923 resultados para Graxaim-do-mato


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

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

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O nitrogênio é o nutriente aplicado em maior quantidade à cultura do feijão, o mais limitante ao crescimento e desenvolvimento das plantas e o que mais onera o custo de produção. Uma boa opção para o produtor diminuir custos, com a utilização de fertilizantes nitrogenados, é a utilização de plantas de cobertura do solo, também conhecidas como adubos verdes. Assim, este trabalho objetivou avaliar os custos de produção e índices de lucratividade de diferentes tratamentos envolvendo coberturas vegetais e doses de nitrogênio em cobertura, na cultura do feijoeiro irrigado, em sistema plantio direto, nas safras de inverno de 2010 e 2011. O trabalho foi realizado em área experimental localizada no município de Selvíria (MS), em Latossolo Vermelho distrófico típico. Os tratamentos constituíram-se de seis coberturas vegetais (Crotalaria juncea, milheto, guandú, Crotalaria juncea + milheto, guandú + milheto e pousio) e quatro doses de N (0 kg ha-1, 30 kg ha-1, 60 kg ha-1 e 90 kg ha-1). Foram estimados o custo operacional total, receita bruta, lucro operacional, índice de lucratividade, produtividade de equilíbrio e o preço de equilíbrio. Concluiu-se que o uso da Crotalaria juncea, como cobertura vegetal do solo, proporcionou os maiores valores de custo operacional total e lucro operacional e os melhores índices de lucratividade, e que o incremento nas doses de nitrogênio aumentou o custo operacional total, com tendência de aumento na produtividade e, consequentemente, no preço de equilíbrio.

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

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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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Hemicelluloses are polysaccharides of low molecular weight containing 100 to 200 glycosidic residues. In plants, the xylans or the hemicelluloses are situated between the lignin and the collection of cellulose fibers underneath. The xylan is the most common hemicellulosic polysaccharide in cell walls of land plants, comprising a backbone of xylose residues linked by beta-1,4-glycosidic bonds. So, xylanolytic enzymes from microorganism have attracted a great deal of attention in the last decade, particularly because of their biotechnological characteristics in various industrial processes, related to food, feed, ethanol, pulp, and paper industries. A microbial screening of xylanase producer was carried out in Brazilian Cerrado area in Selviria city, Mato Grosso do Sul State, Brazil. About 50 bacterial strains and 15 fungal strains were isolated from soil sample at 35 A degrees C. Between these isolated microorganisms, a bacterium Lysinibacillus sp. and a fungus Neosartorya spinosa as good xylanase producers were identified. Based on identification processes, Lysinibacillus sp. is a new species and the xylanase production by this bacterial genus was not reported yet. Similarly, it has not reported about xylanase production from N. spinosa. The bacterial strain P5B1 identified as Lysinibacillus sp. was cultivated on submerged fermentation using as substrate xylan, wheat bran, corn straw, corncob, and sugar cane bagasse. Corn straw and wheat bran show a good xylanase activity after 72 h of fermentation. A fungus identified as N. spinosa (strain P2D16) was cultivated on solid-state fermentation using as substrate source wheat bran, wheat bran plus sawdust, corn straw, corncob, cassava bran, and sugar cane bagasse. Wheat bran and corncobs show the better xylanase production after 72 h of fermentation. Both crude xylanases were characterized and a bacterial xylanase shows optimum pH for enzyme activity at 6.0, whereas a fungal xylanase has optimum pH at 5.0-5.5. They were stable in the pH range 5.0-10.0 and 5.5-8.5 for bacterial and fungal xylanase, respectively. The optimum temperatures were 55C and 60 A degrees C for bacterial and fungal xylanase, respectively, and they were thermally stable up to 50 A degrees C.

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Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

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Effect of green manure and sowing date on the productivity of bean no-tillage in the Cerrado region. Green manure and sowing date are two important factors that influence the productivity of cultivars. The objective of this study was to evaluate the production of biomass from different vegetation covers (millet, sorghum and Brachiaria brizantha) and the accumulation of nutrients and their effects on the bean cultivars (Pearl, IAC Tuna and Carioca Precoce) at different sowing dates (6/22 and 7/6). The experiment was conducted at the experimental area of the Universidade Estadual Paulista - Unesp, located in Selviria, Mato Grosso do Sul State, in the 2006/2007 agricultural year. The randomized blocks design was used with four replications, and the evaluations of the coverage were: the biomass of fresh and dry matter and nutrients accumulated in plants; for the beans: cycle, final stand, number of pods/plant, number of seeds per pod, mass of 100 seeds, and productivity. It was observed that millet and sorghum showed higher productivity of fresh and dry mass, and accumulate greater quantity of nutrients in straw; the time most suitable for sowing was in June, and the late sowing of cv. Carioca Precoce did not affect their productivity, the use of Brachiaria brizantha straw in coverage provided better conditions for productivity in the bean no-tillage system.

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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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Realizou-se a análise comparativa de custos de produção de feijão, após um ano em sistemas de plantio direto e convencional, no período de inverno, com irrigação por pivô central. Os experimentos foram desenvolvidos na Fazenda Dois Irmãos, em Pereira Barreto (SP), em delineamento experimental de blocos ao acaso, com 11 tratamentos e quatro repetições, para cada sistema de plantio. Os tratamentos constaram de uma testemunha sem N, duas fontes de N (uréia e nitrato de amônio) e cinco dosagens (20, 40, 60, 80 e 100 kg.ha-1 de N), aplicados em cobertura aos 27 dias após a emergência das plantas. Utilizou-se densidade de 15 plantas por metro de linha e 0,50 m entre sulcos, com semeadura realizada em 20/5/2001. Na área do sistema de plantio direto, as plantas daninhas foram dessecadas após o cultivo do milho, e na de plantio convencional, realizaram uma aração e duas gradagens, sendo uma pesada e uma niveladora, no preparo do solo. Durante o desenvolvimento da cultura foram aplicados herbicidas em pós-emergência para o controle do mato. As duas fontes de nitrogênio mostraram efeito positivo na produção de grãos. A análise econômica revelou melhor resultado para uréia, na dose de 60 kg.ha-1 de N, em preparo convencional do solo, com índice de lucratividade de 40,6%. Para o plantio direto, o nitrato de amônio, na base de 40 kg.ha-1 de N, mostrou maior acréscimo na receita e lucratividade de 25,6%.

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Este trabalho teve como objetivo verificar o efeito de seis concentrações de ácido indolbutírico (IBA) no enraizamento de estacas herbáceas de figueira (Ficus carica L.) sob nebulização intermitente, em três épocas diferentes. Os ensaios foram instalados em maio/2004, setembro/2004 e janeiro/2005, e, em cada época, o delineamento experimental utilizado foi o inteiramente casualizado, com seis concentrações de IBA (0, 500, 1.000, 1.500, 2.000, 2.500 e 3.000 mg L-1). As estacas foram coletadas na Fazenda de Ensino, Pesquisa e Extensão da Unesp, localizada no município de Selvíria, Estado de Mato Grosso do Sul, sendo padronizadas com 10 cm de comprimento e duas folhas. Após o preparo das estacas, estas foram tratadas com solução de Metiltiofan, posteriormente imersas nas soluções de IBA por 10 min. em seguida, realizou-se o plantio em jardineiras plásticas de cor preta, contendo vermiculita, que foram transportadas para telado, com 50% de redução de luz, com sistema de irrigação do tipo nebulização intermitente. As variáveis analisadas foram: porcentagem de estacas sobreviventes e enraizadas, número de raízes, comprimento máximo do sistema radicular e massa da matéria seca da raiz. Nas condições em que o trabalho foi conduzido, permite-se concluir que: é viável a propagação herbácea de figueira; houve efeito do IBA apenas em maio, em que a melhor dose foi de 1.000 mg L-1; as melhores épocas para estaquia de estacas herbáceas de figueira são em setembro e janeiro, sem utilização de IBA, nas quais foram obtidos melhores resultados quanto à porcentagem de estacas enraizadas.

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

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This thesis deals with the sedimentological/stratigraphic and structural evolution of the sedimentary rocks that occur in the NW continental border of the Potiguar Basin. These rocks are well exposed along coastal cliffs between the localities of Lagoa do Mato and Icapuí, Ceará State (NE Brazil). The sedimentological/stratigraphic study involved, at the outcrop scale, detailed facies descriptions, profile mapping of the vertical succession of different beds, and columnar sections displaying inferred lateral relationships. The approach was complemented by granulometric and petrographic analyses, including the characterization of heavy mineral assemblages. The data set allowed to recognize two kinds of lithological units, a carbonate one of very restricted occurrence at the base of the cliffs, and three younger, distinct siliciclastic units, that predominate along the cliffs, in vertical and lateral extent. The carbonate rocks were correlated to the late Cretaceous Jandaíra Formation, which is covered by the siliciclastic Barreiras Formation. The Barreiras Formation occurs in two distinct structural settings, the usual one with nondeformed, subhorizontal strata, or as tilted beds, affected by strong deformation. Two lithofacies were recognized, vertically arranged or in fault contacts. The lower facies is characterized by silty-argillaceous sandstones with low-angle cross bedding; the upper facies comprises medium to coarse grained sandstones, with conglomeratic layers. The Tibau Formation (medium to coarse-grained sandstones with argillite intercalations) occurs at the NW side of the studied area, laterally interlayered with the Barreiras Formation. Eolic sediments correlated to the Potengi Formation overly the former units, either displaying an angular unconformity, or simply an erosional contact (stratigraphic unconformity). Outstanding structural features, identified in the Barreiras Formation, led to characterize a neocenozoic stress field, which generated faults and folds and/or reactivated older structures in the subjacent late cretaceous (to paleogene, in the offshore basin) section. The structures recognized in the Barreiras Formation comprise two distinct assemblages, namely a main extensional deformation between the localities of Ponta Grossa and Redonda, and a contractional style (succeeded by oblique extensional structures) at Vila Nova. In the first case, the structural assemblage is dominated by N-S (N±20°Az) steep to gently-dipping extensional faults, displaying a domino-style or listric geometry with associated roll-over structures. This deformation pattern is explained by an E-W/WNW extension, contemporaneous with deposition of the upper facies of the Barreiras Formation, during the time interval Miocene to Pleistocene. Strong rotation of blocks and faults generated low-angle distensional faults and, locally, subvertical bedding, allowing to estimate very high strain states, with extension estimates varying between 40% up to 200%. Numerous detachment zones, parallel to bedding, help to acommodate this intense deformation. The detachment surfaces and a large number of faults display mesoscopic features analoguous to the ones of ductile shear zones, with development of S-C fabrics, shear bands, sigmoidal clasts and others, pointing to a hydroplastic deformation regime in these cases. Local occurrences of the Jandaíra limestone are controled by extensional faults that exhume the pre-Barreiras section, including an earlier event with N-S extension. Finally, WNWtrending extensional shear zones and faults are compatible with the Holocene stress field along the present continental margin. In the Vila Nova region, close to Icapuí, gentle normal folds with fold hinges shallowly pluging to SSW affect the lower facies of the Barreiras Formation, displaying an incipient dissolution cleavage associated with an extension lineation at high rake (a S>L fabric). Deposition of the upper facies siliciclastics is controlled by pull-apart graben structures, bordered by N-NE-trending sinistral-normal shear zones and faults, characterizing an structural inversion. Microstructures are compatible with tectonic deformation of the sedimentary pile, burried at shallow depths. The observed features point to high pore fluid pressures during deformation of the sediments, producing hydroplastic structures through mechanisms of granular flow. Such structures are overprinted by microfractures and microfaults (an essentially brittle regime), tracking the change to microfracturing and frictional shear mechanisms accompanying progressive dewatering and sediment lithification. Correlation of the structures observed at the surface with those present at depth was tested through geophysical data (Ground Penetrating Radar, seismics and a magnetic map). EW and NE-trending lineaments are observed in the magnetic map. The seismic sections display several examples of positive flower structures which affect the base of the cretaceous sediments; at higher stratigraphic levels, normal components/slips are compatible with the negative structural inversion characterized at the surface. Such correlations assisted in proposing a structural model compatible with the regional tectonic framework. The strong neogenepleistocene deformation is necessarily propagated in the subsurface, affecting the late cretaceous section (Açu and Jandaíra formations), wich host the hydrocarbon reservoirs in this portion of the Potiguar Basin. The proposed structural model is related to the dextral transcurrent/transform deformation along the Equatorial Margin, associated with transpressive terminations of E-W fault zones, or at their intersections with NE-trending lineaments, such as the Ponta Grossa-Fazenda Belém one (the LPGFB, itself controlled by a Brasiliano-age strike-slip shear zone). In a first step (and possibly during the late Cretaceous to Paleogene), this lineament was activated under a sinistral transpressional regime (antithetic to the main dextral deformation in the E-W zones), giving way to the folds in the lower facies of the Barreiras Formation, as well as the positive flower structures mapped through the seismic sections, at depth. This stage was succeeded (or was penecontemporaneous) by the extensional structures related to a (also sinistral) transtensional movement stage, associated to volcanism (Macau, Messejana) and thermal doming processes during the Neogene-Pleistocene time interval. This structural model has direct implications to hydrocarbon exploration and exploitation activities at this sector of the Potiguar Basin and its offshore continuation. The structure of the reservoirs at depth (Açu Formation sandstones of the post-rift section) may be controlled (or at least, strongly influenced) by the deformation geometry and kinematics characterized at the surface. In addition, the deformation event recognized in the Barreiras Formation has an age close to the one postulated for the oil maturation and migration in the basin, between the Oligocene to the Miocene. In this way, the described structural cenario represents a valid model to understand the conditions of hydrocarbon transport and acummulation through space openings, trap formation and destruction. This model is potentially applicable to the NW region of the Potiguar Basin and other sectors with a similar structural setting, along the brazilian Equatorial Atlantic Margin