190 resultados para JATROPHA CURCAS


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Objetivou-se, na condução deste trabalho, a avaliação das silagens de capim-elefante aditivadas com tortas de nabo forrageiro, pinhão manso e tremoço pela técnica de produção de gás. O experimento foi desenvolvido no Laboratório de Nutrição Animal do Centro de Energia Nuclear na Agricultura da Universidade de São Paulo (LANA/CENA/USP). Como doadores de líquido de rúmen, foram utilizados 2 ovinos da raça Santa Inês, machos, adultos, castrados e providos de cânula ruminal permanente. A alimentação dos animais doadores foi constituída de forragem de gramínea cultivada e uma suplementação, ao final do dia, com feno de Tifton, concentrado comercial e sal mineral à vontade. Os substratos foram secos a 60ºC, moídos em moinho do tipo Willey, provido de peneira com perfurações de 2 mm. Os gases produzidos durante os diferentes períodos de fermentação (0, 4, 8, 12, 24, 36, 48, 72 e 96 h) foram medidos com um transducer - medidor de pressão.O experimento foi instalado segundo um delineamento de blocos ao acaso em que os tratamentos foram arranjados em um esquema de parcelas subdivididas no tempo. Os maiores valores de produção de gás observados para os tratamentos em que adicionou-se torta de tremoço quando comparados com as outras tortas, decorreu do fato da torta de tremoço apresentar menor teor de fibras, propiciando assim, uma maior fermentação ruminal e, consequentemente, maior produção de gás em relação a outros alimentos com maior proporção de carboidratos estruturais (parede celular).As taxas de degradação da fração solúvel da matéria seca foi menor para NF 8% e PM 11% em relação às outras silagens estudadas. Foram encontradas diferenças significativas para as TNF, TPM e TT, nos diferentes níveis, em relação ao volume de gases em 96 h de incubação (P<0,05). As silagens contendo torta de tremoço apresentaram maior produção de gases quando comparadas Às outras tortas. em todos os tratamentos, exceto naqueles em que adicionou-se TT, houve diminuição (P<0,05) nos valores médios de degradabilidade da matéria seca às 96 horas, à medida que aumentou-se o nível de inclusão das tortas. As silagens de capim-elefante adicionadas de tortas de nabo forrageiro ou tremoço, nos diferentes níveis, apresentaram maiores taxas de degradação e maiores produções de gases que as adicionadas de torta de pinhão manso.

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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

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Pós-graduação em Agronomia - FEIS

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Pós-graduação em Agronomia - FEIS

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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

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

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The present literature review aimed to describe biodisel’s physicochemical properties obtained from different raw materials. Were studied data concerning viscosity, density, cetane number, fl ash point, pour point and calorifi c power of biodiesel produced from soybean oil, coconut, rice bran, cotton, pequi, babassu, mamona, palm, castor, sunfl ower, corn, canola, jatropha and karanja. Considering the diversity of vegetal and animal sources that can be used on the biodiesel production, it is noteworthy the lack of data concerning physicochemical properties of unexplored raw materials. This work may contribute for the creation of database about physicochemical properties of oil and biodiesel from different sources which will allow design and scale-up, both the necessary equipment to the production line and reciprocating engines.

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Pós-graduação em Agronomia - FEIS

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The jatropha plant produces seeds containing 25–40% oil by weight. This oil can be made into biodiesel. During the recent global fuel crisis, the price of crude oil peaked at over USD 130 per barrel. Jatropha attracted huge interest – it was touted as a wonder crop that could generate biodiesel oil on “marginal lands” in semi-arid areas. Its promise appeared especially great in East Africa. Today, however, jatropha’s value in East Africa appears to lie primarily in its multipurpose use by small-scale farmers, not in large-scale biofuel production.

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Leafing phenology of two dry-forest sites on soils of different depth (S = shallow, D = deep) at Shipstern Reserve, Belize, were compared at the start of the rainy season (April-June 2000). Trees greater than or equal to 2.5 cm dbh were recorded weekly for 8 wk in three 0.04-ha plots per site. Ten species were analysed individually for their phenological patterns, of which the three most common were Bursera simaruba, Metopium brownei and Jatropha gaumeri. Trees were divided into those in the canopy (> 10 cm dbh) and the subcanopy (less than or equal to 10 cm dbh). Site S had larger trees on average than site D. The proportion of trees flushing leaves at any one time was generally higher in site S than in site D, for both canopy and subcanopy trees. Leaf flush started 2 wk earlier in site S than site D for subcanopy trees, but only 0.5 wk earlier for the canopy trees. Leaf flush duration was 1.5 wk longer in site S than site D. Large trees in the subcanopy flushed leaves earlier than small ones at both sites but in the canopy just at site D. Large trees flushed leaves earlier than small ones in three species and small trees flushed leaves more rapidly in two species. Bursera and Jatropha followed the general trends but Metopium, with larger trees in site D than site S, showed the converse with onset of flushing I wk earlier in site D than site S. Differences in response of the canopy and subcanopy trees on each site can be accounted for by the predominance of spring-flushing or stem-succulent species in site S and a tendency for evergreen species to occur in site D. Early flushing of relatively larger trees in site D most likely requires access to deeper soil water reserves but small and large trees utilize stored tree water in site S.

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Pliocene vegetation dynamics and climate variability in West Africa have been investigated through pollen and XRF-scanning records obtained from sediment cores of ODP Site 659 (18°N, 21°W). The comparison between total pollen accumulation rates and Ti/Ca ratios, which is strongly correlated with the dust input at the site, showed elevated aeolian transport of pollen during dusty periods. Comparison of the pollen records of ODP Site 659 and the nearby Site 658 resulted in a robust reconstruction of West African vegetation change since the Late Pliocene. Between 3.6 and 3.0 Ma the savannah in West Africa differed in composition from its modern counterpart and was richer in Asteraceae, in particular of the Tribus Cichorieae. Between 3.24 and 3.20 Ma a stable wet period is inferred from the Fe/K ratios, which could stand for a narrower and better specified mid-Pliocene (mid-Piacenzian) warm time slice. The northward extension of woodland and savannah, albeit fluctuating, was generally greater in the Pliocene. NE trade wind vigour increased intermittently around 2.7 and 2.6 Ma, and more or less permanently since 2.5 Ma, as inferred from increased pollen concentrations of trade wind indicators (Ephedra, Artemisia, Pinus). Our findings link the NE trade wind development with the intensification of the Northern Hemisphere glaciations (iNHG). Prior to the iNHG, little or no systematic relation could be found between sea surface temperatures of the North Atlantic with aridity and dust in West Africa.