976 resultados para AXIAL CHIRALITY
Resumo:
O objetivo do trabalho foi caracterizar a morfologia do fruto e da semente de três espécies florestais nativas do Brasil, Solanum granuloso-leprosum Dunal, S. lycocarpum A.St.-Hil. e S. pseudoquina A.St.-Hil., recomendadas para plantações destinadas à recuperação de áreas degradadas. Os frutos são indeiscentes, carnosos, do tipo baga, globosos, polispérmicos e constituídos por dois ou mais lóculos. As sementes são estenospérmicas, campilótropas, elipsóides, comprimidas, apresentando seção longitudinal largo-ovalada ou achatado-ovalada e seção transversal elíptica. Hilo mediano-marginal localizado em uma depressão e micrópila arredondada. Sementes albuminosas, com endosperma abundante, periférico, carnoso-firme, semitransparente e de coloração esbranquiçada. Embrião axial, linear, contínuo e curvado. Em Solanum lycocarpum e S. pseudoquina o embrião é circinado e em S. granuloso-leprosum é espiralado.
Resumo:
A Guazuma ulmifolia Lam. é uma espécie arbórea pioneira de ocorrência natural em quase todo o Brasil, desde a Amazônia até o Paraná. Pertence a família Sterculiaceae, sendo recomendada para recuperação de áreas degradadas. O objetivo deste trabalho foi descrever os caracteres morfológicos dos frutos, sementes, plântula e planta jovem. No fruto foram observados: forma, coloração, dimensões, textura, deiscência, e o número de sementes por fruto. Na semente foram observados: coloração, peso de 1000 sementes, forma, tegumento, embrião e endosperma. O estádio de plântula foi considerado até o momento em que tinha apenas os cotilédones e a partir da emissão de folhas passou a ser considerada planta jovem. Os aspectos vegetativos descritos e ilustrados foram: raiz primária, raízes secundárias e terciárias, hipocótilo, epicótilo, cotilédones, caule, folhas e gema apical. Fruto e uma cápsula loculicida globoso, de coloração preta, com faixas estreitas e superfície muricada. Semente de coloração acinzentada e formas variadas, envolta pela testa que quando umedecida torna-se gelatinosa. Embrião axial e contínuo; com cotilédones foliáceos, plicados e que após a emergência são arredondados, verdes e com nervuras. Após a emergência o hipocótilo e a raiz primária são brancos e cilíndricos, mas com passar do tempo se tornam mais escuros. Caule de coloração verde-escura; folhas pecioladas, com nervura principal e secundária; limbo com margem dentada.
Resumo:
A utilização das popularmente chamadas, sementes crioulas de soja ou sementes salvas pelos produtores é uma constante no Centro-Oeste Brasileiro. Este trabalho teve o objetivo de avaliar a qualidade das sementes de soja produzidas, colhidas e armazenadas por uma empresa produtora de sementes, e das sementes utilizadas pelos produtores de grãos, produzidas sem seguir os procedimentos técnicos de produção de sementes. As parcelas conduzidas para produção de sementes comerciais, foram retiradas do campo logo que atingiram a maturação de campo com umidade de 16,3%, receberam quatro aplicações de inseticidas durante o seu ciclo, para o controle de percevejos e, foram colhidas com colhedora de fluxo axial com rotação de cilindro de 500 rpm, enquanto as outras parcelas foram retiradas do campo com umidades de 14,7 e 12,3%, receberam apenas três aplicações de inseticida e, foram colhidas com colhedora de cilindro côncavo com velocidade de rotação do cilindro de 700 rpm. Após a colheita foram utilizados diferentes processos de secagem, beneficiamento e armazenamento para as sementes comerciais e para as sementes salvas. No início e no final do armazenamento, todas as unidades experimentais foram analisadas com os seguintes testes: de germinação, de tetrazólio 1-8 , do pH do exsudato, de envelhecimento acelerado, de desenvolvimento de plântula, de tetrazólio 1-3 e de 1º contagem do teste de germinação. Os resultados permitem concluir que: sementes comerciais, produzidas de acordo com as recomendações técnicas de produção de sementes, apresentam qualidade fisiológica superior; a qualidade fisiológica de materiais conduzidos como grãos é reduzida com o armazenamento, impedindo sua utilização como sementes para formação de lavouras de grãos comerciais.
Resumo:
Foi analisado o comportamento físico da secagem estacionária com distribuição axial de ar, com utilização de um secador comercial, em comparação com protótipos para secagem de sementes de milho, em camada de 0,70m. A temperatura do ar de secagem foi de 47 ±3ºC, no secador comercial e de 40 ±1ºC, nos protótipos de secador. Foram considerados o tempo de operação, a posição das sementes na massa e o efeito na qualidade física. Para tanto, foram caracterizados o ar ambiente, o ar de secagem, as temperaturas e os teores de água na massa de sementes e realizados exame visual de fissuras internas e teste de coloração com tintura de iodo. Com baixa umidade relativa ocorre super secagem na camada inferior e retardamento na camada superior, resultando em gradientes de umidade das sementes, no final da secagem, de até 4,5 pontos percentuais. O aumento da temperatura do ar de secagem determina uma elevação na taxa de remoção de água e aumento da percentagem de sementes de milho com fissuras internas e quando a camada de sementes mais próxima da entrada do ar aquecido atinge teor de água inferior a 14%, se inicia a secagem da camada seguinte.
Resumo:
O conhecimento dos aspectos morfológicos de sementes e plântulas pode ser usado em estudos de taxonomia, na interpretação de testes de germinação em laboratório, trabalhos em viveiro e em estudos relacionados à ecologia da espécie. Os objetivos deste trabalho foram o de descrever e ilustrar a morfologia externa e interna dos frutos e sementes, as fases de germinação, a plântula e as plantas de mulungu (Erythrina velutina Willd.). Os frutos e sementes foram coletados no solo, embaixo de árvores matrizes distribuídas em diferentes fragmentos florestais, no município de Areia - PB. Para a descrição morfológica dos frutos, sementes, germinação e desenvolvimento da plântula foram examinados cem unidades que foram selecionadas aleatoriamente. A semente é reniforme; embrião axial com cotilédones carnosos; germinação epígea fanerocotiledonar e na fase de plântula foi observado heterofilia. Os aspectos descritos e ilustrados mostraram-se homogêneos e confiáveis para a identificação da espécie. Deste modo, podem ser úteis em trabalhos de tecnologia de sementes, para a avaliação qualidade fisiológica de sementes e avaliação de plântulas em testes de germinação, além de servirem para identificação da espécie em viveiros e também para estudos de regeneração natural.
Resumo:
Bauhinia monandra, espécie popularmente conhecida na Amazônia como pata-de-vaca, é indicada entre outros usos como planta medicinal nessa região. Visando contribuir para um melhor conhecimento foram coletadas sementes dessa espécie do banco de germoplasma da EMBRAPA - CPATU, Amazônia Oriental, no estado do Pará. O estudo morfo-anatômico revelou sementes estenospérmicas, oblongas, base arredondada, margem inteira, ápice assimétrico, perfil convexo pouco acentuado e hilo em forma de "V" na região apical. A testa é monocrômica, brilhante, lisa e constituída por dois estratos epidérmicos; linha lúcida presente. O endosperma é contínuo, espesso, adnato a testa. O embrião é axial e invaginado, apresenta dois cotilédones foliáceos e eixo embrionário com plúmula rudimentar e radícula imperceptível. Foram vistos grãos de amido no interior dos cotilédones.
Resumo:
Este trabalho objetivou caracterizar morfologicamente as sementes e o desenvolvimento da plântula de Curitiba prismatica e verificar as melhores temperaturas, substratos e condição de luz para a germinação das sementes. A semente caracteriza-se como exalbuminosa e possui forma elíptica espiralada com tegumento coriáceo, de coloração castanho-escura. O embrião é descrito como cotiledonar pimentóide, axial, carnoso e cilíndrico, curvado em forma de "C" e de coloração branca. O desenvolvimento da plântula se inicia com a abertura do opérculo e uma pequena expansão do hipocótilo nesta região. Após esta expansão, ocorre o desenvolvimento de pêlos na base do hipocótilo, e a emissão da radícula por volta do 18o dia, sendo que aos 45 dias já se tem a plântula propriamente dita, caracterizada pelo surgimento dos eofilos. Os melhores valores para a porcentagem, tempo médio e velocidade de germinação das sementes de C. prismatica foram obtidos com a temperatura 25 ºC, nos substratos papel toalha e areia. A espécie pode ser classificada como fotoblástica positiva preferencial.
Resumo:
Optical microscopy is living its renaissance. The diffraction limit, although still physically true, plays a minor role in the achievable resolution in far-field fluorescence microscopy. Super-resolution techniques enable fluorescence microscopy at nearly molecular resolution. Modern (super-resolution) microscopy methods rely strongly on software. Software tools are needed all the way from data acquisition, data storage, image reconstruction, restoration and alignment, to quantitative image analysis and image visualization. These tools play a key role in all aspects of microscopy today – and their importance in the coming years is certainly going to increase, when microscopy little-by-little transitions from single cells into more complex and even living model systems. In this thesis, a series of bioimage informatics software tools are introduced for STED super-resolution microscopy. Tomographic reconstruction software, coupled with a novel image acquisition method STED< is shown to enable axial (3D) super-resolution imaging in a standard 2D-STED microscope. Software tools are introduced for STED super-resolution correlative imaging with transmission electron microscopes or atomic force microscopes. A novel method for automatically ranking image quality within microscope image datasets is introduced, and it is utilized to for example select the best images in a STED microscope image dataset.
Resumo:
The production of biodiesel through transesterification has created a surplus of glycerol on the international market. In few years, glycerol has become an inexpensive and abundant raw material, subject to numerous plausible valorisation strategies. Glycerol hydrochlorination stands out as an economically attractive alternative to the production of biobased epichlorohydrin, an important raw material for the manufacturing of epoxy resins and plasticizers. Glycerol hydrochlorination using gaseous hydrogen chloride (HCl) was studied from a reaction engineering viewpoint. Firstly, a more general and rigorous kinetic model was derived based on a consistent reaction mechanism proposed in the literature. The model was validated with experimental data reported in the literature as well as with new data of our own. Semi-batch experiments were conducted in which the influence of the stirring speed, HCl partial pressure, catalyst concentration and temperature were thoroughly analysed and discussed. Acetic acid was used as a homogeneous catalyst for the experiments. For the first time, it was demonstrated that the liquid-phase volume undergoes a significant increase due to the accumulation of HCl in the liquid phase. Novel and relevant features concerning hydrochlorination kinetics, HCl solubility and mass transfer were investigated. An extended reaction mechanism was proposed and a new kinetic model was derived. The model was tested with the experimental data by means of regression analysis, in which kinetic and mass transfer parameters were successfully estimated. A dimensionless number, called Catalyst Modulus, was proposed as a tool for corroborating the kinetic model. Reactive flash distillation experiments were conducted to check the commonly accepted hypothesis that removal of water should enhance the glycerol hydrochlorination kinetics. The performance of the reactive flash distillation experiments were compared to the semi-batch data previously obtained. An unforeseen effect was observed once the water was let to be stripped out from the liquid phase, exposing a strong correlation between the HCl liquid uptake and the presence of water in the system. Water has revealed to play an important role also in the HCl dissociation: as water was removed, the dissociation of HCl was diminished, which had a retarding effect on the reaction kinetics. In order to obtain a further insight on the influence of water on the hydrochlorination reaction, extra semi-batch experiments were conducted in which initial amounts of water and the desired product were added. This study revealed the possibility to use the desired product as an ideal “solvent” for the glycerol hydrochlorination process. A co-current bubble column was used to investigate the glycerol hydrochlorination process under continuous operation. The influence of liquid flow rate, gas flow rate, temperature and catalyst concentration on the glycerol conversion and product distribution was studied. The fluid dynamics of the system showed a remarkable behaviour, which was carefully investigated and described. Highspeed camera images and residence time distribution experiments were conducted to collect relevant information about the flow conditions inside the tube. A model based on the axial dispersion concept was proposed and confronted with the experimental data. The kinetic and solubility parameters estimated from the semi-batch experiments were successfully used in the description of mass transfer and fluid dynamics of the bubble column reactor. In light of the results brought by the present work, the glycerol hydrochlorination reaction mechanism has been finally clarified. It has been demonstrated that the reactive distillation technology may cause drawbacks to the glycerol hydrochlorination reaction rate under certain conditions. Furthermore, continuous reactor technology showed a high selectivity towards monochlorohydrins, whilst semibatch technology was demonstrated to be more efficient towards the production of dichlorohydrins. Based on the novel and revealing discoveries brought by the present work, many insightful suggestions are made towards the improvement of the production of αγ-dichlorohydrin on an industrial scale.
Resumo:
This thesis seeks to elucidate a motif common to the work both of Jean-Paul Sartre and Alain Badiou (with special attention being given to Being and Nothingness and Being and Event respectively): the thesis that the subject 's existence precedes and determines its essence. To this end, the author aims to explicate the structural invariances, common to both philosophies, that allow this thesis to take shape. Their explication requires the construction of an overarching conceptual framework within which it may be possible to embed both the phenomenological ontology elaborated in Being and Event and the mathematical ontology outlined in Being and Event. Within this framework, whose axial concept is that of multiplicity, the precedence of essence by existence becomes intelligible in terms of a priority of extensional over intensional determination. A series of familiar existentialist concepts are reconstructed on this basis, such as lack and value, and these are set to work in the task of fleshing out the more or less skeletal theory of the subject presented in Being and Event.
Resumo:
The Rankin Inlet area, on the west shore of Hudson Bay in the Northwest Territories, is in the Churchill Structural Province. Metamorphosed volcanic and sedimentary rocks, previously mapped as Archean and part of the Kaminak Group, underlie most of the area. The Rankin Inlet Group consists of greywacke, with minor conglomeratic greywacke, quartzite and dolomite, overlain by massive and pillowed basaltic flows. Gabbro sills intrude the sediments near the base of the volcanic sequence and three serpentinite sills outcrop at the base of the volcanic sequence. The sediments are in fault-contact with quartz monzonite to the south and were intruded by granitic rocks to the northwest. Two periods of folding were defined by the mapping. The first generation folds are recumbent isoclinal folds, with northwest-trending and northeast-dipping axial planes, formed through gravitational sliding. The second generation folds are symmetrically disposed about the axis of the granitic intrusion and have east-southeast trending and nearly vertical axial planes. Whole-rock analysis of 64 rock samples indicates that metasomatic alteration accompanied the intrusion of both the granitic rocks and the serpentinite. The volcanic rocks, gabbro and serpentinite were derived from a magma of oceanic tholeiitic affinities. The stratigraphic sequence and chemistry of the volcanic rocks of the Rankin Inlet Group indicate that this assemblage is correlative with the Hurwitz Group rather than the Kaminak Group and is therefore Aphebian in age.
Resumo:
The McArthur Township area in the Archean Abitibi Belt of northeast Ontario contains northwesterly trending volcanic rocks which are located on a limb of a large syncline. The axial trace of the syncline passes through the adjacent Douglas Township. The Archean volcanic rocks and associated sedimentary rocks are intruded and deformed by two large plutons and a few smaller hypabyssal intrusions. A petrographic and geochemical study of the Precambrian rocks exposed 1n the study area was undertaken in order to investigate the metamorphic grade and geochemical characteristics of the rocks. All the samples were studied with the microscope and analysis of 20 major and trace elements were determined on a selection of the less altered specimens by x-ray fluorescence. Three different periods of igneous activity have occurred in the study area. The first two periods were dominated by volcanic extrusive rocks accompanied by gabbroic sills. The third cycle is the diapiric intrusion of the granitic plutons and subsequent metamorphism of the older rocks to the low to medium grade. Two periods of sedimentation are also recognized in the study area which occurred after the first and second cycle of volcanism. Chemically, the lavas are subdivided into three main associations: (1) The komatiitic association is characterized by high MgO, high Ni, low Ti02 and a low FeO*/(FeO* + MgO) ratio. They occupy the base of each volcanic cycle and some of the flows exhibit spinifex textures. (2) The tholeiitic association displays distinct iron and titanium enrichment trends in the intermediate membersor -i r (3) The calc-alkaline association contains low FeO* and TI02 and high Ni contents relative to modern calc-alkaline types. They are formed at the end of each cycle of volcanism and overlie the tholeiitic flows. All three associations of the first volcanic cycle are exposed in the study area, while the second cycle is represented by a komatiltic sequence. The volcanic rocks were possibly formed by multiple partial melting of the Archean mantle to produce parental magmas under various P - T conditions.
Resumo:
Confocal and two-photon microcopy have become essential tools in biological research and today many investigations are not possible without their help. The valuable advantage that these two techniques offer is the ability of optical sectioning. Optical sectioning makes it possible to obtain 3D visuahzation of the structiu-es, and hence, valuable information of the structural relationships, the geometrical, and the morphological aspects of the specimen. The achievable lateral and axial resolutions by confocal and two-photon microscopy, similar to other optical imaging systems, are both defined by the diffraction theorem. Any aberration and imperfection present during the imaging results in broadening of the calculated theoretical resolution, blurring, geometrical distortions in the acquired images that interfere with the analysis of the structures, and lower the collected fluorescence from the specimen. The aberrations may have different causes and they can be classified by their sources such as specimen-induced aberrations, optics-induced aberrations, illumination aberrations, and misalignment aberrations. This thesis presents an investigation and study of image enhancement. The goal of this thesis was approached in two different directions. Initially, we investigated the sources of the imperfections. We propose methods to eliminate or minimize aberrations introduced during the image acquisition by optimizing the acquisition conditions. The impact on the resolution as a result of using a coverslip the thickness of which is mismatched with the one that the objective lens is designed for was shown and a novel technique was introduced in order to define the proper value on the correction collar of the lens. The amoimt of spherical aberration with regard to t he numerical aperture of the objective lens was investigated and it was shown that, based on the purpose of our imaging tasks, different numerical apertures must be used. The deformed beam cross section of the single-photon excitation source was corrected and the enhancement of the resolution and image quaUty was shown. Furthermore, the dependency of the scattered light on the excitation wavelength was shown empirically. In the second part, we continued the study of the image enhancement process by deconvolution techniques. Although deconvolution algorithms are used widely to improve the quality of the images, how well a deconvolution algorithm responds highly depends on the point spread function (PSF) of the imaging system applied to the algorithm and the level of its accuracy. We investigated approaches that can be done in order to obtain more precise PSF. Novel methods to improve the pattern of the PSF and reduce the noise are proposed. Furthermore, multiple soiu'ces to extract the PSFs of the imaging system are introduced and the empirical deconvolution results by using each of these PSFs are compared together. The results confirm that a greater improvement attained by applying the in situ PSF during the deconvolution process.
Resumo:
The Horwood Peninsula - Gander Bay area is located at NE Newfoundland in the Botwood Zone (Williams et a1., 1974) or in the Dunnage Zone (Williams, 1979) of the Central Mobile Belt of the Newfoundland Appalachians. The area is underlain by Middle Ordovician to possible Lower Silurian rocks of the Davidsville and Indian Islands Groups, respectively. Three conformable formations named informally : the Mafic Volcanic Formation, the Greywacke and Siltstone Formation and the Black Slate Formation, have been recognized in the Davidsville Group. The Greywacke and the Black Slate Formations pass locally into a Melange Formation. From consideration of regional structure and abundant locally-derived mafic volcanic olisto- 1iths in the melange, it is considered to have originated by gravity sliding rather than thrusting. Four formations have been recognized in the Indian Islands Group. They mainly contain silty slate and phyllite, grey cherty siltstone, green to red micaceous siltstone and limestone horizons. Repetition of lithological units by F1 folding are well-demonstrated in one of formations in this Group. The major structure in this Group on the Horwood Peninsula is interpreted to be a synclinal complex. The lithology of this Group is different from the Botwood Group to the west and is probably Late Ordovician and/or Early Silurian in age. The effects of soft-sediment deformation can be seen from the lower part of the Davidsville Group to the middle part of the Indian Islands Group indicating continuous and/or episodic slumping and sliding activities throughout the whole area. However, no siginificant depOSitional and tectonic break that could be assigned to the Taconian Orogeny has been recognized in this study. Three periods of tectonic deformation were produced by the Acadian Orogeny. Double boudinage in thin dikes indicates a southeast-northwest sub-horizontal compression and main northeast-southwest sub-horizontal extension during the D1 deformation. A penetrative, axial planar slaty cleavage (Sl) and tight to isocJ.ina1 F1 folds are products of this deformation. The D2 and D3 deformations formed S2 and S3 fabrics associated with crenulations and kink bands which are well-shown in the slates and phyllites of the Indian Islands Group. The D2 and D3 deformations are the products of vertical and northeast-southwest horizontal shortening respectively. The inferred fault between the Ordovician slates (Davidsville Group) and the siltstones (Indian Islands Group) suggested by Williams (1963, 1964b, 1972, 1978) is absent. Formations can be followed without displacement across this inferred fault. Chemically, the pillow lavas, mafic agglomerates, tuff beds and diabase dikes are subdivided into three rock suites : (a) basaltic komatiite (Beaver Cove Assemblage), (b) tholeiitic basalt (diabase dikes), (c) alkaline basalt (Shoal Bay Assemblage). The high Ti02 , MgO, Ni contents and bimodal characteristic of the basaltic komatiite in the area are comparable to the Svartenhuk Peninsula at Baffin Bay and are interpreted to be the result of an abortive volcano-tectonic rift-zone in a rear-arc basin. Modal and chemical analyses of greywackes and siltstones show the trend of maturity of these rocks increasing from poorly sorted Ordovician greywackes to fairly well-sorted Silurian siltstones. Rock fragments in greywackes indicate source areas consisting of plagiogranite, low grade metamorphic rocks and ultramafic rocks. Rare sedimentary structures in both Groups indicate a southeasterly provenance. Trace element analyses of greywackes also reveal a possible island-arc affinity.
Synthesis of Chiral Benzimidazolylidenes from 1,10-Phenathrolines and 1,10-Phenathroline-2,9-dione /
Resumo:
A^-heterocyclic carbenes (NHCs) have become the focus of much interest as ancillary ligands for transition metal catalysts in recent years. Their structural variability and strong cy-donation properties have led to the preparation of demonstrably useful organometallic catalysts. Among the three general structural types of NHCs (imidazolylidenes, imidazolinylidenes, and benzimidazolylidenes), benzimidazolylidenes are the least investigated because of the limitation of current synthetic approaches. The preparation of chiral analogues is even more challenging. Previously, our group has demonstrated an alternative approach to synthesizing benzimidazolylidenes with a tetracyclic framework in three steps from 1,10-phenanthroline. This thesis is focused on approaches to chiral benzimidazolylidenes derived from substituted 1,10-phenanthrolines. A key step in the preparation of these ligands involves a reduction of the pyridyl rings in 1,10-phenanthrolines. Chirality can be introduced to phenanthrolines before, during, or after the reduction as illustrated by three approaches: 1) de novo construction of the phenanthroline from chiral ketones with endo and exo faces to provide a degree of diastereoselectivity during subsequent reduction; 2) introduction of substituents into the 2- and 2,9- position of phenanthroline by nucleophilic aromatic substitution, followed by a reduction-resolution sequence; and 3) use of the protected octahydrophenanthroline as a substrate for chiral induction a to nitrogen.