1000 resultados para Contabilidade brasileira


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Al-pillared clay was prepared with a Brazilian bentonite from the Campina Grande region (Paraíba, BRAZIL). It was intercalated at 298 K, during 48 hours, with a solution containing [Al3+] = 0.10 mol/L and molar ratio OH/Al = 2.0 prepared at 333 K, and was calcined at 773K. The catalytic activity was evaluated by alkylation of benzene with 1-dodecene. The characterization methods were: X-ray fluorescence and diffraction analysis; 27Al, 29Si and 23Na MAS NMR and textural analysis by N2 adsorption. The thermal stability of the natural clay was improved by the pillaring procedure, as well as the catalytic activity. The intercalated clay presented the highest initial rate of reaction among the systems tested.

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A natural clay from Campina Grande region (Paraíba, Brazil), with 8.57% of Fe2O3, was used to study the most appropriate condition to carry out the iron extraction, without altering the clay structure in a significant way. Samples were treated with the Dithionite-Citrate-Bicarbonate method (DCB) for 30 and 120 minutes (pH=9.1), and also with citric acid (pH=1.8; time=15min), at 75°C. Conductivity measurements, X-ray fluorescence, X-ray diffraction, energy-dispersive spectrometry, electron-diffraction with transmission electron microscopy and textural evaluation by nitrogen adsorption were done. The treatment in a basic medium was more selective for iron removal than in acid condition. The time of 30 minutes, with 1.6 g Na2S2O4/10 g clay, was the best condition for the iron extraction.

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This work presents an overview of the development of analytical chemistry in Brazil in the last 25 years under the influence of Brazilian Chemical Society (SBQ). It is shown that the common sense that analytical chemistry is still an under-developed area is not true. Data from specialized literature show a significant contribution of Brazilian analytical chemists in high impact periodicals and for several areas there is a good adherence among works carried out in Brazil and abroad according to a comparison of studies presented in the 11th Brazilian Meeting on Analytical Chemistry (Campinas, September, 2001) and the XI European Conference on Analytical Chemistry (Lisboa, September, 2000). According to the opinion of investigators in this area, there are some topics that require a focused attention for proper evolution. However, there is an absolute consensus about the evolution of graduate programs and the need to improve and extend strategies to absorb newcomers in the area. Some suggestions are presented considering possible pathways of analytical chemistry in Brazil.

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This paper describes a comparative analysis on natural product chemistry between the Brazilian Chemical Society journals and twelve representative international publications in the area. The search using the ISI Web of Knowledge disclosed 41,362 publications in the years 2000-2002 containing at least one researcher from a Brazilian Institution, from which 12% belongs to natural products.

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The monitoring of the pollution status of the Brazilian coast is hampered by the lack of a consistent environmental indicator. We propose Hg as an environmental proxy to anthropogenic pollution of coastal regions due to its absence in the Brazilian geology, its ubiquity in anthropogenic effluents, and its toxicity. Available data suggest Hg "backgrounds" in coastal sediments of 1-10 ng g-1, in the East and 15-30 ng g-1 in the South. We suggest short sediment cores to establish these values estimating a geo-accumulation index to compare all areas. The distribution of index values showed the majority of southern coast at least moderately contaminated whereas many eastern areas are still pristine.

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Montmorillonite clay from Brazil was pillared with aluminium polyhydroxications. The influence of aging of the pillaring solution and the concentration of the clay suspension on the properties of the prepared materials was studied. The materials were characterized by chemical analysis, XRD and pore analysis by N2 adsorption. The catalytic properties were evaluated in the cumene cracking reaction. Results showed that the pillarization process increases the basal spaces of natural clay from 9.7 to 18.5 Å and the surface area from 41 to 300 m²/g.

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Phosphorus geochemistry as a proxy of environmental estuarine processes at the Jaguaribe River, Northeastern Brazil. Sedimentation of different phosphorus geochemical fractions can characterize the natural or anthropogenic processes dominant in the watershed. Selective chemical extraction of different phosphorus geochemical forms in estuarine sediments showed the predominance of inorganic over organic forms suggesting an increase in inorganic phosphorus input from anthropogenic sources. Local hydrochemistry favors the dominance of inorganic ferric and carbonatic phosphorus. Ongoing changes in the estuarine throphy, from mesothrophic to euthrophic, may decrease the immobilization of these forms, increasing dissolved phosphorus and favoring euthrophy. Detritic phosphorus suggests a fluvial origin of this fraction and acts as a tracer of river influence upon the estuary.

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This article offers an overview on the historical facts and the recent state of the Regional Secretaries and the Scientific Divisions in the course of 30 years of SBQ.

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This paper presents some aspects involved in the internationalization of SBQ. The importance of journals, meetings and agreements in this process is discussed.

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The main aspects of the modern Medicinal Chemistry, among the classic and industrial paradigms, used in the drug discovery process will be treated. The contribution of the Brazilian science in the knowledge generation in Medicinal Chemistry will be demonstrated, with base in searches accomplished in the portal Web of Science® 7.10 and in the directory of groups of research of CNPq.

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Higher education was precariously installed in Brazil in colonial times, and during that period it led a difficult life. From the early nineteenth century on several institutions were founded and developed in different parts of the country. Those institutions were kept independent from one another without forming full universities until the beginning of the twentieth century, in a peculiar historical process that sets the country apart in this respect. This article examines this unique development and searches the past for the earliest origins of the nation's present university network.