Phosphorus reduction by sifting fish waste meal

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

Suplementação com vitamina d (25-ohd3) e sua influência na produtividade e qualidade óssea de frangos de corte

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Desempenho de frangos de corte e produção de energia em biodigestores, utilizando-se três tipos de cama

Pós-graduação em Zootecnia - FCAV

Estudo do desempenho de barreiras de geotêxtil para contenção de sedimentos carreados pelo escoamento superficial

Pós-graduação em Engenharia Civil e Ambiental - FEB

Obtenção de um ataque químico padrão, zona de annealing parcial e temperatura de fechamento para o epídoto através do método dos traços de fissão

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

Avaliação do potencial mutagênico e bioacumulador de metais pesados de Baccharis trimera Less e Equisetum hyemale L

Pós-graduação em Biociências - FCLAS

Análise faciológica e estratigráfica das formações Taciba (parte superior) e Rio Bonito (membro Triunfo) em poços testemunhados da área de Monte Alegre (PR)

The Triunfo Member, from Rio Bonito Formation, is a potential reservoir for hydrocarbons and water, and contains coal deposits in the northern state of Paraná. On the eastern edge of the Paraná Basin, the Triunfo Member has two depocenters in Santa Catarina and offlap to the North of Paraná; here in two adjacent areas characterized his final lapout. These areas have a number of wells core/logged with the initials MA and NF, Monte Alegre and Figueira North, which were drilled by the Companhia de Pesquisa e Recursos Minerais (CPRM), in order to research for coal in the Rio Bonito Formation. In this study, three wells in the MA area, and they were MA-4, MA-6 and MA-7 was subjected to vertical facies analysis (1D), from the description of wells and processing of data, so that later it was possible to chronocorrelate thereof, together with MA-5 well, through cycles facies (2D). This is a thesis which has never been developed in these wells mentioned above, it was possible to observe the development of part of the Member Taciba (top) and the Member Triunfo as a whole, can be determined three cycles facies to the latter, as well as their depositional environments. Finally, the chronocorrelate showed that there is a tabular architecture between the wells studied, this occurred because of subsidence uniform

Geologia de uma área na porção centro leste da folha Cássia (1:50.000), MG

This study aimed the geological characterization at scale 1:50.000 of an area belonging to the southern sector of the Brasilia Belt, located in the western portion of the Passos Nappe, near the town of Cássia, MG. In this region, outcrops rock types belonging to Araxá Group, composed of metasediments associated with metavolcanics which form a tectonometamorphic terrain of great importance for understanding the geological evolution of southeast and midwest regions of Brazil. With the development of work was possible to group the rocks in 10 lithostratigraphic units and had been identified 3 different zones of metamorphism generated during the peak metamorphism. The structural pattern of the area shows that the main foliation has average dip 30 ° NW and mineral lineation parallel to the stretching direction with 290 °. Still, we can conf irm that this inverse gradient metamorphic rocks of the Passos Nappe, described by several authors. Also, were seen lithotypes of economic interest, some already in exploitation, such as clay and sand, and other mineral commodities, which are occurring and can be used: quartz, quartzite, garnet, kyanite, rutile and zircon.

Caracterização geológica do perfil laterítico no município de Rondon do Pará, bloco sul do projeto Alumina Rondon

This completion of course work has as its object of study the Bauxite Province of Paragominas regarded as the richest Amazon bauxite province and whose genesis is related to laterization processes responsible for the formation of mineral deposits of the Rondon Alumina Project, designed to assess areas in the southeast of Pará State, for mineral resources exploration of bauxite, which is the main source of aluminum in the country. Located in the region of Rondon do Pará - PA, the study area is geologically inserted in Lithostratigraphic Unit called Cobertura Laterítica Matura (Mature Lateritic Cover), formed by alteration of paleotropics Cretaceous siliciclastic rocks, and its geomorphology corresponds to a broad plateau with displays of representative profiles of the processes that acted in the region. In this context, the present research aims to characterize the geological evolution of the laterite profile, with detailed studies in the area, geological description of the formations from the bauxite surfaces, and mineralogical composition litochemical of different horizons that were correlated and deployed in an evolutionary model compatible with its traits. The data collected during the analysis subsidized metalogenetic understanding of the processes that acted in the enrichment of aluminum and iron as well as the redistribution of the latter modified profile. The results and information were embodied in the form of geological characterization of the different constituents of mineral associations of bauxite horizons, similarities or differences in both textural and structural aspects, in order to propose a evolutionary model with retaken of gibbsitization processes

Aplicações de isótopos estáveis na área da saúde no Brasil

The use of stable isotopes in Brazil is being improved, mainly through research conducted at main universities in the country. Some applications in health allow to studying, for example, processes involving synthesis and protein degradation, energy expenditure, body composition, kinetics of vitamins, mineral absorption and diagnose diseases related to Helicobacter pylori. The big motivation is to encourage the growth of investments in health in the few centers that have mass spectrometers in Brazil, as the technique is harmless to humans, in other words, no has problems to use it like when you use radioactive isotopes

Caracterização hidroquímica dos sistemas aquíferos Serra Geral e Guarani da sub-bacia do Rio Pardo e municípios adjacentes, no sudoeste do estado de São Paulo

The main purpose of this work is to evaluate the chemical composition of the groundwaters from Guarani Aquifer System and Serra Geral Aquifer System in the Rio Pardo basin, located at the southwestern of São Paulo state. To the hydrochemical characterization, physicalchemical analyses from 32 sampled wells were used. These results were plotted in Piper diagrams allowing the classification of groundwater as calcium or calcium-magnesium bicarbonate type and sodium bicarbonate type for both aquifer systems. Distribution of hydrochemical facies over the study area was obtained using Stiff diagrams. The groundwater can be classified, representing in this sequence its hydrochemical evolution. The recognized mechanisms responsible for groundwater evolution are dissolution of minerals magnesium, such as olivine, present in the basalt, dissolution of feldspars and removal of the carbonate cement of the sandstones mineral framework. Ionic exchange may represent an important processes in the groundwater evolution, responsible for the increase in the sodium concentration and decrease of calcium

Estudo de rochas alcalinas intrusivas na região de Três Fontes - MG

Geological researches conducted in the past few years detected, through deep drill hole data, the presence of alkaline rocks in the region of Três Fontes-MG, where the Barbacena Group rocks, the Morro do Ferro Greenstone Belt rocks and Araxá/Canastra groups‟ rocks are exposed. This paper aimed the petrographic and chemical characterization of these alkaline rock types, which have not yet been described in the literature. Based on petrographic descriptions and geochemical and Scanning Electron Microscopy analysis, it was possible to characterize the rock in question as lamprophyre, rich in carbonates, phlogopite, pyroxene, olivine, titaniferous opaque minerals and apatite concentrations that reach 7%. This occurrence corresponds to an alkaline intrusion, which caused brecciation of host rocks, possibly indicating that the material is explosive, however, in the study area there was no evidence of volcanic activity on the surface

Estudo geofísico em um depósito de manganês supergênico no município de Itapira - SP

The mining research is a complex activity, which should preferably involve the combination of direct and indirect techniques of geological research. The increasing demand for base metals in domestic and international markets provide the revaluation of mineral occurrences, which can be converted into deposits and mines. This paper presents the results of the application of geophysical methods of electric resistivity and induced polarization in main foliation parallel to the arrangement of the area, in a deposit of oxides and hydroxides in massive and disseminated ores, docked in gneisses and quartzites, located in the municipality of Itapira, in the North of the State of São Paulo in Brazil. Inversion models indicate the predominance of high cargabilidade that partially coincide with low resistivity values. Integration of geophysical data made possible the drafting of sections of electric walking with cross-checking distance x depth, for detailing your target. The integrated analysis of geophysical and geological structural data leads to the conclusion that the primary mining suffers structural control with the regional foliation in ores

Levantamento de diferentes técnicas de controle de cupins subterrâneos (Isoptera, Rhinotermitidae) em áreas urbanas e rurais

Os cupins são conhecidos também como térmitas ou térmites, formam um grupo extenso e diverso e, atualmente, há mais de 2.800 espécies descritas que se distribuem em sete famílias. Pertencentes à ordem Isoptera, os térmitas são insetos eussociais que apresentam uma organização social altamente desenvolvida e vivem em ninhos denominados de cupinzeiros, geralmente, construídos no solo. Os cupinzeiros podem ser bem resistentes e estruturalmente complexos, e neles são encontrados indivíduos morfologicamente distintos adaptados a determinadas funções que constituem as diferentes castas (reprodutores, operários e soldados), além de indivíduos imaturos (“ninfas” e “larvas”) e ovos. A presença dos cupins nos ecossistemas é de extrema importância em diversos e diferentes processos. Em linhas gerais, os cupins são bastante importantes como decompositores de matéria orgânica fragmentando os detritos orgânicos, são mediadores da humificação, participam da ligação e formação de agregados e complexos minerais argilosos, e também atuam na fixação do nitrogênio, pois seus simbiontes têm a capacidade de fixar o gás nitrogênio da atmosfera, contribuindo, dessa forma, com a fertilidade do solo. Contudo, os cupins são bem conhecidos porque causam prejuízos enormes, ou seja, pelo potencial como pragas, danificando diversos tipos de materiais celulósicos e não celulósicos, além de edificações, monumentos, plantações, etc. Os cupins subterrâneos são os que causam maiores problemas, pois possuem grande capacidade de dispersão e são animais, que devido aos hábitos crípticos, têm o estudo e o controle dificultado. Além disso, estão entre os insetos mais abundantes, sendo a maioria pertencente à família Rhinotermitidae. O controle de cupins subterrâneos é um controle diferenciado, já que possuem o ninho sob o solo e com um grande número de indivíduos. A eliminação de uma parte da colônia muitas...

Biodegradação de óleos derivados do petróleo e de origem vegetal estimulada por biossurfactantes em meio aquoso e monitoramento de sua toxicidade

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