21 resultados para macera


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Chronic exposure to ethanol may results in pathophysiologic changes in cellular function. The present work was designed to investigate the morphology of testis submitted to experimental ethanol ingestion. Experimental animals were divided into two groups. The control group (n = 23) received a solid diet and tap water and the alcoholic group (n = 23) received the same solid diet and ethanol P.A. diluted 20% in water (v/v). After 120 days of treatment, all animals were anesthetized, weighed and sacrificed. Testosterone and luteinizing hormone levels in serum were lower in the alcoholic group than in the control group. Histological and ultrastructural alterations were observed in the testicular alcoholic germinative cells like enormous spaces, lipid droplets accumulation, digestive vacuoles, irregular diameter of the seminiferous tubules and interstitial dilated blood vessels. It was concluded that 20% ethanol provokes lesions on the testis germinative epithelium probably inducing gonadal dysfunction. (C) 2008 Elsevier Ltd. All rights reserved.

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Para avaliar o potencial do araçá-boi para produção de licores, foi estudada a composição química da polpa e o efeíto de alguns parâmetros do processamento, tais como, tipo de líquido extrator, tempo de maceração, proporção polpa/líquido extrator, proporção xarope/extrato c método de preparo do xarope. O araçá-boi apresentou boas características para o processamento de licor, como o pH ácido, altos teores de acidez titulável, sólidos solúveis e carotcnóides totais. Os parâmetros ideais para obtenção de licor de boa qualidade foram: cinco dias de maceração na proporção de 1:2 (p/v) de polpa:álcool de milho, relação de 1:0,5 (v/v) de xarope:cxtrato na formulação, utilizando-se xarope preparado com dissolução do açúcar sob aquecimento.

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La EPOC (Enfermedad Pulmonar Obstructiva Crónica) es una enfermedad crónica progresiva causada por la inhalación de partículas nocivas presentes principalmente en el humo del cigarrillo y en el humo de la leña, los cuales ocasionan un daño irreversible en el funcionamiento del aparato respiratorio y generan muchas consecuencias a nivel físico, mental y social en la persona que la padece, síntomas como la disnea o dificultad para respirar y la fatiga, afectan la capacidad funcional del individuo progresivamente y en ocasiones llegan a comprometer la realización de las actividades de la vida diaria, como bañarse, alimentarse y pueden limitar al individuo para desempeñarse dentro de su círculo familiar y social; esto puede conducir a la persona con EPOC a una discapacidad inminente con dependencia y aislamiento. Por fortuna, el conocimiento de la enfermedad, que avanza cada día, ha permitido conocer aspectos del tratamiento que pueden llevar a que los individuos con esta patología tengan alivio y control de sus síntomas y puedan vivir activamente y con la mejor calidad de vida posible.

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Resumen basado en el de la publicación

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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

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Composition and distribution of megabenthic communities around Svalbard were investigated in June/July 1991 with 20 Agassiz trawl and 5 bottom trawl hauls in depths between 100 and 2100 m. About 370 species, ranging from sponges to fish, were identified in the catches. Species numbers per station ranged from 21 to 86. Brittle stars, such as Ophiacantha bidentata, Ophiura sarsi and Ophiocten sericeum, were most important in terms of constancy and relative abundance in the catches. Other prominent faunal elements were eunephthyid alcyonarians, bivalves, shrimps, sea stars and fish (Gadidae, Zoarcidae, Cottidae). Multivariate analyses of the species and environmental data sets showed that the spatial distribution of the megabenthos was characterized by a pronounced depth zonation: abyssal, bathyal, off-shore shelf and fjordic communities were discriminated. However, a gradient in sediment properties, especially the organic carbon content, seemed to superimpose on the bathymetric pattern. Both main factors are interpreted as proxies of the average food availability, which is, hence, suggested to have the strongest influence in structuring megabenthic communities off Svalbard.

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During ODP Leg 107, the basement of the Tyrrhenian Sea was drilled at Site 650, located in the Marsili basin, and at Sites 651 and 655, both located in the Vavilov basin. In addition, a lava flow was drilled at Site 654 on the Sardinia rifted margin. Mineral and whole rock major and trace element chemistry, including rare earth element (REE) and Sr and Nd isotopic ratios, were determined in samples of these rocks. Site 654 lava was sampled within uppermost Pliocene postrift sediments. This lava is a basaltic andesite of intraplate affinity, and is analogous to some Plio-Pleistocene tholeiitic lavas from Sardinia. Site 650 basalts, drilled beneath 1.7-1.9-Ma-old basal sediment, are strongly altered and vesicular suggesting a rapid subsidence of the Marsili basin. Based on incompatible trace elements, these basalts show calc-alkaline affinity like some products of the Marsili Seamount and the Eolian arc. The basement of the two sites drilled within Vavilov basin shows contrasting petrologies. Site 655, located along the Gortani ridge in the western part of the basin, drilled a 116-m-thick sequence of basalt flows beneath 3.4-3.6-Ma-old basal sediments. These basalts are chemically relatively homogeneous and show affinity to transitional MORB. Four units consisting of slightly differentiated basaltic lavas, have been identified. Site 655 basalts are geochemically similar to the high Ti lavas from DSDP Leg 42, Site 373 (Vavilov Basin). The basement at Site 651, overlain by 40 m of metalliferous dolostone covered by fossiliferous sediments with an age of 2 Ma, consists of two basalt units separated by a dolerite-albitite intrusive body; serpentinized harzburgites were drilled for 30 m at the base of the hole. The two basalt units of Site 651 are distinct petrochemically, though both show incompatible elements affinity with high-K calc-alkaline/calc-alkaline magmas from Eolian arc. The cpx chemistry and high K/Na ratio of the lower unit lavas suggest a weak alkaline tendency of potassic lineage. Leg 107 basement rock data, together with data from DSDP Site 373 and from dredged samples, indicate that the deepest basins of the central Tyrrhenian Sea are underlain by a complex back-arc basin crust produced by magmas with incompatible element affinities to transitional MORB (Site 655 and DSDP Site 373), and to calc-alkaline and high-K calc-alkaline converging plate margin basalts (Sites 650 and 651). This petrogenetic complexity is in accordance with the back-arc setting of the Vavilov and Marsili basins. Other back-arc basin basalts, particularly those from ensialic basins such as the Bransfield Strait (Antarctica), show a comparable petrogenetic complexity (cf., Sounders and Tarney, 1984).