816 resultados para Electrophoretic depositions


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The studies described here base mainly on sedimentary material collected during the "Indian Ocean Expedition" of the German research vessel "Meteor" in the region of the Indian-Pakistan continental margin in February and March 1965. Moreover,samples from the mouth of the Indus-River were available, which were collected by the Pakistan fishing vessel "Machhera" in March 1965. Altogether, the following quantities of sedimentary material were collected: 59.73 m piston cores. 54.52 m gravity cores. 33 box grab samples. 68 bottom grab samples Component analyses of the coarse fraction were made of these samples and the sedimentary fabric was examined. Moreover, the CaCO3 and Corg contents were discussed. From these investigations the following history of sedimentation can be derived: Recent sedimentation on the shelf is mainly characterized by hydrodynamic processes and terrigenous supply of material. In the shallow water wave action and currents running parallel to the coast, imply a repeated reworking which induces a sorting of the grains and layering of the sediments as well as a lack of bioturbation. The sedimentation rate is very high here. From the coast-line down to appr. 50 m the sediment becomes progressively finer, the conditions of deposition become less turbulent. On the outer shelf the sediment is again considerably coarser. It contains many relicts of planktonic organisms and it shows traces of burrowing. Indications for redeposition are nearly missing, a considerable part of the fine fraction of the sediments is, however, whirled up and carried away. In wide areas of the outer shelf this stirring has gained such a degree that recent deposits are nearly completely missing. Here, coarse relict sands rich in ooids are exposed, which were formed in very shallow stirred water during the time when the sea reached its lowest level, i.e. at the turn of the Pleistocene to the Holocene. Below the relict sand white, very fine-grained aragonite mud was found at one location (core 228). This aragonite mud was obviously deposited in very calm water of some greater depth, possibly behind a reef barrier. Biochemic carbonate precipitation played an important part in the formation of relict sands and aragonite muds. In postglacial times the relict sands were exposed for long periods to violent wave action and to areal erosion. In the present days they are gradually covered by recent sediments proceeding from the sides. On the continental margin beyond the shelf edge the distribution of the sediments is to a considerable extent determined by the morphology of the sea bottom. The material originating from the continent and/or the shelf, is less transported by action of the water than by the force of gravity. Within the range of the uppermost part of the continental slope recent sedimentation reaches its maximum. Here the fine material is deposited which has been whirled up in the zone of the relict sands. A laminated fine-grained sediment is formed here due to the very high sedimentation rate as well as to the extremely low O2-content in the bottom water, which prevents life on the bottom of the sea and impedes thus also bioturbation. The lamination probaly reflects annual variation in deposition and can be attributed to the rhythm of the monsoon with its effects on the water and the weather conditions. In the lower part of the upper continental slope sediments are to be found which show in varying intensity, intercalations of fine material (silt) from the shelf, in large sections of the core. These fine intercalations of allochthonous material are closely related to the autochthonous normal sediment, so that a great number of small individual depositional processes can be inferred. In general the intercalations are missing in the uppermost part of the cores; in the lower part they can be met in different quantities, and they reach their maximum frequency in the upper part of the lower core section. The depositions described here were designated as turbid layer sediments, since they get their material from turbid layers, which transport components to the continental slope which have been whirled up from the shelf. Turbidites are missing in this zone. Since the whole upper continental slope shows a low oxygen-content of the bottom water the structure of the turbid layer sediments is more or less preserved. The lenticular-phacoidal fine structure does, however, not reflect annual rhythms, but sporadic individual events, as e.g. tsunamis. At the lower part of the continental slope and on the continental rise the majority of turbidites was deposited, which, during glacial times and particularly at the beginning of the post-glacial period, transported material from the zone of relict sands. The Laccadive Ridge represented a natural obstacle for the transport of suspended sediments into the deep sea. Core SIC-181 from the Arabian Basin shows some intercalations of turbidites; their material, however, does not originate from the Indian Shelf, but from the Laccadive Ridge. Within the range of the Indus Cone it is surprising that distinct turbidites are nearly completely missing; on the other hand, turbid layer sediments are to be found. The bottom of the sea is showing still a slight slope here, so that the turbidites funneled through the Canyon of the Swatch probably rush down to greater water depths. Due to the particularly large supply of suspended material by theIndus River the turbid layer sediments show farther extension than in other regions. In general the terrigenous components are concentrated on the Indus Cone. It is within the range of the lower continental slope that the only discovery of a sliding mass (core 186) has been located. It can be assumed that this was set in motion during the Holocene. During the period of time discussed here the following development of kind and intensity of the deposition of allochthonous material can be observed on the Indian-Pakistan continental margin: At the time of the lowest sea level the shelf was only very narrow, and the zone in which bottom currents were able to stir up material by oscillating motion, was considerably confined. The rivers flowed into the sea near to the edge of the shelf. For this reason the percentage of terrigenous material, quartz and mica is higher in the lower part of many cores (e.g. cores 210 and 219) than in the upper part. The transition from glacial to postglacial times caused a series of environmental changes. Among them the rise of the sea level (in the area of investigation appr. 150 m) had the most important influence on the sedimentation process. In connection with this event many river valleys became canyons, which sucked sedimentary material away from the shelf and transported it in form of turbidites into the deep sea. During the rise of the sea level a situation can be expected with a maximum area of the comparatively plane shelf being exposed to wave action. During this time the process of stirring up of sediments and formation of turbid layers will reach a maximum. Accordingly, the formation of turbidites and turbid layer sediments are most frequent at the same time. This happened in general in the older polstglacial period. The present day high water level results in a reduced supply of sediments into the canyons. The stirring up of sediments from the shelf by wave action is restricted to the finest material. The missing of shelf material in the uppermost core sections can thus be explained. The laminated muds reflect these calm sedimentation conditions as well. In the southwestern part of the area of investigation fine volcanic glass was blown in during the Pleistocene, probably from the southeast. It has thus become possible to correlate the cores 181, 182, 202. Eolian dust from the Indian subcontinent represents probably an important component of the deep sea sediments. The chemism of the bottom as well as of the pore water has a considerable influence on the development of the sediments. Of particular importance in this connection is a layer with a minimum content of oxygen in the sea water (200-1500 m), which today touches the upper part of the continental slope. Above and beyond this oxygen minimum layer somewhat higher O2-values are to be observed at the sea bottom. During the Pleistocene the oxygen minimum layer has obviously been locatedin greater depth as is indicated by the facies of laminated mud occuring in the lower part of core 219. The type of bioturbation is mainly determined by the chemism. Moreover, the chemism is responsible for a considerable selective dissolution, either complete or partial, of the sedimentary components. Within the range of the oxygen minimum layer an alkaline milieu is developed at the bottom. This causes a complete or partial dissolution of the siliceous organisms. Here, bioturbation is in general completely missing; sometimes small pyrite-filled burrowing racks are found. In the areas rich in O2 high pH-values result in a partial dissolution of the calcareous shells. Large, non-pyritized burrowing tracks characterize the type of bioturbation in this environment. A study of the "lebensspuren" in the cores supports the assumption that, particularly within the region of the Laccadive Basin, the oxygen content in the bottom sediments was lower than during the Holocene. This may be attributed to a high sedimentation rate and to a lower O2-content of the bottom water. The composition of the allochthonous sedimentary components, detritus and/or volcanic glass may locally change the chemism to a considerable extent for a certain time; under such special circumstances the type of bioturbation and the state of preservation of the components may be different from those of the normal sediment.

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Particulate matter export fuels benthic ecosystems in continental margins and the deep sea, removing carbon from the upper ocean. Gelatinous zooplankton biomass provides a fast carbon vector that has been poorly studied. Observational data of a large-scale benthic trawling survey from 1994 to 2005 provided a unique opportunity to quantify jelly-carbon along an entire continental margin in the Mediterranean Sea and to assess potential links with biological and physical variables. Biomass depositions were sampled in shelves, slopes and canyons with peaks above 1000 carcasses per trawl, translating to standing stock values between 0.3 and 1.4 mg C m2 after trawling and integrating between 30,000 and 175,000 m2 of seabed. The benthopelagic jelly-carbon spatial distribution from the shelf to the canyons may be explained by atmospheric forcing related with NAO events and dense shelf water cascading, which are both known from the open Mediterranean. Over the decadal scale, we show that the jelly-carbon depositions temporal variability paralleled hydroclimate modifications, and that the enhanced jelly-carbon deposits are connected to a temperature-driven system where chlorophyll plays a minor role. Our results highlight the importance of gelatinous groups as indicators of large-scale ecosystem change, where jelly-carbon depositions play an important role in carbon and energy transport to benthic systems.

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In the framework of the European Project for Ice Coring in Antarctica (EPICA), a comprehensive glaciological pre-site survey has been carried out on Amundsenisen, Dronning Maud Land, East Antarctica, in the past decade. Within this survey, four intermediate-depth ice cores and 13 snow pits were analyzed for their ionic composition and interpreted with respect to the spatial and temporal variability of volcanic sulphate deposition. The comparison of the non-sea-salt (nss)-sulphate peaks that are related to the well-known eruptions of Pinatubo and Cerro Hudson in AD 1991 revealed sulphate depositions of comparable size (15.8 ± 3.4 kg/km**2) in 11 snow pits. There is a tendency to higher annual concentrations for smaller snow-accumulation rates. The combination of seasonal sodium and annually resolved nss-sulphate records allowed the establishment of a time-scale derived by annual-layer counting over the last 2000 years and thus a detailed chronology of annual volcanic sulphate deposition. Using a robust outlier detection algorithm, 49 volcanic eruptions were identified between AD 165 and 1997. The dating uncertainty is ±3 years between AD 1997 and 1601, around ±5 years between AD 1601 and 1257, and increasing to ±24 years at AD 165, improving the accuracy of the volcanic chronology during the penultimate millennium considerably.

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The main objective of this study was to determine if isozyme systems can be used as markers of genetic deterioration in Brassicaceae seed accessions under different storage conditions. Seed samples of Brassica oleracea, Cardaria draba, Erysimum cheiri, Iberis sempervirens and Rapistrum rugosum were stored for periods of 9 to 30 years at -10°C and 3-4% seed moisture content (long-term or LT conditions) and at 5°C and uncontrolled relative humidity (RH) (short-term or ST conditions). Starch Gel Electrophoresis (SGE) was used to analyse six enzyme systems oriented to determine the genetic deterioration of the accessions studied. The results obtained show that long-term storage conditions (LT) were extremely effective in maintaining the viability of seeds of the five Brassicaceae species studied. The final germination percentages reached by seeds from LT samples ranged from 75 to 100%, while the germination percentages of ST samples (except for B. oleracea) were very low (from 0 to 10%). Similar conclusions were obtained studying the integrity of electrophoretic bands for several isozymes. Two enzyme systems were of special interest: malate dehydrogenase and alcohol dehydrogenase.

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Glutens, the storage proteins in wheat grains, are a major source of protein in human nutrition. The protein composition of wheat has therefore been an important focus of cereal research. Proteomic tools have been used to describe the genetic diversity of wheat germplasms from different origins at the level of polymorphisms in alleles encoding glutenin and gliadin, the two main proteins of gluten. More recently, proteomics has been used to understand the impact of specific gluten proteins on wheat quality. Here we review the impact of proteomics on the study of gluten proteins as it has evolved from fractionation and electrophoretic techniques to advanced mass spectrometry. In the postgenome era, proteomics is proving to be essential in the effort to identify and understand the interactions between different gluten proteins. This is helping to fill in gaps in our knowledge of how the technological quality of wheat is determined by the interaction between genotype and environment. We also collate information on the various storage protein alleles identified and their prevalence, which makes it possible to infer the effects of wheat selection on grain protein content. We conclude by reviewing the more recent use of transgenesis aimed at improving the quality of gluten.

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Recently, a novel method to trap and pattern ensembles of nanoparticles has been proposed and tested. It relies on the photovoltaic (PV) properties of certain ferroelectric crystals such as LiNbO3 [1,2]. These crystals, when suitably doped, develop very high electric fields in response to illumination with light of suitable wavelength. The PV effect lies in the asymmetrical excitation of electrons giving rise to PV currents and associated space-charge fields (photorefractive effect). The field generated in the bulk of the sample propagates to the surrounding medium as evanescent fields. When dielectric or metal nanoparticles are deposited on the surface of the sample the evanescent fields give rise to either electrophoretic or dielectrophoretic forces, depending on the charge state of the particles, that induce the trapping and patterning effects [3,4]. The purpose of this work has been to explore the effects of such PV fields in the biology and biomedical areas. A first work was able to show the necrotic effects induced by such fields on He-La tumour cells grown on the surface of an illuminated iron-doped LiNbO3 crystal [5]. In principle, it is conceived that LiNbO3 nanoparticles may be advantageously used for such biomedical purposes considering the possibility of such nanoparticles being incorporated into the cells. Previous experiments using microparticles have been performed [5] with similar results to those achieved with the substrate. Therefore, the purpose of this work has been to fabricate and characterize the LiNbO3 nanoparticles and assess their necrotic effects when they are incorporated on a culture of tumour cells. Two different preparation methods have been used: 1) mechanical grinding from crystals, and 2) bottom-up sol-gel chemical synthesis from metal-ethoxide precursors. This later method leads to a more uniform size distribution of smaller particles (down to around 50 nm). Fig. 1(a) and 1(b) shows SEM images of the nanoparticles obtained with both method. An ad hoc software taking into account the physical properties of the crystal, particullarly donor and aceptor concentrations has been developped in order to estimate the electric field generated in noparticles. In a first stage simulations of the electric current of nanoparticles, in a conductive media, due to the PV effect have been carried out by MonteCarlo simulations using the Kutharev 1-centre transport model equations [6] . Special attention has been paid to the dependence on particle size and [Fe2+]/[Fe3+]. First results on cubic particles shows large dispersion for small sizes due to the random number of donors and its effective concentration (Fig 2). The necrotic (toxicity) effect of nanoparticles incorporated into a tumour cell culture subjected to 30 min. illumination with a blue LED is shown in Fig.3. For each type of nanoparticle the percent of cell survival in dark and illumination conditions has been plot as a function of the particle dilution factor. Fig. 1a corresponds to mechanical grinding particles whereas 1b and 1c refer to chemically synthesized particles with two oxidation states. The light effect is larger with mechanical grinding nanoparticles, but dark toxicity is also higher. For chemically synthesized nanoparticles dark toxicity is low but only in oxidized samples, where the PV effect is known to be larger, the light effect is appreciable. These preliminary results demonstrate that Fe:LiNbO· nanoparticles have a biological damaging effect on cells, although there are many points that should be clarified and much space for PV nanoparticles optimization. In particular, it appears necessary to determine the fraction of nanoparticles that become incorporated into the cells and the possible existence of threshold size effects. This work has been supported by MINECO under grant MAT2011-28379-C03.

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Photovoltaic tweezers are a promising tool to place and move particles on the surface of a photovoltaic material in a controlled way. To exploit this new technique it is necessary to accurately know the electric field created by a specific illumination on the surface of the crystal and above it. This paper describes a numerical algorithm to obtain this electric field generated by several relevant light patterns, and uses them to calculate the electrophoretic potential acting over neutral, polarizable particles in the proximity of the crystal. The results are compared to experiments carried out in LiNbO3 with good overall agreement.

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The use of microsatellite markers in large-scale genetic studies is limited by its low throughput and high cost and labor requirements. Here, we provide a panel of 45 multiplex PCRs for fast and cost-efficient genome-wide fluorescence-based microsatellite analysis in grapevine. The developed multiplex PCRs panel (with up to 15-plex) enables the scoring of 270 loci covering all the grapevine genome (9 to 20 loci/chromosome) using only 45 PCRs and sequencer runs. The 45 multiplex PCRs were validated using a diverse grapevine collection of 207 accessions, selected to represent most of the cultivated Vitis vinifera genetic diversity. Particular attention was paid to quality control throughout the whole process (assay replication, null allele detection, ease of scoring). Genetic diversity summary statistics and features of electrophoretic profiles for each studied marker are provided, as are the genotypes of 25 common cultivars that could be used as references in other studies.

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El objetivo de esta tesis doctoral es la investigación del nuevo concepto de pinzas fotovoltaicas, es decir, del atrapamiento, ordenación y manipulación de partículas en las estructuras generadas en la superficie de materiales ferroeléctricos mediante campos fotovoltaicos o sus gradientes. Las pinzas fotovoltaicas son una herramienta prometedora para atrapar y mover las partículas en la superficie de un material fotovoltaico de una manera controlada. Para aprovechar esta nueva técnica es necesario conocer con precisión el campo eléctrico creado por una iluminación específica en la superficie del cristal y por encima de ella. Este objetivo se ha dividido en una serie de etapas que se describen a continuación. La primera etapa consistió en la modelización del campo fotovoltaico generado por iluminación no homogénea en substratos y guías de onda de acuerdo al modelo de un centro. En la segunda etapa se estudiaron los campos y fuerzas electroforéticas y dielectroforéticas que aparecen sobre la superficie de substratos iluminados inhomogéneamente. En la tercera etapa se estudiaron sus efectos sobre micropartículas y nanopartículas, en particular se estudió el atrapamiento superficial determinando las condiciones que permiten el aprovechamiento como pinzas fotovoltaicas. En la cuarta y última etapa se estudiaron las configuraciones más eficientes en cuanto a resolución espacial. Se trabajó con distintos patrones de iluminación inhomogénea, proponiéndose patrones de iluminación al equipo experimental. Para alcanzar estos objetivos se han desarrollado herramientas de cálculo con las cuales obtenemos temporalmente todas las magnitudes que intervienen en el problema. Con estas herramientas podemos abstraernos de los complicados mecanismos de atrapamiento y a partir de un patrón de luz obtener el atrapamiento. Todo el trabajo realizado se ha llevado a cabo en dos configuraciones del cristal, en corte X ( superficie de atrapamiento paralela al eje óptico) y corte Z ( superficie de atrapamiento perpendicular al eje óptico). Se ha profundizado en la interpretación de las diferencias en los resultados según la configuración del cristal. Todas las simulaciones y experimentos se han realizado utilizando como soporte un mismo material, el niobato de litio, LiNbO3, con el f n de facilitar la comparación de los resultados. Este hecho no ha supuesto una limitación en los resultados pues los modelos no se limitan a este material. Con respecto a la estructura del trabajo, este se divide en tres partes diferenciadas que son: la introducción (I), la modelización del atrapamiento electroforético y dielectroforético (II) y las simulaciones numéricas y comparación con experimentos (III). En la primera parte se fijan las bases sobre las que se sustentarán el resto de las partes. Se describen los efectos electromagnéticos y ópticos a los que se hará referencia en el resto de los capítulos, ya sea por ser necesarios para describir los experimentos o, en otros casos, para dejar constancia de la no aparición de estos efectos para el caso en que nos ocupa y justificar la simplificación que en muchos casos se hace del problema. En esta parte, se describe principalmente el atrapamiento electroforético y dielectroforético, el efecto fotovoltaico y las propiedades del niobato de litio por ser el material que utilizaremos en experimentos y simulaciones. Así mismo, como no debe faltar en ninguna investigación, se ha analizado el state of the art, revisando lo que otros científicos del campo en el que estamos trabajando han realizado y escrito con el fin de que nos sirva de cimiento a la investigación. Con el capítulo 3 finalizamos esta primera parte describiendo las técnicas experimentales que hoy en día se están utilizando en los laboratorios para realizar el atrapamiento de partículas mediante el efecto fotovoltaico, ya que obtendremos ligeras diferencias en los resultados según la técnica de atrapamiento que se utilice. En la parte I I , dedicada a la modelización del atrapamiento, empezaremos con el capítulo 4 donde modelizaremos el campo eléctrico interno de la muestra, para a continuación modelizar el campo eléctrico, los potenciales y las fuerzas externas a la muestra. En capítulo 5 presentaremos un modelo sencillo para comprender el problema que nos aborda, al que llamamos Modelo Estacionario de Separación de Carga. Este modelo da muy buenos resultados a pesar de su sencillez. Pasamos al capítulo 6 donde discretizaremos las ecuaciones que intervienen en la física interna de la muestra mediante el método de las diferencias finitas, desarrollando el Modelo de Distribución de Carga Espacial. Para terminar esta parte, en el capítulo 8 abordamos la programación de las modelizaciones presentadas en los anteriores capítulos con el fn de dotarnos de herramientas para realizar las simulaciones de una manera rápida. En la última parte, III, presentaremos los resultados de las simulaciones numéricas realizadas con las herramientas desarrolladas y comparemos sus resultados con los experimentales. Fácilmente podremos comparar los resultados en las dos configuraciones del cristal, en corte X y corte Z. Finalizaremos con un último capítulo dedicado a las conclusiones, donde resumiremos los resultados que se han ido obteniendo en cada apartado desarrollado y daremos una visión conjunta de la investigación realizada. ABSTRACT The aim of this thesis is the research of the new concept of photovoltaic or optoelectronic tweezers, i.e., trapping, management and manipulation of particles in structures generated by photovoltaic felds or gradients on the surface of ferroelectric materials. Photovoltaic tweezers are a promising tool to trap and move the particles on the surface of a photovoltaic material in a monitored way. To take advantage of this new technique is necessary to know accurately the electric field created by a specifc illumination in the crystal surface and above it. For this purpose, the work was divided into the stages described below. The first stage consisted of modeling the photovoltaic field generated by inhomogeneous illumination in substrates and waveguides according to the one-center model. In the second stage, electrophoretic and dielectrophoretic fields and forces appearing on the surface of substrates and waveguides illuminated inhomogeneously were studied. In the third stage, the study of its effects on microparticles and nanoparticles took place. In particular, the trapping surface was studied identifying the conditions that allow its use as photovoltaic tweezers. In the fourth and fnal stage the most efficient configurations in terms of spatial resolution were studied. Different patterns of inhomogeneous illumination were tested, proposing lightning patterns to the laboratory team. To achieve these objectives calculation tools were developed to get all magnitudes temporarily involved in the problem . With these tools, the complex mechanisms of trapping can be simplified, obtaining the trapping pattern from a light pattern. All research was carried out in two configurations of crystal; in X section (trapping surface parallel to the optical axis) and Z section (trapping surface perpendicular to the optical axis). The differences in the results depending on the configuration of the crystal were deeply studied. All simulations and experiments were made using the same material as support, lithium niobate, LiNbO3, to facilitate the comparison of results. This fact does not mean a limitation in the results since the models are not limited to this material. Regarding the structure of this work, it is divided into three clearly differentiated sections, namely: Introduction (I), Electrophoretic and Dielectrophoretic Capture Modeling (II) and Numerical Simulations and Comparison Experiments (III). The frst section sets the foundations on which the rest of the sections will be based on. Electromagnetic and optical effects that will be referred in the remaining chapters are described, either as being necessary to explain experiments or, in other cases, to note the non-appearance of these effects for the present case and justify the simplification of the problem that is made in many cases. This section mainly describes the electrophoretic and dielectrophoretic trapping, the photovoltaic effect and the properties of lithium niobate as the material to use in experiments and simulations. Likewise, as required in this kind of researches, the state of the art have been analyzed, reviewing what other scientists working in this field have made and written so that serve as a foundation for research. With chapter 3 the first section finalizes describing the experimental techniques that are currently being used in laboratories for trapping particles by the photovoltaic effect, because according to the trapping technique in use we will get slightly different results. The section I I , which is dedicated to the trapping modeling, begins with Chapter 4 where the internal electric field of the sample is modeled, to continue modeling the electric field, potential and forces that are external to the sample. Chapter 5 presents a simple model to understand the problem addressed by us, which is called Steady-State Charge Separation Model. This model gives very good results despite its simplicity. In chapter 6 the equations involved in the internal physics of the sample are discretized by the finite difference method, which is developed in the Spatial Charge Distribution Model. To end this section, chapter 8 is dedicated to program the models presented in the previous chapters in order to provide us with tools to perform simulations in a fast way. In the last section, III, the results of numerical simulations with the developed tools are presented and compared with the experimental results. We can easily compare outcomes in the two configurations of the crystal, in section X and section Z. The final chapter collects the conclusions, summarizing the results that were obtained in previous sections and giving an overview of the research.

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El principal objetivo de esta tesis fue incrementar la eficiencia proteica en las dietas de rumiantes mediante el uso de proteínas protegidas (harina de girasol y guisante de primavera), así como mejorar la predicción de los aportes de proteína microbiana. Una partida de harinas comerciales de girasol (HG) y de guisante de primavera (GP) fueron tratadas con soluciones 4 N de ácido málico (268,2 g/L) o ácido ortofosfórico (130,6 g/L). Para cada harina, ácido y día de tratamiento, dos fracciones de 12,5 kg fueron pulverizadas sucesivamente en una hormigonera con la solución de ácido correspondiente mediante un pulverizador de campo. Las dos fracciones fueron mezcladas posteriormente y se dejaron reposar durante 1 h a temperatura ambiente. La mezcla fue luego secada en una estufa de aire forzado a 120 ºC durante 1 h. La estufa fue apagada inmediatamente después y el material tratado se mantuvo dentro de ésta hasta la mañana siguiente. El material fue removido durante el proceso de secado cada 30 min durante las primeras 2 h y cada 60 min durante las 5 h posteriores. Este proceso se repitió hasta conseguir las cantidades de harinas tratadas necesarias en los distintos ensayos. En el primer experimento (capitulo 3) se llevaron a cabo estudios de digestión ruminal e intestinal para evaluar los efectos de la aplicación de las soluciones ácidas indicadas y calor a fin de proteger las proteínas de HG y GP contra la degradación ruminal. Estos estudios se realizaron con tres corderos canulados en el rumen y en el duodeno. El estudio de digestión ruminal fue realizado en tres periodos experimentales en los que los corderos fueron alimentados sucesivamente con tres dietas isoproteicas que incluían HG y GP, sin tratar o tratadas con ácidos málico u ortofosfórico. Cada periodo experimental de 21 días incluyó sucesivamente: 10 días de adaptación a las dietas, un estudio del tránsito ruminal de las partículas de HG y GP (días 11 a 14), y la incubación de las muestras de ambos alimentos en bolsas de nailon (días 15–21). Las harinas incubadas en cada periodo experimental correspondieron a las que fueron incluidas en las dietas. Las bacterias ruminales fueron marcadas desde el día 11 hasta el día 21 del periodo experimental mediante infusión intra-ruminal continua con una fuente de 15N. Tras finalizar las incubaciones in situ el día 21 el rumen fue vaciado en cada periodo para aislar las bacterias asociadas a la fase sólida y liquida del rumen. El estudio de digestión intestinal fue realizado veinte días después del final del estudio ruminal a fin de eliminar el enriquecimiento en 15N de la digesta. En este estudio se incubaron muestras compuestas obtenidas mediante la combinación de los diferentes residuos no degradados en el rumen de forma que fuesen representativas de la composición química de la fracción no degradada en el rumen (RU). En esta fase los corderos fueron alimentados con la dieta sin tratar para determinar la digestibilidad de las harinas tanto tratadas como sin tratar mediante la técnica de las bolsas móviles. Además, las proteínas contenidas en las harinas tratadas y sin tratar, así como en las muestras correspondientes a los residuos a 0 h, las muestras compuestas anteriormente indicadas y las muestras no digeridas intestinalmente fueron extraídas y sometidas a electroforesis para determinar el sitio de digestión de las diferentes fracciones proteicas. Las estimaciones de la RU y la digestibilidad intestinal de la materia seca, la materia orgánica (solamente para RU), la proteína bruta (PB) y el almidón (solamente en GP) fueron obtenidos considerando la contaminación microbiana y las tasas de conminución y salida de partículas. Las estimaciones de RU y de la digestibilidad intestinal disminuyeron en todas las fracciones evaluadas de ambos alimentos al corregir por la contaminación microbiana acaecida en el rumen. Todas las estimaciones de RU aumentaron con los tratamientos de protección, incrementándose también la digestibilidad intestinal de la materia seca en la HG. Los bajos valores de la digestibilidad de la proteína de GP tratado y sin tratar sugieren la presencia de algún factor antitripsico no termolábil es esta harina. Los tratamientos de protección incrementaron consistentemente la fracción de materia seca y PB digerida intestinalmente en los dos alimentos, mientras que la fracción de almidón en la muestra de GP solamente aumentó numéricamente (60,5% de media). Sin embargo, los tratamientos también redujeron la fermentación de la materia orgánica, lo cual podría disminuir la síntesis de proteína microbiana. Los estudios de electroforesis muestran la práctica desaparición de la albumina por la degradación ruminal en ambos alimentos, así como que los cambios en otras proteínas de la muestra RU fueron más pronunciados en GP que en HG. La composición de las bacterias asociadas con las fases de digesta ruminal sólida (BAS) y líquida (BAL) fue estudiada para revisar la precisión de un sistema de predicción previo que determinaba la infravaloración del aporte de nutrientes correspondiente a las BAS cuando de usa 15N como marcador y las BAL como referencia microbiana (capitulo 4). Al comparar con BAS, BAL mostraron menores contenidos en materia orgánica, polisacáridos de glucosa y lípidos totales y un mayor contenido en PB, así como un mayor enriquecimiento en 15N. Los datos obtenidos en el estudio actual se ajustan bien a la ecuación previa que predice el enriquecimiento en 15N de las BAS a partir del mismo valor en BAL. Esta nueva ecuación permite establecer que se produce una infravaloración de un 22% en el aporte de PB al animal a partir de las BAS sintetizadas si las BAL son usadas como muestras de referencia. Una segunda relación calculada utilizando los valores medios por dieta expuestos en numerosos trabajos encontrados en la literatura confirma la magnitud de este error. Esta infravaloración asociada al uso de BAL como referencia fue mayor para el aporte de glucosa (43,1%) y todavía mayor para el aporte de lípidos (59,9%), como consecuencia de los menores contenidos de ambas fracciones en BAL frente a SAB. Estos errores deberían ser considerados para obtener mayor precisión en la estimación del aporte de nutrientes microbianos y mejorar la nutrición de los rumiantes. En el experimento 2 se realizó un estudio de producción (capitulo 5) para evaluar los efectos del tratamiento de las harinas HG y GP con soluciones de ácido málico o ácido ortofosfórico sobre el crecimiento, el consumo de concentrado y el rendimiento y engrasamiento de las canales de corderos de engorde. Noventa corderos machos de cruce entrefino procedentes de tres granjas comerciales (peso inicial medio = 14,6, 15,3 y 13,3 kg, respectivamente) fueron asignados aleatoriamente a cinco dietas con diferentes niveles de proteína y diferentes tratamientos con ácidos y engordados hasta un peso medio al sacrificio de 25 kg. Las fuentes de proteína en el pienso control (C; PB=18,0%) fueron harina de soja, HG y GP sin tratar. En tres de los piensos experimentales, las harinas tratadas con ácido ortofosfórico sustituyeron a las de HG y GP sin tratar (Control Ortofosfórico, PC; PB=18,0% sobre materia seca), sustituyéndose, además, la harina de soja parcialmente (Sustitución Media Ortofosfórico, MSP; PB=16,7%) o totalmente (Sustitución Total Ortofosfórico, TSP; PB=15,6%). Finalmente, en uno de los piensos el ácido ortofosfórico fue reemplazo por acido málico para proteger ambas harinas (Sustitución Media Málico, MSM; PB= 16,7%). La paja de trigo (fuente de forraje) y el concentrado fueron ofrecidos ad libitum. Dieciocho corderos fueron distribuidos en seis cubículos con tres animales para cada dieta. Los datos fueron analizados según un análisis factorial considerando el peso inicial como covariable y la granja de procedencia como bloque. Los datos de consumo de concentrado y eficiencia de conversión fueron analizados usando el cubículo como unidad experimental, mientras que los datos sobre ganancia media diaria, rendimiento a la canal, grasa dorsal y grasa pélvico renal fueron analizados usando el cordero como unidad experimental. No se encontró ningún efecto asociado con el nivel de PB sobre ninguna variable estudiada. Esto sugiere que usando proteínas protegidas es posible utilizar concentrados con 15,6% de PB (sobre materia seca) disminuyendo así la cantidad de concentrados de proteína vegetal a incluir en los piensos y la calidad de los concentrados proteicos. Los corderos alimentados con la dieta MSM tuvieron mayores ganancias medias diarias (15,2%; P= 0,042), y mejores rendimiento a la canal en caliente (1,3 unidades porcentuales; P= 0,037) que los corderos alimentados con el concentrado MSP. Esto podría ser explicado por los efectos benéficos ruminales del malato o por el mayor efecto de protección conseguido con el ácido málico. ABSTRACT The main objective of this thesis project was to increase the protein efficiency in ruminant diets by using protected protein (sunflower meal and spring pea), and improving the prediction of microbial protein supply. Commercial sunflower meal (SFM) and spring pea (SP) were treated with 4 N solutions (200 mL/kg) of malic acid (268.2 g/L) or orthophosphoric acid (130.6 g/L). Daily, two fractions of 12.5 kg of one of these meals were successively sprayed with the tested acid solution in a concrete mixer using a sprayer. Both fractions were then mixed and allowed to rest for 1 h at room temperature. The blend was then dried in a forced air oven at 120 ºC for 1 h. Then the oven was turned off and the treated material was left in the oven overnight. During the drying process, the material was stirred every 30 min during the first 2 h and then every 60 min for the subsequent 5 h. This process was repeated until the amounts of treated flour needed for the different trials performed. In the first experiment (chapter 3), ruminal and intestinal digestion trials were conducted to study the effects of the application of these acid solutions and heat to protect proteins of SFM and SP against ruminal degradation using three wethers fitted with rumen and duodenum cannulae. The ruminal digestion study was carried out in three experimental periods in which the wethers were successively fed three isoproteic diets including SFM and SP, untreated or treated with malic or orthophosphoric acids. The experimental periods of 21 days included successively: 10 days of diet adaptation, SFM and SP particle ruminal transit study (days 11–14) and ruminal nylon-bag incubations (days 15–21). The meals incubated in each experimental period were those corresponding to the associated diet. Rumen bacteria were labelled from days 11 to 21 by continuous intra-ruminal infusion of a 15N source and the rumen was emptied at the end of in situ incubations in each period to isolate solid adherent bacteria and liquid associate bacteria. The intestinal digestion trial was conducted twenty days after the end of the ruminal studies to eliminate the 15N enrichment in the digesta. The tested samples were composite samples obtained pooling the different ruminally undegraded residues to be representative of the chemical composition of the ruminally undegraded fraction (RU). Wethers were fed the untreated diet to determine the intestinal digestibility of untreated and treated meals using the mobile nylon bag technique. In addition, protein in untreated and treated meals and their 0 h, composite and intestinally undigested samples were extracted and subjected to electrophoresis to determine the digestion site of the different protein fractions. Estimates of the RU and its intestinal digestibility of dry matter, organic matter (only for RU), crude protein (CP) and starch (only in SP) were obtained considering ruminal microbial contamination and particle comminution and outflow rates. When corrected for the microbial contamination taking place in the rumen, estimates of RU and intestinal digestibility decreased in all tested fractions for both feeds. All RU estimates increased with the protective treatments, whereas intestinal digestibility-dry matter also increased in SFM. Low intestinal digestibility-CP values in untreated and treated samples suggested the presence of non-heat labile antitrypsin factors in SP. Protective treatments of both feeds led to consistent increases in the intestinal digested fraction of dry matter and CP, being only numerically different for SP-starch (60.5% as average). However, treatments also reduced the organic matter fermentation, which may decrease ruminal microbial protein synthesis. Electrophoretic studies showed albumin disappearance in both SFM and SP, whereas changes in other RU proteins were more pronounced in SP than SFM. The chemical composition of bacteria associated with solid (SAB) and liquid (LAB) rumen-digesta phases was studied to examine the accuracy of a previous regression system determining the underevaluation of SAB-nutrient supply using 15N as marker and LAB as microbial reference (chapter 4). Compared with SAB, LAB showed lower contents of organic matter, polysaccharide-glucose and total lipids and the opposite for the CP content and the 15N enrichment. Present data fitted well to the previous relationship predicting the 15N enrichment of SAB from the same value in LAB. This new equation allows establishing an underevaluation in the supply of CP from the synthesized SAB in 22.0% if LAB is used as reference. Another relationship calculated using mean diet values from the literature confirmed the magnitude of this error. This underevaluation was higher for the supply of glucose (43.1%) and still higher for the lipid supply (59.9%) as a consequence of the lower contents of these both fractions in LAB than in SAB. These errors should be considered to obtain more accurate estimates of the microbial nutrient supply and to improve ruminant nutrition. A production study was performed in experiment 2 (chapter 5) to examine the effects of treating SFM and SP meals with orthophosphoric or malic acid solutions on growth performance, concentrate intake, and carcass yield and fatness of growing-fattening lambs. Ninety "Entrefino" cross male lambs from three commercial farms (average initial body weights (BW) = 14.6, 15.3 and 13.3 kg) were randomly assigned to five diets with different acid treatment and protein levels, and fattened to an average slaughter weight of 25 kg. Protein sources in the control concentrate (C; CP=18%) were soybean meal and untreated SFM and SP. In three of the experimental concentrates, orthophosphoric acid-treated meals substituted untreated SFM and SP (Orthophosphoric Control, PC; CP=18% dry matter basis), and soybean meal was partially (Medium Substitution Orthophosphoric, MSP; CP=16.7%) or totally removed (Total Substitution Orthophosphoric, TSP; CP=15.6%). In addition, in one concentrate orthophosphoric acid was replaced by malic acid to protect these meals (Medium Substitution Malic, MSM; CP= 16.7%). Wheat straw (roughage source) and concentrate were offered ad libitum. Eighteen lambs were allocated to six pens of three animals on each diet. Data were analyzed using a factorial analysis with initial body weight BW as covariate and farm of origin as block. Data on concentrate intake and feed conversion efficiency were analyzed using pen as experimental unit, while data on average daily gain, carcass yield, dorsal fat, and kidney-pelvic-fat were analyzed with lamb as experimental unit. No effect associated with the CP level was observed on any parameter. This suggests that with protected proteins it is possible to feed concentrates with 15.6% CP (dry matter basis) reducing the quantity of vegetable protein meals to include in the concentrate as well as the quality of the protein concentrates. Lambs feed MSM had higher average daily gains (15.2%; P= 0.042), and better hot carcass yields (1.3 percentage points; P= 0.037) than lambs feed MSP. This probably can be explained by ruminal malate actions and by greater protection effects obtained with malic acid.

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La presente tesis revisa y analiza algunos aspectos fundamentales relativos al comportamiento de los sensores basados en resonadores piezoeléctricos TSM (Thickness Shear Mode), así como la aplicación de los mismos al estudio y caracterización de dos medios viscoelásticos de gran interés: los fluidos magnetoreológicos y los biofilms microbianos. El funcionamiento de estos sensores está basado en la medida de sus propiedades resonantes, las cuales varían al entrar en contacto con el material que se quiere analizar. Se ha realizado un análisis multifrecuencial, trabajando en varios modos de resonancia del transductor, en algunas aplicaciones incluso de forma simultánea (excitación pulsada). Se han revisado fenómenos como la presencia de microcontactos en la superficie del sensor y la resonancia de capas viscoelásticas de espesor finito, que pueden afectar a los sensores de cuarzo de manera contraria a lo que predice la teoría convencional (Sauerbrey y Kanazawa), pudiéndonos llevar a incrementos positivos de la frecuencia de resonancia. Además, se ha estudiado el efecto de una deposición no uniforme sobre el resonador piezoeléctrico. Para ello se han medido deposiciones de poliuretano, modelándose la respuesta del resonador con estas deposiciones mediante FEM. El modelo numérico permite estudiar el comportamiento del resonador al modificar distintas variables geométricas (espesor, superficie, no uniformidad y zona de deposición) de la capa depositada. Se ha demostrado que para espesores de entre un cuarto y media longitud de onda aproximadamente, una capa viscoelástica no uniforme sobre la superficie del sensor, amplifica el incremento positivo del desplazamiento de la frecuencia de resonancia en relación con una capa uniforme. Se ha analizado también el patrón geométrico de la sensibilidad del sensor, siendo también no uniforme sobre su superficie. Se han aplicado sensores TSM para estudiar los cambios viscoelásticos que se producen en varios fluidos magneto-reológicos (FMR) al aplicarles distintos esfuerzos de cizalla controlados por un reómetro. Se ha podido ver que existe una relación directa entre diversos parámetros reológicos obtenidos con el reómetro (fuerza normal, G’, G’’, velocidad de deformación, esfuerzo de cizalla…) y los parámetros acústicos, caracterizándose los FMR tanto en ausencia de campo magnético, como con campo magnético aplicado a distintas intensidades. Se han estudiado las ventajas que aporta esta técnica de medida sobre la técnica basada en un reómetro comercial, destacando que se consigue caracterizar con mayor detalle algunos aspectos relevantes del fluido como son la deposición de partículas (estabilidad del fluido), el proceso de ruptura de las estructuras formadas en los FMR tanto en presencia como en ausencia de campo magnético y la rigidez de los microcontactos que aparecen entre partículas y superficies. También se han utilizado sensores de cuarzo para monitorear en tiempo real la formación de biofilms de Staphylococcus epidermidis y Eschericia coli sobre los propios resonadores de cristal de cuarzo sin ningún tipo de recubrimiento, realizándose ensayos con cepas que presentan distinta capacidad de producir biofilm. Se mostró que, una vez que se ha producido una primera adhesión homogénea de las bacterias al sustrato, podemos considerar el biofilm como una capa semi-infinita, de la cual el sensor de cuarzo refleja las propiedades viscoelásticas de la región inmediatamente contigua al resonador, no siendo sensible a lo que sucede en estratos superiores del biofilm. Los experimentos han permitido caracterizar el módulo de rigidez complejo de los biofilms a varias frecuencias, mostrándose que el parámetro característico que indica la adhesión de un biofilm tanto en el caso de S. epidermidis como de E. coli, es el incremento de G’ (relacionado con la elasticidad o rigidez de la capa), el cual viene ligado a un incremento de la frecuencia de resonancia del sensor. ABSTRACT This thesis reviews and analyzes some key aspects of the behavior of sensors based on piezoelectric resonators TSM (Thickness Shear Mode) and their applications to the study and characterization in two viscoelastic media of great interest: magnetorheological fluids and microbial biofilms. The operation of these sensors is based on the analysis of their resonant properties that vary in contact with the material to be analyzed. We have made a multi-frequency analysis, working in several modes of resonance of the transducer, in some applications even simultaneously (by impulse excitation). We reviewed some phenomena as the presence of micro-contacts on the sensor surface and the resonance of viscoelastic layers of finite thickness, which can affect quartz sensors contrary to the conventional theory predictions (Sauerbrey and Kanazawa), leading to positive resonant frequency shifts. In addition, we studied the effect of non-uniform deposition on the piezoelectric resonator. Polyurethane stools have been measured, being the resonator response to these depositions modeled by FEM. The numerical model allows studying the behavior of the resonator when different geometric variables (thickness, surface non-uniformity and deposition zone) of the deposited layer are modified. It has been shown that for thicknesses between a quarter and a half of a wavelength approximately, non-uniform deposits on the sensor surface amplify the positive increase of the resonance frequency displacement compared to a uniform layer. The geometric pattern of the sensor sensitivity was also analyzed, being also non-uniform over its surface. TSM sensors have been applied to study the viscoelastic changes occurring in various magneto-rheological fluids (FMR) when subjected to different controlled shear stresses driven by a rheometer. It has been seen that there is a direct relationship between various rheological parameters obtained with the rheometer (normal force, G', G'', stress, shear rate ...) and the acoustic parameters, being the FMR characterized both in the absence of magnetic field, and when the magnetic field was applied at different intensities. We have studied the advantages of this technique over the characterization methods based on commercial rheometers, noting that TSM sensors are more sensitive to some relevant aspects of the fluid as the deposition of particles (fluid stability), the breaking process of the structures formed in the FMR both in the presence and absence of magnetic field, and the rigidity of the micro-contacts appearing between particles and surfaces. TSM sensors have also been used to monitor in real time the formation of biofilms of Staphylococcus epidermidis and Escherichia coli on the quartz crystal resonators themselves without any coating, performing tests with strains having different ability to produce biofilm. It was shown that, once a first homogeneous adhesion of bacteria was produced on the substrate, the biofilm can be considered as a semi-infinite layer and the quartz sensor reflects only the viscoelastic properties of the region immediately adjacent to the resonator, not being sensitive to what is happening in upper layers of the biofilm. The experiments allow the evaluation of the biofilm complex stiffness module at various frequencies, showing that the characteristic parameter that indicates the adhesion of a biofilm for the case of both S. epidermidis and E. coli, is an increased G' (related to the elasticity or stiffness of the layer), which is linked to an increase in the resonance frequency of the sensor.

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The effects of solutions of malic or orthophosphoric acids (0.752 Eqg/kg of feed) and heat to protect proteins of sunflower meal (SFM) and spring pea (SP) against ruminal degradation were studied using particle transit, 15N infusion, in situ and electrophoretic techniques. Three wethers fitted with rumen and duodenum cannulae were successively fed three isoproteic diets including SFM and SP, untreated or treated with malic or orthophosphoric acids. Incubations of tested meals were only performed while feeding the respective diet. Estimates of the ruminally undegraded fraction (RU) and its intestinal digestibility of dry matter, organic matter (only for RU), crude protein and starch (only in SP) were obtained considering ruminal microbial contamination and particle comminution and outflow rates. When corrected for microbial contamination, estimates of RU and intestinal digestibility decreased in all tested fractions for both feeds. All RU estimates increased with the protective treatments, whereas intestinal digestibility-dry matter also increased in SFM. Low intestinal digestibility-crude protein values suggested the presence of antitrypsin factors in SP. Protective treatments of both feeds led to consistent increases in the intestinal digested fraction of dry matter and crude protein, being only numerically different for SP-starch (60.5% as average). However, treatments also reduced the organic matter fermentation, which may decrease ruminal microbial protein synthesis. Electrophoretic studies showed albumin disappearance in both SFM and SP, whereas changes in other RU proteins were more pronounced in SP than SFM.

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Charles Hamilton Houston and other NAACP attorneys assembled in early October 1939 to take depositions in preparation for the hearing scheduled a week later in Columbia to determine whether the university had complied with the Gaines decision. Attorneys took depositions from all of the instructors of the new LU law school as their preparation for the court proceedings wound down. The deposition of Lloyd Gaines was next. Attorneys planned to ask Gaines whether he considered Lincoln to be as good of a law school as Missouri and whether he planned to enroll. Called for questioning, Gaines did not respond. He could not be located anywhere. Lloyd’s mother, Callie Gaines, recalled that in January her son “left here to go to Kansas City to make a speech. That’s the last I saw of him.” While in Kansas City, Gaines spoke at the Centennial Methodist Church. He also looked for work, but not finding any caught a train for Chicago, telling people in Kansas City that he would stay a few days and return home.

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BRUNELLI, Conceição Aparecida Garcia: Gênero, raça, discriminação: o tom da cor na direção da escola pública. Mestrado em Educação. Universidade Metodista de São Paulo, São Bernardo do Campo - SP. 1 v. 244 p. 2007. Esse trabalho teve por objetivo investigar a trajetória das mulheres negras diretoras de escola pública e o processo de construção de sua identidade social, cultural, de gênero e raça. De fato, as mulheres negras em questão constroem suas identidades nadando entre águas profundas e revoltas: a das relações de gênero e a das relações raciais. A pesquisa permitiu-nos desvendar o processo seletivo pelo qual passam essas mulheres que conseguiram romper o duplo bloqueio formado pelas relações de gênero e de raça e atingiram a posição profissional de diretoras de escola pública. A questão central que norteia essa pesquisa diz respeito à trajetória de vida da mulher negra que optou pela carreira do magistério, as intercorrências encontradas ao longo de sua trajetória pessoal, de formação acadêmica e profissional, suas experiências, frustrações, expectativas, preconceitos e discriminações sofridos na caminhada até chegar ao exercício de sua atividade pública, sua ascensão social, o ingresso na carreira pública e as relações de poder que perpassam as questões de gênero e raça. Aborda ainda como essas intercorrências incidem sobre o processo de construção da identidade dessas mulheres negras e de suas relações com seus colegas brancos, homens e mulheres. A coleta de dados empíricos foi realizada através da história oral representada pela memória dessas mulheres, baseada nos depoimentos escritos e em entrevistas semi-estruturadas. Os depoimentos colhidos permitiram reunir material que foram interpretados segundo as relações de poder elaboradas por Foucault e que nos possibilitam a compreensão e uma reflexão do processo de construção das identidades individual e coletiva.

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BRUNELLI, Conceição Aparecida Garcia: Gênero, raça, discriminação: o tom da cor na direção da escola pública. Mestrado em Educação. Universidade Metodista de São Paulo, São Bernardo do Campo - SP. 1 v. 244 p. 2007. Esse trabalho teve por objetivo investigar a trajetória das mulheres negras diretoras de escola pública e o processo de construção de sua identidade social, cultural, de gênero e raça. De fato, as mulheres negras em questão constroem suas identidades nadando entre águas profundas e revoltas: a das relações de gênero e a das relações raciais. A pesquisa permitiu-nos desvendar o processo seletivo pelo qual passam essas mulheres que conseguiram romper o duplo bloqueio formado pelas relações de gênero e de raça e atingiram a posição profissional de diretoras de escola pública. A questão central que norteia essa pesquisa diz respeito à trajetória de vida da mulher negra que optou pela carreira do magistério, as intercorrências encontradas ao longo de sua trajetória pessoal, de formação acadêmica e profissional, suas experiências, frustrações, expectativas, preconceitos e discriminações sofridos na caminhada até chegar ao exercício de sua atividade pública, sua ascensão social, o ingresso na carreira pública e as relações de poder que perpassam as questões de gênero e raça. Aborda ainda como essas intercorrências incidem sobre o processo de construção da identidade dessas mulheres negras e de suas relações com seus colegas brancos, homens e mulheres. A coleta de dados empíricos foi realizada através da história oral representada pela memória dessas mulheres, baseada nos depoimentos escritos e em entrevistas semi-estruturadas. Os depoimentos colhidos permitiram reunir material que foram interpretados segundo as relações de poder elaboradas por Foucault e que nos possibilitam a compreensão e uma reflexão do processo de construção das identidades individual e coletiva.