Your browser doesn't support javascript.
loading
Mostrar: 20 | 50 | 100
Resultados 1 - 3 de 3
Filtrar
Mais filtros










Base de dados
Intervalo de ano de publicação
1.
Ultrason Sonochem ; 28: 230-239, 2016 Jan.
Artigo em Inglês | MEDLINE | ID: mdl-26384903

RESUMO

Maritime pine sawdust, a by-product from industry of wood transformation, has been investigated as a potential source of polyphenols which were extracted by ultrasound-assisted maceration (UAM). UAM was optimized for enhancing extraction efficiency of polyphenols and reducing time-consuming. In a first time, a preliminary study was carried out to optimize the solid/liquid ratio (6g of dry material per mL) and the particle size (0.26 cm(2)) by conventional maceration (CVM). Under these conditions, the optimum conditions for polyphenols extraction by UAM, obtained by response surface methodology, were 0.67 W/cm(2) for the ultrasonic intensity (UI), 40°C for the processing temperature (T) and 43 min for the sonication time (t). UAM was compared with CVM, the results showed that the quantity of polyphenols was improved by 40% (342.4 and 233.5mg of catechin equivalent per 100g of dry basis, respectively for UAM and CVM). A multistage cross-current extraction procedure allowed evaluating the real impact of UAM on the solid-liquid extraction enhancement. The potential industrialization of this procedure was implemented through a transition from a lab sonicated reactor (3 L) to a large scale one with 30 L volume.


Assuntos
Fracionamento Químico/métodos , Resíduos Industriais , Fenóis/isolamento & purificação , Pinus/química , Ondas Ultrassônicas , Madeira/química , Cinética , Tamanho da Partícula , Fenóis/química
2.
J Environ Radioact ; 85(2-3): 369-79, 2006.
Artigo em Inglês | MEDLINE | ID: mdl-16102877

RESUMO

The Boréon area in the Mercantour Massif, S.E. France, was contaminated by radionuclides after the Chernobyl accident in the first days of May 1986. Sediments from a small mountain lake in this area were collected, as well as forest soils in its vicinity, in order to obtain 137Cs and 210Pb profiles. Calculated from the 210Pb inventory in a soil of a horizontal area, the flux is high in the area (0.06 Bqcm(-2)y(-1)) probably because of the great frequency of rain and uranium ores outcropping in the massif. The comparison of the 137Cs soil inventories and the unsupported 210Pb suggests that the 137Cs fallout due to the Chernobyl accident in the study site (Boréon) was at least 3.5 Bqcm(-2), more probably the double. The recent lake sediments still undergo a rather strong contamination by 137Cs and the sediment profiles show that the residence time of 137Cs in the catchment area is long. The study area is frequented by many inhabitants of the city of Nice and other cities at the Mediterranean coast during week-end and during summer and winter holidays. Thus the 137Cs external exposure impact was evaluated at 2 mSvy(-1) for 2002 in the most contaminated point.


Assuntos
Radioisótopos de Césio/análise , Exposição Ambiental/análise , Cinza Radioativa , Poluentes Radioativos do Solo/análise , Poluentes Radioativos da Água/análise , Acidente Nuclear de Chernobyl , França , Água Doce , Sedimentos Geológicos/análise , Humanos , Radioisótopos de Chumbo/análise , Guerra Nuclear , Doses de Radiação , Monitoramento de Radiação , Liberação Nociva de Radioativos , Medição de Risco , Árvores
3.
J Environ Radioact ; 82(3): 371-81, 2005.
Artigo em Inglês | MEDLINE | ID: mdl-15885382

RESUMO

Groundwaters from the Sebkhet Essijoumi drainage basin, situated in northern Tunisia, West of the city of Tunis, were sampled and analyzed for uranium and radium isotopes. Low (234)U/(238)U activity ratios coupled with relatively high (228)Ra and (238)U concentrations were found in the Manouba plain phreatic aquifer, at the northern part of the basin, where remote sensing has indicated that this plain corresponds to the main humid zone of the area. Low (234)U/(238)U ratios probably reflected short residence time for waters in the Manouba plain, and high ratios longer residence time in the south, where water reaching the phreatic aquifer seems to have previously circulated in rocks constituting the southern hills. Assuming that, in the Manouba plain aquifer, the groundwater flows downstream from the Oued Lill pass area to the South-West of the Sebkha, the difference in the (228)Ra/(226)Ra activity ratio suggests that the residence time of water has been 2.8 years longer near the Sebkha than upstream.


Assuntos
Rádio (Elemento)/análise , Urânio/análise , Poluentes Radioativos da Água/análise , Abastecimento de Água , Clima Desértico , Monitoramento Ambiental , Fenômenos Geológicos , Geologia , Tunísia
SELEÇÃO DE REFERÊNCIAS
DETALHE DA PESQUISA
...