338 resultados para Tucumã cake
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Part I What makes science hard for newcomers? 1) The background (briefly) of my research - (why the math anxiety model doesn’t fit) 2) The Tier analysis (a visual) – message: there are many types of science learners in your class than simply younger versions of yourself 3) Three approaches (bio, chem, physics) but only one Nature 4) The (different) vocabularies of the three Sciences 5) How mathematics is variously used in Science Part II Rules and rules-driven assignments- lQ vs OQ1) How to incorporate creativity into assignments and tests? 2) Tests- borrowing “thought questions" from other fields (If Columbus hadn't discovered the new World, when and under whose law would it have been discovered?) 3) Grading practices (partial credit, post-exam credit for finding and explaining nontrivial errors 4) Icing on the cake – applications, examples of science/engineering from Tuesdays NY Times Part III Making Change at the Departmental Level 1) Taking control of at least some portion of the curriculum 2) Varying style of presentation 3) Taking control of at least some portion of the exams 4) GRADING pros and cons of grading on a curve 5) Updating labs and lab reporting.
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ContentsFacing ObstaclesStudent interests influence catalogMisconceptions inspire professor to author bookOsemele, Cyclones work out at Pro DayCelebrate events with cake popsTaking flight from hectic everyday life
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There is still discussion regarding whether liquid biofuels can contribute to rural energy security in the global South. We argue that transitioning to a village energy supply based on jatropha hedges around smallholder plots is possible, but requires collective effort for the acquisition and maintenance of processing equipment and for the running of village generators. The use of jatropha oil for lighting in rural households is affordable and technically possible, but not ideal if more efficient electric solutions exist. Cooking with jatropha oil or press cake is also possible, but quantities produced in hedges can only substitute a small part of the firewood used by rural households.
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The 23rd Annual Biochemical Engineering Symposium was held at the University of Oklahoma on April 17, 1993. The objectives of the symposium were to provide 1) a forum for informal discussion of biochemical engineering research being carried at the participating universities and 2) an opportunity for students to present and publish their work. Thirteen papers presented at the symposium are included in the proceedings. Because final publication usually takes place in refereed journals, the articles included here are typically brief and often cover work in progress. The program of the symposium and a list of participants are included in the proceedings. ContentsA Low-Cost Bioreactor Strategy for RNA Synthesis, H. Anthony Marble, Eleni Chrisikos, and Robert H. Davis Development of a CELSS Bioreactor: Oxygen Transfer and Micromixing in Parabolic Flight, P.E. Villeneuve, K.S. Wenger, B.G. Thompson, T. Kedar, and E.H. Dunlop Scale-up of Dexter Murine Bone Marrow Cultures Utilizing a Three-Dimensional Fiberglass Support Matrix, John G. Highfill, Paul Todd, Steve Haley, and Dhinaker Kompala Modeling and Estimation of States of Recombinant Fermentations Using Nonlinear Input/Output Models, Vicotr M. Saucedo and M. Nazmul Karim Deadent Microfiltration of Bovine Serum Albumin Suspension Through Yeast Cake Layers and Assymetric Polymeric Membranes, Naveen Arora and Robert H. Davis Monitoring the Fate of Toluene and Phenol in the Rhizosphere, N. Muralidharan, Lawrence C. Davis, and Larry E. Erickson Hydrodynamic Motions Associated with Bubble Coalescence and Breakup, T.Y. Yiin, L.A. Glasgow, and L.E. Erickson Expression and Purification of a-Human Atrial Natriuretic Peptide in Escherichia coli by Fusion with L-Asparaginase, Nien-Tung Ma and Roger G. Harrison High Pressure Crystallization of Proteins, Mungara V. Saikumar, Charles E. Glatz, and Maurice A. Larson Structure/Function Relationships in the Catalytic and Starch Binding Domains of Glucoamylase, Pedro M. Coutinho, Clark Ford, Peter J. Reilly Cellular Responses of Insect Cell Spodoptera frugiperda to Environmental Stresses, Paul Yeh, Grace Y. Sun, Gary A. Weisman, Rakesh Bajpai A Novel Approach to Understanding the Antimicrobial Activity of Peptides, Naveen Pathak, Marie-Helene Janna, Gael Ruche, David McCarthy, and Roger Harrison Mass Transfer in the Bioremediation of Soils Contaminated with Trapped Non-Aqueous Phase Liquids, Xiaoqing Yang, Larry E. Jacobson, and L.T. Fan
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The relative effects of paleoceanographic and paleogeographic variations, sediment lithology, and diagenetic processes on the final preserved chemistry of Japan Sea sediments are evaluated by investigating the rare earth element (REE), major element, and trace element concentrations in 59 squeeze-cake whole-round and 27 physical-property sample residues from Sites 794, 795, and 797, cored during ODP Leg 127. The most important variation in sedimentary chemical composition is the increase in SiO2 concentration through the Pliocene diatomaceous sequences, which dilutes most other major and trace element components by various degrees. This biogenic input is largest at Site 794 (Yamato Basin), moderately developed at Site 797 (Yamato Basin), and of only minor importance at Site 795 (Japan Basin), potentially reflecting basinal contrasts in productivity with the Yamato Basin recording greater biogenic input than the Japan Basin and with the easternmost sequence of Site 794 lying beneath the most productive waters. There are few systematic changes in solid-phase chemistry resulting from the opal-A/opal-CT or opal-CT/quartz silica phase transformations. Most major and trace element concentrations are controlled by the aluminosilicate fraction of the sediment, although the effects of diagenetic silica phases and manganese carbonates are of localized importance. REE total abundances (Sum REE) in the Japan Sea are strongly dependent upon the paleoceanographic position of a given site with respect to terrigenous and biogenic sources. REE concentrations at Site 794 overall correspond well to aluminosilicate chemical indices and are strongly diluted by SiO2 within the upper Miocene-Pliocene diatomaceous sequence. Eu/Eu* values at Site 794 reach a maximum through the diatomaceous interval as well, most likely suggesting an association of Eu/Eu* with the siliceous component, or reflecting slight incorporation of a detrital feldspar phase. SumREE at Site 795 also is affiliated strongly with aluminosilicate phases and yet is diluted only slightly by siliceous input. At Site 797, SumREE is not as clearly associated with the aluminosilicate fraction, is correlated moderately to siliceous input, and may be sporadically influenced by detrital heavy minerals originating from the nearby rifted continental fragment composing the Yamato Rise. Ce/Ce* profiles at all three sites increase essentially monotonically with depth and record progressive diagenetic LREE fractionation. The observed Ce/Ce* increases are not responding to changes in the paleoceanographic oxygenation state of the overlying water, as there is no independent evidence to suggest the proper oceanographic conditions. Ce/Ce* correlates slightly better with depth than with age at the two Yamato Basin sites. The downhole increase in Ce/Ce* at Sites 794 and 797 is a passive response to the diagenetic transfer of LREE (except Ce) from sediment to interstitial water. At Site 795, the overall lack of correlation between Ce/Ce* and Lan/Ybn suggests that other processes mask the diagenetic behavior of all LREEs. First-order calculations of the Ce budget in Japan Sea waters and sediment indicate that ~20% of the excess Ce adsorbed by settling particles is recycled within the water column and that an additional ~38% is recycled at or near the seafloor. Thus, because the remaining excess Ce is only ~10% of the total Ce, there is not a large source of Ce to the deeply buried sediment, further suggesting that the downhole increase in Ce/Ce* is a passive response to diagenetic behavior of the other LREEs. The REE chemistry of Japan Sea sediment therefore predicts successive downhole addition of LREEs to deeply buried interstitial waters.
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En el presente trabajo se muestran los resultados de las investigaciones realizadas en el Instituto de Investigaciones Fundamentales en Agricultura Tropical (INIFAT), acerca de la acción del almacenamiento sobre la semilla de Nim y sus componentes. Se pudo determinar que durante el proceso de beneficio de los frutos de Nim cosechados sólo una cuarta parte del volumen de los frutos se convierte en semillas, definiéndose además que el peso de un fruto maduro es de 1.8 g y de una semilla seca 0.4 g. Por otra parte, se pudo conocer que en el proceso de almacenamiento de la semilla seca de Nim se produce una disminución notable del peso de la misma y sus componentes (almendra, aceite, torta y residuo), dada por la influencia del tiempo de almacenamiento y factores ambientales tales como humedad relativa y temperatura. Además, se observó de igual forma, que la mayor pérdida de peso de la semilla se produjo durante los dos primeros meses de almacenadas, que incluyen el período de envejecimiento fisiológico.
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Este trabalho é parte de uma investigação mais ampla e se relaciona com os jogos tradicionais praticados pelos povos indígenas da Amazônia. Neste artigo apresentamos o jogo da malha ou jogo da linha praticado pelos nativos das etnias Tikuna e Cambeba, utilizando o fio de tucum, resultante da folha de uma palmeira do mesmo nome. Observou-se que entre os nativos as figuras mais desenhadas e que fazem parte do seu patrimônio, são ferramentas da vida diária, ou de figuras relativas à caça e à pesca. Sem esquecer os motivos que caracterizam as teceduras artesanais de cada grupo étnico. Verificamos também que o Tikuna e o Cambeba desenvolvem figuras idênticas às encontradas do outro extremo do mundo, e entre eles, alguns figuras em três dimensões. Podemos então concluir, em conformidade com a Praxiologia Motriz, que o jogo do fio é classificado como uma atividade psicomotora.
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Este trabalho é parte de uma investigação mais ampla e se relaciona com os jogos tradicionais praticados pelos povos indígenas da Amazônia. Neste artigo apresentamos o jogo da malha ou jogo da linha praticado pelos nativos das etnias Tikuna e Cambeba, utilizando o fio de tucum, resultante da folha de uma palmeira do mesmo nome. Observou-se que entre os nativos as figuras mais desenhadas e que fazem parte do seu patrimônio, são ferramentas da vida diária, ou de figuras relativas à caça e à pesca. Sem esquecer os motivos que caracterizam as teceduras artesanais de cada grupo étnico. Verificamos também que o Tikuna e o Cambeba desenvolvem figuras idênticas às encontradas do outro extremo do mundo, e entre eles, alguns figuras em três dimensões. Podemos então concluir, em conformidade com a Praxiologia Motriz, que o jogo do fio é classificado como uma atividade psicomotora.
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Este trabalho é parte de uma investigação mais ampla e se relaciona com os jogos tradicionais praticados pelos povos indígenas da Amazônia. Neste artigo apresentamos o jogo da malha ou jogo da linha praticado pelos nativos das etnias Tikuna e Cambeba, utilizando o fio de tucum, resultante da folha de uma palmeira do mesmo nome. Observou-se que entre os nativos as figuras mais desenhadas e que fazem parte do seu patrimônio, são ferramentas da vida diária, ou de figuras relativas à caça e à pesca. Sem esquecer os motivos que caracterizam as teceduras artesanais de cada grupo étnico. Verificamos também que o Tikuna e o Cambeba desenvolvem figuras idênticas às encontradas do outro extremo do mundo, e entre eles, alguns figuras em três dimensões. Podemos então concluir, em conformidade com a Praxiologia Motriz, que o jogo do fio é classificado como uma atividade psicomotora.
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The density, species composition, and possible change in the status of pack ice seals within the Weddell Sea were investigated during the 1997/1998 summer cruise of the RV "Polarstern" (ANT-XV/3, PS48). Comparisons were made with previous surveys in the Weddell Sea where it was assumed that all seals were counted in a narrow strip on either side oft he ship or aircraft. A total of 15 aerial censuses were flown during the period 23 January - 7 March 1998 in the area bounded by 07°08' and 45°33' West longitude. The censused area in the eastern Weddell Sea was largely devoid of pack ice while a well circumscribed pack ice field remained in the western Weddell Sea. A total of 3,636 (95.4 %) crabeater seals, 21 (0.5 %) Ross seals, 45 (1.2 %) leopard seals and 111 (2.9 %) Weddell seals were observed on the pack ice during a total of 1,356.57 linear nautical miles (244.2 nm) of transect line censused. At a mean density of 21.16 1/nm**2 over an area of 244.2 nm, it is the highest densities on record for crabeater seals, density of up to 411.7 1/nm**2 being found in small areas. The overall high densities of seals (30.18 1/nm**2) recorded for the eastern Weddell Sea (27.46 1/nm**2, 0.27 1/nm**2, and 0.66 1/nm**2 for crabeater, leopard and Weddell seals respectively) is a consequence of the drastically reduced ice cover and the inverse relationship that exists between cover and seal densities. Ross seal densities (0.08 1/nm**2) were the lowest on record fort the area. It is suggested that seals largely remain within the confines of the pack ice despite seasonal and annual changes in its distribution. Indications are that in 1998 the El Niño has manifested itself in the Weddell Sea, markedly influencing the density and distribution of pack ice seals.
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The Cretaceous and Paleogene sediments recovered during Ocean Drilling Program Leg 207 can be divided into three broad modes of deposition: synrift clastics (lithologic Unit V), organic matter-rich, laminated black shales (Unit IV), and open-marine chalk and calcareous claystones (Units III-I). The aim of this study is to provide a quantitative geochemical characterization of sediments representing these five lithologic units. For this work we used the residues (squeeze cakes) obtained from pore water sampling. Samples were analyzed for bulk parameters (total inorganic carbon, total organic carbon, and S) and by X-ray fluorescence for major (Si, Ti, Al, Fe, Mn, Mg, Ca, Na, K, and P) and selected minor (As, Ba, Co, Cr, Cu, Mo, Ni, Pb, Rb, Sr, U, V, Y, Zn, and Zr) elements. Inductively coupled plasma-mass spectrometry analyses for rare earth elements (REEs) were performed on acid digestions of the squeeze cake samples from Site 1258. The major element composition is governed by the mixture of a terrigenous detrital component of roughly average shale (AS) composition with biogenous carbonate and silica. The composition of the terrigenous detritus is close to AS in Units II-IV. For Unit I, a more weathered terrigenous source is suggested. Carbonate contents reach >60 wt% on average in chalks and calcareous claystones of Units II-IV. The SiO2 contribution in excess of the normal terrigenous-detrital background indicates the presence of biogenous silica, with highest amounts in Units II and III. The contents of coarse-grained material (quartz) are enhanced in Unit V, where Ti and Zr contents are also high. This indicates a high-energy depositional environment. REE patterns are generally similar to AS. A more pronounced negative Ce anomaly in Unit IV may indicate low-oxygen conditions in the water column. The Cretaceous black shales of Unit IV are clearly enriched in redox-sensitive and stable sulfide-forming elements (Mo, V, Zn, and As). High phosphate contents point toward enhanced nutrient supply and high bioproductivity. Ba/Al ratios are rather high throughout Unit IV despite the absence of sulfate in the pore water, indicating elevated primary production. Manganese contents are extremely low for most of the interval studied. Such an Mn depletion is only possible in an environment where Mn was mobilized and transported into an expanded oxygen minimum zone ("open system"). The sulfur contents show a complete sulfidation of the reactive iron of Unit IV and a significant excess of sulfur relative to that of iron, which indicates that part of the sulfur was incorporated into organic matter. We suppose extreme paleoenvironmental conditions during black shale deposition: high bioproductivity like in recent coastal upwelling settings together with severe oxygen depletion if not presence of hydrogen sulfide in the water column.
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A obtenção de etanol a partir de rotas alcoolquímicas consagradas gera resíduos com potencial de aproveitamento, tanto em outros setores produtivos como no ciclo produtivo do próprio combustível. Este é o caso de torta de filtro e vinhaça. A vinhaça em particular costuma ser devolvida ao campo com o intuito de ajustar teores nutricionais do solo no cultivo da cana. No entanto, estudos ambientais destacam que esta alternativa traz efeitos negativos sobre os meios receptores (água e solo), condição que abre a perspectiva para exploração de usos alternativos dessas substâncias. Este estudo se propôs a contribuir para o tema ao avaliar de forma sistêmica o desempenho ambiental de duas alternativas de reaproveitamento de vinhaça: (i) reuso no campo em processos de fertirrigação, alternativa consolidada no Brasil, e (ii) reuso da fração líquida da vinhaça em etapas diversas do processo industrial de obtenção de etanol. Em qualquer das situações fez-se uso da técnica de Avaliação de Ciclo de Vida - ACV para proceder tal verificação. A análise ambiental da prática de reuso de vinhaça e torta para fertirrigação foi conduzida a partir da comparação de cenários que consideraram a forma de suprimento de nutrientes para a cana e o método de colheita. A avaliação de impactos ocorreu em dois níveis: quanto ao consumo de recursos, a partir de Primary Energy Demand (PED); e em termos de emissões para o ambiente por meio da elaboração do Perfil Ambiental. Uma Análise de Sensibilidade foi também realizada para verificar o efeito de oscilações dos teores de Nitrogênio (N), Fósforo (P) e Potássio (K) na composição da vinhaça sobre os resultados obtidos, caso da primeira alternativa. Concluiu-se para esse caso que a substituição parcial de fertilizantes químicos por vinhaça traz aumento da Demanda de Energia Primária global para ambos os métodos de colheita. Em termos de Perfil Ambiental, a comparação entre cenários das mesmas práticas de manejo mostrou que a troca de adubos por vinhaça e torta é positiva para o desempenho ambiental do etanol por reduzir impactos quanto a Mudanças Climáticas (CC), Acidificação Terrestre (TA) e Toxicidade Humana (HT). Por outro lado, o tratamento de vinhaça para reposição de água na etapa industrial resultou em aumento global das contribuições para as categorias acima mencionadas além de incrementos para Eutrofização de água doce (FEut) e Ecotoxicidade de água doce (FEC), a despeito de ser constatada a redução de 45% quanto a Depleção de água (WD). Os aumentos no impacto se deveram principalmente aos efeitos negativos causados durante a produção do CaO usado no processo de tratamento da vinhaça. No entanto, a substituição deste insumo por NaOH só representou melhora em termos de CC. Pode-se concluir que a reutilização de vinhaça e de torta de filtro como complemento nutricional para o cultivo de cana-de-açúcar resultou em uma alternativa mais adequada de reaproveitamento do que o se este fluído fosse reutilizado para suprir parte da demanda hídrica de processo, mesmo quando o consumo de água na etapa industrial tenha inexoravelmente se reduzido a partir da implantação dessa medida.
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This article describes an effective procedure for reducing the water content of excess sludge production from a wastewater treatment plant by increasing its concentration and, as a consequence, minimizing the volume of sludge to be managed. It consists of a pre-dewatering sludge process, which is used as a preliminary step or alternative to the thickening. It is made up of two discontinuous sequential stages: the first is resettling and the second, filtration through a porous medium. The process is strictly physical, without any chemical additives or electromechanical equipment intervening. The experiment was carried out in a pilot-scale system, consisting of a column of sedimentation that incorporates a filter medium. Different sludge heights were tested over the filter to verify the influence of hydrostatic pressure on the various final concentrations of each stage. The results show that the initial sludge concentration may increase by more than 570% by the end of the process with the final volume of sludge being reduced in similar proportions and hydrostatic pressure having a limited effect on this final concentration. Moreover, the value of the hydrostatic pressure at which critical specific cake resistance is reached is established.
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El presente trabajo se ha desarrollado conjuntamente con alumnos de la asignatura obligatoria “Gestión Integrada y Seguridad Industrial” del Máster de Ingeniería Química y la asignatura optativa de cuarto curso “Gestión Integrada en la Industria Química” del grado de Ingeniería Química. Se ha diseñado una actividad práctica con el fin de aplicar los conceptos teóricos impartidos en estas asignaturas. Con el reto de cocinar un Mug Cake o “bizcocho en taza” se ha logrado poner en práctica varios de los contenidos teóricos de las asignaturas, especialmente el capítulo 7 de la norma ISO 9001:2008, “Realización del producto”; así como otros conceptos de liderazgo y mejora continua. Los alumnos se dividieron en dos equipos formados por el mismo número de miembros y en los que se mantenía el mismo número de alumnos del grado y del máster. Previamente a la realización del taller los alumnos elaboraron una serie de procedimientos, registros y listados de verificación. La experiencia ha resultado altamente fructífera puesto que los alumnos se han enfrentado al reto de aplicar contenidos teóricos a procesos reales, ha mejorado su motivación e interés por la materia y han desarrollado técnicas de trabajo en equipo y organización personal aumentando su productividad.