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No description available.

Shrinking alpine glaciers alter the geochemistry of sensitive mountain streams by exposing reactive freshly-weathered bedrock and releasing decades of atmospherically-deposited trace elements from glacier ice. Changes in the timing and quantity of glacial melt also affect discharge and temperature of alpine streams. To investigate the effects of glacier ice melt on the geochemistry and hydrology of proglacial streams in the arid Intermountain West, we sampled supraglacial meltwaters and proglacial streams in the Dinwoody Creek watershed in the Wind River Range, Wyoming during late summer 2015, when the contributions of glacier meltwater were highest. Supraglacial meltwater was enriched in 8 trace elements (Cd, Co, Cu, MeHg, Mn, Pb, THg, Zn) relative to proglacial meltwaters. Concentrations of major ions (Mg2+, K+, Na+, Ca2+, SO42-) and the remaining 30+ analyzed trace elements were enriched in proglacial streams relative to supraglacial meltwater. To evaluate the diurnal effects of glacial meltwater on the chemistry and hydrology of proglacial streams, we collected hourly water samples of Dinwoody Creek and deployed loggers to monitor water depth, temperature, and specific conductance (SPC) at 15-min intervals over a 1-week period. The influx of glacial meltwater between 10:00 and 20:00 diluted solute concentrations and affected the relative enrichment/depletion of highly soluble elements (major ions, alkaline earth elements), less than REEs. Stable isotopes of H and O (δD, δ18O) in Dinwoody Creek were more depleted during peak runoff (10:00 – 20:00) than base flow, reflecting contributions from isotopically depleted glacial meltwaters. Looping hysteresis patterns were observed between water depth versus DO, pH, temperature and SPC in glaciated streams. Hysteresis patterns were affected by changes in weather and varied depending on the type of stream (glaciated versus non-glaciated) and the distance to glacier toe. Combination of multiple hydrologic tracers (solute concentrations, high frequency logger data, stable isotopes) shows strong potential to improve estimates of glacial meltwater contributions to Dinwoody Creek. Our results suggest that elevated concentrations of heavy metals in glacier ice melt across the Intermountain West may negatively impact sensitive alpine streams.

[pt] A presença de metais-traço nos cigarros oferece uma fonte de informação potencial do ponto de vista forense e criminológico, na determinação e classificação de marcas de tabaco, com o intuito de diferenciar as marcas legalizadas das contrabandeadas. Por isso, neste trabalho, almejou-se desenvolver e validar métodos para determinação metais e semimetais presentes nos cigarros, com o intuito de avaliar a viabilidade de discriminação entre as diferentes marcas, analisando as amostras após o processo de calcinação e dissolução ácida. Estes métodos englobam as análises químicas por técnicas espectrométricas (CV-AAS, ICP-OES e DRC-ICP-MS) e posterior interpretação de dados por ACP (Análise dos Componentes Principais) e AAH (Análise de Agrupamento Hierárquico). As concentrações de metais e semimetais (As, Ba, B, Cd, Co, Cu, Fe, Mn, Hg, Ni, Sr e Zn) foram estudadas para dez diferentes marcas de cigarros, obtidas em tabacarias e lojas locais, representando as marcas mais consumidas no país. A utilização da ACP indicou a presença de quatro componentes principais que, em conjunto, explicavam mais de 80 por cento da variabilidade dos dados amostrais. Esses resultados comprovaram a existência de diferenças significativas entre as marcas de tabaco em seus conteúdos elementares, possibilitando a diferenciação entre marcas ilegais e marcas legalizadas e o agrupamento das marcas legalizadas de acordo com as empresas de tabaco as quais pertencem, sendo corroborado pela AAH, feita pelo método da distância média de ligação (UPGMA). Os teores de umidade, cinzas totais e pH de cada marca também foram determinados, no entanto não contribuíram efetivamente para a diferenciação entre as marcas estudadas. A AAH foi utilizada para a interpretação de possíveis similaridades entre os elementos, e em conjunto com o teste de correlação linear de Pearson, indicou similaridades entre os elementos Ba e Sr . Agrupamentos entre Fe e Zn com o Sr e Co com o Mn também foram detectados. / [en] The presence of trace metals in cigarettes offers potential source of information from a forensic and criminological point of view, which deals with the determination and classification of tobacco brands, with the aim of differentiating legal brands from smuggled brands. Therefore, this work aimed to develop and validate methods for determining the metallic content present in cigarettes, in order to assess the feasibility of discrimination between different brands, analyzing cigarettes after the process of calcination and acid digestion. These methods include chemical analysis by spectrometric techniques (CV-AAS, ICP-OES and DRC-ICPMS) and subsequent data interpretation by PCA (Principal Component Analysis) and HCA (Hierarchical Cluster Analysis). The concentration of metals and semimetals (As, Ba, B, Cd, Co, Cu, Fe, Mn, Hg Ni, Sr and Zn) were studied for ten different brands of cigarettes, obtained in tobacconists and local stores, representing the brands most consumed in the country. The analysis of PCA indicated the presence of four principal components that together explained more than 80 percent of the variability of the sample data. These results proved the existence of significant differences between tobacco brands in their elemental content, allowing the differentiation between illegal brands and legalized brands and the grouping of legal brands according to the tobacco companies to which they belong, being corroborated by the HCA performed by the average link distance method (UPGMA). The moisture content, total ash and pH of each brand were also determined, however they did not contribute effectively to the differentiation between the brands studied. The HCA used for the interpretation of possible similarities between the elements, and interpreted together with Pearson s linear correlation test indicated similarities between the elements Ba, Sr, in addition to indicating the proximity between the Mn and the Cd. Clusters between Fe and Zn with Sr and Co with Mn were also detected.

Thesis (PhD (Soil Science))--University of Stellenbosch, 2007. / Trace elements occur naturally in soils, usually at low concentrations (<0.1% or <1000 mg kg-1 of the earth’s crust), as a result of weathering and pedogenic processes acting on the rock fragments from which soil develops (parent material). Since about 98% of human food is produced on land, soil is the primary source supplying these elements to the food chain. Although cases of trace element deficiency and toxicity have been documented in many parts of South Africa, no comprehensive description of trace element concentration has yet been attempted for South Africa as a whole. The Natural Resources Land Type mapping project, initiated in the mid-1970s, has provided a collection of samples (approximately 4500) from soil profiles selected to represent the main soil forms in each land type and therefore to provide representative coverage of most of the soils of South Africa. These archived samples have now been analysed for a spectrum of trace elements, in terms of both available and total concentrations as well as other soil properties. Although detailed information is available on a wide range of trace metals, the seven trace metals considered to be of most interest in a South African context due to natural geological occurrences were selected for this study, including Cd, Co, Cr, Cu, Pb, Ni and Zn. This data was used to: • determine baseline concentrations in SA soils; • determining threshold values for South African agricultural soils receiving sewage sludge at agronomic rates; • determining the influence of certain soil properties on the baseline concentrations of these trace elements in SA soils; and • development of a bioavailable trace element distribution map for SA. The range, the mean and standard deviation (both arithmetic and geometric), and the median were used to summarize the data statistically. The baseline concentration range was calculated using the quotient and product of the geometric mean and the square of the geometric standard deviation, including data below the instrument detection limit. The upper limit of the baseline concentration range was set at the 0.975 percentile value of the population in order to minimize the influence of contamination and the lower limit at the 0.025 percentile value to minimize problems that might be associated with analytical uncertainty near the lower limit of detection. The quantile regression statistical approach was followed to illustrate the relationship between soil properties and trace element concentrations in soils. The soil properties that showed the strongest relation were CEC, clay content, pH (H2O) and S value (base status). The soils were then divided into different classes according to these soil properties and baseline concentrations were derived for the different classes. Soils with low clay contents have lower trace element concentrations than soils with higher clay contents, soils with low or high pH levels have lower trace element contents than soils with intermediate pH values and mesotrophic soils have higher trace element concentrations than dystrophic soils. This information is useful for the compilation of trace element distribution maps for South Africa where different soil forms and series/families could be classified into different classes to determine areas of potential deficiencies as well as toxicities. South Africa, with its diverse geology, has areas of both trace element toxicities and deficiencies and for decision-making purposes it is necessary to identify these areas. Mapping of trace element levels based on soil samples would provide valuable information, which cannot be obtained from geological or geographical maps. Statistical analyses of the data (clay %, base status, pH (H2O) and NH4EDTA extractable trace element concentrations) indicated that soils could be divided into five trace element classes based on their clay content, pH and base status (dystrophic, mesotrophic and eutrophic). The soil series according to the binomial soil classification system for South Africa were then divided into these different classes. The geometric means for each clay class were determined and the baseline concentration range for each class was calculated. The land type maps were used as basis for the distribution maps. A general trace element distribution map for South Africa was derived from this data as well as Cu and Zn distribution maps. A random selection of 500 soil samples across the country was used to verify the accuracy of the distribution map. The general trace element distribution map indicate, with a confidence level between 89 and 96%, where the potentially available trace element content of South African soils are low (deficient) too moderately high, excluding rocky areas and areas with limited soil. The Cu and Zn maps indicate the distribution and expected baseline concentrations of these specific elements in South African soils. The same methodology could be applied to derive risk maps for all the individual trace elements to indicate the distribution and expected baseline concentrations of the elements in South Africa. This presentation of baseline concentrations, reflecting likely natural ranges in South African soils, is the first quantitative report on the spatial extent and intensity of Zn, Cu and Co deficiency in South African soils. The proposal of new threshold values for trace elements in agricultural soils will be valuable in setting more realistic norms for environmental contamination that accommodate the geochemical peculiarities of the region, one example being rather high Cr and Ni concentrations with low bio-availability. This information should be of value not only in environmental pollution studies but also in health, agriculture, forestry and wildlife management. The following recommendations are made: • The baseline concentrations could be used to determine site specific threshold values based on soil properties and soil type. Soils with lower pH, clay content and CEC would require more protection than soils with high pH, clay content and CEC and therefore the threshold levels for these soils should be lower. • Although the distribution maps can be used to indicate broad areas of trace element deficiencies and toxicities, more detailed investigations are recommended for areas where problems are experienced. The same methodology could be applied on smaller scale to increase the value of the map and to add more value on a regional scale. The maps could be used for regional soil quality assessment especially in areas where trace element deficiencies or toxicities could result in negative effects on plants and animals.

La présente étude porte sur l’évaluation d’une méthode d’acquisition de la solution de sol présente à l’interface sol-racine, dans la rhizosphère. Cette interface constitue le lieu privilégié de prise en charge par les plantes des contaminants, tels que les métaux traces. Comme les plantes acquièrent ces éléments à partir de la phase liquide, la solution de sol de la rhizosphère est une composante clé pour déterminer la fraction de métaux traces biodisponibles. La microlysimétrie est la méthode in situ la plus appropriée pour aborder les difficultés liées à l’échelle microscopique de la rhizosphère. Ainsi, dans les études sur la biodisponibilité des métaux traces au niveau de la rhizosphère, les microlysimètres (Rhizon©) gagnent en popularité sans, toutefois, avoir fait l’objet d’études exhaustives. L’objectif de cette étude est donc d’évaluer la capacité de ces microlysimètres à préserver l’intégrité chimique de la solution, tout en optimisant leur utilisation. Pour ce faire, les microlysimètres ont été soumis à une série d’expériences en présence de solutions et de sols, où la quantité de solution prélevée et le comportement des métaux traces (Cd, Cu, Ni, Pb, Zn) ont été étudiés. Les résultats montrent que les microlysimètres fonctionnent de façon optimale lorsque le contenu en eau du sol est au-dessus de la capacité au champ et lorsqu’il y a peu de matière organique et d’argile. Les sols sableux ayant un faible contenu en C organique reproduisent mieux le volume prélevé et la solution sous la capacité au champ peut être récoltée. L’utilisation des microlysimètres dans ces sols est donc optimale. Dans les essais en solution, les microlysimètres ont atteint un équilibre avec la solution après 10 h de prélèvement. En respectant ce délai et les conditions optimales préalablement établies (pH acide et COD élevé), les microlysimètres préservent la composition chimique de la solution. Dans les essais en sol, cet équilibre n’a pas été atteint après dix jours et huit prélèvements. Le contenu en matière organique et l’activité microbienne semblent responsables de la modification des concentrations en métaux au cours de ces prélèvements, notamment, dans l’horizon FH où les microlysimètres performent très mal. En revanche, dans l’horizon B, les concentrations tendent à se stabiliser vers la fin de la série de prélèvements en se rapprochant des valeurs de référence. Bien que des valeurs plus élevées s’observent pour les microlysimètres, leurs concentrations en métaux sont comparables à celles des méthodes de référence (extrait à l’eau, lysimètres de terrain avec et sans tension). En somme, les microlysimètres se comportent généralement mieux dans l’horizon B. Même si leur utilisation est plus optimale dans un sol sableux, cet horizon est privilégié pour de futures études sur le terrain avec les microlysimètres. / This study focuses on evaluating a method of acquiring soil solution in the soil-root interface of the rhizosphere. The liquid phase of the rhizosphere constitutes the main area where plants absorb contaminants like trace metals. Thus the rhizosphere soil solution is key to determine the amount of bioavailable trace metals. Microlysimetry has been described as the most appropriate in situ method to tackle difficulties inherent to the microscopic scale of the rhizosphere. Despite the lack of an exhaustive evaluation of their performance, microlysimeters have gained popularity for in situ studies on the bioavailability of trace metals. The objective of this study was to evaluate the capacity of microlysimeter to preserve the chemical integrity of the soil solution and also to determine their optimum use conditions. To do this, microlysimeter have been submitted to a series of laboratory experiments with solutions and soils. The volume of solution extracted and trace metals (Cd, Cu, Ni, Pb, Zn) behaviour were studied. Results show that microlysimeters work optimally when soil water content is above field capacity and when the amount of clay and organic matter is low. Sandy soils with low organic carbon content have a better reproducibility for extracted volume and soil solution extraction is possible even when soil water content is below field capacity. Using microlysimeters in this soil type is thus optimal. In solution experiments, microlysimeters reached equilibrium with the control solution after ten hours of extraction. In optimal conditions (acidic pH and high DOC) and after this ten hours period, microlysimeters preserve the chemical composition of the solution. In soil experiments, this equilibrium has not been reached after eight samplings throughout ten days. Organic matter content and microbial activity could be responsible for the modification of concentrations of trace metals during sampling. This is especially true for FH horizon where microlysimeters perform poorly. In contrast, the concentrations reach the reference values toward the end of sampling serie in the B horizon and microlysimeters have a better overall performance in this horizon. Although higher values are observed for microlysimeters, trace metals concentrations are comparable to other extraction methods, specifically for the B horizon. Even if their uses are optimized in sandy soil, the B horizon should be privileged for future field studies involving microlysimeters.

Le changement d’occupation des sols contaminés est susceptible de modifier la nature et la quantité des matières organiques du sol (MOS). Les matières organiques sont connues pour avoir un rôle de source trophique pour les organismes des sols et un rôle de ligand vis-à-vis des éléments traces métalliques (ETM) dans les sols contaminés. Des changements de matières organiques dus aux changements d’occupation des sols contaminés peuvent modifier la spéciation des ETM et leur disponibilité. Mais dans ce cas, le rôle de la matière organique dans le déterminisme de la disponibilité des ETM est peu documenté. L’objectif du travail présenté dans cette thèse était de mettre en évidence le rôle des matières organiques dans la disponibilité des ETM, dans le cas de sols agricoles contaminés après un changement de cultures annuelles vers des cultures pérennes à vocation non-alimentaire. Le travail a concerné l’étude de la disponibilité du Cu, Pb, Zn et Cd dans les sols de deux sites différents en texture et en origine de pollution i.e. le site de Metaleurop (Nord de la France) avec des sols limoneux contaminés par des retombées atmosphériques et le site de Pierrelaye (Région Parisienne) avec des sols sableux contaminés par les apports d’eaux usées brutes de la ville de Paris. Le rôle de la matière organique a été étudié en travaillant 1) sur des échantillons de sols sous deux cultures différentes i.e. sous culture annuelle et culture pérenne à vocation énergétique miscanthus depuis trois ans, 2) sur les échantillons de sol avant et après incubation in vitro afin d’accélérer la minéralisation de la matière organique, et 3) sur des échantillons de sol avec et sans matières organiques particulaires (MOP) i.e. les fractions libres des MOS afin de mettre en évidence leur rôle spécifique. Une approche combinée d’évaluation de la disponibilité par des extractions chimiques des ETM et d’étude de la localisation des ETM dans des fractions granulométriques a été utilisée. Les résultats obtenus montrent que l’impact de l’occupation des sols (sous culture annuelle ou pérenne miscanthus) sur la disponibilité des ETM était différent pour les deux sites étudiés. Pour les sols du site de Metaleurop les résultats ont montré que la disponibilité de Cu et Pb diminuait sous miscanthus tandis qu’une augmentation de leur localisation dans les fractions fines était observée. Par contre aucun changement n’a été observé pour Zn ni Cd dans ce site. Au contraire pour les sols sableux riches en matières organiques de Pierrelaye le changement d’occupation a impacté la disponibilité de Zn et Cd tandis que celle de Pb et Cu n’a pas évolué. Les résultats des sols avant et après incubation montrent que l’impact de la minéralisation des MOS sur la disponibilité des ETM était site dépendant pour Pb et Cd alors que l’effet sur Cu et Zn était similaire pour les sols des deux sites. En travaillant sur les sols avec et sans MOP, nous avons pu observer que les MOP en tant que fraction organique libre participaient à la disponibilité des ETM telle qu’étudiée, et que une partie du cuivre lié aux MOP était disponible pour un organisme dans nos conditions. Ces résultats de disponibilités des ETM dans des sols qui varient avec la nature et la quantité des matières organiques sont discutés. / The changes in land use of contaminated agricultural soils are susceptible to modify their trace metal availabilities by changing the quality and quantity of soil organic matter. But the role of soil organic matter in the determinism of trace metal availabilities in contaminated soils is not well known. The objective of the present study was to assess the role of soil organic matter in determinism of trace metal availabilities and their dynamics in contaminated soils varying in their texture and nature of pollution. A strategy of studying Cu, Pb, Zn and Cd availabilities of two sites with different texture and origin of pollution was adopted and the role of organic matter was assessed through; 1) sampling the soils of two parcels at each site with two different land uses i.e. under annual crop and under perennial energy crop miscanthus, 2) changing the soil organic matter of these soils through in vitro soil incubations. A combined approach of chemical metal extractions and metal localization study in different soil size fractions was used. The results of the trace metal availabilities of the soil under miscanthus compared to annual crop soil showed that the influence of changes in organic matter through land use was different at both sites. In the silty clayed soil, the availability of Cu and Pb which are the metals known to be preferentially bound to organic matter was decreased with an increase in their localization in soil finer fractions. In the site with organic matter rich sandy soils the availability of metals which are known to be bound to soil mineral phases i.e. Zn and Cd was changed without a change in their localization. The results of laboratory incubation experiments revealed that the mineralization of soil organic matter affects the trace metal availability in two ways. Cu and Zn availabilities are changed in all soils whatever the texture while Pb and Cd availabilities changed only in sandy soils. This difference of the change of metal availabilities in both cases of organic matter variations i.e. between the soil samples under different land use and in the samples of laboratory incubations can be explained by the fact that the changes in organic matter were not similar in both cases. Our work on the metal enriched particulate organic matter (POM) fractions, the most labile organic matter fractions showed that POM act as source and sink of the metals in our conditions and POM associated copper is bioavailable in liquid medium but its bioavailability is less than the metal added as salt solution. These results, increasing the understanding of the role of soil organic matter in the determinism of trace metal availability in different textured soils, are discussed.

Le Morvan et les Cévennes sont des massifs protégés pour leur paysage et leur biodiversité exceptionnels. Cependant dès la Protohistoire, ces régions réputées pour la qualité de leur environnement ont été le lieu d’activités minières et métallurgiques. Les effets de telles activités peuvent être rémanents sur les écosystèmes, il est donc important dans un premier temps de les localiser, puis de quantifier leur impact sur la faune et la flore. Le présent travail propose une démarche pluridisciplinaire alliant archéologie, géochimie, écologie et écotoxicologie. L’application de méthodes statistiques empruntées à la prospection minière a permis de dresser des cartes de potentiel minier, supposées guider l’archéologue dans ses recherches de terrain. Des cartes de distribution spatiale des éléments traces métalliques ont été construites sur six sites (trois dans chaque parc). La biodisponibilité des éléments traces métalliques a été estimée sur des mulots, des truites et des bryophytes. Bien que la plupart de ces éléments semblent appartenir à la fraction non-extractible des sols, la part biodisponible restante peut être détectée dans des bioindicateurs. Une relation négative entre les indices de condition et la concentration en plomb dans les animaux, et dans certains cas une plus grande instabilité de développement a été trouvée, suggérant la présence d’effets délétères sur les organismes. L’impact des anciens sites miniers et métallurgiques est donc toujours décelable dans les écosystèmes actuels. Ces sites doivent être surveillés, notamment au sein des zones protégées supposées à tort comme éloignées de toutes contaminations anthropiques. / The Morvan and the Cevennes Massifs are nowadays protected for their outstanding landscape and biodiversity. However since Prehistory, these regions experienced mining and smelting activities. Because of remnant properties, locating these ancient sites is capital and then impact on fauna and flora must be estimated. This present work is based in on a pluridisciplinary approach combining archeology, geochemistry, ecology and ecotoxicology. Statistical methods, from modern prospection technique, have been applied in order to delineate geochemical anomalies, potentially due to mining exploitation and thus facilitate the archeological prospection. Spatial distribution maps of trace metals were built on six sites (three in each park). Biodisponibility was assessed thanks to the analyses of wood mice, trout and bryophytes. Even if it seems that most of these elements belong to the non-extractible fraction of soil, the remaining bioavailable trace metals can be detected in the bioindicators. A negative relationship between Pb concentrations in animals and their body condition indices was found, and in some cases developmental instability was higher, suggesting deleterious effect on current wildlife. As a consequence, the impact of past mining and smelting works is still traceable in ecosystems. For this reason, these sites should be monitored, particularly in protected areas thought to be relatively free of anthropogenic contamination.

Os recursos hídricos urbanos são de grande importância para os municípios que têm desenvolvimento econômico crescente e aumento demográfico, sendo que a manutenção da qualidade da água dos mananciais de abastecimento para a população é imprescindível para a saúde e para diminuir o custo econômico. A bacia do Alto Jacaré-Guaçu, em cuja área está inserido o município de São Carlos/SP, tem como principais sub bacias a do Rio do Monjolinho e a do Ribeirão do Feijão, sendo este a principal fonte de abastecimento de água para a cidade. O trabalho foi proposto para avaliar a qualidade da água dos recursos hídricos da bacia do Alto Jacaré-Guaçu, através da análise das características limnológicas, das substâncias tóxicas e da comunidade de macroinvertebrados que permitem a indicação da qualidade da água. Foram efetuadas duas campanhas de amostragem em 1999: a) no período chuvoso (em março) e b) no período de estiagem (em agosto). Em março foram realizadas amostragens em 8 pontos e, em agosto, foram acrescidos mais 6 pontos, totalizando 14. Paralelamente, com o intuito de visualizar espacialmente os resultados e desta forma identificar as áreas com maior ou menor grau de impacto, foi elaborado um mapa com as sub-bacias correspondentes às áreas cuja água drena para cada um dos pontos de coleta. Os resultados obtidos demonstram que a qualidade da água no período da estiagem se torna mais critica devido à diminuição do fluxo da água. Com relação à poluição orgânica, a sub bacia do Monjolinho pode ser classificada em 3 grupos: a) trecho sem influência urbana, portanto não poluída ou ligeiramente poluída; b) trecho com influência da área urbana da cidade de São Carlos, sendo assim, fortemente poluída e c) trecho final do Rio Monjolinho, com uma poluição moderada ou em processo de recuperação. Quanto à presença de substâncias tóxicas analisadas as concentrações dos metais, em geral, apresentaram-se dentro dos limites da Resolução CONAMA 20/86, exceto o cobre, ferro, manganês e zinco. Já para os organoclorados, a maior parte da área da bacia não atende a Resolução Brasileira, detectando-se concentrações acima dos limites permitidos. Quanto à identificação dos diferentes impactos no uso da terra e da água na bacia do Alto Jacaré-Guaçu, pode-se citar, entre as atividades antrópicas que vem acelerando o processo de degradação ambiental, principalmente a qualidade da água :1- Falta de tratamento do esgoto doméstico, principalmente na área urbana; 2- Desmatamento contínuo levando a substituição da vegetação natural por monoculturas e pastagens; 3- Uso irregular do solo, causando erosão e assoreamento nos corpos de água; 4- Expansão sem controle da área urbana próximo às margens e principalmente nas nascentes dos corpos de água e 5-Falta de controle na comercialização e uso de defensivos agrícolas. / The water resources in urban areas are important for the municipalities in stage of economical development and demographic increase. The maintenance of quality of the water sources is indispensable for the human health and to reduce the economic costs. The Alto Jacaré-Guaçu basin, situated in São Carlos municipality, has as a principal sub-basins the Monjolinho River and Ribeirão do Feijão basins. Both are the main souce of water supply for the city. This study was proposed to analyze the water quality of the Alto Jacaré-Guaçu basin, according to the limnological conditions, toxic substances and utilization of macroinvertebrates as indicative of the water quality. Sampling was carried out in two periods: a) in the rainy season (March 1999) and b) in the dry season (August 1999). In March 8 stations were sampled, while in August 6 more stations were sampled, totalizing 14 stations. In Parallel, a map was elaborated with the sub-basins corresponding to the drainage area for each station in order to show spatially the results and to identify the areas with bigger or minor degree of impact. The results demonstrated that the water quality in the dry period became critical due to decreasing of the water flow. Concerning to the organic pollution, the sub-basin of Monjolinho can be classified under 3 groups: a) section without urban influence, with no or few pollution; b) section with no or few pollution; b) section with influence of the urban area of São Carlos city, being strongly contaminated and c) final section the Monjolinho River, with a moderate pollution or in process of recovery. In relation to the presence of toxic substances analyzed, the concentrations of metals generally appeared inside the limits of the Resolution CONAMA 20/86, except for copper, iron, manganese and zinc. For the organochlorine pesticides, the concentrations oberseved do not attend to the Brazilian Resolution, because the values were higler than the acceptable limits. Concerning to the identification of different impacts of the land and water uses in the Alto Jacaré-Guaçu basin, it is possible to identify the human activities that accelerate the process of environmental degration, specially for the water quality: 1- The lack of teatment of the domestic residues, specially in the urban area; 2- Continous deforestation and changing of natural vegetation to monocultures and pastures; 3-Irregular uses of the soil causing erosion and collapsing the water bodies; 4- Expansion without control of the urban area next to the margins and specially in the headwaters, and 5- Lack of control in the selling and uses of agricultural pesticides.

Submitted by Biblioteca de Pós-Graduação em Geoquímica BGQ (bgq@ndc.uff.br) on 2017-10-04T15:44:46Z No. of bitstreams: 1 tese_renata_maria_completa.pdf: 1532064 bytes, checksum: db3c7a043c5eecc779b264a3e956dea2 (MD5) / Made available in DSpace on 2017-10-04T15:44:46Z (GMT). No. of bitstreams: 1 tese_renata_maria_completa.pdf: 1532064 bytes, checksum: db3c7a043c5eecc779b264a3e956dea2 (MD5) / Conselho Nacional de Desenvolvimento Científico e Tecnológico / Universidade Federal Fluminense. Instituto de Química. Programa de Pós-Graduação em Geoquímica, Niterói, RJ / Nos últimos anos observa-se um aumento crescente das atividades humanas, tanto científicas quanto turísticas, no ambiente antártico, sendo motivo de preocupação considerando-se que a Antártica é um ambiente de lenta recuperação. Ainda são escassos os estudos sobre o estabelecimento de relações entre a presença de contaminantes e seus efeitos na biota antártica. A contaminação pode ocorrer por processos antrópicos ou naturais e os efeitos destes impactos podem ser detectados e monitorados através da análise das alterações nas comunidades bentônicas. Estas comunidades podem ser consideradas boas indicadoras de impactos ambientais, já que possuem uma relação direta com a origem dos contaminantes acumulados nos sedimentos. Este trabalho avaliou os níveis de metais-traço encontrados no sedimento e em duas espécies circumpolares da megafauna bentônica antártica, a estrela-domar Odontaster validus e o molusco bivalve Laternula elliptica, com a finalidade de determinar se as mesmas podem ser utilizadas como indicadoras de impacto ambiental. Durante o verão austral de 2005/2006 foram realizadas coletas através de diferentes procedimentos, entre 15 e 40m de profundidade, em cinco estações dentro da Área Antártica Especialmente Gerenciada da Baía do Almirantado, Ilha Rei George: 1) Estação Antártica Comandante Ferraz; 2) Botany Point; 3) Punta Ullman; 4) Punta Plaza e 5) Refúgio II. Os seguintes metais foram quantificados tanto para o sedimento quanto para os organismos: Al, V, Cr, Mn, Fe, Ni, Cu, Cd, Ba, Pb e Zn. A concentração de metais variou entre os diferentes compartimentos corpóreos analisados. Para a espécie O. validus, as maiores concentrações de metais-traço (Mn, Ni, Cd, Ba, Pb) e do macronutriente Al, foram encontradas na parede do corpo. Cu, Cr, V e Zn apresentaram maior concentração no estômago, enquanto o macronutriente Fe concentrou-se preferencialmente nos cecos pilóricos. Para a espécie L. elliptica, as maiores concentrações de metais-traço (Mn, V, Ba, Cu) e dos macronutrientes Fe e Al, foram encontradas no sifão. Cd, Ni, Pb e Zn apresentaram maior concentração no rim enquanto o Cr foi mais concentrado no compartimento restos. A concentração de elementostraço nos compartimentos corpóreos de O. validus e L. elliptica não foi influenciada pelo tamanho do organismo (peso total do indivíduo). / Once the Antarctic environment has low recovery rates, the recent growth in the touristic and scientific activities is a serious issue for the scientific community. Few studies have tried to establish the links between the presence of contaminants and the antarctic biota. The contamination may be related to human or natural processes, and be monitored trough the benthic communities. These communities have a direct relation with the contaminants sources in the sediment. The present work analyzed the trace-metals levels found in the sediment and two circumpolar benthic megafauna species in Antarctica, the starfish Odontaster validus and the Antarctic clam Laternula elliptica. The objective was to establish if these species can be used as environmental indicators. Five stations was occupied during the austral summer of 2005/2006, between 15 and 40m deep, in the Antarctic Special Management Area of Admiralty Bay, George King Island: 1) Comandante Ferraz Antarctic Base; 2) Botany Point; 3) Punta Ullman; 4) Punta Plaza and 5) Refúgio II. Analyzes were conducted to quantify the presence of Al, V, Cr, Mn, Fe, Ni, Cu, Cd, Ba, Pb and Zn, both in the sediment and organisms. The metals concentrations vary in the different body compartments. Larger concentrations of (Mn, Ni, Cd, Ba, Pb) trace metals and Al macronutrient were found in the body walls of O. validus. Cu, Cr, V and Zn showed larger concentrations in the stomach and the Fe macronutrient in the caeca pyloric. For L. elliptica, larger trace metals (Mn, V, Ba, Cu) and macronutrients (Fe and Al) concentrations were found in the sifon, while Cd, Ni, Pb and Zn showed larger concentrations in the kidney. Cr presented larger concentrations in the remains compartment. The concentrations of trace elements in both O. validus and L. elliptica were not influenced by the body size (total individual weight).