968 resultados para crop contents
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Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)
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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)
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ABSTRACT: The eastern border of the Transition Subdomain of the Carajás Province is constituteddominantly of Archean tonalite-trondhjemite-granodiorite (TTG). Deformed monzogranites, similar to the Planalto granite suite, and metagabbros inserted in association mafic-enderbitic also occur. Paleoproterozoic isotropic granites and mafic dykes devoid of significant deformation crosscut the Archean lithologies. The TTGs are exposed as blocks or as flat outcrops in areas of low relief and commonly include quartz-diorite enclaves. The TTG rocks display gray colour and are generally medium-grained, showing compositional banding or, sometimes, homogeneous aspect. They show commonly a NW-SW to E-W trending foliation with vertical to subvertical dips and were submitted to NE-SW stress. Locally, it was identified a NE-SW foliation transposed to E-W along shear zones. In some instances, they exhibit mylonitic to protomilonitics features, registered in the oval form of plagioclase porphyroclasts or boudinated leucogranitics veins. Two petrographic varieties are recognized for this association: biotite-trondjhemite and subordinate biotite-granodiorites, both have similar mineralogical and textural aspects and are characterized by a poorly preserved igneous texture, partially overwritten by an intense recrystallization. EDS analyses revealed that the plagioclase is a calcic oligoclase (An27-19), with Or ranging from 0.6 - 2.3%. The biotites are ferromagnesian, with dominance of Fe over Mg (Fe / [Fe + Mg] ranging from 0.54 to 0.59) and the analyzed epidote presents pistacite contents ranging from 23 to 27.6 % and plot mostly in the range of magmatic epidotes. The trondhjemite shows all typical characteristics of Archean TTG suites. They have high La/Yb and Sr/Y ratios, suggesting they were derived from the partial melting of garnet amphibolite sources at high pressures (ca. 1.5 GPa) or, at least, that their magmatic evolution was controlled by the fractionation of garnet and possibly amphibole, without significant influence of plagioclase. The studied TTGs show similarities with Mariazinha tonalite and Mogno trondjemite, of the Rio Maria Domain, Colorado trondhjemite and, in at a lesser degree, to the Rio Verde trondhjemite, of the Carajás Domain. The granodiorites display a calc-alkaline signature and shows LILE enrichment, specifically K2O, Rb and Ba, when compared to the trondhjemites, but still preserving some geochemical features of the TTG. The geochemical data indicate that the trondhjemite and granodiorite are not related by fractional crystallization. An origin of the granodiorite by partial melting of the TTG rocks is also discarded. The granodiorite could, however, result of contamination of TTG magmas by lithosphere metasomatism or assimilation of sediments from subducted oceanic crust along trondhjemite liquid genesis. In the eastern portion of the mapped area, it was identified a small, E-W trending granite stock clearly controlled by shear zones. The rocks have mylonitic textures, characterized by ovoid-shaped feldspar porphyroclasts, wrapped by recrystallized quartz and mica. These granitic rocks have geochemical signatures of reduced A-type granites and are similar to the Planalto granite suite. Boulders of mafic rocks crop out locally in the northern portion of the area. These rocks show a dominant granoblastic texture, and are mainly composed of amphibole and plagioclase, with subordinate biotite and quartz. In the northern part of the mapped area, it was identified a body of isotropic granite without significant deformation and showing locally rapakivi textures. This granitic pluton was correlated to the Paleoproterozoic A-type granites, represented in the Carajás Domain by the Serra dos Carajás suite and Rio Branco Granite. These granites were not studied in detail. The geological and geochemical aspects shown by the Archean granitoids identified in the eastern part of the Transition Subdomain implies in the existence of significant TTG rocks in the Transition Subdomain. This reinforces the hypothesis that the Transition Subdomain could represent an extension of the Rio Maria Domain, but affected by crustal reworking events in the Neoarchean.
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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)
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Pós-graduação em Agronomia - FEIS
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Pós-graduação em Agronomia - FEIS
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Pós-graduação em Agronomia (Agricultura) - FCA
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The proper management of agricultural crop residues could produce benefits in a warmer, more drought-prone world. Field experiments were conducted in sugarcane production areas in the Southern Brazil to assess the influence of crop residues on the soil surface in short-term CO2 emissions. The study was carried out over a period of 50 days after establishing 6 plots with and without crop residues applied to the soil surface. The effects of sugarcane residues on CO2 emissions were immediate; the emissions from residue-covered plots with equivalent densities of 3 (D50) and 6 (D100) t ha-1 (dry mass) were less than those from non-covered plots (D0). Additionally, the covered fields had lower soil temperatures and higher soil moisture for most of the studied days, especially during the periods of drought. Total emissions were as high as 553.62 ± 47.20 g CO2 m-2, and as low as 384.69 ± 31.69 g CO2 m-2 in non-covered (D0) and covered plot with an equivalent density of 3 t ha-1 (D50), respectively. Our results indicate a significant reduction in CO2 emissions, indicating conservation of soil carbon over the short-term period following the application of sugarcane residues to the soil surface.
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Two experiments were carried out under greenhouse conditions to study the accumulation and distribution of dry mass and macronutrients in maize and Ipomoea hederifolia. Plants of both species had grown, separately, in pots with sand substrate and irrigation with nutrient solution. Treatments were represented by the times of evaluation, realized in intervals of 14 days, starting at 21 days after emergence (DAE). A maize plant showed slight growth up to 30 DAE, when dry mass allocation was higher in roots and leaves (80%); while an I. hederifolia plant, up to 50 DAE, when the allocation of dry mass was higher in offshoots and leaves (79). Dry mass accumulation was almost five times greater in maize (134 g per plant) than in I. hederifolia (29 g per plant). The average values of N and K contents were greater in I. hederifolia. Maximum accumulations of macronutrients by maize were 1,431; 474; 1,832; 594; 340, and 143 mg per plant, while by I. hederifolia, 727; 52; 810; 350; 148, and 65 mg per plant, for N, P, K, Ca, Mg, and S, respectively. Mean accumulation rate of dry mass and macronutrients by maize plants was crescent up to 87 DAE, reaching the maximum value at 103 DAE; while being crescent up to 121 DAE by I. hederifolia plants, reaching the maximum value at 138 DAE. Thus, beyond the interference on harvesting process, a population of I. hederifolia also can compete with maize crop for nutrients.
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Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
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Making bioproducts available to the market requires finding appropriate processes for mass production and formulation of biological agents. This study aimed at evaluating the Bipolaris euphorbiae production in a solid medium (fermentation in solid substrate) and in a biphasic system (growth in a liquid medium followed by growth in a solid medium), as well as determining the processes for collecting and drying conidia, under laboratory conditions. The influence of the incubation period and inoculum quantity were also investigated. The conidia were dried by using an oven (30ºC, 35ºC, 40ºC, 45ºC, 50ºC, 55ºC and 60ºC), and laminar flow, continuous air flow and aseptic chamber at room temperature. Dry conidia were obtained by sieving and grinding in a ball mill, hammer mill or grain grinder. The conidia viability and sporulation efficiency were evaluated in the solid medium and in the biphasic system. For growth period, the best sporulation on solid medium was obtained after 10 days of incubation, reaching 8.3 x 10(7) conidia g-1 of substrate. The biphasic system did not increase the B. euphorbiae sporulation (4.5 x 10(7) conidia g-1 of substrate), after 14 days, and the amount of liquid inoculum used in this system was not an important factor for increasing its production. The continuous air flow and laminar flow preserved the conidial viability (94.6% and 99.1%, respectively), while promoting a great moisture loss (62.6% and 54.0%, respectively). All the grinding processes reduced the conidia germination (86.2%, 10.5% and 12%, respectively), while sieving allowed the collecting of powdered conidia with high viability (94.8%).
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Soil physical quality is an important factor for the sustainability of agricultural systems. Thus, the aim of this study was to evaluate soil physical properties and soil organic carbon in a Typic Acrudox under an integrated crop-livestock-forest system. The experiment was carried out in Mato Grosso do Sul, Brazil. Treatments consisted of seven systems: integrated crop-livestock-forest, with 357 trees ha-1 and pasture height of 30 cm (CLF357-30); integrated crop-livestock-forest with 357 trees ha-1 and pasture height of 45 cm (CLF357-45); integrated crop-livestock-forest with 227 trees ha-1 and pasture height of 30 cm (CLF227-30); integrated crop-livestock-forest with 227 trees ha-1 and pasture height of 45 cm (CLF227-45); integrated crop-livestock with pasture height of 30 cm (CL30); integrated crop-livestock with pasture height of 45 cm (CL45) and native vegetation (NV). Soil properties were evaluated for the depths of 0-10 and 10-20 cm. All grazing treatments increased bulk density (r b) and penetration resistance (PR), and decreased total porosity (¦t) and macroporosity (¦ma), compared to NV. The values of r b (1.18-1.47 Mg m-3), ¦ma (0.14-0.17 m³ m-3) and PR (0.62-0.81 MPa) at the 0-10 cm depth were not restrictive to plant growth. The change in land use from NV to CL or CLF decreased soil organic carbon (SOC) and the soil organic carbon pool (SOCpool). All grazing treatments had a similar SOCpool at the 0-10 cm depth and were lower than that for NV (17.58 Mg ha-1).
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The objective of this work was to evaluate the chemical composition and fatty acid contents of Amazonian and giant river prawns. After four-month farming, with the same diet for both species, palmitic and stearic acids were the main saturated fatty acids. Oleic acid was the main monounsatured fatty acid, and the eicosapentaenoic and docosahexaenoic acids were the most abundant polyunsaturated acids. Amazonian prawn has higher levels of protein and polyunsaturated fatty acids than those of the giant river prawn, which shows its potential for aquaculture.
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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)