Reaproveitamento de lamas residuais do processo de fabricação do concreto.

Nos dias atuais, um dos maiores problemas de uma central dosadora de concreto são as sobras de resíduos de concretos que retornam nos caminhões, das obras gerando lamas decantadas com pH elevado caracterizando-a como resíduo perigoso e representando gastos elevados com destinação. O objetivo do presente trabalho visa estudar em detalhes a composição da lama residual do processo de fabricação do concreto excluindo o agregado graúdo, verificando qual é a influência de sua adição no concreto. Com isso, pretende-se estudar algumas formas de tratamento e viabilizar economicamente o seu reaproveitamento em substituição ao agregado miúdo. Para esse estudo foram coletadas duas amostras desse material cimentício, sendo uma coletada diretamente do tanque de decantação e a segunda coletada da própria lavagem dos caminhões betoneiras. Elas foram submetidas a ensaios de caracterização como: análise termogravimétrica (TG), granulometria a laser e calorimetria e ensaios de concreto fresco (reologia e abatimento) e concreto endurecido. Para a viabilização econômica foi realizado um estudo de caso em três centrais dosadoras de concreto, afim de identificar perdas de materiais, custos de destinação e custo variável na fabricação de concreto. Os resultados mostraram que a forma de coleta do material cimentício influencia na finura do material conforme ensaio de granulometria e densidade aparente, mas não foi possível obter cimento anidro. A possibilidade de utilização da lama em concretos foi possível com ajuda de aditivos superplastificantes, mas para a viabilização economicamente viável a cadeia produtiva do concreto estudou-se um teor ótimo de substituição da lama pelo agregado miúdo.

Estudo da extração de índio a partir de telas de cristal líquido (LCD).

Ao longo dos últimos anos, o crescimento ao acesso a esse tipo de tecnologia pelos consumidores brasileiros tem intensificado o aumento no interesse ambiental e econômico dos LCDs. Os displays de cristal líquido são utilizados em televisores, calculadoras, telefones celulares, computadores (portáteis e tablets), vídeo games entre outros equipamentos eletrônicos. O avanço tecnológico neste campo tem tornado estes aparelhos obsoletos cada vez mais rápido, aumentando o volume de resíduos de LCDs a ser dispostos em aterros o que contribui para a redução da sua vida útil. Neste contexto, os LCDs provenientes de televisores de LED LCD tem se tornado uma fonte importante de resíduos de equipamentos eletroeletrônicos (REEE). Assim, torna-se essencial o desenvolvimento de métodos e processos para tratamento e reciclagem de LCDs. Deste modo, o objetivo do presente trabalho é a caracterização física e química de telas de cristal líquido provenientes de displays de televisores de LED LCDs e o estudo de uma rota hidrometalúrgica para recuperação de índio. Para tanto se utilizou técnicas de tratamento de minérios e análises físicas e químicas (separação granulométrica, perda ao fogo, visualização em lupa binocular, TGA, FRX, FT-IR) para caracterização do material e quantificação do índio antes e, após, a rota hidrometalúrgica que, por sua vez, foi realizada em reatores de bancada utilizando três agentes lixiviantes (ácido nítrico, sulfúrico e clorídrico), três temperaturas (25ºC, 40ºC e 60ºC) e quatro tempos (0,5h; 1h; 2h e 4h). Encontrou-se que a tela de cristal líquido representa cerca de 20% da massa total do display de televisores de LCD e que é composta por aproximadamente 11% em massa de polímeros e 90% de vidro + cristal líquido. Verificou-se também que há seis camadas poliméricas nas telas de cristal líquido, onde: um conjunto com 3 polímeros compõe o analisador e o polarizador, sendo que o polímero da primeira e da terceira camada de cada conjunto é triacetato de celulose e corresponde a 64% da massa de polímeros das telas. Já o polímero da segunda camada é polivinilalcool e representa 36% da massa de polímeros. Os melhores resultados obtidos nos processos de lixiviação foram com o ácido sulfúrico, nas condições de 60°C por 4h, relação sólido-líquido 1/5. Nessas condições, foi extraído em torno de 61% do índio contido tela de LCD.

Utilização de resíduo de mármore e de óxido de boro em escórias sintéticas dessulfurantes para aços.

O mercado atual exige das indústrias siderúrgicas aços de melhor qualidade produzidos por meio de processos que causem menor impacto ao meio ambiente. Dessa forma, este trabalho teve como objetivo reciclar o resíduo de mármore gerado na indústria de rochas ornamentais, que possui em sua composição óxido de cálcio (CaO) e óxido de magnésio (MgO). O CaO é suficiente para substituir a cal nas escórias e o MgO contribui para a diminuição do desgaste dos refratários, através do emprego do resíduo no processo produtivo do aço. Além disso, foi realizada a substituição da fluorita por óxido de boro como fluxante na composição de misturas dessulfurantes. O resíduo de mármore foi caracterizado utilizando as seguintes técnicas: análise química via EDXFR, análise granulométrica via espalhamento de luz, área de superfície específica pelo método BET, difração de raios-X, microscopia eletrônica de varredura (MEV) e análise de micro-regiões por EDS. Visando verificar a eficiência na dessulfuração, foram formuladas misturas sintéticas utilizando a cal convencional ou resíduo de mármore, e a fluorita ou o óxido de boro. As misturas foram formuladas com o auxílio dos programas de termodinâmica computacional, Thermo-Calc e FactSage. Estas misturas foram adicionadas no aço fundido a temperatura de 1600°C sob atmosfera de argônio e agitadas por meio de um rotor de alumina. Amostras de metal foram retiradas para verificar a variação do teor de enxofre durante o experimento. O resíduo de mármore caracterizado, apresentou em sua composição 40% de CaO e 14% de MgO, na forma dos carbonatos CaCO3 e MgCO3. Obteve uma perda de massa de 42,1%, na forma de CO2 a temperatura de 780°C. Os experimentos mostraram que, as misturas testadas apresentaram, na maioria dos casos, eficiência de dessulfuração acima de 60%.

Thermal decomposition of the different particles size fractions of almond shells and olive stones. Thermal behaviour changes due to the milling processes

The aim of this study is to investigate the effect of particle size on the non-isothermal pyrolysis of almond shells (AS) and olive stones (OS) and to show possible differences in the composition of the different fractions obtained after milling and sieving. The results obtained from the study of different particle size of AS and OS samples show significant differences in the solid residue obtained and in the shape and overlapping degree of the peaks, especially with the smaller particle size. These differences can be due to different factors: (a) the amount of inorganic matter, which increases as particle size decreases, (b) heat and mass transfer processes, (c) different sample composition as a consequence of the milling process which may provoke changes in the structure and the segregation of the components (in addition to the ashes) increasingly changes the composition of the sample as the particle size decreases.

Synthesis of palladium nanoparticles on carbon nanotubes and graphene for the chemoselective hydrogenation of para-chloronitrobenzene

We have studied the synthesis of palladium nanoparticles over carbon nanotubes (Pd/CNT) and graphene (Pd/G) and we have tested their catalytic performance in the liquid phase chemoselective hydrogenation of para-chloronitrobenzene at room temperature. The catalysts were characterized by N2 adsorption/desorption isotherms, TEM, X-ray diffraction, infrared and X-ray photoelectron spectroscopy and ICP-OES. The palladium particle size on Pd/G (3.4 nm) and Pd/CNT (2.8 nm) was similar though the deposition was higher on Pd/G. Pd/CNT was more active which can be ascribed to the different surface area and electronic properties of the Pd nanoparticles over CNT, while the selectivity was 100% to the corresponding haloaniline over both catalysts and they were quite stable upon recycling.

(Table 1) Porosity, particle diameter, ATP content and carbon and nitrogen composition of ODP Site 164-994 sediments

Sediment samples were obtained for detailed Adenosine 5'-Triphosphate (ATP) analysis down to 57.8 m below the seafloor (mbsf). The samples were also analyzed for particle-size distribution, calcium carbonate (CaCO3), organic carbon, and total nitrogen. The concentrations of ATP ranged between 360 and 7050 pg/g (dry weight sediment), which agree well with a limited number of direct bacteria counts. Principal component analyses show that 63% of the total variance can be accounted for by the first two principal components. The concentration of ATP (bacterial numbers by inference) is virtually independent of the concentration of sedimentary organic carbon, but correlates with CaCO3 and coarse particles.

Particel size distribution and microstructures of sediments from ODP Leg 205 sites (Table 1)

Ocean Drilling Program Legs 170 and 205 offshore Costa Rica provide structural observations which support a new model for the geometry and deformation response to the seismic cycle of the frontal sedimentary prism and decollement. The model is based on drillcore, thin section, and electron microscope observations. The decollement damage zone is a few tens of meters in width, it develops mainly within the frontal prism. A clear cm-thick fault core is observed 1.6 km from the trench. The lower boundary of the fault core is coincident with the lithological boundary between the frontal prism and the hemipelagic and pelagic sediment of the Cocos plate. Breccia clast distributions in the upper portion of the decollement damage zone were studied through fractal analysis. This analysis shows that the fractal dimension changes with brecciated fragment size, implying that deformation was not accommodated by self-similar fracturing. A higher fractal dimensionality correlates with smaller particle size, which indicates that different or additional grain-size reduction processes operated during shearing. The co-existence of two distinct fracturing processes is also confirmed by microscopic analysis in which extension fracturing in the upper part of the damage zone farthest from the fault core is frequent, while both extension and shear fracturing occur approaching the fault core. The coexistence of extensional and shear fracturing seems to be best explained by fluid pressure variations in response to variations of the compressional regime during the seismic cycle. During the co-seismic event, sub-horizontal compression and fluid pressure increase, triggering shear fracturing and fluid expulsion. Fractures migrate upward with fluids, contributing to the asymmetric shape of the decollement, while slip propagates. In the inter-seismic interval the frontal prismrelaxes and fluid pressure drops. The frontal prismgoes into diffuse extension during the intervalwhen plate convergence is accommodated by creep along the ductile fault core. The fault core is typically a barrier to deformation, which is explained by its weak, but impermeable, nature. The localized development of a damage zone beneath the fault core is characterized by shear fracturing that appears as the result of local strengthening of the detachment.

(Table 1) Grain size composition of recent sediments from the eastern Barents Sea shelf

Based on materials on geomorphology, hydrology, lithology, and sedimentation dynamics obtained during cruises of the P.P. Shirshov Institute of Oceanology in the Barents Sea, the author prepared a number of charts on content of the main particle size facies in shelf surface sediments, as well as a chart of lithologic types of sediments in the Barents Sea. Factors of sedimentation control and basic features of distribution of sedimentary material over its bottom area are taken into consideration.

10Be/9Be-based chronostratigraphy of ODP Hole 181-1121B from the Southwest Pacific Ocean

A 10Be/9Be-based chronostratigraphy has been determined for ODP 181, Site 1121 sediment core, recovered from the foot of the Campbell Plateau, Southwest Pacific Ocean. This core was drilled through the Campbell 'skin drift' in ca. 4500 m water depth on the mid-western margin of the extensive Campbell Nodule Field, beneath the flow of the major cold-water Deep Western Boundary Current (DWBC). In the absence of detailed biostratigraphy, beryllium isotopes have provided essential time information to allow palaeo-environmental interpretation to be undertaken on the upper 7 m of the core. Measured 10Be/9Be ratios of sediment, and of ferromanganese nodules entrapped in the sediment, decrease systematically with depth in the core, in accordance with radioactive decay. However, the 10Be/9Be data diverge from ca. 3 m below the seafloor (mbsf) to the top of the core, giving rise to several possible geochronological models. The preferred model assumes that the measured 10Be/9Be ratios of the nodule rims reflect initial 10Be/9Be ratios equivalent to contemporary seawater, and that these can be used to derive the true age of the sediment where the nodules occur. The nodule rim ages can be then used to interpret the sediment 10Be/9Be data, which indicate an overall age to ca. 7 mbsf of ca. 17.5 Ma. The derived chronology is consistent with diatom biostratigraphy, which indicates an age of 2.2-3.6 Ma at 1 mbsf. Calculated sedimentation rates range from 8 to 95 cm m.y.**-1, with an overall rate to 7 mbsf of ca. 39 cm m.y.**-1. The lowest rates generally coincide with the occurrence of entrapped nodules, and reflect periods of increased bottom current flow causing net sediment loss. Growth rates of individual nodules decrease towards the top of the sediment core, similar to the observed decrease in growth rate from core to rim of seafloor nodules from the Campbell Nodule Field. This may be related to an overall increase in the vigour of the DWBC from ca. 10 Ma to the present.

Mineral, chemical and isotope compositions of clay subfractions from formations of the Srednii Peninsula, Murmansk coast of the Barents Sea

Fine-grained clay subfractions (SFs) with particle size of <0.1, 0.1-0.2, 0.2-0.3, 0.3-0.6, 0.6-2.0, and 2-5 µm separated from claystone of Upper Precambrian Pumanskaya and Poropelonskaya formations on the Srednii Peninsula were studied by transmission electron microscopy, X-ray diffraction, and Rb-Sr methods. All subfractions consist of low-temperature illite and chlorite, and contribution of chlorite decreases with diminishing particle size. The crystallinity index and I002/I001 ratio increase from coarse- to fine-grained SFs. Leaching by ammonium acetate solution and Rb-Sr systematics in combination with mineralogical and morphological data indicate that illite in Upper Proterozoic claystone from the Srednii Peninsula formed during three time intervals: 810-830, 610-620, and about 570 Ma ago. The first generation of this mineral with low Rb/Sr ratio dominates in coarse-grained SFs while the second and third generations with a high Rb/Sr ratio prevail in fine-grained SFs. All of three generations are known in Poropelon claystone, whereas Puman claystone contains only illite of the first and second generations. Geological processes responsible for multistage illite evolution in claystones are discussed.

(Table 1) Summary of maximum clast size and bed thickness of ODP Leg 126 samples

Subaerial debris flows, with water contents ranging from as little as 10 wt% up to no more than about 25 wt% (Pierson, 1986; Pierson and Costa, 1987), are non-Newtonian fluids that move as fairly coherent masses with yield strength (owing to bulk densities and viscosity that are much greater than those of clear water), which enables them to suspend and transport large clasts. Their flow behavior is thought to be predominantly laminar, although the relative importance of laminar and turbulent flow has not been established and is debatable. They leave deposits (debrites) that are characteristically poorly sorted with large clasts in their middle portions and commonly protruding from their tops. Although generally ungraded or normally graded in their upper portions, many have centimeter- to decimeter-thick inversely graded basal zones (Arguden and Rodolfo, 1990, doi:10.1130/0016-7606(1990)102<0865:SADDBH>2.3.CO;2).