Petrologia e geoquímica do magmatismo ediacarano Serra do Caramuru, Rio Grande do Norte, NE do Brasil

The Serra do Caramuru and Tapuio stocks, located in the extreme NE of Rio Piranhas-Seridó Domain (RN), are representative of the Ediacaran-Cambrian magmatism, an important magmatic feature of the Brasilian / Panafrican orogeny of the Borborema Province. These bodies are lithologically similar, intrusive in paleoproterozoic gneiss embasement, being separated by a thin belt of mylonitic orthogneiss. The field relations show a magmatic stratigraphy initiated by dioritic facies that coexists with the porphyritic granitic and equigranular granitic I facies, and less frequently with equigranular granitic II facies. These rocks are crosscut by late granitic dykes and sheets with NE-SW / NNE-SSW orientation. The dioritic facies (diorite, quartz diorite, quartz monzodiorites, tonalite and granodiorite) is leucocratic to melanocratic, rich in biotite and hornblende. The granitic facies are hololeucocratic to leucocratic, and have biotite ± hornblende. Petrographic and geochemical (whole rock) data, especially from Serra do Caramuru pluton, suggest fractionation of zircon, apatite, clinopyroxene (in diorites), opaque minerals, titanite, biotite, hornblende, allanite, plagioclase, microcline and garnet (in dykes). The behavior of trace elements such as Zr, La and Yb indicates that the dioritic magma does not constitute the parental magma for the granitic facies. On the other hand, the granitic facies seems to be cogenetic to each other, displaying differentiation trends and very similar rare earth elements (REE) spectra [12.3≤(La/Yb)N≤190.8; Eu/Eu*=0.30-0.68]. Field relationships and REE patterns [6.96≤(La/Yb)N≤277.8; Eu/Eu*=0.18-0.58] demonstrate that the granitic dykes and sheets are not cogenetically related to the Serra do Caramuru magmatism. The dioritic facies is metaluminous (A/CNK = 0.88-0.74) and shoshonitic, whereas the granitic ones are metaluminous to peraluminous (A/CNK = 1.08-0.93) and high potassium calc-alkaline. Dykes and sheets are strictly peraluminous (A/CNK = 1.01-1.04). Binary diagrams relating compatible and incompatible trace elements and microtextures indicate the fractional crystallization as the dominant mechanism of magmatic evolution of the various facies. The Serra do Caramuru and Tapuio stocks have well preserved magmatic fabric, do not show metamorphic minerals and are structurally isotropic, showing crosscutting contact with the ductile fabric of the basement. These observations lead to interpretate a stage of relative tectonic stability, consistent with the orogenic relaxation period of the Brasiliano / Pan-African orogeny. Chemical plots involving oxides and trace elements indicate late to post-collisional emplacement. In this context, the assumed better mechanism to describe the stocks emplacement within an extensional T Riedel joint, with ENE-WSW extensional vector. The U-Pb zircon age of 553 ± 10 Ma allows correlating the Serra do Caramuru magmatism to the group of post-collisional bodies, equigranular high potassium calc-alkaline granites of the NE of Rio Piranhas-Seridó Domain.

Petrologia e geoquímica do magmatismo ediacarano Serra do Caramuru, Rio Grande do Norte, NE do Brasil

The Serra do Caramuru and Tapuio stocks, located in the extreme NE of Rio Piranhas-Seridó Domain (RN), are representative of the Ediacaran-Cambrian magmatism, an important magmatic feature of the Brasilian / Panafrican orogeny of the Borborema Province. These bodies are lithologically similar, intrusive in paleoproterozoic gneiss embasement, being separated by a thin belt of mylonitic orthogneiss. The field relations show a magmatic stratigraphy initiated by dioritic facies that coexists with the porphyritic granitic and equigranular granitic I facies, and less frequently with equigranular granitic II facies. These rocks are crosscut by late granitic dykes and sheets with NE-SW / NNE-SSW orientation. The dioritic facies (diorite, quartz diorite, quartz monzodiorites, tonalite and granodiorite) is leucocratic to melanocratic, rich in biotite and hornblende. The granitic facies are hololeucocratic to leucocratic, and have biotite ± hornblende. Petrographic and geochemical (whole rock) data, especially from Serra do Caramuru pluton, suggest fractionation of zircon, apatite, clinopyroxene (in diorites), opaque minerals, titanite, biotite, hornblende, allanite, plagioclase, microcline and garnet (in dykes). The behavior of trace elements such as Zr, La and Yb indicates that the dioritic magma does not constitute the parental magma for the granitic facies. On the other hand, the granitic facies seems to be cogenetic to each other, displaying differentiation trends and very similar rare earth elements (REE) spectra [12.3≤(La/Yb)N≤190.8; Eu/Eu*=0.30-0.68]. Field relationships and REE patterns [6.96≤(La/Yb)N≤277.8; Eu/Eu*=0.18-0.58] demonstrate that the granitic dykes and sheets are not cogenetically related to the Serra do Caramuru magmatism. The dioritic facies is metaluminous (A/CNK = 0.88-0.74) and shoshonitic, whereas the granitic ones are metaluminous to peraluminous (A/CNK = 1.08-0.93) and high potassium calc-alkaline. Dykes and sheets are strictly peraluminous (A/CNK = 1.01-1.04). Binary diagrams relating compatible and incompatible trace elements and microtextures indicate the fractional crystallization as the dominant mechanism of magmatic evolution of the various facies. The Serra do Caramuru and Tapuio stocks have well preserved magmatic fabric, do not show metamorphic minerals and are structurally isotropic, showing crosscutting contact with the ductile fabric of the basement. These observations lead to interpretate a stage of relative tectonic stability, consistent with the orogenic relaxation period of the Brasiliano / Pan-African orogeny. Chemical plots involving oxides and trace elements indicate late to post-collisional emplacement. In this context, the assumed better mechanism to describe the stocks emplacement within an extensional T Riedel joint, with ENE-WSW extensional vector. The U-Pb zircon age of 553 ± 10 Ma allows correlating the Serra do Caramuru magmatism to the group of post-collisional bodies, equigranular high potassium calc-alkaline granites of the NE of Rio Piranhas-Seridó Domain.

Aditivo polimérico derivado de fonte renovável para aplicação em cimento asfáltico de petróleo

This study evaluated the effects of incorporating an additive from an agro-industrial residue, after some chemical modification reactions, to petroleum asphalt cement (CAP) through the polymerization reaction of a viscous polyol obtained by bagasse biomass oxypropylation reaction sugarcane with anhydrides. The polyol is obtained by biomass oxypropylation reaction with propylene oxide, the reaction was performed in an autoclave sealed with pressure and temperature control using 25 mL of OP for every 5 grams of biomass 200°C, which time reaction was two hours. The reaction is revealed by varying the system pressure, initially at atmospheric pressure to reach a maximum pressure value and its subsequent return to atmospheric pressure. For the choice of the most suitable reaction time for polymerization of the polyol with pyromellitic anhydride, the reaction was also conducted in an autoclave sealed with temperature controller (150 ° C) using 20 g of polyol, 1 g of sodium acetate (catalyst) and 8 g of pyromellitic anhydride with the times 30 and 60 minutes. The polymerized materials with different times were characterized by determining the relative viscosity and percentage content of extractable in cyclohexane / ethanol. Given the results with the polymerized material 30 minutes showed the lowest percentage content of extractives and an increased viscosity relative indicating that this time is highlighted with respect to time 60 minutes, because the material is possibly in the form of a crosslinked polymer. Given the choice of time of 30 minutes other polymerization reactions were performed with various anhydrides and other conditions employed different proportions by mass of polyol anhydrides we were referred to as condition I (20 g anhydride and 8 g of polyol), II (20 g anhydride and 20 g of polyol) and III (8 g anhydride and 20 g of polyol). The FTIR spectra of polymeric materials with different polymerization conditions used to prove the occurrence of chemical modification due to the appearance of a characteristic band ester groups (1750 cm-1) present in the polymerized material. He chose to work with the condition III, as is the condition which employs a larger amount of polyol, and even with the smaller amount of anhydride used FTIR spectra revealed that the polymerization reaction was performed. Among the various anhydrides (phthalic, maleic and pyromellitic) of the different conditions used that stood out before the solubility test with solvents analyzed was polymerized material with pyromellitic anhydride because the polymerized material likely in the form of a crosslinked polymer because it was insoluble or poorly soluble in the solvents tested. Polymerization of the polyol with pyromellitic anhydride using condition III, that is, BCPP30, CSPP30, PCPP30 e BCPPG30, provided an increase in thermal stability relative to material in the form of polyol. Applicability tests concerning the incorporation of 16% m / m BCPP30, CSPP30, PCPP30 e BCPPG30 additive in relation to the mass of 600 g CAP showed through characterization tests used, softening point, elastic recovery and marshall dosage, it is possible to use BCPP30 as an additive the conventional CAP, because even with the incorporation of this new additive modified CAP met the specifications of the appropriate standard.

Simulação computacional de materiais bidimensionais: funcionalização de defeitos extensos no grafeno e retenção de contaminantes por argilominerais

In this work are considered two bidimensional systems, with distints chacacteristcs and applicabilitys. Is studied the adsorption of transition metals (MT) Fe, Co, Mn and Ru in extended defects, formed by graphene grain boundaries. First in pristine graphene The hollow site of carbon hexagon, in pristine graphene, are the most stable for MT adsorption. The Dirac cone in eletronic structure of graphene was manteined with the presence of MT. For the considered grain boundaries the MT has a greater stability for absorption in the grain boundaries sites in comparison with pristine graphene. Through the energy barrier values, are observed diffusion chanels for MT localized on the grain boundaries. This diffusion chanels indicate a possible formation of nanolines of MT in graphene. For the first stage of the nanolines, ate observed a better stability for the system with greater MT concentration, due to MT-MT interactions. Also, due to the magnetic moment of the MT, the nanolines show a magnetization. For the most stable configurations the system are metallics, particularly for Fe the band structure indicates an anisotropic spin current. In a second study, are considereted the retention capacity for metallic contaminants Cd and Hg in clayminerals, kaolinite (KAO) and montmorillonite (MMT). Through the adsorption energies of contaminantes in the clayminerals, was observed a increase in stability with the increase of contaminants concentration, due to the interaction Cd-Cd and Hg-Hg. Also, was observed that KAO has a strong interaction beteween monolayers than MMT. In this sence, for the adsoption process of contaminantes in the natural form of KAO and MMT, the latter has a better retention capacity, due to the small net work for contaminant intercalation. However, when the modification of clayminerals, with molecules that increase the spacing between monolayers, exist a optimal condition, which the contaminant absorption are more stable in KAO system than in MMT. In the Langmuir adsorption model for the clayminerals in the optimal monolayer spacing, the retention capacity for Cd and Hg in KAO system are 21% greater than in MMT system. Also, for the X-ray Absorption Near Edge Spectroscopy (XANES) for the K edge of Cd and Hg, are found a positive shift of absorption edge with the decreasing of monolayer spacing. This result indicates a possible way to determine the concentration of adsorbed contaminats in relation to unabsorbed ones, from the decomposition of experimental XANES in the obteined spectras.

Desarrollo de herramientas bioinformáticas para estudios de proteómica a gran escala de "Candida albicans"

El concepto de Proteómica, acuñado en analogía al de Genómica, fue usado por primera vez por Marc Wilkins a mediados de los años 90 para describir al conjunto total de proteínas que se expresan por los genes de una célula, tejido u organismo. Anteriormente, a finales de los 80, el desarrollo de las técnicas de ionización suave, como la Ionización por Electrospray, ESI (Electrospray Ionization) o la Desorción Suave por Láser, SLD (Soft Laser Desorption), permitió ionizar grandes biomoléculas como los péptidos y proteínas manteniéndolas relativamente intactas. Esto sentó las bases de la espectrometría de masas aplicada a la proteómica. En la proteómica shotgun (el término inglés está muy asentado), el primer paso del experimento generalmente consiste en la digestión de las proteínas de la muestra en péptidos por acción de una enzima proteolítica como la tripsina. Esto incrementa notablmente el rendimiento en términos de número de proteínas que pueden ser identificadas en un sólo experimento comparado con los experimentos basados en gel. Sin embargo, tiene el coste asociado de provocar una gran complejidad de la mezcla de péptidos y el problema añadido de la inferencia de las proteínas originarias. Los péptidos son separados por cromatografía líquida e ionizados para entrar a continuación en el espectrómetro de masas donde son separados en función de la proporción entre su masa y su carga (m/z) y los valores obtenidos son registrados en un espectro MS1. En la espectrometría de masas en tándem (MS/MS), los péptidos con mayor intensidad son seleccionados para ser fragmentados de modo que se generan espectros MS/MS, colecciones de valores m/z y de intensidad para cada precursor y sus fragmentos...

Ensayo acerca del tiempo barroco en W. Benjamin

Nuestra exposición parte de la siguiente hipótesis: el barroco mantiene una relación particular con el tiempo que configura dimensiones de posibilidad y modos de producción específicos. Esta relación particular - que intentaremos asir a la manera de un "tiempo barroco"-, está marcada por los efectos del Racionalismo que, a la vez que deposita en el hombre la centralidad de su proyecto, también desplaza a los dioses de su cielo enfrentándolo a una fragilidad y una impotencia que no hacen sino confirmar la finitud que le es humana. El hombre, vuelto a un estado de criatura, pareciera no poder hacer con su tiempo más que la producción de una experiencia doliente. El hombre barroco llora su momento y dilata su tiempo presente con un sinfín de figuras como si quisiera de alguna manera nombrar, dibujar, el infinito que le falta. La producción alegórica recabada por Walter Benjamin en su Ursprung des deustchen Trauerspiels (1928), nos provee de pistas -la naturaleza, los cadáveres, las intrigas, los espectros, el Príncipe-, para esbozar la reconstrucción de este paisaje acechado por la desolación que trae consigo el racionalismo. En efecto, el tiempo se verá dislocado en la escena que la obra de Benjamin nos trae: la escatología ya no es más garantía de conocimiento de las cosas del mundo sino la fuerza propia de un momento de muerte que, al fin, produce un éxtasis último y redentor de todos los sufrimientos humanos. Las posibilidades para una producción cualitativa del tiempo, para la producción de otra experiencia, quedarán encerradas en esta suerte de espacio espiralado, donde las alegorías son los engranajes de un poder creativo capaz de producir una multiplicidad de desplazamientos simbólicos y reenvíos significantes ad infinitum aunque sin verdaderamente cambiar cosa alguna. Sin más, la catástrofe de las impotencias humanas deviene la fuerza y la visión del horizonte de nuestros posibles; una catástrofe ya incluida, que no puede dejar de tener lugar. Esta dilación de las posibilidades del 'cada vez' del tiempo presente, interpela, por la proximidad de sus desafíos, también nuestras dinámicas contemporáneas de aprovechamiento del tiempo

Humanism is a violence typical of the beasts. Philosozing with a Hammer, using Levinas and Derrida, the Measure of the Human and the Human as a measure

Levinas’s reflections arose as a critique of traditional philosophy which, since it was based on presence and identity, leads to the exclusion of the other. Instead of an onto-logical thought the Lithuanian proposes that the ipseity of the human being be constituted by alterity, and that it be so ethically, because the subject is sub-ject, that is, that which upholds, responsibility. In an attempt to take the obligatory attention to the otherness of the other even further, Derrida would develop a radical critique of the Levinasian posture. Deconstruction of every trace of ipseity and sovereignty in the relationship with the other, the reading that we have done of the work of Derrida opts for a no definable understanding of the human. That is why every de-limitation of an ethical field as a properly human implies a brutal violence that the levinasian humanism of the other tried to exceed.

Clarinetas em Si Bemol e em Fá: diferenças acústicas e interpretativas

ALBERTO,Gabriel Gagliano Pinto. Clarinetas em Si Bemol e em Lá: diferenças acústicas e interpretativas. Belo Horizonte, MG, 2004. Orientador: Prof. Dr. Maurício Alves Loureiro. Dissertação (Mestrado) - Escola de Música da Universidade Federal de Minas Gerais.

Diferenças acústicas e interpretativas entre as clarinetas em Si Bemol e em Lá

ALBERTO, Gabriel Gagliano Pinto. Diferenças acústicas e interpretativas entre as clarinetas em Si Bemol e La. In: CONGRESSO DA ANPPOM, 15., 2005. Rio de Janeiro. Anais ... Rio de Janeiro, 2005.

Efectos de la microestructura sobre la transmisión de neutrones en materiales de interés nuclear.

Cuando un haz policromático de neutrones pasa a través de un material, los neutrones de distintas longitudes de onda son atenuados en formas muy diferentes. Como resultado, el espectro de energía del haz de neutrones cambia cuando una muestra es colocada frente el haz. Un análisis detallado del cociente de intensidad entre los haces de transmitido e incidente puede proporcionar una gran cantidad de información acerca de la estructura cristalina y microestructura de la muestra, definidas a través de la sección eficaz total del material. Para neutrones térmicos y sub-térmicos, el ordenamiento y movimiento de los átomos a escala microscópica define en forma precisa la dependencia de esta magnitud con la energía del neutrón incidente. Así, la variación con la energía de la sección eficaz total de los sólidos debido a la estructura de los átomos para distancias entre 0,1 y 100 Å se encuentra bien establecida, y es explotada en el estudio de estructuras cristalinas y de los movimientos vibracionales y rotacionales. Como contrapartida, el efecto de la estructura mesoscópica de los materiales, esto es para dimensiones entre 0,1 y 100 µm, sobre la sección eficaz total ha sido mucho menos estudiado, a pesar de provocar cambios profundos en esta magnitud. En esta Tesis estudiamos y formalizamos la dependencia de la sección eficaz total con características microestructurales tales como la porosidad, y la distribución de tamaños y orientaciones de los granos que componen los materiales, y desarrollamos modelos teóricos a partir de las características microestructurales de muestras de interés nuclear con diferente microestructura. Estos modelos permiten describir la contribuci ón de la componente elástica coherente de la seción eficaz total sobre los espectros de transmisión de neutrones e introducen parámetros como la cantidad de cristales que conforman el material, su estructura cristalina, parámetros de red, mosaicidad, estructura de poros u orientación preferencial de granos, para describir la sección total de materiales monocristalinos o policristalinos. En todos los casos, los modelos desarrollados fueron implementados en una biblioteca basada en el lenguaje computacional MATLAB y fueron comparados con secciones eficaces totales obtenidas en experimentos de transmisión de neutrones realizados en el Departamento de Física de Neutrones del Centro Atómico Bariloche y en ISIS Facility, Reino Unido. Los novedosos modelos microestructurales propuestos describen fielmente los experimentos desarrollados sobre muestras con distinta microestructura, lo que permite el empleo de los mismos en un código de refinamiento sobre los datos experimentales. Aquí, desarrollamos herramientas computacionales que ajustan por cuadrados mínimos no lineales los modelos paramétricos representativos de cada microestructura, sobre la sección eficaz total o la transmisión experimental, para determinar parámetros microestructurales de la muestra a partir de experimentos de transmisión de neutrones con resolución en longitud de onda. Los resultados son de particular relevancia para la interpretación y el análisis cuantitativo de las imágenes realizadas por la técnica de radiografía neutrónica con resolución en energía, que ha recibido un gran impulso en años recientes.

Efectos de la microestructura sobre la transmisión de neutrones en materiales de interés nuclear.

Cuando un haz policromático de neutrones pasa a través de un material, los neutrones de distintas longitudes de onda son atenuados en formas muy diferentes. Como resultado, el espectro de energía del haz de neutrones cambia cuando una muestra es colocada frente el haz. Un análisis detallado del cociente de intensidad entre los haces de transmitido e incidente puede proporcionar una gran cantidad de información acerca de la estructura cristalina y microestructura de la muestra, definidas a través de la sección eficaz total del material. Para neutrones térmicos y sub-térmicos, el ordenamiento y movimiento de los átomos a escala microscópica define en forma precisa la dependencia de esta magnitud con la energía del neutrón incidente. Así, la variación con la energía de la sección eficaz total de los sólidos debido a la estructura de los átomos para distancias entre 0,1 y 100 Å se encuentra bien establecida, y es explotada en el estudio de estructuras cristalinas y de los movimientos vibracionales y rotacionales. Como contrapartida, el efecto de la estructura mesoscópica de los materiales, esto es para dimensiones entre 0,1 y 100 µm, sobre la sección eficaz total ha sido mucho menos estudiado, a pesar de provocar cambios profundos en esta magnitud. En esta Tesis estudiamos y formalizamos la dependencia de la sección eficaz total con características microestructurales tales como la porosidad, y la distribución de tamaños y orientaciones de los granos que componen los materiales, y desarrollamos modelos teóricos a partir de las características microestructurales de muestras de interés nuclear con diferente microestructura. Estos modelos permiten describir la contribuci ón de la componente elástica coherente de la seción eficaz total sobre los espectros de transmisión de neutrones e introducen parámetros como la cantidad de cristales que conforman el material, su estructura cristalina, parámetros de red, mosaicidad, estructura de poros u orientación preferencial de granos, para describir la sección total de materiales monocristalinos o policristalinos. En todos los casos, los modelos desarrollados fueron implementados en una biblioteca basada en el lenguaje computacional MATLAB y fueron comparados con secciones eficaces totales obtenidas en experimentos de transmisión de neutrones realizados en el Departamento de Física de Neutrones del Centro Atómico Bariloche y en ISIS Facility, Reino Unido. Los novedosos modelos microestructurales propuestos describen fielmente los experimentos desarrollados sobre muestras con distinta microestructura, lo que permite el empleo de los mismos en un código de refinamiento sobre los datos experimentales. Aquí, desarrollamos herramientas computacionales que ajustan por cuadrados mínimos no lineales los modelos paramétricos representativos de cada microestructura, sobre la sección eficaz total o la transmisión experimental, para determinar parámetros microestructurales de la muestra a partir de experimentos de transmisión de neutrones con resolución en longitud de onda. Los resultados son de particular relevancia para la interpretación y el análisis cuantitativo de las imágenes realizadas por la técnica de radiografía neutrónica con resolución en energía, que ha recibido un gran impulso en años recientes.

Avaliação da interação entre aflatoxina M1 e B1 com a fração proteica do leite

Dissertação composta por 02 artigos.

Clarinetas em Si Bemol e em Fá: diferenças acústicas e interpretativas

ALBERTO,Gabriel Gagliano Pinto. Clarinetas em Si Bemol e em Lá: diferenças acústicas e interpretativas. Belo Horizonte, MG, 2004. Orientador: Prof. Dr. Maurício Alves Loureiro. Dissertação (Mestrado) - Escola de Música da Universidade Federal de Minas Gerais.

Diferenças acústicas e interpretativas entre as clarinetas em Si Bemol e em Lá

ALBERTO, Gabriel Gagliano Pinto. Diferenças acústicas e interpretativas entre as clarinetas em Si Bemol e La. In: CONGRESSO DA ANPPOM, 15., 2005. Rio de Janeiro. Anais ... Rio de Janeiro, 2005.

Coupling of magnetic, strain and electric polarization fields in the structure of multiferroic material

The comprehensive study on the coupling of magnetism, electrical polarization and the crystalline lattice with the off-stoichiometric effects in self-doped multiferroic hexagonal h-LuMnxO3±δ (0.92≤x≤1.12) ceramic oxides was carried out for the PhD work. There is a complex coupling of the three ferroic degrees. The cancelation of the magnetic moments of ions in the antiferromagnetic order, electric polarization with specific vortex/antivortex topology and lattice properties have pushed researchers to find out ways to disclose the underlying physics and chemistry of magneto-electric and magneto-elastic couplings of h-RMnO3 multiferroic materials. In this research work, self-doping of Lu-sites or Mn-sites of h-LuMnxO3±δ ceramics prepared via solid state route was done to pave a way for deeper understanding of the antiferromagnetic transition, the weak ferromagnetism often reported in the same crystalline lattices and the ferroelectric properties coupled to the imposed lattice changes. Accordingly to the aim of the PhD thesis, the objectives set for the sintering study in the first chapter on experimental results were two. First, study of sintering off-stoichiometric samples within conditions reported in the bibliography and also extracted from the phase diagrams of the LuMnxO3±δ, with a multiple firings ending with a last high temperature step at 1300ºC for 24 hours. Second, explore longer annealing times of up to 240 hours at the fixed temperature of 1300 ºC in a search for improving the properties of the solid solution under study. All series of LuMnxO3±δ ceramics for each annealing time were characterized to tentatively build a framework enabling comparison of measured properties with results of others available in literature. XRD and Rietveld refinement of data give the evolution the lattice parameters as a function to x. Shrinkage of the lattice parameters with increasing x values was observed, the stability limit of the solid solution being determined by analysis of lattice parameters. The evolution of grain size and presence of secondary phases have been investigated by means of TEM, SEM, EDS and EBSD techniques. The dependencies of grain growth and regression of secondary phases on composition x and time were further characterized. Magnetic susceptibility of samples and magnetic irreversibility were extensively examined in the present work. The dependency of magnetic susceptibility, Neel ordering transition and important magnetic parameters are determined and compared to observation in other multiferroics in the following chapter of the thesis. As a tool of high sensitivity to detect minor traces of the secondary phase hausmannite, magnetic measurements are suggested for cross-checking of phase diagrams. Difficulty of previous studies on interpreting the magnetic anomaly below 43 K in h-RMnO3 oxides was discussed and assigned to the Mn3O4 phase, with supported of the electron microscopy. Magneto-electric coupling where AFM ordering is coupled to dielectric polarization is investigated as a function of x and of sintering condition via frequency and temperature dependent complex dielectric constant measurements in the final chapter of the thesis. Within the limits of solid solubility, the crystalline lattice of off-stoichiometric ceramics was shown to preserve the magneto-electric coupling at TN. It represents the first research work on magneto-electric coupling modified by vacancy doping to author’s knowledge. Studied lattices would reveal distortions at the atomic scale imposed by local changes of x dependent on sintering conditions which were widely inspected by using TEM/STEM methods, complemented with EDS and EELS spectroscopy all together to provide comprehensive information on cross coupling of distortions, inhomogeneity and electronic structure assembled and discussed in a specific chapter. Internal interfaces inside crystalline grains were examined. Qualitative explanations of the measured magnetic and ferroelectric properties were established in relation to observed nanoscale features of h-LuMnxO3±δ ceramics. Ferroelectric domains and topological defects are displayed both in TEM and AFM/PFM images, the later technique being used to look at size, distribution and switching of ferroelectric domains influenced by vacancy doping at the micron scale bridging to complementary TEM studies on the atomic structure of ferroelectric domains. In support to experimental study, DFT simulations using Wien2K code have been carried out in order to interpret the results of EELS spectra of O K-edge and to obtain information on the cation hybridization to oxygen ions. The L3,2 edges of Mn is used to access the oxidation state of the Mn ions inside crystalline grains. In addition, rehybridization driven ferroelectricity is also evaluated by comparing the partial density of states of the orbitals of all ions of the samples, also the polarization was calculated and correlated to the off-stoichiometric effect.