494 resultados para Luiz Roberto Ayoub
Resumo:
Este trabalho foi conduzido na área abrangida pelo campus da Escola Superior de Agricultura Luiz de Queiroz da Universidade de São Paulo, no município de Piracicaba, Estado de São Paulo. Teve como objetivos, determinar a composição do gênero Anastrepha Schiner e verificar a associação das espécies de plantas hospedeiras, estabelecidas na área, com as espécies de Anastrepha. Foram examinadas 23.277 fêmeas de Anastrepha coletadas por meio de armadilhas McPhail e 18 espécies pertencentes a nove grupos de espécies foram registradas. Um total de 563 amostras de frutos pertencentes a nove famílias e, pelo menos, 23 espécies de plantas foi coletado em 47 estações de capturas. Foram identificadas 10.243 fêmeas e das 18 espécies de Anastrepha capturadas em armadilhas somente seis emergiram das amostras de frutos: A. bistrigata Bezzi, A. fraterculus (Wied.), A. obliqua (Macquart), A. pseudoparallela (Loew), A. serpentina (Wied.) e A. sororcula Zucchi. A. fraterculus infestou maior diversidade de frutos. Os hospedeiros preferidos de A. obliqua foram as espécies da família Anacardiaceae. A. pseudoparallela e A. serpentina infestaram exclusivamente Passifloraceae e Sapotaceae, respectivamente. A. fraterculus é registrada pela primeira vez em sapoti (Manilkara zapota L.) no Brasil.
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Phlebotomine specimens were captured in domiciliary and forest environments in 47 municipalities between 1982 and 2005 with the aid of CDC light traps. A total of 91 species were found, of which four belonged to genus Brumptomyia and 87 to genus Lutzomyia, distributed among the following subgenera: Evandromyia (6), Lutzomyia (5), Micropygomyia (2), Nyssomyia (9), Pintomyia (2), Pressatia (3), Psathyromyia (6), Psychodopygus (14), Sciopemyia (4), Trichophoromyia (2), Viannamyia (2); species groups: Aragaoi (2), Baityi (1), Dreisbachi (1), Migonei (12), Oswaldoi (8), Pilosa (1), Saulensis (2), Verrucarum (4) and ungrouped (1). Species diversity was greatest in areas where there was dense evergreen seasonal forest (52 species), ombrophilous forest (31) and meridional cerrados (23) and lowest in areas with mixed forest (forest with babassu palms, cerrado and caatinga). The greatest similarity index was observed for restinga and open evergreen seasonal forest (J=0.48). Dense evergreen seasonal forest had greatest similarity with ombrophilous forest (J=0.38). The phlebotomine fauna was species rich and unevenly distributed in Maranhão, reflecting the phytogeographical complexity of the state, which is a result of the great variety of ecosystems and climate zones.
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The nuptial flight allows males and females to meet and copulate and both need energy to perform this activity. Before leaving the nest, males and females are well nourished and ready to mate. However, little is known about the lipid and energy contents in females before the nuptial flight (virgins) and after it (mated females). In this work we measured lipid concentrations in relation to body weight in these individuals. Our results showed that 16.82% of the bodies of young virgin females one month before mating flight are composed of lipids, contrasting with the 32.62% lipid content in mated females who had not excavated their nest yet, and 32.88% in those who had. The energy content measured for virgin females was 2942.63 J, contrasting with 6110.01 J for queens before excavating the nest and 5677.51 J after excavation. Based on our results, we conclude that the body mass, and therefore the lipid and energy contents in the bodies of Atta sexdens rubropilosa queens double during the last month before the nuptial flight. This energy resource is fundamental to the activities required during the nuptial flight, digging the nest and the founding of the colony.
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Energy substrate used by workers of leaf-cutting ants during nest excavation. In this study we aimed to ascertain whether leaf-cutting ant workers lose body reserves (fat or sugars) as a function of nest excavation. For each treatment, we isolated 10 workers of Atta sexdens into two experimental groups, Control (C- without excavation) and Soil (S- with excavation), which were kept for different time intervals (0, 24, 48 or 72 hours), totaling 700 tested workers. We then determined the concentration of soluble carbohydrates and total lipid content in them. The total carbohydrates were determined colorimetrically, based on the reaction between carbohydrates and sulfuric acid-phenol. For determination of lipids, the insects were immersed in organic solvent until they reached a constant weight. Our results showed that carbohydrates are consumed during nest excavation activities. In the experimental groups S24, S48 and S72, there was an average reduction of 5.82 (20.42%), 14.31 (44.96%) and 13.27 (43.96%) µ.mg-1 in soluble sugar when compared with the experimental groups that did not excavate. Furthermore, the lipids were not used during this activity. With respect to dry mass of the workers, their values were C0 = 8%, C24 = 10.4%, C48 = 9.2%, C72 = 10%, S24 = 9.2%, S48 = 8.7% and S72 = 8.5%. Our results show experimentally that the source of energy for nest excavation is carbohydrates, whereas lipids are conserved for other activities.
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Energetic cost of digging behavior in workers of the leaf-cutting ant Atta sexdens (Fabricius). During nest excavation, leaf-cutting ant workers undergo reduction in their body reserve, particularly carbohydrates. In order to estimate the energetic cost of digging, groups of 30 workers of the leaf-cutting ant Atta sexdens were sealed in a hermetic chamber for 24, 48 and 72 hours, with and without soil for digging, and had the CO2 concentration measured using respirometric chambers as well as volume of soil excavated (g). As expected, the worker groups that carried out soil excavation expelled more carbon dioxide than the groups that did not excavate. Therefore, a worker with body mass of 9.65 ± 1.50 mg dug in average 0.85 ± 0.27 g of soil for 24 hours, consuming ca. 0.58 ± 0.23 J. In this study, we calculate that the energetic cost of excavation per worker per day in the experimental set-up was ca. 0.58 J.
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Protein content of leaf-cutting ant queens before the nuptial flight and during the post-claustral phase. This study evaluated the crude protein content of queens of Atta sexdens before the nuptial flight and after the claustral phase in laboratory and field colonies. The hypothesis was that protein is used for survival of the queen and for early colony growth during the claustral phase. Additionally, the nest morphology, live biomass and adult population of field colonies were evaluated. Crude protein was determined by digestion of the organic material with sulfuric acid at high temperatures. The mean crude protein content was 123.23 ± 11.20 mg for females before the nuptial flight and 70.44 ± 12.21 mg for laboratory-reared queens after the claustral phase. The post-claustral crude protein content of field-collected queen was 55.90 ± 9.18 mg. With respect to the loss of crude protein as a function of duration of the claustral phase, laboratory-reared queens lost 52.79 mg and field-collected queens lost 67.33 mg compared to females before the nuptial flight. A positive linear correlation was observed between the weight of field-collected queens (256.4 ± 36.3 mg) and colony biomass (13.02 ± 9.12 g), but there was no correlation between biomass and nest depth (13.11 ± 3.82 cm). As expected, the present results support the hypothesis that protein is used for survival of the queen and for early colony growth, as demonstrated by the reduction in crude protein content as a function of duration of the claustral phase. To our knowledge, this is the first study to provide data of the dynamics of protein reserves in leaf-cutting ant queens during the claustral phase.
Resumo:
ABSTRACT Dynamics of the restoration of physical trails in the grass-cutting ant Atta capiguara. Leaf-cutting ants of the genus Atta build long physical trails by cutting the vegetation growing on the soil surface and removing the small objects they find across their path. Little is known on the dynamics of trail construction in these ants. How much time do they need to build a trail? To answer this question we selected six trails belonging to two different nests of A. capiguara and removed on each trail a block of soil of 20 cm × 15 cm that included a portion of the physical trail. This block was then replaced by a new block of the same size that was removed in the pasture near the trail and that was uniformly covered by the same type of vegetation as that found on the block of soil that was removed. The time required to restore the trail was then evaluated by the length of the grass blades found along the former location of the trail. The results show that ants rapidly restore the portion of the physical trail that was interrupted, which suggests that they could also do the same after their trails have been recolonized by the vegetation.
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The timing of N application to maize is a key factor to be considered in no-till oat/maize sequential cropping. This study aimed to evaluate the influence of pre-planting, planting and sidedress N application on oat residue decomposition, on soil N immobilisation and remineralisation and on N uptake by maize plants in no-till oat/maize sequential cropping. Undisturbed soil cores of 10 and 20 cm diameter were collected from the 0-15 cm layer of a no-till Red Latossol, when the oat cover crop was in the milk-grain stage. Two greenhouse experiments were conducted simultaneously. Experiment A, established in the 10 cm diameter cores and without plant cultivation, was used to asses N dynamics in soil and oat residues. Experiment B, established in the 20 cm diameter cores and with maize cultivation, was used to assess plant growth and N uptake. An amount of 6.0 Mg ha-1 dry matter of oat residues was spread on the surface of the cores. A rate of 90 kg N ha-1 applied as ammonium sulphate in both experiments was split in pre-planting, planting and sidedress applications as follows: (a) 00-00-00 (control), (b) 90-00-00 (pre-planting application, 20 days before planting), (c) 00-90-00 (planting application), (d) 00-30-60 (split in a planting and a sidedress application 31 days after emergence), (e) 00-00-00* (control, without oat residue) and (f) 90-00-00* (pre-planting application, without oat residue). The N concentration and N content in oat residues were not affected during decomposition by N fertilisation. Most of the fertiliser NH4+-N was converted into NO3--N within 20 days after application. A significant decrease in NO3--N contents in the 0-4 cm layer was observed in all treatments between 40 and 60 days after the oat residue placement on the soil surface, suggesting the occurrence of N immobilisation in this period. Considering that most of the inorganic N was converted into NO3- and that no immobilisation of the pre planting fertiliser N occurred at the time of its application, it was possible to conclude that pre-planting applied N was prone to losses by leaching. On the other hand, with split N applications, maize plants showed N deficiency symptoms before sidedress application. Two indications for fertiliser-N management in no-till oat/maize sequential cropping could be suggested: (a) in case of split application, the sidedress should be earlier than 30 days after emergence, and (b) if integral application is preferred to save field operations, this should be done at planting.
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O objetivo deste trabalho foi avaliar o estoque e a qualidade da matéria orgânica (MOS) por meio de análises de ressonância magnética nuclear (RMN) de 13C no estado sólido de amostras intactas de solo e de ressonância paramagnética eletrônica (RPE) e fluorescência dos ácidos húmicos (AH) isolados de um Cambissolo cultivado com cana-de-açúcar por longo tempo. Numa situação, a cana-de-açúcar foi cultivada por 55 anos sem a queima por ocasião da colheita. A outra situação envolveu uma área cultivada com queima da palhada, na qual em uma parte foi realizada a adição de vinhaça (120 m³ ano-1) durante 35 anos e a outra não recebeu esse tratamento. O aumento no estoque de AH em 157 e 57 % nas camadas de 0-0,20 e 0,20-0,40 m, respectivamente, na área cultivada durante 55 anos com preservação do palhiço, correspondeu ao aumento observado no grau de aromaticidade e diminuição da acidez da MOS, obtido por RMN 13C. Nas áreas com manejos que envolviam a preservação da MOS foram obtidos AH com maior concentração de radicais livres do tipo semiquinona, determinada por RPE, e maior intensidade de emissão de fluorescência. Mudanças significativas no processo de humificação da MOS e, portanto, na sua qualidade foram decorrentes da preservação do palhiço por ocasião da colheita. Por sua vez, a adição de vinhaça durante 35 anos ao canavial no qual foi realizada a queima do palhiço não alterou significativamente a qualidade da MOS, sugerindo rápida evolução do material orgânico solúvel adicionado ao solo.
Resumo:
A resistência do solo ao penetrômetro exerce grande influência sobre o crescimento e desenvolvimento vegetal, uma vez que o crescimento das raízes, assim como o rendimento das culturas, varia de forma inversamente proporcional ao seu valor. Dessa forma, a análise da variabilidade espacial da resistência do solo ao penetrômetro e da produtividade, por meio da geoestatística, pode indicar alternativas de manejo para reduzir os efeitos da variabilidade do solo sobre a produtividade e também melhorar a estimativa de respostas das culturas sob determinadas práticas de manejo. Diante do exposto, o objetivo deste trabalho foi relacionar e caracterizar a variabilidade espacial da resistência do solo ao penetrômetro (RP) e a produtividade do feijoeiro irrigado em sistema de semeadura direta, em duas safras consecutivas. O experimento foi realizado em Latossolo Vermelho distroférrico típico, no campo experimental da Faculdade de Engenharia Agrícola da Unicamp, no município de Campinas-SP, cujas coordenadas geográficas são: 22 ° 48 ' 57 " de latitude sul, 47 ° 03 ' 33 " de longitude oeste e altitude média de 640 m. As avaliações foram realizadas em uma malha regular de amostragem de 3 x 3 m, totalizando 60 pontos amostrais por parcela. A análise da dependência espacial foi avaliada pela geoestatística, e os parâmetros dos semivariogramas utilizados para construir mapas de isolinhas, por meio do interpolador de krigagem do programa Surfer 8.0. A regressão linear simples entre mapas (pixel-a-pixel) mostrou correlação negativa entre os valores de RP e a produtividade; no entanto, a produtividade do feijoeiro irrigado apresentou baixa correlação com a resistência do solo ao penetrômetro em sistema semeadura direta nas duas safras.
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Com o incremento exponencial da avicultura no Brasil, a disponibilidade de dejetos de aves e de cama de aviário tem aumentado de maneira semelhante. A proibição de uso desses produtos na ração animal tem feito com que eles sejam direcionados para a produção agrícola como fertilizantes. Ainda há na literatura carência de informação sobre lixiviação de bases no perfil do solo em conseqüência do efeito de ânions inorgânicos acompanhantes, como cloreto, nitrato e sulfato, e do efeito complexante de ácidos orgânicos de baixa massa molecular. O objetivo deste trabalho foi estudar o efeito da aplicação de cama de aviário na lixiviação de Ca, Mg, K e Na em solos e sua associação com ânions inorgânicos e ácidos orgânicos de baixa molecular. Amostras de dois Latossolos Vermelho-Amarelos, um de textura média e outro de textura argilosa, foram colocadas em colunas de PVC constituídas de cinco anéis, cada um com 10 cm de altura e 5 cm de diâmetro, ligados entre si com fita adesiva. O solo colocado no anel superior recebeu, homogeneamente, cinco tipos de camas de aviário: casca de café, casca de arroz, sabugo de milho, capim-napier e maravalha, totalizando 160 t ha-1 de material seco, comparado à testemunha (sem a cama de aviário). O experimento constituiu um fatorial 5 x 2, com cinco camas e dois solos, dispostos em blocos casualizados com três repetições. As colunas foram submetidas a 10 percolações com água deionizada, duas vezes por semana, até atingirem o volume de 1.200 mm de chuvas. Nos 10 percolados, foram analisadas as concentrações de Ca, Mg, K e Na, dos ânions Cl-, NO3-e SO4(2-) e de ácidos orgânicos de baixa massa molecular. Houve grande lixiviação de bases nas colunas, principalmente até a terceira percolação. Esse fato foi causado pela adição dessas bases, em doses elevadas, pelas camas de aviário e, aparentemente, também pelo efeito dos ânions acompanhantes Cl-, NO3-e SO4(2-)no solo de textura média, Cl-e NO3-no solo de textura argilosa e, de maneira menos expressiva, pelo efeito acompanhante/complexante dos ácidos orgânicos de baixa massa molecular. No solo argiloso, a percolação de Ca esteve positivamente correlacionada com a concentração dos ácidos málico e oxálico. A concomitante elevada concentração de ácido acético nos percolados de solos tratados com todas as camas sugere que este pode estar favorecendo a lixiviação de bases no solo, provavelmente como ânion acompanhante.
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Two bacterial strains that amplified part of the nifH gene, RP1p and RP2p, belonging to the genus Enterobacter and Serratia, were isolated from the rhizoplane of Lupinus albescens. These bacteria are Gram-negative, rod-shaped, motile, facultative anaerobic, and fast-growing; the colonies reach diameters of 3-4 mm within 24 h of incubation at 28 ºC. The bacteria were also able to grow at temperatures as high as 40 ºC, in the presence of high (2-3 % w/v) NaCl concentrations and pH 4 -10. Strain RP1p was able to utilize 10 of 14 C sources, while RP2p utilized nine. The isolates produced siderophores and indolic compounds, but none of them was able to solubilize phosphate. Inoculation of L. albescens with RP1p and RP2p strains resulted in a significant increase in plant dry matter, indicating the plant-growth-promoting abilities of these bacteria.
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The eutrophication of aquifers is strongly linked to the mobility of P in soils. Although P mobility was considered irrelevant in a more distant past, more recent studies have shown that P, both in organic (Po) and inorganic forms (Pi), can be lost by leaching and eluviation through the soil profile, particularly in less weathered and/or sandier soils with low P adsorption capacity. The purpose of this study was to determine losses of P forms by leaching and eluviation from soil columns. Each column consisted of five PVC rings (diameter 5 cm, height 10 cm), filled with two soil types: a clayey Red-Yellow Latosol and a sandy loam Red-Yellow Latosol, which were exposed to water percolation. The soils were previously treated with four P rates (as KH2PO4 ) to reach 0, 12.5, 25.0 and 50 % of the maximum P adsorption capacity (MPAC). The P source was homogenized with the whole soil volume and incubated for 60 days. After this period the soils were placed in the columns; the soil of the top ring was mixed with five poultry litter rates of 0, 20, 40, 80, and 160 t ha-1 (dry weight basis). Treatments consisted of a 4 x 5 x 2 factorial scheme corresponding to four MPAC levels, five poultry litter rates, two soils, with three replications, arranged in a completely randomized block design. Deionized water was percolated through the columns 10 times in 35 days to simulate about 1,200 mm rainfall. In the leachate of each column the inorganic P (reactive P, Pi) and organic P forms (unreactive P, Po) were determined. At the end of the experiment, the columns were disassembled and P was extracted with the extractants Mehlich-1 (HCl 0.05 mol L-1 and H2SO4 0.0125 mol L-1) and Olsen (NaHCO3 0.5 mol L-1; pH 8.5) from the soil of each ring. The Pi and Po fractions were measured by the Olsen extractant. It was found that under higher poultry litter rates the losses of unreactive P (Po) were 6.4 times higher than of reactive P (Pi). Both the previous P fertilization and increasing poultry litter rates caused a vertical movement of P down the soil columns, as verified by P concentrations extracted by Mehlich-1 and NaHCO3 (Olsen). The environmental critical level (ECL), i.e., the P soil concentration above which P leaching increases exponentially, was 100 and 150 mg dm-3 by Mehlich-1 and 40 and 60 mg dm-3 by Olsen, for the sandy loam and clay soils, respectively. In highly weathered soils, where residual P is accumulated by successive crops, P leaching through the profile can be significant, particularly when poultry litter is applied as fertilizer.
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Alterações no pH da rizosfera de plantas fixadoras de N2 parecem exercer papel fundamental na absorção de micronutrientes que têm sua disponibilidade dependente de alterações da acidez do solo. Estudaram-se variações na absorção de B, Cu, Fe, Mn e Zn durante o ciclo de crescimento e desenvolvimento da soja, induzidas pela fixação biológica de N2 e pelo pH inicial de amostras de dois solos (um LV argiloso e outro arenoso), em um ensaio conduzido em casa de vegetação. Essas amostras foram incubadas com doses de CaCO3 + MgCO3 (4:1) para elevar o pH (H2O) a valores de 5,2, 5,6, 6,2 e 6,6 no solo argiloso e 5,3, 5,6, 5,9 e 6,3 no solo arenoso. Após 60 dias de incubação, essas amostras receberam 450 mg dm-3 de P e 120 mg dm-3 de K no solo. Sementes de soja (Glycine max (L) Merrill), variedade Paranaíba, inoculadas com Bradyrhizobium japonicum, estirpes SEMIA 587 e SEMIA 5019, foram colocadas para germinar. Foram cultivadas quatro plantas por vaso (2,2 dm³) e colhidas aos 16, 20, 24, 28, 32, 36, 40, 46 e 54 dias após a emergência. Determinaram-se o pH da rizosfera (pHr), o pH do solo entre raízes - não rizosférico (pHnr), os teores de B, Cu, Fe, Mn e de Zn na parte aérea e raiz, o N apenas na parte aérea, o número de nódulos e o peso da matéria seca de parte aérea, raiz e nódulos. Observou-se que as mudanças ocorridas no pHr e pHnr foram dependentes do pH inicial dos solos (pHs) e da fixação biológica de N2. O acúmulo de B e de Fe na parte aérea não foi alterado pelos valores de pHr, modificados em função do pHs, exceto para o Fe no solo argiloso. Todavia, aumentos significativos no acúmulo destes nutrientes na parte aérea ocorreram com o aparecimento dos nódulos, a partir de 24 dias após a emergência. Para Cu, Mn e Zn, as diferenças apareceram sobretudo quanto ao pHs. O conteúdo de micronutrientes na planta revelou-se sensível a mudanças no pH rizosférico, principalmente após a nodulação.
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O penetrômetro de impacto Stolf, em uso desde o seu lançamento em 1982, é um aparelho para medida da resistência do solo, tipo dinâmico. No projeto original, uma escala centimétrica, de profundidade, foi gravada na própria haste de penetração. O objetivo desse procedimento, na época, foi facilitar o entendimento pelos agricultores e permitir a leitura direta na haste de penetração, além de evitar peças adicionais. O objetivo do presente estudo foi incorporar ao projeto original uma régua em escala milimétrica, a fim de trazer a leitura da profundidade ao nível da visão do operador, evitando o agachamento, e aumentar a precisão da leitura. A utilização do equipamento e o procedimento para posicionar o zero da escala são descritos e esquematizados. Foi realizada comparação entre o equipamento original, com leitura na haste, e o equipamento proposto, com leitura na régua, avaliando-se quanto aos valores da resistência determinados e ao tempo de execução de um perfil de solo. A utilização do equipamento com leitura na régua resultou em um tempo médio 21 % menor (teste t, 1 %). Além de reduzir o tempo de amostragem, verificou-se a preferência de usuários pelo novo procedimento, em razão do maior conforto ao operador, sendo essa modificação finalmente incorporada ao modelo comercial. Fez-se um histórico do desenvolvimento da tecnologia do penetrômetro de impacto, sendo o presente estudo complementar à primeira modificação no projeto construtivo, que permaneceu inalterado por 30 anos.