Proposta de modelo para o desenvolvimento de projetos minerais sustentáveis no Brasil.

A mineração brasileira, assim como todo o setor da industria de transformação, tem perdido competitividade ao longo do tempo, além disso o Brasil necessita tornar suas operações mais sustentáveis e agregar valor a sua produção industrial. A mineração é um setor onde esta questão se torna mais crítica, pois além de poder gerar forte impacto ambiental, a produção é fortemente baseada em commodities, com baixo valor agregado. Um dos caminhos para superar os obstáculos ao crescimento sustentável da mineração no Brasil é o desenvolvimento de projetos minerais inovadores. As condições estabelecidas pelo governo brasileiro para incentivo à inovação são muito abrangentes, práticas e atrativas; os recursos para financiamento são abundantes e os mecanismos para operacionalização extremamente profissionais. No entanto, na maioria das empresas brasileiras estão presentes a aversão ao risco, a falta das práticas de planejamento e de gestão de projetos e a visão de curto prazo focada na atuação corretiva, fatores que não favorecem o ambiente inovador nas empresas. Ou seja, o grande desafio para a mudança da mineração brasileira, tornando-a mais sustentável e competitiva, está na forma de pensar dos seus lideres; pois as condições existentes para desenvolvimento tecnológico estão disponíveis, mas as empresas necessitam aprender a utilizá-las. Este é um trabalho de pesquisa aplicada, que apresenta uma proposta de metodologia para desenvolvimento de projetos minerais sustentáveis, que foi utilizada por algumas empresas e obteve resultados muito positivos; com isto, é possível estabelecer um caminho que favoreça a mudança da cultura predominante, facilitando o desenvolvimento de inovações na mineração e contribuindo para o seu ganho de competitividade e sustentabilidade. A aplicação da metodologia proposta foi aplicada em um caso hipotético de mineração de ferro e os resultados foram muito positivos, demonstrando que o projeto inovador e sustentável seria muito mais competitivo que um tradicional, principalmente, em momentos de mercado em baixa.

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.

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.

Estudo da adição de resíduos de quartzitos para obtenção de grés porcelanato

In States of Paraíba (PB) and Rio Grande do Norte (RN), northeast of Brazil, the most significant deposits of non-metallic industrial minerals are pegmatites, quartzites and granites, which are located in Seridó region. Extraction of clay, quartz, micas and feldspars occurs mainly in the cities of Várzea (PB), OuroBranco (RN) and Parelhas (RN). Mining companies working in the extraction and processing of quartzite generate large volumes of waste containing about 90% SiO2 in their chemical composition coming from quartz that is one of the basic constituents of ceramic mass for the production of ceramic coating. Therefore, this work evaluates the utilization of these wastes on fabrication of high-quality ceramic products, such as porcelain stoneware, in industrial scale. Characterization of raw materials was based on XRF, XRD, GA, TGA and DSC analysis, on samples composed by 57% of feldspar, 37% of argil and 6% of quartzite residues, with 5 different colors (white, gold, pink, green and black). Samples were synthesized in three temperatures, 1150°C, 1200°C and 1250°C, with one hour isotherm and warming-up tax of 10°C/min. After synthesizing, the specimens were submit to physical characterization tests of water absorption, linear shrinkage, apparently porosity, density, flexural strain at three points. The addition of 6% of quartzite residue to ceramic mass provided a final product with technological properties attending technical norms for the production of porcelain stoneware; best results were observed at a temperature of 1200°C. According to the results there was a high iron oxide on black quartzite, being their use in porcelain stoneware discarded by ethic and structural question, because the material fused at 1250°C. All quartzite formulations had low water absorption when synthesized at 1200°C, getting 0.1% to 0.36% without having gone through the atomization process. Besides, flexural strain tests overcame 27 MPa reaching the acceptance limits of the European Directive EN 100, at 1200°C synthesizing. Thus, the use of quartzite residues in ceramic masses poses as great potential for the production of porcelain stoneware.

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.