198 resultados para mimosa
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A utilização do lodo de esgoto para fins agrícolas e florestais tem se apresentado como a alternativa mais adequada para a sua disposição final, tanto do ponto de vista ambiental quanto do agronômico, principalmente em processos de recuperação de áreas degradadas, pois transforma um rejeito em importante insumo agrícola. Este trabalho apresentou como objetivo principal verificar a viabilidade da aplicação do lodo produzido pela Estação de Tratamento de Esgoto do Aeroporto Internacional do Rio de Janeiro (ETAR-APOIO) no processo de revegetação de uma área degradada, denominada Jazida do Itacolomi, situada na área patrimonial do Aeroporto Internacional do Rio de Janeiro. Foram introduzidas duas espécies vegetais Mimosa caesalpiniifolia (Sabiá) e Mimosa bimucronata (Maricá) na área experimental, adubadas com doses de lodo de esgoto equivalentes a 0,00; 2,85; 5,70; 11,40 e 22,80 t ha-1. Alterações na fertilidade do solo foram avaliadas através das seguintes variáveis: valor pH, teor de matéria orgânica, capacidade de troca catiônica (CTC) e disponibilidade de macro e micronutrientes. O comportamento das espécies vegetais mediante às doses de lodo de esgoto foi avaliado através de medições da altura e do diâmetro das copas das mudas. Os resultados obtidos indicaram que o processo de revegetação empregado na recuperação de áreas degradadas pode tornar-se uma alternativa viável para a disposição final do lodo de esgoto. Observou-se também que a adição do lodo de esgoto ao solo aumentou consideravelmente os teores de matéria orgânica, nitrogênio, fósforo e cálcio, bem como a CTC e em menor extensão os teores de magnésio e potássio, em contrapartida houve pouca alteração no pH do solo. Não foi observado efeito depressivo, causado por qualquer dose de lodo, sobre o desenvolvimento de Mimosa caesalpiniifolia e Mimosa bimucronata.
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1981
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Field lab in marketing: Children consumer behaviour
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Resumen basado en la publicaci??n. T??t. en los cr??ditos del CD: La vaca mimosa : programa de reeducaci??n de problemas de voz
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El tradicional relato de los tres machos cabríos y el trol se acompaña de actividades relacionadas con éste para que los niños desarrollen distintas habilidades con el ordenador,la lectura y la escritura.
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Un día un pájaro, lanza un grano de trigo sobre la cabeza de Chicken Little que después desaparece en la hierba. Éste pía y dice que va a contarle al rey que ha caído un trozo de cielo. En el camino se encuentra con Turkey Lurkey, Henny Penny, Gossey Lucy y Ducky Dadles. Pero también aparece Foxy Loxy.
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Binding parameters for the interactions of four types of tannins: tea catechins, grape seed proanthocyanidins, mimosa 5-deoxy proanthocyanidins,and sorghum procyanidins (mDP=17), with gelatin and bovine serum albumin (BSA) have been determined from isothermal titration calorimetry data. Equilibrium binding constants determined for the interaction with gelatin were in the range 10(4) to 10(6) M-1 and in the order: sorghum procyanidins > grape seed proanthocyanidins > mimosa 5-deoxy proanthocyanidins > tea catechins. Interaction with BSA was generally weaker, with equilibrium binding constants of <= 10(3) M-1 for grape seed proanthocyanidins, mimosa 5-deoxy proanthocyanidins and tea catechins, and 10(4) M-1 for the sorghum procyanidins. In all cases the interactions with proteins were exothermic and involved multiple binding sites on the protein. The data are discussed in relation to the structures and the known nutritional effects of the condensed tannins.
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We present ozone loss estimated from airborne measurements taken during January–February and March in the Arctic winter 2002/2003. The first half of the winter was characterized by unusually cold temperatures and the second half by a major stratospheric sudden warming around 15–18 January 2003. The potential vorticity maps show a vortex split in the lower stratosphere during the major warming (MW) in late January and during the minor warming in mid-February due to wave 1 amplification. However, the warming can be termed as a vortex displacement event as there was no vortex split during the MW period at 10 hPa. Very low temperatures, large areas of polar stratospheric clouds (PSCs), and high chlorine activation triggered significant ozone loss in the early winter, as the vortex moved to the midlatitude regions. The ozone depletion derived from the ASUR measurements sampled inside the vortex, in conjunction with the Mimosa-Chim model tracer, shows a maximum of 1.3 ± 0.2 ppmv at 450–500 K by late March. The partial column loss derived from the ASUR ozone profiles reaches up to 61 ± 4 DU in 400–550 K in the same period. The evolution of ozone and ozone loss assessed from the ASUR measurements is in very good agreement with POAM observations. The reduction in ozone estimated from the POAM measurements shows a similar maximum of 1.3 ± 0.2 ppmv at 400–500 K or 63 ± 4 DU in 400–550 K in late March. Our study reveals that the Arctic winter 2002/2003 was unique as it had three minor warmings and a MW, yet showed large loss in ozone. No such feature was observed in any other Arctic winter in the 1989–2010 period. In addition, an unusually large ozone loss in December, around 0.5 ± 0.2 ppmv at 450–500 K or 12 ± 1 DU in 400–550 K, was estimated for the first time in the Arctic. A careful and detailed diagnosis with all available published results for this winter exhibits an average ozone loss of 1.5 ± 0.3 ppmv at 450–500 K or 65 ± 5 DU in 400–550 K by the end of March, which exactly matches the ozone depletion derived from the ASUR, POAM and model data. The early ozone loss together with considerable loss afterwards put the warm Arctic winter 2002/2003 amongst the moderately cold winters in terms of the significance of the ozone loss.
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In mid-March 2005 the northern lower stratospheric polar vortex experienced a severe stretching episode, bringing a large polar filament far south of Alaska toward Hawaii. This meridional intrusion of rare extent, coinciding with the polar vortex final warming and breakdown, was followed by a zonal stretching in the wake of the easterly propagating subtropical main flow. This caused polar air to remain over Hawaii for several days before diluting into the subtropics. After being successfully forecasted to pass over Hawaii by the high-resolution potential vorticity advection model Modèle Isentrope du transport Méso-échelle de l'Ozone Stratosphérique par Advection (MIMOSA), the filament was observed on isentropic surfaces between 415 K and 455 K (17–20 km) by the Jet Propulsion Laboratory stratospheric ozone lidar measurements at Mauna Loa Observatory, Hawaii, between 16 and 19 March 2005. It was materialized as a thin layer of enhanced ozone peaking at 1.6 ppmv in a region where the climatological values usually average 1.0 ppmv. These values were compared to those obtained by the three-dimensional Chemistry-Transport Model MIMOSA-CHIM. Agreement between lidar and model was excellent, particularly in the similar appearance of the ozone peak near 435 K (18.5 km) on 16 March, and the persistence of this layer at higher isentropic levels for the following three days. Passive ozone, also modeled by MIMOSA-CHIM, was at about 3–4 ppmv inside the filament while above Hawaii. A detailed history of the modeled chemistry inside the filament suggests that the air mass was still polar ozone–depleted when passing over Hawaii. The filament quickly separated from the main vortex after its Hawaiian overpass. It never reconnected and, in less than 10 days, dispersed entirely in the subtropics
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In mid-March 2005, a rare lower stratospheric polar vortex filamentation event was observed simultaneously by the JPL lidar at Mauna Loa Observatory, Hawaii, and by the EOS MLS instrument onboard the Aura satellite. The event coincided with the beginning of the spring 2005 final warming. On 16 March, the filament was observed by lidar around 0600 UT between 415 K and 455 K, and by MLS six hours earlier. It was seen on both the lidar and MLS profiles as a layer of enhanced ozone, peaking at 1.7 ppmv in a region where the climatological values are usually around or below 1 ppmv. Ozone profiles measured by lidar and MLS were compared to profiles from the Chemical Transport Model MIMOSA-CHIM. The agreement between lidar, MLS, and the model is excellent considering the difference in the sampling techniques. MLS was also able to identify the filament at another location north of Hawaii.
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Simulations of polar ozone losses were performed using the three-dimensional high-resolution (1∘ × 1∘) chemical transport model MIMOSA-CHIM. Three Arctic winters 1999–2000, 2001–2002, 2002–2003 and three Antarctic winters 2001, 2002, and 2003 were considered for the study. The cumulative ozone loss in the Arctic winter 2002–2003 reached around 35% at 475 K inside the vortex, as compared to more than 60% in 1999–2000. During 1999–2000, denitrification induces a maximum of about 23% extra ozone loss at 475 K as compared to 17% in 2002–2003. Unlike these two colder Arctic winters, the 2001–2002 Arctic was warmer and did not experience much ozone loss. Sensitivity tests showed that the chosen resolution of 1∘ × 1∘ provides a better evaluation of ozone loss at the edge of the polar vortex in high solar zenith angle conditions. The simulation results for ozone, ClO, HNO3, N2O, and NO y for winters 1999–2000 and 2002–2003 were compared with measurements on board ER-2 and Geophysica aircraft respectively. Sensitivity tests showed that increasing heating rates calculated by the model by 50% and doubling the PSC (Polar Stratospheric Clouds) particle density (from 5 × 10−3 to 10−2 cm−3) refines the agreement with in situ ozone, N2O and NO y levels. In this configuration, simulated ClO levels are increased and are in better agreement with observations in January but are overestimated by about 20% in March. The use of the Burkholder et al. (1990) Cl2O2 absorption cross-sections slightly increases further ClO levels especially in high solar zenith angle conditions. Comparisons of the modelled ozone values with ozonesonde measurement in the Antarctic winter 2003 and with Polar Ozone and Aerosol Measurement III (POAM III) measurements in the Antarctic winters 2001 and 2002, shows that the simulations underestimate the ozone loss rate at the end of the ozone destruction period. A slightly better agreement is obtained with the use of Burkholder et al. (1990) Cl2O2 absorption cross-sections.
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The stabilization of alumina suspensions is key to the development of high-performance materials for the ceramic industry, which has motivated extensive research into synthetic polymers used as stabilizers. In this study, mimosa tannin extract and a chitosan derivative, that is, macromolecules obtained from renewable resources, are shown to be promising to replace synthetic polymers, yielding less viscous suspensions with smaller particles and greater fluidity, that is, more homogeneous suspensions that may lead to better-quality products. The functional groups of tannin present in mimosa extract and N,N,N-trimethylchitosan (TMC) are capable of establishing interactions with the alumina surface, thus leading to repulsion between the particles mainly due to steric and electrosteric mechanisms, respectively. The stabilization of the suspension induced by either TMC or mimosa tannin was confirmed by a considerable decrease in viscosity and average particle size, in comparison with alumina suspensions without stabilizing agents. The viscosity/average particle size decreased by 49/84% and 52/87% for suspensions with TMC and mimosa tannin, respectively. In addition, the increase in the absolute zeta potential upon addition of either TMC or mimosa tannin extract, especially at high pHs, points to an increased stability of the suspension. The feasibility of using derivatives of macromolecules from renewable sources to stabilize aqueous alumina suspensions was therefore demonstrated. (C) 2010 Wiley Periodicals, Inc. J Appl Polym Sci 117: 58-66, 2010
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As florestas ciliares são formações vegetais extremamente importantes em termos ecológicos, principalmente para a manutenção da qualidade dos cursos d’água. Porém, apesar de serem protegidas por lei, elas vêm sendo erradicadas, principalmente em áreas urbanas. Desta forma, estudos detalhados sobre a composição florística e a ecologia dos remanescentes dessas florestas são fundamentais para embasar qualquer iniciativa de proteger e restaurar essas formações vegetais. Com o objetivo de avaliar a estrutura, o estado de preservação da floresta ciliar e fornecer subsídios para as adequadas ações de manejo na restauração dessa formação, foi realizado um levantamento florístico e fitossociológico da vegetação arbóreo/arbustiva do Arroio da Brigadeira na cidade de Canoas/RS, numa área remanescente dentro do Parque Municipal Fazenda Guajuviras. Para a caracterização da composição do estrato arbóreo dominante da floresta e categorias sucessionais, a vegetação lenhosa foi separada em três componentes: regenerante (0,20m ≤ h < 1m); arbóreo-arbustivo (1m ≥ h e DAP < 5cm); arbóreo (DAP ≥ 5cm). O delineamento amostral foi de 20 parcelas para todos os componentes, sendo as dimensões de 4m², 25m² e de 100m² para cada parcela, respectivamente para o primeiro, segundo e terceiro componente. A estrutura da vegetação foi verificada através da distribuição horizontal e vertical dos seus indivíduos. A estimativa da regeneração natural baseou-se nos valores relativos de freqüência e densidade de cada espécie em três classes de altura. A organização das comunidades vegetais foi analisada por análise de agrupamentos através do programa MULVA 5. Na composição florística encontraram-se 56 espécies distribuídas em 27 famílias botânicas. As espécies com maiores valores de regeneração natural total (RNT), responsáveis por mais de 50%, foram: Myrcia multiflora (Lam.) DC. (22,03%), Eugenia hyemalis Cambess. (14,04%), Daphnopsis racemosa Griseb. (10,60%) e Ocotea pulchella Mart. (10,16%). O alto potencial de regeneração natural, com abundância de espécies típicas de sub-bosque, ressalta a importância do estudo dos componentes dos estratos inferiores da floresta para o conhecimento da dinâmica florestal. No componente arbóreo constatou-se a densidade total por área (DTA) de 2120 ± 617 indivíduos.ha-1. O Índice de Diversidade de Shannon foi de 2,80. O DAP médio foi de 10,45 ± 5,65cm. As espécies com maior valor de importância (VI) foram Eugenia hyemalis Cambess. (44,09), Prunus myrtifolia Urb. (34,51), Myrsine coriacea (Sw.) R.Br. (30,12) e Mimosa bimucronata (DC.) Kuntze (29,68). Os exemplares mortos apresentaram alta DTA, 280 ± 204,17 indivíduos.ha-1, possivelmente em decorrência da competição por espaço a ser ocupado. Pelos resultados obtidos, é possível afirmar que a floresta está em processo de regeneração, no estádio secundário inicial, e que existem agrupamentos vegetais. Conclui-se que o processo de restauração da floresta ciliar pode darse de forma natural, desde que seja garantido o isolamento de fatores desestabilizadores, preservando os processos naturais de estruturação das comunidades vegetais e interações bióticas.
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Dengue, amongst the virus illnesses one can get by vectorial transmission, is the one that causes more impact in the morbidity and mortality of world s population. The resistance to the insecticides has caused difficulties to control of vector insect (Aedes aegypti) and has stimulated a search for vegetables with larvicidal activity. The biodiversity of Caatinga is barely known and it is potential of use even less. Some plants of this biome are commercialized in free fairs northeast of Brazil, because of its phytotherapics properties. The vegetables in this study had been selected by means of a questionnaire applied between grass salesmen and natives of the Serido region from Rio Grande do Norte state; culicids eggs had been acquired with traps and placed in container with water for the larva birth. Thirty larvae had been used in each group (a group control and five experimental groups), with four repetitions four times. The vegetables had been submitted to the processes of decoction, infusion and maceration in the standard concentration of 100g of the vegetable of study in 1l of H2O and analyzed after ½, 1, 2, 4, 8, 12, 24 and 48 hours for verification of the average lethal dose (LD50) from the groups with thirty larva. The LD50 was analyzed in different concentrations (50g/l, 100g/l, 150g/l, 200g/l e 300g/l) of Aspidosperma pyrifolium Mart. 48 extracts of rind, leaf and stem of the seven vegetal species: Aspidosperma pyrifolium Mart., Mimosa verrucosa Benth, Mimosa hostilis (Mart.) Benth., Myracrodruon urundeuva Allemão, Ximenia americana L, Bumelia sartorum Mart Zizyphus joazeiro Mart, had been analyzed. The extracts proceeding from the three methods were submitted to the freezedrying, to evaluate and to quantify substances extracted in each process. The results had shown that Aspidosperma pyrifolium Mart. and Myracrodruon urundeuva Allemão are the species that are more distinguished as larvicidal after 24 hours of experiment, in all used processes of extraction in the assays. The Zizyphus joazeiro Mart species has not shown larvicidal activity in none of the assays. In relation to the extraction method, the decoction was the most efficient method in the mortality tax of the A. aegypti larvae
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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior