962 resultados para potassium permanganate


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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

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Pós-graduação em Medicina Veterinária - FMVZ

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Pós-graduação em Agronomia (Energia na Agricultura) - FCA

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O gênero Macrobrachium contém mais de 120 espécies e ocorre nas regiões tropicais e subtropicais de todo o mundo (VALENTI, 1987). São camarões de água doce da família Palaemonidae e da ordem Decapoda (RAFINESQUE, 1815; LATREILLER, 1802). No Brasil existem 18 espécies, até agora classificadas, distribuídas ao longo da bacia amazônica (MELO 2003). Entre estas, o Macrobrachium amazonicum (HELLER, 1862) conhecido popularmente como camarão-sossego ou camarão-canela, amplamente empregados na carcinicultura. Os crustáceos dispõem de estruturas sensitivas localizadas no cefalotórax, que permitem receber estímulos do meio para localizar e capturar o alimento (BARNES, 1998). Os olhos compostos estão presentes em todas as classes de crustáceo. Assim, a hipótese levantada nessa pesquisa foi que no Macrobrachium amazonicum, estes olhos são do tipo de superposição reflexiva, onde o aparelho dióptrico e o rabdômero se estendem em camadas e está separado por uma zona clara não pigmentada. Neste trabalho temos como objetivos: Avaliar os aspectos morfológicos do olho do Macrobrachium amazonicum em microscopia eletrônica de varredura; Caracterizar a morfologia das células fotorreceptoras; Descrever as estruturas morfológicas do olho do M. amazonicum; Caracterizar as relações morfométricas entre o olho e as demais estruturas do M. amazonicum. Os animais foram adquiridos no distrito de Mosqueiro nos períodos de chuvas, março de 2009 e março de 2010, com pescadores no município de Santa Bárbara, área metropolitana de Belém, e transportados para o laboratório em caixas de isopor, sendo mantidos em quarentena em um recipiente contendo uma solução de permanganato de potássio a 1,3 mg/L (CARNEIRO et al., 005). Os animais foram fixados em Davidson e Karnovisky, em seguida os olhos de cada animal foram cuidadosamente seccionados e colocados em frascos plásticos. Nas relações biométricas foram realizadas a análise de variância com α = 0,05, foi realizada com Bio Estat 5.0 para os comprimentos do olho látero-lateral e ântero-posterior dos quatro morfotipos, e SigmaPlot 11.0 e regressão linear simples, para as variáveis olho total e cefalotórax. Observou-se que o tamanho médio do cefalotórax, do corpo, do olho é respectivamente: 21,03 mm; 70,62 mm e 4,52 mm, sendo que, o peso médio do camarão foi de 7,97 g. Os valores máximos registrados dessas estruturas foram de 31,95 mm para o cefalotórax; 100,10 mm para o tamanho do corpo; 6,80 mm para o tamanho do olho e de 20,54 g para o peso do camarão. Após análise histológica foram identificadas as seguintes estruturas (Figs. 13 e 14 A-B): córnea, cone cristalino, pigmento distal, haste do cone, zona clara, cutícula, retina, rabdoma, fibras do nervo óptico e lamina. Com relação à microscopia eletrônica de varredura, foram selecionadas para observação as principais estruturas e especialmente o arranjo em seção transversal quadrada dos omatídeos (Figs. 16 A-B). As análises morfométrica e morfológica (por histologia e microscopia eletrônica de varredura) apontaram características próprias de Macrobrachium amazonicum adultos oriundos da região metropolitana de Belém. Estes achados incluem uma óptica de superposição reflexiva com olhos adaptados a percepção de estímulos luminosos.

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O presente consiste no estudo de caracterização e proposta de tratamento de lixiviados de resíduos de madeira produzidos em laboratório. Lixiviados de madeira ou chorumes de madeira são originados quando resíduos de madeira, decorrente do processo de transformação, são dispostos de forma inadequada, no ambiente, possibilitando a interação destes com água, geralmente de precipitações climáticas, o que resulta na geração de líquido de cor escura que pode conter uma série de substâncias com potencial impacto negativo sobre os ambientes aquáticos. O efluente estudado foi gerado em laboratório por meio de dois experimentos distintos. No Experimento A, em frascos de polietileno, foram misturadas água e pó-de-serra, na proporção 9:1, permanecendo em contato, em sistema aberto e temperatura ambiente, por 90 dias. Nos tempos de 0, 1, 5, 10, 20, 30, 45, 60, 75, 80 e 90 dias, a solução foi filtrada e levada ao laboratório para análise. No Experimento B, armazenou-se em um recipiente plástico aproximadamente 5 Kg de resíduos de madeira, onde na parte inferior foi adaptado um dreno para coleta de efluente. Este sistema ficou exposto ao sol e a precipitações climáticas, de tal forma a simular as condições reais de geração de lixiviados de uma pilha de resíduos de madeira em caso real. Em ambos experimentos (A e B) observou-se a geração de um líquido de cor âmbar claro a negro, com odor forte característico, levemente ácido @H 5,53 — 6,97), alta demanda de oxigênio (DBO 17 — 310 mg.L-1; DQO 857 — 3.161 mg.L-1 e OD 0,63 — 5,56 mg.L-1), altas cargas de matéria orgânica (CT 170,93 — 425,19 mg.L-1, COT 167,66 — 415,66 mg.L-1 e CIT 2,22 — 34,05 mg.L-1), grande concentração de sólidos (SS 10 — 23 mL.L-1; STS 463 — 1.330 mg.L-1; STD 31 — 640 mg.L-1) e turbidez (10,0 — 638,5 UT). Devido a estas características foi proposto um tratamento fisico-químico para o chorume produzido, por meio da combinação dos processos de coagulação/floculação e oxidação com permanganato de potássio, que resultou, respectivamente, na redução dos níveis de DQO 20,95% e 88,53%, cor 43,31% e 98,18%, turbidez 40,45% e 98,16%, STS 65,71% e 100%, por processo. A eficiência global do tratamento proposto foi de 90,93% nos valores de DQO, 98,97% nos valores de cor verdadeira, 98,90% nos valores de turbidez e 100,00% nos valores de STS.

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Pós-graduação em Agronomia - FEIS

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This study's aim was to evaluate the degradation rate of hydrogen peroxide (H2O2) and to quantify its penetration in tooth structure, considering the residence time of bleaching products on the dental enamel. For this study, bovine teeth were randomly divided according to the bleaching product received: Opalescence Xtra Boost 38%, White Gold Office 35%, Whiteness HP Blue 35%, Whiteness HP Maxx 35%, and Lase Peroxide Sensy 35%. To analyze the degradation of H2O2, the titration of bleaching agents with potassium permanganate was used, while the penetration of H2O2 was measured via spectrophotometric analysis of the acetate buffer solution, collected from the artificial pulp chamber. The analyses were performed immediately as well as 15 minutes, 30 minutes, and 45 minutes after product application. The data of degradation rate of H2O2 were submitted to analysis of variance (ANOVA) and Tukey tests, while ANOVA and Fisher tests were used for the quantification of H2O2, at the 5% level. The results showed that all products significantly reduced the concentration of H2O2 activates at the end of 45 minutes. It was also verified that the penetration of H2O2 was enhanced by increasing the residence time of the product on the tooth surface. It was concluded that the bleaching gels retained substantial concentrations of H2O2 after 45 minutes of application, and penetration of H2O2 in the dental structure is time-dependent.

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Potassium permanganate oxidative degradations were conducted for kerogens isolated from Cretaceous black shales (DSDP Leg 41, Site 368), thermally altered during the Miocene by diabase intrusions and from unaltered samples heated under laboratory conditions (250-500°C). Degradation products of less altered kerogens are dominated by normal C4-C15 alpha,omega-dicarboxylic acids, with lesser amounts of n-C16 and n-C18 monocarboxylic acids, and benzene mono-to-tetracarboxylic acids. On the other hand, thermally altered kerogens show benzene di-to-tetracarboxylic acids as dominant degradation products, with lesser or no amounts (variable depending on the degree of thermal alteration) of alpha,omega-dicarboxylic acids. Essentially no differences between the oxidative degradation products of naturally- and artificially-altered kerogens are observed. As a result of this study, five indices of aromatization (total aromatic acids/kerogen; apparent aromaticity; benzenetetracarboxylic acids/total aromatic acids; benzene-1,2-dicarboxylic acid/benzenedicarboxylic acids; benzene-1,2,3-tricarboxylic acid/benzenetricarboxylic acids) and two indices of aliphatic character (Total aliphatic acids/kerogen; Aliphaticity) are proposed to characterize the degree of thermal alteration of kerogens. Furthermore, a good correlation is observed between apparent aromaticity estimated by the present KMnO4 oxidation method and that from the 13C NMR method (Dennis et al., 1982; doi:10.1016/0016-7037(82)90046-1).

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In the last 20 years directed shark and ray fishery has increased alarmingly everywhere in the world. For most species though, no data on growth rate, mortality, fecundity and other life history aspects exist as of now and management of the fishery is therefore insufficient. Also there still exist methodological difficulties in the age determination of elasmobranchs fishes, a fact which complicates the investigation of growth parameters. This study tried to identify the best ageing methods and estimate growth parameters for ten skate species of the genus Bathyraja, all occurring in the southwest Atlantic in depths of 50m and more. 720 samples were collected on board of argentine research vessels in between 2003 and 2005. Crystal violet and a new staining method using potassium permanganate, both applied on sagittal sections of vertebral centra, proved to be most effective in enhancing the banding pattern in most of the species. Thorns were also tested and readings were consistent with the ones made on vertebral sections. Growth parameters could be derived for six species and for the other four estimates could be made. Growth rate as well as infinite length varied between species, with those attaining bigger sizes having lower growth rates. No latitudinal differences in growth rate could be detected but a comparison with samples from other studies showed that total lengths were always reported to be higher around the Malvinas Islands.

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Transcription from the middle promoter, Pm, of phage Mu is initiated by Escherichia coli RNA polymerase holoenzyme (E sigma 70; RNAP) and the phage-encoded activator, Mor. Point mutations in the spacer region between the -10 hexamer and the Mor binding site result in changes of promoter activity in vivo. These mutations are located at the junction between a rigid T-tract and adjacent, potentially deformable G + C-rich DNA segment, suggesting that deformation of the spacer region may play a role in the transcriptional activation of Pm. This prediction was tested by using dimethyl sulfate and potassium permanganate footprinting analyses. Helical distortion involving strand separation was detected at positions -32 to -34, close to the predicted interface between Mor and RNAP. Promoter mutants in which this distortion was not detected exhibited a lack of melting in the -12 to -1 region and reduced promoter activity in vivo. We propose that complexes containing the distortion represent stressed intermediates rather than stable open complexes and thus can be envisaged as a transition state in the kinetic pathway of Pm activation in which stored torsional energy could be used to facilitate melting around the transcription start point.

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Elemental composition, functional groups, and molecular mass distribution were determined in humic acids from the Western Pacific abyssal and coastal bottom sediments. Humic acid structure was studied by oxidative degradation with alkaline nitrobenzene and potassium permanganate, p-coumaric, guaiacilic, and syringilic structural units typical for lignin of terrestrial plants were identified in humic acids by chromatographic analysis of oxidation products. Polysubstituted and polycondensed aromatic systems with minor proportion of aliphatic structures were basic structural units of humic acids in abyssal sediments.

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Compared to packings trays are more cost effective column internals because they create a large interfacial area for mass transfer by the interaction of the vapour on the liquid. The tray supports a mass of froth or spray which on most trays (including the most widely used sieve trays) is not in any way controlled. The two important results of the gas/liquid interaction are the tray efficiency and the tray throughput or capacity. After many years of practical experience, both may be predicted by empirical correlations, despite the lack of understanding. It is known that the tray efficiency is in part determined by the liquid flow pattern and the throughput by the liquid froth height which in turn depends on the liquid hold-up and vapour velocity. This thesis describes experimental work on sieve trays in an air-water simulator, 2.44 m in diameter. The liquid flow pattern, for flow rates similar to those used in commercial scale distillation, was observed experimentally by direct observation; by water-cooling, to simulate mass transfer; use of potassium permanganate dye to observe areas of longer residence time; and by height of clear liquid measurements across the tray and in the downcomer using manometers. This work presents experiments designed to evaluate flow control devices proposed to improve the gas liquid interaction and hence improve the tray efficiency and throughput. These are (a) the use of intermediate weirs to redirect liquid to the sides of the tray so as to remove slow moving/stagnant liquid and (b) the use of vapour-directing slots designed to use the vapour to cause liquid to be directed towards the outlet weir thus reducing the liquid hold-up at a given rate i.e. increased throughput. This method also has the advantage of removing slow moving/stagnant liquid. In the experiments using intermediate weirs, which were placed in the centre of the tray. it was found that in general the effect of an intermediate weir depends on the depth of liquid downstream of the weir. If the weir is deeper than the downstream depth it will cause the upstream liquid to be deeper than the downstream liquid. If the weir is not as deep as deep as the downstream depth it may have little or no effect on the upstream depth. An intermediate weir placed at an angle to the direction of flow of liquid increases the liquid towards the sides of the tray without causing an increase in liquid hold-up/ froth height. The maximum proportion of liquid caused to flow sideways by the weir is between 5% and 10%. Experimental work using vapour-directing slots on a rectangular sieve tray has shown that the horizontal momentum that is imparted to the liquid is dependent upon the size of the slot. If too much momentum is transferred to the liquid it causes hydraulic jumps to occur at the mouth of the slot coupled with liquid being entrained, The use of slots also helps to eliminate the hydraulic gradient across sieve trays and provides a more uniform froth height on the tray. By comparing the results obtained of the tray and point efficiencies, it is shown that a slotted tray reduces both values by approximately 10%. This reduction is due to the fact that with a slotted tray the liquid has a reduced residence time Ion the tray coupled also with the fact that large size bubbles are passing through the slots. The effectiveness of using vapour-directing slots on a full circular tray was investigated by using dye to completely colour the biphase. The removal of the dye by clear liquid entering the tray was monitored using an overhead camera. Results obtained show that the slots are successful in their aim of reducing slow moving liquid from the sides of the tray, The net effect of this is an increase in tray efficiency. Measurements of slot vapour-velocity found it to be approximately equal to the hole velocity.

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The organic matter in five oil shales (three from the Kimmeridge Clay sequence, one from the Oxford Clay sequence and one from the Julia Creek deposits in Australia) has been isolated by acid demineralisation, separated into kerogens and bitumens by solvent extraction and then characterised in some detail by chromatographic, spectroscopic and degradative techniques. Kerogens cannot be characterised as easily as bitumens because of their insolubility, and hence before any detailed molecular information can be obtained from them they must be degraded into lower molecular weight, more soluble components. Unfortunately, the determination of kerogen structures has all too often involved degradations that were far too harsh and which lead to destruction of much of the structural information. For this reason a number of milder more selective degradative procedures have been tested and used to probe the structure of kerogens. These are: 1. Lithium aluminium hydride reduction. - This procedure is commonly used to remove pyrite from kerogens and it may also increase their solubility by reduction of labile functional groups. Although reduction of the kerogens was confirmed, increases in solubility were correlated with pyrite content and not kerogen reduction. 2. O-methylation in the presence of a phase transfer catalyst. - By the removal of hydrogen bond interactions via O-methylation, it was possible to determine the contribution of such secondary interactions to the insolubility of the kerogens. Problems were encountered with the use of the phase transfer catalyst. 3. Stepwise alkaline potassium permanganate oxidation. - Significant kerogen dissolution was achieved using this procedure but uncontrolled oxidation of initial oxidation products proved to be a problem. A comparison with the peroxytrifluoroaceticacid oxidation of these kerogens was made. 4. Peroxytrifluoroacetic acid oxidation. - This was used because it preferentially degrades aromatic rings whilst leaving any benzylic positions intact. Considerable conversion of the kerogens into soluble products was achieved with this procedure. At all stages of degradation the products were fully characterised where possible using a variety of techniques including elemental analysis, solution state 1H and 13C nuclear magnetic resonance, solid state 13C nuclear magnetic resonance, gel-permeationchromatography, gas chromatography-mass spectroscopy, fourier transform infra-red spectroscopy and some ultra violet-visible spectroscopy.

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The binding of iron (59Fe) and gallium (67Ga) to the plasma protein transferrin (Tf) was investigated by G75 gel filtration chromatography in control patients and treated and untreated patients with Parkinson's disease (PD). Fe-Tf binding was 100% in all controls and PD patients suggesting that a defect in Fe-Tf binding was not involved in the aetiology of PD. Ga-Tf binding was significantly reduced in both untreated and treated PD patients compared to controls. In addition, treated PD patients had significantly higher Ga-Tf binding than untreated patients. A reduction in metal binding to Tf could result in the increase of a low molecular weight species which may more readily enter the CNS. Alternatively, it could lead to a decrease in the transport of essential metals into the brain via the Tf receptor system. A significant elevation in neopterin was demonstrated within the plasma of untreated PD patients compared to controls suggesting the activation of a cellular immune response. Furthermore, plasma neopterin was lower in treated compared to untreated PD patients, although the difference was not significant. There was no evidence for the activation of the humoral immune response in untreated or treated PD patients as measured by circulating immune complex (CIC) levels within the plasma. An inverse relationship between Ga-Tf binding and neopterin was observed in untreated PD patients. The addition of oxidants in the form of potassium permanganate and activated manganese dioxide reduced Ga-Tf binding in control plasma. However, relatively little response was observed using monocyte preparations. The results suggest that oxidants produced by activation of the cellular immune system could damage the Tf molecule thereby reducing its ability to bind metals.

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Under defined laboratory and field conditions, the investigation of percolating water through soil columns (podsol, lessive and peat) down to groundwater table shows that the main factors which control the chemical characteristics of the percolates are: precipitation, evaporation, infiltration rate, soil type, depth and dissolved organic substances. Evaporation and percolation velocity influences the Na+, SO4**2- and Cl- concentrations. Low percolation velocity leads also to longer percolation times and water logging in less permeable strata, which results in lower Eh-values and higher CO2-concentrations due to low gas exchange with the atmosphere. Ca2+ and Mg2+ carbonate concentration depends on soil type and depth. Metamorphism and decomposition of organic substances involve NO3 reduction and K+, Mg2+, SO4**2-, CO2, Fe2+,3+ transport. The analytical data were evaluated with multi variate statistical methods.