976 resultados para Tolerância a Pb e Zn
Resumo:
The Yanque nonsulfide Pb-Zn deposit (inferred resources 12.5 Mt @ 3.7% Pb and @ 3.5% Zn) is located in the Andahuaylas-Yauri ore province (Cuzco, southern Peru). The deposit occurs within a base metal mineralized district, centered on the medium-sized Dolores porphyry copper. A thorough geological, mineralogical and geochemical study has carried out in order to define: the relationships between the Dolores Cu-porphyry ore and the Yanque Zn-Pb polymetallic mineralization, and the characteristics of the economic nonsulfide concentrations. Both sedimentary and igneous rocks constitute the backbone of the Yanque-Dolores area. The sedimentary lithologies belong to the Soraya, Mara and Ferrobamba Fms. (upper Jurassic-middle Cretaceous). The Yanque orebody is hosted by the Mara Fm., which prevailingly consists of a siliciclastic sedimentary breccia. The original sulfide mineralization consisted of galena, pyrite and sphalerite. The host rock has been affected by a strong hydrothermal alteration, characterized by prevailing sericite/illite, as in the typical porphyry-related phyllic-argillic alteration stage, and by minor kaolinite, dolomite and quartz. Minor element geochemistry, characterized by Sb, As, Mn, Ag and locally also by Cu, points to magmatic-hydrothermal related mineralizing fluids. The Pb isotopic compositions from Dolores and Yanque sulfides are similar, and are typical of the Tertiary magmatically-derived ores in this part of Peru. The hydrothermally altered rocks at Yanque have the same Pb isotopic compositions as the sulfides, thus confirming the hypothesis that the Yanque primary Zn-Pb mineralization may have been produced by hydrothermal circulation related to the emplacement of the Dolores Cu-porphyry, as it is the case of other porphyry Cu systems associated with polymetallic mineralization elsewhere. However, no simple genetic model for the mineralization involving just one fluid circulation episode is able to explain the data. The Yanque economic nonsulfide ore association consists of sauconite, hemimorphite, smithsonite and cerussite, which result from the weathering and alteration of the original sulfide mineralization. Zinc is allocated mainly in sauconite (Zn-smectite), rather than in carbonates: a factor strictly related to the prevailing siliciclastic character of the host rock. Distinctive features of the Yanque orebody are the comparable ore grades for both Pb and Zn (3.5% Zn and 3.7% Pb), and the inverse supergene chemical zoning. In fact, contrary to other supergene ores of this type, zinc prevails in the top zone of the Yanque deposit, whereas lead content increases with depth. Considering the different mobility of the two metals in solution, it may be assumed that most of the primary zinc that was the source for the Yanque nonsulfides was originally located far from the position occupied by the galena mineralization, whose remnants have been observed on site. Zinc sulfides may have been originally contained in the eroded rock volumes that surrounded the actual deposit: the zinc-rich solutions have possibly migrated through the siliciclastic Mara Fm. and precipitated the nonsulfide minerals by porosity filling and replacement processes. In this sense, the Yanque secondary Zn-Pb deposit could be considered as a special type of “Exotic” mineralization.
Resumo:
En Mendoza, Argentina, no existen antecedentes respecto de la presencia de elementos trazas, totales y disponibles, relacionados con el uso de los suelos en los oasis irrigados. El objetivo del trabajo, en esta etapa, fue determinar los contenidos totales de plomo (Pb), cadmio (Cd), cinc (Zn) y cobre (Cu) en la capa superficial de suelos (0-25 cm), diferenciados en siete tipos según una clasificación utilitaria: suelos vírgenes (SV); suelos de banquina (SB); suelos vecinos a banquina (SVB); suelos de agricultura intensiva (SAI); suelos de agricultura protegidos por lucha antigranizo (SLAG); suelos afectados por actividad industrial (SI) y suelos urbanos (SU). Sobre un total de 200 muestras se efectuó una digestión ácida en caliente y en los extractos se determinaron los metales en su fracción total, mediante espectrofotometría de absorción atómica (AAS). El análisis estadístico de los datos muestra que los niveles más elevados de Cu y Cd se detectan en SAI, con medias de 39,3 y 2,5 mg kg-1 respectivamente. En SI se observan los mayores valores de Pb, con una media de 80,6 mg kg-1 y en SU los mayores tenores de Zn, con un valor medio de 740 mg kg-1. La Ciudad de Mendoza, con mayor densidad poblacional, presentó los mayores contenidos de Zn, Pb y Cd. Las concentraciones encontradas se ubican por debajo de las exigencias de la legislación argentina y la mayoría de los suelos pueden clasificarse como no contaminados (SNC) o ligeramente contaminados (SLC). Se prevé completar este estudio con la determinación de las fracciones disponibles de los elementos estudiados, correlacionándolos con variables edáficas físico-químicas como textura, pH y materia orgánica.
Resumo:
Wydział Biologii
Resumo:
O depósito Tocantinzinho, localizado em um lineamento de direção NW–SE, a SW de Itaituba (PA), é atualmente o maior depósito aurífero conhecido na Província Tapajós. Está hospedado no granito homônimo, essencialmente isótropo, no qual dominam rochas sieno e monzograníticas, que foram fraca a moderadamente alteradas por fluidos hidrotermais. Microclinização (mais precoce), cloritização, sericitização, silicificação e carbonatação (mais tardia) são os mais importantes tipos de alteração. O principal estágio de mineralização é contemporâneo à sericitização/silicificação e é representado por vênulas com sulfetos (pirita ± calcopirita ± galena ± esfalerita) e ouro associado, as quais mostram localmente trama stockwork. Além de teores expressivos de Cu, Pb e Zn, são anômalos, em algumas amostras, os de As, Bi e Mo. A relação dos teores do Au com os dos metais-base é aleatória e as razões Au/Ag variam de 0,05 a 5,0. O Au é mais enriquecido nas porções com maior abundância de sulfetos de metais-base, embora ocorra principalmente incluso na pirita. Monocristais de zircão, extraídos do granito Tocantinzinho, forneceram idade Pb-Pb média de 1982 ± 8 Ma, permitindo interpretá-lo como uma manifestação magmática precoce do arco Creporizão. Valores de δ13CPDB em calcita do estágio de carbonatação, dominantemente entre -3,45 e -2,29‰, são compatíveis com fonte crustal profunda, quiçá carbonatítica, enquanto os de δ18OSMOW (+5,97 a +14,10‰) indicam forte contribuição magmática, ainda que mascarada por influxo de águas provavelmente superficiais. Estudos de inclusões fluidas em andamento revelam a presença de fluidos aquocarbônicos, cujo CO2 poderia ter estado dissolvido no magma granítico em vez de ser relacionado à zona de cisalhamento. Os dados até aqui disponíveis permitem classificar o depósito aurífero Tocantinzinho como do tipo relacionado à intrusão.
Resumo:
Fours sets of PM10 samples were collected in three sites in SEQ from December 2002 to August 2004. Three of these sets of samples were collected by QLD EPA as a part of their regular air monitoring program at Woolloongabba, Rocklea and Eagle Farm. Half of the samples were used in this study for the analysis of water-soluble ions, which are Na+, K+, Mg2+, Ca2+, NH4 +, Cl-, NO3 -, SO4 2-, F-, Br-, NO2 -, PO4 -3 and the other half was retained by QLD EPA. The fourth set of samples was collected at Rocklea, specifically for this study. A quarter of the samples obtained from this set of samples were used to analyse water-soluble ions; a quarter of the sample was used to analyse Pb, Cu, Al, Fe, Mn and Zn; and the rests were used to analyse US EPA 16 priority PAHs. The water-soluble ions were extracted ultrasonically with water and the major watersoluble anions as well as NH4 + were analysed using IC. Na+, K+, Mg2+, Ca2+ Pb, Cu, Al, Fe, Mn and Zn were analysed using ICP-AES while PAHs were extracted by acetonitrile and analysed using HPLC. Of the analysed water-soluble ions, Cl-, NO3 -, SO4 2-, Na+, K+, Mg2+ and Ca2+ were high in concentration and determined in all the samples. F-, Br-, NO2 -, PO4 -3 and NH4 + ions were lower in concentration and determined only in some samples. Na+ and Cl- were high in all samples indicating the importance of a marine source. Principal Component Analysis (PCA) was used to examine the temporal variations of the water-soluble ions at the three sites. The results indicated that there was no major difference between the three sites. However, comparing the average concentrations of ions and Cl-/Na+ it was concluded that Woolloongabba had more marine influence than the other sites. Al, Fe and Zn were detected in all samples. Al and Fe were high in all samples indicating the significance of a source of crustal matter. Cu, Mn and Pb were in low concentrations and were determined only in some samples. The lower Pb concentrations observed in the study than in previous studies indicate that the phasing-out of leaded petrol had an appreciable impact on Pb levels in SEQ. This study reports for the first time, simultaneous data on the water-soluble, metal ion and PAH levels of PM10 aerosols in Brisbane, and provides information on the most likely sources of these chemical species. Such information can be used alongside those that already exist to formulate PM10 pollution reduction strategies for SEQ in order to protect the community from the adverse effects of PM pollution.
Resumo:
Solids are widely identified as a carrier of harmful pollutants in stormwater runoff exerting a significant risk to receiving waters. This paper outlines the findings of an in-depth investigation on heavy metal adsorption to solids surfaces. Pollutant build-up samples collected from sixteen road sites in residential, industrial and commercial land uses were separated into four particle size ranges and analysed for a range of physico-chemical parameters and nine heavy metals including Iron (Fe), Aluminum (Al), Lead (Pb), Zinc (Zn), Cadmium (Cd), Chromium (Cr), Manganese (Mn), Nickel (Ni) and Copper (Cu). High specific surface area (SSA) and total organic carbon (TOC) content in finer particle size ranges was noted, thus confirming strong correlations with heavy metals. Based on their physico-chemical characteristics, two different types of solids originating from traffic and soil sources were identified. Solids generated by traffic were associated with high loads of heavy metals such as Cd and Cr with strong correlation with SSA. This suggested the existence of surface dependent bonds such as cation exchange between heavy metals and solids. In contrast, Fe, Al and Mn which can be attributed to soil inputs showed strong correlation with TOC suggesting strong bonds such as chemsorption. Zn was found to be primarily attached to solids by bonding with the oxides of Fe, Al and Mn. The data analysis also confirmed the predominance of the finer fraction, with 70% of the solids being finer than 150 µm and containing 60% of the heavy metal pollutant load.
Resumo:
In the context of increasing demand for potable water and the depletion of water resources, stormwater is a logical alternative. However, stormwater contains pollutants, among which metals are of particular interest due to their toxicity and persistence in the environment. Hence, it is imperative to remove toxic metals in stormwater to the levels prescribed by drinking water guidelines for potable use. Consequently, various techniques have been proposed, among which sorption using low cost sorbents is economically viable and environmentally benign in comparison to other techniques. However, sorbents show affinity towards certain toxic metals, which results in poor removal of other toxic metals. It was hypothesised in this study that a mixture of sorbents that have different metal affinity patterns can be used for the efficient removal of a range of toxic metals commonly found in stormwater. The performance of six sorbents in the sorption of Al, Cr, Cu, Pb, Ni, Zn and Cd, which are the toxic metals commonly found in urban stormwater, was investigated to select suitable sorbents for creating the mixtures. For this purpose, a multi criteria analytical protocol was developed using the decision making methods: PROMETHEE (Preference Ranking Organisation METHod for Enrichment Evaluations) and GAIA (Graphical Analysis for Interactive Assistance). Zeolite and seaweed were selected for the creation of trial mixtures based on their metal affinity pattern and the performance on predetermined selection criteria. The metal sorption mechanisms employed by seaweed and zeolite were defined using kinetics, isotherm and thermodynamics parameters, which were determined using the batch sorption experiments. Additionally, the kinetics rate-limiting steps were identified using an innovative approach using GAIA and Spearman correlation techniques developed as part of the study, to overcome the limitation in conventional graphical methods in predicting the degree of contribution of each kinetics step in limiting the overall metal removal rate. The sorption kinetics of zeolite was found to be primarily limited by intraparticle diffusion followed by the sorption reaction steps, which were governed mainly by the hydrated ionic diameter of metals. The isotherm study indicated that the metal sorption mechanism of zeolite was primarily of a physical nature. The thermodynamics study confirmed that the energetically favourable nature of sorption increased in the order of Zn < Cu < Cd < Ni < Pb < Cr < Al, which is in agreement with metal sorption affinity of zeolite. Hence, sorption thermodynamics has an influence on the metal sorption affinity of zeolite. On the other hand, the primary kinetics rate-limiting step of seaweed was the sorption reaction process followed by intraparticle diffusion. The boundary layer diffusion was also found to limit the metal sorption kinetics at low concentration. According to the sorption isotherm study, Cd, Pb, Cr and Al were sorbed by seaweed via ion exchange, whilst sorption of Ni occurred via physisorption. Furthermore, ionic bonding is responsible for the sorption of Zn. The thermodynamics study confirmed that sorption by seaweed was energetically favourable in the order of Zn < Cu < Cd < Cr . Al < Pb < Ni. However, this did not agree with the affinity series derived for seaweed suggesting a limited influence of sorption thermodynamics on metal affinity for seaweed. The investigation of zeolite-seaweed mixtures indicated that mixing sorbents have an effect on the kinetics rates and the sorption affinity. Additionally, the theoretical relationships were derived to predict the boundary layer diffusion rate, intraparticle diffusion rate, the sorption reaction rate and the enthalpy of mixtures based on that of individual sorbents. In general, low coefficient of determination (R2) for the relationships between theoretical and experimental data indicated that the relationships were not statistically significant. This was attributed to the heterogeneity of the properties of sorbents. Nevertheless, in relative terms, the intraparticle diffusion rate, sorption reaction rate and enthalpy of sorption had higher R2 values than the boundary layer diffusion rate suggesting that there was some relationship between the former set of parameters of mixtures and that of sorbents. The mixture, which contained 80% of zeolite and 20% of seaweed, showed similar affinity for the sorption of Cu, Ni, Cd, Cr and Al, which was attributed to approximately similar sorption enthalpy of the metal ions. Therefore, it was concluded that the seaweed-zeolite mixture can be used to obtain the same affinity for various metals present in a multi metal system provided the metal ions have similar enthalpy during sorption by the mixture.
Resumo:
In the context of increasing threats to the sensitive marine ecosystem by toxic metals, this study investigated the metal build-up on impervious surfaces specific to commercial seaports. The knowledge generated in this study will contribute to managing toxic metal pollution of the marine ecosystem. The study found that inter-modal operations and main access roadway had the highest loads followed by container storage and vehicle marshalling sites, while the quay line and short term storage areas had the lowest. Additionally, it was found that Cr, Al, Pb, Cu and Zn were predominantly attached to solids, while significant amount of Cu, Pb and Zn were found as nutrient complexes. As such, treatment options based on solids retention can be effective for some metal species, while ineffective for other species. Furthermore, Cu and Zn are more likely to become bioavailable in seawater due to their strong association with nutrients. Mathematical models to replicate the metal build-up process were also developed using experimental design approach and partial least square regression. The models for Cr and Pb were found to be reliable, while those for Al, Zn and Cu were relatively less reliable, but could be employed for preliminary investigations.
Resumo:
Fly ash is a waste by-product obtained from the burning of coal by thermal power plants for generating electricity. When bulk quantities are involved, in order to arrest the fugitive dust, it is stored wet rather than dry. Fly ash contains trace concentrations of heavy metals and other substances in sufficient quantities to be able to leach out over a period of time. In this study an attempt was made to study the leachabilities of a few selected trace metals: Cd, Cu, Cr, Mn, Pb and Zn from two different types of class F fly ashes. Emphasis is also laid on developing an alternative in order to arrest the relative leachabilities of heavy metals after amending them with suitable additives. A standard laboratory leaching test for combustion residues has been employed to study the leachabilities of these trace elements as a function of liquid to solid ratio and pH. The leachability tests were conducted on powdered fly ash samples before and after amending them suitably with the matrices lime and gypsum; they were compacted to their respective proctor densities and cured for periods of 28 and 180 days. A marked reduction in the relative leachabilities of the trace elements was observed to be present at the end of 28 days. These relative leachability values further reduced marginally when tests were performed at the end of 180 days.
Resumo:
Nanocomposites of Al?In, Al?Pb, and Zn?Pb have been prepared and characterized using rapid quenching techniques and the nature of superconducting transitions in them has been studied by resistivity measurements. The precipitated second phases (In and Pb) have particle sizes (d) of a few tens of nanometers such that ?0?d?dmin, where ?0 is the superconducting zero temperature coherence length and dmin is the minimum particle size that supports superconductivity. The onset of superconductivity generally starts in samples with d??0 and progressively other grains with d??0 become superconducting. We suggest that the proximity effect of the matrix plays a significant role. In an Al?In system, even with 40?wt.% In, the zero resistivity state is obtained at T?1.33 times the Tc of Al. But in Al?Pb and Zn?Pb, the zero resistivity state is obtained at T?4 and 5 times the Tc of Al and Zn with only 10�15 wt?% Pb, respectively.
Resumo:
Experimental work was performed to delineate the system of digested sludge particles and associated trace metals and also to measure the interactions of sludge with seawater. Particle-size and particle number distributions were measured with a Coulter Counter. Number counts in excess of 1012 particles per liter were found in both the City of Los Angeles Hyperion mesophilic digested sludge and the Los Angeles County Sanitation Districts (LACSD) digested primary sludge. More than 90 percent of the particles had diameters less than 10 microns.
Total and dissolved trace metals (Ag, Cd, Cr, Cu, Fe, Mn, Ni, Pb, and Zn) were measured in LACSD sludge. Manganese was the only metal whose dissolved fraction exceeded one percent of the total metal. Sedimentation experiments for several dilutions of LACSD sludge in seawater showed that the sedimentation velocities of the sludge particles decreased as the dilution factor increased. A tenfold increase in dilution shifted the sedimentation velocity distribution by an order of magnitude. Chromium, Cu, Fe, Ni, Pb, and Zn were also followed during sedimentation. To a first approximation these metals behaved like the particles.
Solids and selected trace metals (Cr, Cu, Fe, Ni, Pb, and Zn) were monitored in oxic mixtures of both Hyperion and LACSD sludges for periods of 10 to 28 days. Less than 10 percent of the filterable solids dissolved or were oxidized. Only Ni was mobilized away from the particles. The majority of the mobilization was complete in less than one day.
The experimental data of this work were combined with oceanographic, biological, and geochemical information to propose and model the discharge of digested sludge to the San Pedro and Santa Monica Basins. A hydraulic computer simulation for a round buoyant jet in a density stratified medium showed that discharges of sludge effluent mixture at depths of 730 m would rise no more than 120 m. Initial jet mixing provided dilution estimates of 450 to 2600. Sedimentation analyses indicated that the solids would reach the sediments within 10 km of the point discharge.
Mass balances on the oxidizable chemical constituents in sludge indicated that the nearly anoxic waters of the basins would become wholly anoxic as a result of proposed discharges. From chemical-equilibrium computer modeling of the sludge digester and dilutions of sludge in anoxic seawater, it was predicted that the chemistry of all trace metals except Cr and Mn will be controlled by the precipitation of metal sulfide solids. This metal speciation held for dilutions up to 3000.
The net environmental impacts of this scheme should be salutary. The trace metals in the sludge should be immobilized in the anaerobic bottom sediments of the basins. Apparently no lifeforms higher than bacteria are there to be disrupted. The proposed deep-water discharges would remove the need for potentially expensive and energy-intensive land disposal alternatives and would end the discharge to the highly productive water near the ocean surface.
Resumo:
O presente trabalho teve como objetivo principal comparar dois métodos de extração de elementos-traço em sedimentos que são assistidos por radiação micro-ondas. Foram coletadas amostras de sedimentos superficiais em um manguezal localizado na baía da Ilha Grande e em três manguezais localizados na baía de Sepetiba, RJ. As amostras de sedimentos coletadas foram secas, destorroadas e peneiradas. Sub-amostras foram submetidas a análises de caracterização física e química. Os métodos de extração de elementos-traço comparados foram o EPA-3051A e o método água régia assistido por micro-ondas. Os elementos-traço analisados foram: Cd, Cr, Cu, Ni, Pb e Zn. As concentrações dos elementos-traço nos extratos produzidos foram determinadas por FAAS (Espectrometria de absorção atômica com chama). Foram encontradas nos sedimentos dos manguezais estudados concentrações acima dos níveis estabelecidos pela Resolução CONAMA 344/2004 para os elementos-traço: Cd, Ni, Pb e Zn. Os resultados mostraram que as capacidades de extração de elementos-traço dos métodos EPA-3051A e água régia assistido por micro-ondas variam em função das características físico-químicas dos sedimentos. A análise estatística pela técnica de regressão linear simples mostrou que as duas metodologias são estatisticamente similares apenas para o Cr e os valores dos coeficientes de determinação (R2) obtidos obedeceram à seqüência: Cu > Pb > Zn > Ni > Cr > Cd. Na análise pela técnica estatística de regressão linear múltipla ocorreram melhorias estatisticamente significativas nos coeficientes de determinação quando foram incluídas as seguintes variáveis independentes: potencial redox e fósforo total para o Cd, argila para o Cr, areia para o Ni e fósforo total para o Pb e para o Zn
Resumo:
Estudos ambientais têm demonstrado que substâncias geradas por processos antropogênicos podem causar efeitos prejudiciais interferindo no equilíbrio natural do ecossistema. Manguezais exercem funções essenciais nos ciclos biológicos e constituem Área de Proteção Permanente no Brasil. Infelizmente, eles estão sendo degradados acima do seu limite de suporte, levando a uma redução das áreas remanescentes no mundo. Este trabalho apresenta os resultados de mutagenicidade e genotoxicidade observados em quatro amostragens (PI, V, O e PII) entre 2009 e 2010, relacionados com metais e hidrocarbonetos policíclicos aromáticos (HPA) em sedimento de mangue para a caracterização dos valores de referência. Os testes de genotoxicidade foram feitos a partir de hemócitos do caranguejo Goniopsis cruentata, coletados em um ecossistema potencialmente não poluído do Brasil, localizado no sul do Rio de Janeiro (Parati/RJ), chamado de "Saco do Mamanguá". Coleta, armazenamento e manipulação dos sedimentos e material biológico de cinco pontos de amostragem (M1- M5) foram processados de acordo com normas norte-americanas reconhecidas. A identificação das substâncias químicas foi realizada com extratos de sedimentos e utilizada no bioensaio Salmonella/microssoma (Kado). A avaliação de potenciais danos genotóxicos estabelecidos foi realizada através do Teste de Micronúcleo, que apresentou valores significativos na amostra V. Resultados negativos foram observados para as cepas de Salmonella typhimurium TA97, TA98, TA100 e TA102, tanto na ausência quanto na presença de fração de metabolização exógena de mamíferos (S9 mix 4%) em todas as análises. A quantificação por cromatografia gasosa com detecção por espectrometria de massas dos 16 HPA prioritários em termos de conservação ambiental apresentou valores baixos nas duas primeiras amostragens (PI e V) e nulos nas coletas seguintes (O e PII), nos mesmos pontos. De acordo com os valores utilizados nos Estados Unidos e Canadá como referência, os detectados por nós não são considerados como toxicantes ambientais positivos, com exceção do Benzo(a)pireno, que em M1V apresentou valores um pouco acima do limite a partir do qual já podem ser observados pequenos efeitos na biota. A análise dos metais (Cd, Cr, Cu, Fe, Mn, Ni, Pb e Zn) por Espectrometria de Absorção Atômica inicialmente realizada com a água intersticial foi melhor interpretada a partir da matriz sedimento. Este estudo contribuirá com a implementação de indicadores para valores de referência em mangue.
Resumo:
A toxicidade dos metais em ambientes aquáticos está relacionada à sua biodisponibilidade e esta, por sua vez, pode ser influenciada por diversos fatores. As características do sedimento fazem dele um importante compartimento para avaliação do nível de contaminação no ambiente aquático. A presente pesquisa teve por objetivo quantificar e avaliar a biodisponibilidade de metais em sedimentos da baía da Ribeira. Nessa região, encontram-se os bairros mais populosos de Angra dos Reis RJ. Essa baía está localizada na parte nordeste da baía da Ilha Grande, que consiste de um espaço pesqueiro, turístico e de importante valor econômico e industrial. Foram coletados 12 sedimentos na baía da Ribeira e determinados os teores dos metais Al, Cu, Cd , Cr, Fe, Mn, Ni, Pb e Zn, através da extração com água régia (protocolo BCR-701), e o potencial de toxicidade dos metais Cd, Cu, Ni, Pb e Zn pelo método de extração dos sulfetos voláteis em meio ácido e quantificação dos metais extraídos simultaneamente (em inglês Acid Volatile Sulfide and Simultaneously Extracted Metal, AVS/SEM). Também foram efetuadas medidas de pH, potencial redox (Eh), carbono orgânico, fósforo total e granulometria. Através desses dados, foi possível estudar correlações entre essas variáveis. As concentrações de cada metal são similares nas diferentes localizações dos sedimentos e não apresentam significativas diferenças com relação a estudos reportados para a área, com exceção do Pb que apresentou a mais alta concentração já reportada. Os valores de SEM/AVS (entre 0,02 e 0,2) menores que 1, indicam que há quantidade de sulfetos suficiente para o aprisionamento dos metais investigados. As correlações obtidas através da Análise dos Componentes Principais demonstram relação direta entre as concentrações da maioria dos metais extraídos por água-régia (Ni, Fe, Cr, Cu, Zn); entre os metais Mn, Pb, Al e o fósforo total; entre os teores de matéria orgânica, carbono orgânico total, fósforo total com as frações finas de silte e argila com o Eh. Os resultados sugerem que a região não sofre influência significativa de fontes antrópicas em relação a metais e que, segundo o AVS/SEM, esses se encontram pouco disponíveis para o ambiente e, portanto, apresentam baixo potencial tóxico
Resumo:
A Costa Verde se localiza no estado do Rio Janeiro, onde também está localizada a Ilha Grande, importante polo turístico do estado. É composta pelas baías Sepetiba e Ilha Grande, que podem ser compartimentadas em diversas enseadas. As principais enseadas são Sepetiba, Marambaia, Mangaratiba, Angra dos Reis, Ribeira, Frade e Paraty. O presente estudo foi realizado nas enseadas de Mangaratiba, Angra dos Reis e Ribeira e foram compilados dados de Sepetiba e Marambaia estudado por outros autores. O objetivo do estudo destas enseadas foi identificar os metais e suas fontes e os mecanismos que os controlam, além de propor novos parâmetros de concentração de metais que indiquem processos de contaminação. O método utilizado foi a coleta de sedimento de fundo através da utilização de Van Veen e analisados por digestão total em espectrômetro de massa da qual se obteve a concentração dos elementos Ca, Cd, Co, Cr, Cu, K, Pb, Na, Ni, Sr, S, U, V e Zn, além das razões isotópicas de chumbo, com prioridade da razão 206Pb/207Pb. Foram obtidos resultados que indicam que a enseada de Mangaratiba apresenta as maiores concentrações de metais e com predominante contribuição antrópica cujas fontes são, os empreendimentos localizados na costa dessa enseada, incluindo o TEBIG. A enseada de Angra dos Reis também apresenta concentrações elevadas de metais, provenientes de efluentes domésticos, rejeito industrial ao qual se inclui o estaleiro Verolme e com forte controle do embasamento da enseada. A enseada da Ribeira tem seus metais fornecidos pelo porto de Bracuhy e uma fonte desconhecida que são controlados, em parte, pelos efluentes da CNAAA. Em relação a interação entre as cinco enseadas existe mútua troca de metais controlados pela dinâmica da Costa e acentuada pelo Canal de Ilha Grande (que liga as duas baias), onde a dispersão dos metais também é controlada por temperatura, fração sedimentar, profundidade e salinidade. Os principais metais relacionados às fontes antrópicas na Costa Verde são Co, Cr, Cu, Mn, Ni, Pb e Zn. As concentrações hoje apresentadas na resolução CONAMA não atendem a realidade da Costa Sul brasileira, sendo então propostos novos parâmetros de controle, menos permissivo