the wetness, emissions increased strongly.

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Atualmente na agricultura, a soja ocupa lugar de destaque garantido pela alta produtividade e excelente rentabilidade no mercado nacional, principalmente na exportação de grãos. Sabe-se que para uma boa produtividade é necessário um bom planejamento, além de técnicas de preparo do solo adequadas a cada região do País. Este trabalho, desenvolvido na Universidade Estadual Paulista, Faculdade de Ciências Agrárias e Veterinárias, Campus de Jaboticabal, SP, teve por objetivo, analisar o efeito de diferentes sistemas de preparo no solo e na cultura da soja (Glycine max (L.) Merrill) em Latossolo Vermelho Eutroférrico. Os tratamentos foram 3 preparos convencionais (arado de discos + duas passadas de grade leve, arado de aivecas + duas passadas de grade leve, grade pesada + grade leve), 2 preparos reduzidos (escarificador com rolo destorroador + grade leve, escarificador com rolo destorroador) e semeadura direta, resultando em 6 tratamentos com 4 repetições, totalizando 24 observações. O teor de água no solo não difere entre tratamentos. Na camada superficial (0-5 cm) a semeadura direta apresenta maior resistência à penetração em relação ao arado de aivecas com duas gradagens leves e escarificador com uma gradagem leve. As características agronômicas da cultura da soja não são influenciadas pelos tratamentos estudados.

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Apesar da importância na dinâmica dos ecossistemas aquáticos, as macrófitas podem formar densas e extensas colonizações em corpos hídricos cujos equilíbrios ecológicos foram rompidos. Nessas condições, essas plantas promovem uma série de problemas que as tornam alvos de controle. Para elaboração de planos adequados de manejo dessa vegetação, é fundamental o conhecimento das dinâmicas relativas das populações que a compõem. O objetivo deste trabalho foi realizar levantamentos mensais da composição específica da comunidade de macrófitas que coloniza o reservatório de Santana, localizado no município de Piraí/RJ, monitorando 97 pontos georreferenciados, abrangendo toda a lâmina d'água. Foram identificadas 41 espécies, inseridas em 21 famílias botânicas. As famílias Poaceae, Pontederiaceae e Cyperacae foram as que apresentaram os maiores números de espécies ao longo do ano. Salvinia herzogii e Egeria densa apresentaram as maiores notas anuais de colonização do reservatório. As populações de Eichhornia azurea, Brachiaria arrecta e Paspalum repens completaram o grupo das espécies numericamente mais relevantes. As plantas de hábito flutuante tenderam a apresentar populações com padrão de distribuição geográfica casualizado, enquanto as espécies fixadas no sedimento e as submersas apresentaram populações com padrão agregado. Não houve expressivas variações mensais dos valores dos índices de diversidade (H') e de equitabilidade (E') das comunidades de macrófitas aquáticas ao longo do ano. O dendrograma construído com o coeficiente de Odum mostrou uma seqüência lógica dos meses, evidenciando uma definida sucessão de populações divididas em dois grupos de similaridade separados pelo mês de junho. Nessa época, o nível de água do reservatório foi reduzido e o sedimento ficou exposto, favorecendo as espécies de hábito emergente.

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Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)