O contributo da refeição escolar para a ingestão de minerais: estudo preliminar

O almoço escolar constitui uma oportunidade importante para a aprendizagem de hábitos alimentares saudáveis, sendo as refeições escolares equilibradas associadas ao aumento da concentração dos alunos na sala de aula, melhores resultados académicos e redução do número de dias em que as crianças ficam doentes. Os minerais constituem um grupo fundamental de nutrientes, não podem ser sintetizados pelo organismo e, por isso, têm que ser fornecidos pela alimentação. Este trabalho tem como objetivo determinar a composição em minerais, de refeições escolares colhidas em escolas do 1º ciclo do ensino básico público, na região metropolitana de Lisboa, de modo a avaliar os seu contributo para a dose diária recomendada. Foram analisadas 13 refeições constituidas por: sopa, prato principal de carne ou peixe, acompanhamento, salada, sobremesa e pão de mistura. As amostras foram submetidas a uma digestão ácida por micro-ondas. Os minerais Cobre, Manganês, Ferro, Zinco, Magnésio, Cálcio, Fósforo, Sódio e Potássio, foram determinados por espectrometria de emissão atómica acoplada com plasma indutivo (ICP-OES).Entre os minerais analisados, o Sódio e Potássio foram os mais abundantes, com teores entre 190 - 268 mg/100 g e 46,9 - 193 mg/100 g, respetivamente. Verificou-se que as refeições analisadas contribuem com mais de 50% da dose diária recomendada para o Sódio e 100% da dose diária recomendada para o Potássio. Relativamente ao Cálcio e Ferro as refeições analisadas fornecem 11% e 12 % da dose diária recomendada. O almoço escolar deve fornecer os nutrientes essenciais e, simultaneamente, permitir o desenvolvimento de preferências alimentares saudáveis, variadas e equilibradas. Este estudo permitiu conhecer o perfil de minerais do almoço, servido em escolas na região metropolitana de Lisboa. Este diagnóstico da situação poderá fundamentar a elaboração de programas de intervenção em saúde e de educação alimentar.

Real cedula de S.M. y señores del Consejo por la qual se prescriben las reglas convenientes para imponer los capitales de los Depósitos que hay en el reyno sobre la Renta del tabaco á razon de tres por ciento de cuenta de la Real Hacienda

Certifica la copia Pedro Escolano de Arrieta.

Real cedula de S.M. y señores del Consejo, por la qual se manda guardar, y cumplir el Real Decreto y declaracion insertos, en que se prescriben las reglas convenientes para imponer los capitales de los depósitos que hai en el reyno sobre la renta del tabaco á razon de tres por ciento de cuenta de la Real Hacienda.

Certifica la copia Antonio Martínez Salazar.

Métallurgie pratique, ou Exposition détaillée des divers procédés employés pour obtenir des métaux utiles : précédée de l'essai et de la préparation des minerais /

Mode of access: Internet.

Les principaux gisements de minerais de zinc des Êtats-Unis d'Amérique,

"Extrait de la Revue universelle des mines, etc., tome VI, 4e série, pagee 221, 48e année, 1904.

Les combustibles minéraux, les minerais, et les phosphates en Algérie.

Mode of access: Internet.

Élémens pratiques d'exploitation, contenant tout ce qui est relatif à l'art d'explorer la surface des terrains, d'y faire des travaux de recherche et d'y établir des exploitations réglées; la description des moyens employés pour l'extraction et le transport souterrain des minerais et des combustibles; les diverses méthodes de boiser, murailler, aérer et assécher les mines; les secours à donner aux noyés, asphyxiés et brulés; des notions sur l'administration, la comptabilité, etc., etc.

Mode of access: Internet.

Rapport de la Commission nommée pour étudien les divers procédés électro-thermiques pour la réduction des minerais de fer et la fabrication de l'acier employés en Europe.

Mode of access: Internet.

Traité des roches : considérées au point de vue de leur origine, de leur composition, de leur gisement et de leurs applications a la géologie et a l'industrie, suivi de la description des minerais qui fournissent les métaux utiles. /

Includes index.

Pirometamorfismo em calcários da formação Jandaíra, bacia potiguar, nordeste do Brasil

The present study aims the characterization of thermally affected carbonate rocks from Jandaíra Formation in contact with Paleogene and Neogene basic intrusions in the region of the Pedro Avelino and Jandaíra municipalities (RN), northeastern Brazil. For this study, field, petrographic, x-ray diffraction, electron microprobe, and whole rock litogeochemistry data of carbonates were undertaken. The thermally unaffected limestones are classified like wackstones, grainstones and packstones. They may constitute carbonates grains of benthic foraminifera, echinoderm spines, ostracods, algae, corals, bivalves, gastropods, peloids and intraclasts. The porosities are classified like vug, intraparticle, interparticle, intercrystal and moldic types. The major minerals are calcite, ankerite and dolomite; the detrital are montmorillonite, pyrite, limonite, quartz and microcline. The thermally affected limestones are very coarse to very fine-grained and light to dark gray color. The fossiliferous components totally disappear, and the porosity tends to disappear. With the data obtained, it can be inferred that the carbonate protoliths would be calciferous to dolomitic limestones, both with small amount of clay minerals. Crystalline carbonates from dolomitic protolith have rhombohedral calcite and iron oxides / hydroxides, making the rocks much darker. The carbonates from calciferous protolith have a wide variation of grain size according to the recrystallization degree, increasing toward contact with the basic bodies. In this group, it was identified the minerals lizardite and spinel in weakly to moderately affected samples, and spinel and spurrite in strongly affected rocks, as well as calcite, that occur everywhere. The geological context (shallow level diabase intrusions), the crystallization of the pyrometamorphic minerals spurrite and olivine, and comparison with diagrams from the literature allow estimating temperatures and pressures around 1050-1200 °C and 0.5-1.0 kbar, respectively, for PTOTAL=PCO2. The post-intrusion cooling would have afforded the releasing of metasomatic / hydrothermal fluids, allowing the opening of the metamorphic system, with possible contribution of chemical elements from host units (sandstones, shales) and from basic intrusions. This would induce hydration of previous phases, allowing the formation of serpentine, chlorite and brucite. The results discussed here reveal the strong influence of the heat from basic intrusions within the sedimentary pile. Whereas in the offshore portion of the basin occur sills with up to 1000 m thickness, the understanding of pyrometamorphism might be useful for understanding and measuring the thermally affected rocks.

Pirometamorfismo em calcários da formação Jandaíra, bacia potiguar, nordeste do Brasil

The present study aims the characterization of thermally affected carbonate rocks from Jandaíra Formation in contact with Paleogene and Neogene basic intrusions in the region of the Pedro Avelino and Jandaíra municipalities (RN), northeastern Brazil. For this study, field, petrographic, x-ray diffraction, electron microprobe, and whole rock litogeochemistry data of carbonates were undertaken. The thermally unaffected limestones are classified like wackstones, grainstones and packstones. They may constitute carbonates grains of benthic foraminifera, echinoderm spines, ostracods, algae, corals, bivalves, gastropods, peloids and intraclasts. The porosities are classified like vug, intraparticle, interparticle, intercrystal and moldic types. The major minerals are calcite, ankerite and dolomite; the detrital are montmorillonite, pyrite, limonite, quartz and microcline. The thermally affected limestones are very coarse to very fine-grained and light to dark gray color. The fossiliferous components totally disappear, and the porosity tends to disappear. With the data obtained, it can be inferred that the carbonate protoliths would be calciferous to dolomitic limestones, both with small amount of clay minerals. Crystalline carbonates from dolomitic protolith have rhombohedral calcite and iron oxides / hydroxides, making the rocks much darker. The carbonates from calciferous protolith have a wide variation of grain size according to the recrystallization degree, increasing toward contact with the basic bodies. In this group, it was identified the minerals lizardite and spinel in weakly to moderately affected samples, and spinel and spurrite in strongly affected rocks, as well as calcite, that occur everywhere. The geological context (shallow level diabase intrusions), the crystallization of the pyrometamorphic minerals spurrite and olivine, and comparison with diagrams from the literature allow estimating temperatures and pressures around 1050-1200 °C and 0.5-1.0 kbar, respectively, for PTOTAL=PCO2. The post-intrusion cooling would have afforded the releasing of metasomatic / hydrothermal fluids, allowing the opening of the metamorphic system, with possible contribution of chemical elements from host units (sandstones, shales) and from basic intrusions. This would induce hydration of previous phases, allowing the formation of serpentine, chlorite and brucite. The results discussed here reveal the strong influence of the heat from basic intrusions within the sedimentary pile. Whereas in the offshore portion of the basin occur sills with up to 1000 m thickness, the understanding of pyrometamorphism might be useful for understanding and measuring the thermally affected rocks.

Petrologia e geocronologia U-Pb do plúton granítico Serra da Rajada, porção central do domínio Rio Piranhas - Seridó, Província Borborema, NE do Brasil

The ediacaran plutonic activity related to the Brasilian/Pan-African orogeny is one of the most important geological features in the Borborema Province, represented along its extension by numerous batholiths, stocks, and dikes.The object of this study, the Serra Rajada Granitic Pluton (SRGP), located in the central portion of the Piranhas-Seridó River Domain is an example of this activity. This pluton has been the subject of cartographic, petrographic, geochronological and lithogeochemical studies and its rocks were characterized by two facies. First, the granitic facies were described as monzogranites consisting of K-feldspar, plagioclase (oligoclase - An23-24%), quartz and biotite (main mafic) and opaque minerals such as titanite, allanite, apatite, and zircon as accessories. Alteration minerals are chlorite, white mica and carbonate. Second, the dioritic facies consist of rocks formed by quartz diorite containing plagioclase (dominant mineral phase), quartz and K-feldspar. Biotite and amphibole are the dominant mafic minerals; and titanite, opaque minerals, allanite, zircon and apatite are the accessories. However, previous geological mapping work in the region also identified the presence of other lithostratigraphic units. These were described as gneisses and migmatites with undifferentiated amphibolite lenses related to the Caicó Complex (Paleoproterozoic) and metasedimentary rocks of the Seridó Group (Neoproterozoic) composed of paragneiss with calc-silicate lenses, muscovite quartzite and biotite schist (respectively, the Jucurutu formations, Equador and Seridó), the host rocks for the SRGP rocks. Leucomicrogranite and pegmatite dikes have also been identified, both related to the end of the Ediacaran magmatism and colluvial- eluvial and alluvial deposits related to Neogene and Quaternary, respectively. Lithogeochemical data on the SRGP granite facies, highlighted quite evolved rocks (SiO2 69% to 75%), rich in alkalis (Na2O+K2O ≥ 8.0%), depleted of MgO (≤ 0.45%), CaO (≤ 1.42%) and TiO2 (≤ 0.36%) and moderate levels of Fe2O3t (2.16 to 3.53%). They display transitional nature between metaluminous and peraluminous (predominance of the latter) with sub-alkaline/monzonitic (High K calcium-alkali) affinity. Harker diagrams show negative correlations for Fe2O3t, MgO, and CaO, indicating mafic and plagioclase fractionation. REE spectrum shows enrichment of LREE relative to heavy REE (LaN/YbN = 23.70 to 10.13), with negative anomaly in the Eu (Eu/Eu* = 0.70 to 0.23), suggesting fractionation or accumulation in the feldspars source (plagioclase). Data integration allows to correlate the SRGP rocks with those described as Calcium-Alkaline Suite of equigranular High K. The crystallization conditions of the SRGP rocks were determined from the integration of petrographic and lithogeochemical data. These data indicated intermediate to high conditions of ƒO2 (mineral paragenesis titanite + magnetite + quartz), parent magma saturated in H2O (early biotite crystallization), tardi-magmatic processes of fluids rich in ƒCO2, H2O and O2 causing part of the mineral assembly to change (plagioclase carbonation and saussuritization, biotite chloritization and opaques Sphenitization). Thermobarometrical conditions were estimated based on geochemical parameters (Zr and P2O5) and CIPW normative minerals, with results showing the liquidus minimum temperature of about800°C and the solidus temperature of approximately 700°C. The final/minimum crystallization pressure are suggested to be between 3 and 5 Kbar. The presence of zoned minerals (plagioclase and allanite) associated with lithogeochemical data in bi-log diagrams for Rb vs. Ba and Rb vs. Sr suggest the role of fractional crystallization as the dominant process in the magmatic evolution of SRGP. U-Pb Geochronological and Sm-Nd isotope studies indicated, respectively, the crystallization age of biotite monzogranite as 557 ± 13 Ma, with TDM model age of 2.36 Ga, and εNd value of -20.10 to the crystallization age, allowing to infer paleoproterozoic crustal source for the magma.

Petrologia e geocronologia U-Pb do plúton granítico Serra da Rajada, porção central do domínio Rio Piranhas - Seridó, Província Borborema, NE do Brasil

The ediacaran plutonic activity related to the Brasilian/Pan-African orogeny is one of the most important geological features in the Borborema Province, represented along its extension by numerous batholiths, stocks, and dikes.The object of this study, the Serra Rajada Granitic Pluton (SRGP), located in the central portion of the Piranhas-Seridó River Domain is an example of this activity. This pluton has been the subject of cartographic, petrographic, geochronological and lithogeochemical studies and its rocks were characterized by two facies. First, the granitic facies were described as monzogranites consisting of K-feldspar, plagioclase (oligoclase - An23-24%), quartz and biotite (main mafic) and opaque minerals such as titanite, allanite, apatite, and zircon as accessories. Alteration minerals are chlorite, white mica and carbonate. Second, the dioritic facies consist of rocks formed by quartz diorite containing plagioclase (dominant mineral phase), quartz and K-feldspar. Biotite and amphibole are the dominant mafic minerals; and titanite, opaque minerals, allanite, zircon and apatite are the accessories. However, previous geological mapping work in the region also identified the presence of other lithostratigraphic units. These were described as gneisses and migmatites with undifferentiated amphibolite lenses related to the Caicó Complex (Paleoproterozoic) and metasedimentary rocks of the Seridó Group (Neoproterozoic) composed of paragneiss with calc-silicate lenses, muscovite quartzite and biotite schist (respectively, the Jucurutu formations, Equador and Seridó), the host rocks for the SRGP rocks. Leucomicrogranite and pegmatite dikes have also been identified, both related to the end of the Ediacaran magmatism and colluvial- eluvial and alluvial deposits related to Neogene and Quaternary, respectively. Lithogeochemical data on the SRGP granite facies, highlighted quite evolved rocks (SiO2 69% to 75%), rich in alkalis (Na2O+K2O ≥ 8.0%), depleted of MgO (≤ 0.45%), CaO (≤ 1.42%) and TiO2 (≤ 0.36%) and moderate levels of Fe2O3t (2.16 to 3.53%). They display transitional nature between metaluminous and peraluminous (predominance of the latter) with sub-alkaline/monzonitic (High K calcium-alkali) affinity. Harker diagrams show negative correlations for Fe2O3t, MgO, and CaO, indicating mafic and plagioclase fractionation. REE spectrum shows enrichment of LREE relative to heavy REE (LaN/YbN = 23.70 to 10.13), with negative anomaly in the Eu (Eu/Eu* = 0.70 to 0.23), suggesting fractionation or accumulation in the feldspars source (plagioclase). Data integration allows to correlate the SRGP rocks with those described as Calcium-Alkaline Suite of equigranular High K. The crystallization conditions of the SRGP rocks were determined from the integration of petrographic and lithogeochemical data. These data indicated intermediate to high conditions of ƒO2 (mineral paragenesis titanite + magnetite + quartz), parent magma saturated in H2O (early biotite crystallization), tardi-magmatic processes of fluids rich in ƒCO2, H2O and O2 causing part of the mineral assembly to change (plagioclase carbonation and saussuritization, biotite chloritization and opaques Sphenitization). Thermobarometrical conditions were estimated based on geochemical parameters (Zr and P2O5) and CIPW normative minerals, with results showing the liquidus minimum temperature of about800°C and the solidus temperature of approximately 700°C. The final/minimum crystallization pressure are suggested to be between 3 and 5 Kbar. The presence of zoned minerals (plagioclase and allanite) associated with lithogeochemical data in bi-log diagrams for Rb vs. Ba and Rb vs. Sr suggest the role of fractional crystallization as the dominant process in the magmatic evolution of SRGP. U-Pb Geochronological and Sm-Nd isotope studies indicated, respectively, the crystallization age of biotite monzogranite as 557 ± 13 Ma, with TDM model age of 2.36 Ga, and εNd value of -20.10 to the crystallization age, allowing to infer paleoproterozoic crustal source for the magma.

A Comunicação Interna: a eficácia dos meios de comunicação interna na Caixa Geral de Depósitos

No mundo actual, onde a concorrência cresce e a oferta de produtos aumenta, onde a globalização é palavra de ordem, torna-se essencial pensar a sobrevivência das empresas como estando dependentes da adopção de comportamentos transparentes diante dos públicos, sejam eles de dimensão interna e/ou externa. Reconhecer a importância de controlar os aspectos imprevisíveis a que as empresas estão sujeitas, permite às organizações um maior controlo na previsão dos problemas, como os corrigir antes que estes interfiram no seu sucesso, constituindo assim um ambiente previsível e favorável. A comunicação assume pois um papel primordial na visibilidade positiva de uma empresa. O cliente interno, neste trabalho, será visto como fornecedor de uma rede interna de prestação de serviços, responsável pela agregação de valor aos produtos e serviços oferecidos pela organização. Os clientes internos são também vistos como detentores de um propósito comum responsável tanto pela criação como pela continuidade da organização. Ao longo deste trabalho é descrita e focada a ligação especial que existe entre a comunicação empresarial, a comunicação interna e a estratégia do marketing interno evidenciando a importância destes para as organizações. O objectivo deste estudo é analisar a eficácia dos meios de comunicação interna na Caixa Geral de Depósitos, a partir da realização de 39 inquéritos administrados a colaboradores de uma Agência. Os resultados obtidos com este estudo deram ênfase à eficácia dos meios de comunicação interna utilizados na organização em estudo, concluindo que a comunicação deve ser veiculada de acordo com a utilidade das funções a desempenhar. / In today´s world where competition grows and the supply of products increases, where globalization is a slogan, it is essential to consider the survival of business as being dependent of the adoption of transparent behavior in public, in they internal or external dimensions. Recognizing the importance of controlling the unpredictable aspects that companies are subject, allows organizations greater control in forecast the problems, how to correct them before they interfere with their success, providing a predictable and favorable ambient. Communication assumes an essential role in a positive visibility of a company. The internal customer, this work will be seen as a provider of internal network services, responsible for adding value to products and services offered by the organization. Internal customers are also seen as having a common purpose as much responsible for creating the continuity of the organization. Throughout this work is focused and described the special bond that exists between corporate communication, internal communication and internal marketing strategy, highlighting their importance for the organizations. The aim of this study is to analyze the effectiveness of internal communication in the CGD, from conducting 39 surveys administered to employees of an Agency. The results of this study emphasized the effectiveness of internal communication in the organization used in the study, concluding that the communication should be conveyed according to the usefulness of the tasks.