Efeito da variação do ph e da temperatura de síntese no desempenho de adesivos à base de creosoto vegetal desmetilado-formaldeído

O objetivo deste trabalho foi a produção de adesivos para madeira a partir de creosoto desmetilado. Para isto, foram sintetizadas diferentes formulações de adesivos para madeira a partir de creosoto desmetilado e paraformaldeído, variando-se o pH inicial da formulação (12,00, 12,25, 12,50, 12,75, 13,00, 13,25 e 13,50) e a temperatura de síntese (60 e 70 °C), para possibilitar a verificação dos melhores pHs e da melhor temperatura para elaboração do adesivo. Foi verificado, por meio da avaliação do gel time, que a melhor temperatura de síntese foi 70 °C. Foram realizadas, então, análises por DSC (calorimetria diferencial exploratória), para obtenção dos parâmetros cinéticos e caracterização das formulações adesivas de creosoto desmetilado sintetizadas a 70 °C. Os adesivos foram utilizados para colagem, a quente (160 °C) e sob pressão (12 kgf/cm²), de lâminas de Araucaria angustifolia. Após a colagem, foram realizados os ensaios de resistência mecânica ao cisalhamento por tração, para condição seca e úmida. Verificou-se que a resistência da linha de cola e a porcentagem de falha na madeira para os adesivos de creosoto desmetilado sintetizados a 70 °C foram inferiores às do adesivo de fenol-formaldeído sintetizado em laboratório, que foi utilizado como padrão.

Conservative nutrient use by big-leaf mahogany (Swietenia macrophylla king) planted under contrasting environmental conditions

We analyzed the nutritional composition and isotope ratios (C and N) of big-leaf mahogany (Swietenia macrophylla King) leaves in plantations established on contrasting soils and climates in Central America (State of Quintana Roo, Yucatán, México) and South America (State of Pará, Brazil). The objective was to determine the adaptability of this species to large differences in nutrient availability and rainfall regimes. Nutrient concentrations of leaves and soils were determined spectrophotometrically, and isotope ratios were measured using mass spectrometric techniques.In Pará soils were sandier, and acidic, receiving above 2000 mm of rain, whereas in Quintana Roo soils were predominantly clayey, with neutral to alkaline pH due to the underlying calcareous substrate, with about 1300 mm of rain. Leaf area/weight ratio was similar for both sites, but leaves from Quintana Roo were significantly smaller. Average N and K concentrations of adult leaves were similar, whereas Ca concentration was only slightly lower in Pará in spite of large differences in Ca availability. Leaves from this site had slightly higher P and lower Al concentrations. Differences in water use efficiency as measured by the natural abundance of 13C were negligible, the main effect of lower rainfall in Quintana Roo seemed to be a reduction in leaf area. The N isotope signature (δ15N) was more positive in Pará than in Quintana Roo, suggesting higher denitrification rates in the former. Results reveal a calciotrophic behavior and a remarkable capacity of mahogany to compensate for large differences in soil texture and nutrient availability.

DETERMINACIÓN DE MEDIOS DE CULTIVO Y PH PARA LA MASIFICACIÓN in vitro DE CEPAS DE Suillus luteus Aubl. ASOCIADAS A Pinus radiata D. Don Y Scleroderma citrinum Pers. ASOCIADAS A Eucalyptus globulus Labill. DE LA REGIÓN DEL BIOBÍO, CHILE

El uso de agentes biológicos en la producción en vivero ha aflorado como un elemento que permite no sólo mejorar la calidad morfológica y fisiológica de las plantas, sino que también posibilitar un mayor éxito en el ámbito silvicultural de una plantación. Estos agentes biológicos requieren de un ambiente óptimo para crecer, asociarse y reproducirse. El objetivo de este estudio fue determinar la dependencia del pH y el medio de cultivo en el crecimiento in vitro de distintas cepas de Suillus luteus y Scleroderma citrinum asociadas a Pinus radiata y Eucalyptus globulus, respectivamente. El estudio se realizó en condiciones controladas de temperatura y humedad, disponiendo los inóculos en placas Petri con diferentes medios cultivo, evaluando parámetros de crecimiento y biomasa a los 38 días para S. luteus y 105 días para S. citrinum. Los resultados indican que tanto el medio de cultivo, el pH del medio, así como las cepas de cada especie estudiada, son determinantes en las respuestas de crecimiento de los hongos ectomicorrícicos in vitro evaluados. Las cepas de S. luteus se desarrollaron adecuadamente en un medio de cultivo con abundancia de nutrientes (BAF, MMN) como en baja presencia de ellos (EMA), y con pH más bien ácido (4,8 y 5,8). Por otro lado, las cepas de S. citrinum presentaron, para los mismos ambientes, un desarrollo inferior y lento, no obstante, la cepa Sc8 se reprodujo de forma óptima y rápida bajo un medio de cultivo BAF y con un pH moderadamente ácido de 5,8.

Teor de fósforo e pH no bulbo molhado, com diferentes freqüências de fertirrigação, utilizando ácido fosfórico

A aplicação de fertilizantes fosfatados, tais como superfosfofato simples, superfosfofato triplo e monofosfato de amônio, via gotejamento, pode apresentar incrustações nas canalizações e obstruções de emissores. No presente trabalho, realizado na UNESP/Jaboticabal - SP, estudaram-se a distribuição do fósforo e a sua influência sobre o pH e a umidade em Latossolo Vermelho, fertirrigado durante um mês, com cinco aplicações semanais de ácido fosfórico. Utilizaram-se quatro repetições e oito tratamentos, constituídos da combinação de doses de P2O5 (0 e 50 kg ha-1) e freqüências de aplicação de 1; 3; 5 e 7 dias. Pelos resultados obtidos, observou-se que a freqüência de irrigação ou de fertirrigação não influenciou na distribuição final da umidade no bulbo molhado; aplicando-se o ácido fosfórico, o pH do solo até 30 cm do gotejador e até 40 cm em profundidade foi reduzido, atingindo valor de 3,6, e o teor de fósforo foi maior nessa mesma porção do bulbo, ultrapassando 1.500 mg dm-3. Isso permite indicar que o ácido fosfórico pode ser utilizado em irrigação localizada, com controle do pH do solo, pois sua redução influencia no desenvolvimento das culturas e, conseqüentemente, na produtividade.

Efeito da concentração de coagulantes e do pH da solução na turbidez da água, em recirculação, utilizada no processamento dos frutos do cafeeiro

Com o objetivo de determinar a dose e a faixa de pH dos coagulantes sulfato de alumínio (SA), sulfato ferroso clorado (SFC), cloreto férrico (CF) e extrato de semente de moringa (ESM), que proporcionassem maior eficiência na remoção da turbidez na água residuária da despolpa de frutos do cafeeiro (ARDC), após serem efetuadas cinco recirculações, foram conduzidos ensaios de coagulação/floculação utilizando o aparelho "Jar-test". Todos esses coagulantes foram avaliados nas concentrações de 0; 0,5; 1,0; 1,5; 2,0; 2,5 e 3,0 g L-1. No caso da solução preparada com ESM, as doses utilizadas foram: 0; 10; 20; 30; 40; 50 e 60 mL L-1. O pH da solução em teste foi alterado, utilizando-se do hidróxido de sódio (NaOH), na concentração de 0,3 mol L-1, sendo avaliadas as faixas de 4,0 a 5,0; 5,0 a 6,0; 6,0 a 7,0 e 7,0 a 8,0. No ensaio de coagulação/floculação, o ESM proporcionou maior remoção de SS (sólidos em suspensão) da ARDC com a dose de 10 mL L-1 e pH de 4,27 (natural). Para os coagulantes SA e CF, os melhores resultados foram obtidos com a concentração de 3 g L-1 e pH de 7,27 e, para o coagulante SFC, com a concentração de 3 g L-1 e pH de 4,27.

Climate driven changes in temperature, pH and food quality : effects on copepod reproduction

Increased emissions of greenhouse gases into the atmosphere are causing an anthropogenic climate change. The resulting global warming challenges the ability of organisms to adapt to the new temperature conditions. However, warming is not the only major threat. In marine environments, dissolution of carbon dioxide from the atmosphere causes a decrease in surface water pH, the so called ocean acidification. The temperature and acidification effects can interact, and create even larger problems for the marine flora and fauna than either of the effects would cause alone. I have used Baltic calanoid copepods (crustacean zooplankton) as my research object and studied their growth and stress responses using climate predictions projected for the next century. I have studied both direct temperature and pH effects on copepods, and indirect effects via their food: the changing phytoplankton spring bloom composition and toxic cyanobacterium. The main aims of my thesis were: 1) to find out how warming and acidification combined with a toxic cyanobacterium affect copepod reproductive success (egg production, egg viability, egg hatching success, offspring development) and oxidative balance (antioxidant capacity, oxidative damage), and 2) to reveal the possible food quality effects of spring phytoplankton bloom composition dominated by diatoms or dinoflagellates on reproducing copepods (egg production, egg hatching, RNA:DNA ratio). The two copepod genera used, Acartia sp. and Eurytemora affinis are the dominating mesozooplankton taxa (0.2 – 2 mm) in my study area the Gulf of Finland. The 20°C temperature seems to be within the tolerance limits of Acartia spp., because copepods can adapt to the temperature phenotypically by adjusting their body size. Copepods are also able to tolerate a pH decrease of 0.4 from present values, but the combination of warm water and decreased pH causes problems for them. In my studies, the copepod oxidative balance was negatively influenced by the interaction of these two environmental factors, and egg and nauplii production were lower at 20°C and lower pH, than at 20°C and ambient pH. However, presence of toxic cyanobacterium Nodularia spumigena improved the copepod oxidative balance and helped to resist the environmental stress, in question. In addition, adaptive maternal effects seem to be an important adaptation mechanism in a changing environment, but it depends on the condition of the female copepod and her diet how much she can invest in her offspring. I did not find systematic food quality difference between diatoms and dinoflagellates. There are both good and bad diatom and dinoflagellate species. Instead, the dominating species in the phytoplankton bloom composition has a central role in determining the food quality, although copepods aim at obtaining as a balanced diet as possible by foraging on several species. If the dominating species is of poor quality it can cause stress when ingested, or lead to non-optimal foraging if rejected. My thesis demonstrates that climate change induced water temperature and pH changes can cause problems to Baltic Sea copepod communities. However, their resilience depends substantially on their diet, and therefore the response of phytoplankton to the environmental changes. As copepods are an important link in pelagic food webs, their future success can have far reaching consequences, for example on fish stocks.

Testate amoebae (thecamoebians) as indicators of aquatic mine impact

The environmental impacts of a single mine often remain local, but acidic and metal-rich acid mine drainage (AMD) from the waste materials may pose a serious threat to adjacent surface waters and their ecosystems. Testate amoebae (thecamoebian) analysis was used together with lake sediment geochemistry to study and evaluate the ecological effects of sulphidic metal mines on aquatic environments. Three different mines were included in the study: Luikonlahti Cu-mine in Kaavi, eastern Finland, Haveri Cu-Au mine in Ylöjärvi, southern Finland and Pyhäsalmi Zn-Cu-S mine in Pyhäjärvi, central Finland. Luikonlahti and Haveri are closed mines, but Pyhäsalmi is still operating. The sampling strategy was case specific, and planned to provide a representative sediment sample series to define natural background conditions, to detect spatial and temporal variations in mine impacts, to evaluate the possible recovery after the peak contamination, and to distinguish the effects of other environmental factors from the mining impacts. In the Haveri case, diatom analyses were performed alongside thecamoebian analysis to evaluate the similarities and differences between the two proxies. The results of the analyses were investigated with multivariate methods (direct and indirect ordinations, diversity and distance measure indices). Finally, the results of each case study were harmonized, pooled, and jointly analyzed to summarize the results for this dissertation. Geochemical results showed broadly similar temporal patterns in each case. Concentrations of ions in the pre-disturbance samples defined the natural baseline against which other results were compared. The beginning of the mining activities had only minor impacts on sediment geochemistry, mainly appearing as an increased clastic input into the lakes at Haveri and Pyhäsalmi. The active mining phase was followed by the metallic contamination and, subsequently, by the most recent change towards decreased but still elevated metal concentrations in the sediments. Because of the delay in the oxidation of waste material and formation of AMD, the most intense, but transient metal contamination phase occurred in the post-mining period at Luikonlahti and Haveri. At Pyhäsalmi, the highest metal contamination preceded effluent mitigation actions. Spatial gradients were observed besides the temporal evolution in both the pre-disturbance and mine-impacted samples from Luikonlahti and Pyhäsalmi. The geochemical gradients varied with distance from the main source of contaminants (dispersion and dilution) and with water depth (redox and pH). The spatial extent of the highest metal contamination associated with these mines remained rather limited. At Haveri, the metallic impact was widespread, with the upstream site in another lake basin found to be contaminated. Changes in thecamoebian assemblages corresponded well with the geochemical results. Despite some differences, the general features and ecological responses of the faunal assemblages were rather similar in each lake. Constantly abundant strains of Difflugia oblonga, Difflugia protaeiformis and centropyxids formed the core of these assemblages. Increasing proportions of Cucurbitella tricuspis towards the surface samples were found in all of the cases. The results affirmed the indicator value of some already known indicator forms, but such as C. tricuspis and higher nutrient levels, but also elicited possible new ones such as D. oblonga ‘spinosa’ and clayey substrate, high conductivity and/or alkalinity, D. protaeiformis ‘multicornis’ and pH, water hardness and the amount of clastic material and Centropyxis constricta ‘aerophila’ and high metal and S concentrations. In each case, eutrophication appeared to be the most important environmental factor, masking the effects of other variables. Faunal responses to high metal inputs in sediments remained minor, but were nevertheless detectable. Besides the trophic state of the lake, numerical methods suggested overall geochemical conditions (pH, redox) to be the most important factor at Luikonlahti, whereas the Haveri results showed the clearest connection between metals and amoebae. At Pyhäsalmi, the strongest relationships were found between Ca- and S-rich present loading, redox conditions and substrate composition. Sediment geochemistry and testate amoeba analysis proved to be a suitable combination of methods to detect and describe the aquatic mine impacts in each specific case, to evaluate recovery and to differentiate between the effects of different anthropogenic and natural environmental factors. It was also suggested that aquatic mine impacts can be significantly mitigated by careful design and after-care of the waste facilities, especially by reducing and preventing AMD. The case-specific approach is nevertheless necessary because of the unique characteristics of each mine and variations in the environmental background conditions.

Element speciation and behaviour in metal-rich Boreal river and estuarine systems using ultrafiltration and chemical modelling

The bioavailability of metals and their potential for environmental pollution depends not simply on total concentrations, but is to a great extent determined by their chemical form. Consequently, knowledge of aqueous metal species is essential in investigating potential metal toxicity and mobility. The overall aim of this thesis is, thus, to determine the species of major and trace elements and the size distribution among the different forms (e.g. ions, molecules and mineral particles) in selected metal-enriched Boreal river and estuarine systems by utilising filtration techniques and geochemical modelling. On the basis of the spatial physicochemical patterns found, the fractionation and complexation processes of elements (mainly related to input of humic matter and pH-change) were examined. Dissolved (<1 kDa), colloidal (1 kDa-0.45 μm) and particulate (>0.45 μm) size fractions of sulfate, organic carbon (OC) and 44 metals/metalloids were investigated in the extremely acidic Vörå River system and its estuary in W Finland, and in four river systems in SW Finland (Sirppujoki, Laajoki, Mynäjoki and Paimionjoki), largely affected by soil erosion and acid sulfate (AS) soils. In addition, geochemical modelling was used to predict the formation of free ions and complexes in these investigated waters. One of the most important findings of this study is that the very large amounts of metals known to be released from AS soils (including Al, Ca, Cd, Co, Cu, Mg, Mn, Na, Ni, Si, U and the lanthanoids) occur and can prevail mainly in toxic forms throughout acidic river systems; as free ions and/or sulfate-complexes. This has serious effects on the biota and especially dissolved Al is expected to have acute effects on fish and other organisms, but also other potentially toxic dissolved elements (e.g. Cd, Cu, Mn and Ni) can have fatal effects on the biota in these environments. In upstream areas that are generally relatively forested (higher pH and contents of OC) fewer bioavailable elements (including Al, Cu, Ni and U) may be found due to complexation with the more abundantly occurring colloidal OC. In the rivers in SW Finland total metal concentrations were relatively high, but most of the elements occurred largely in a colloidal or particulate form and even elements expected to be very soluble (Ca, K, Mg, Na and Sr) occurred to a large extent in colloidal form. According to geochemical modelling, these patterns may only to a limited extent be explained by in-stream metal complexation/adsorption. Instead there were strong indications that the high metal concentrations and dominant solid fractions were largely caused by erosion of metal bearing phyllosilicates. A strong influence of AS soils, known to exist in the catchment, could be clearly distinguished in the Sirppujoki River as it had very high concentrations of a metal sequence typical of AS soils in a dissolved form (Ba, Br, Ca, Cd, Co, K, Mg, Mn, Na, Ni, Rb and Sr). In the Paimionjoki River, metal concentrations (including Ba, Cs, Fe, Hf, Pb, Rb, Si, Th, Ti, Tl and V; not typical of AS soils in the area) were high, but it was found that the main cause of this was erosion of metal bearing phyllosilicates and thus these metals occurred dominantly in less toxic colloidal and particulate fractions. In the two nearby rivers (Laajoki and Mynäjoki) there was influence of AS soils, but it was largely masked by eroded phyllosilicates. Consequently, rivers draining clay plains sensitive to erosion, like those in SW Finland, have generally high background metal concentrations due to erosion. Thus, relying on only semi-dissolved (<0.45 μm) concentrations obtained in routine monitoring, or geochemical modelling based on such data, can lead to a great overestimation of the water toxicity in this environment. The potentially toxic elements that are of concern in AS soil areas will ultimately be precipitated in the recipient estuary or sea, where the acidic metalrich river water will gradually be diluted/neutralised with brackish seawater. Along such a rising pH gradient Al, Cu and U will precipitate first together with organic matter closest to the river mouth. Manganese is relatively persistent in solution and, thus, precipitates further down the estuary as Mn oxides together with elements such as Ba, Cd, Co, Cu and Ni. Iron oxides, on the contrary, are not important scavengers of metals in the estuary, they are predicted to be associated only with As and PO4.

Saturação de oxigênio fetal medida pela oximetria de pulso durante o trabalho de parto: relações com o ph da artéria umbilical

Objetivos: estudar os níveis de saturação de oxigênio fetal (SpO2) durante o trabalho de parto pela técnica da oximetria de pulso e sua relação com o pH da artéria umbilical (AU). Pacientes e Métodos: a SpO2 fetal foi medida durante o parto por meio da técnica da oximetria de pulso em 50 casos. Comparou-se a média dos valores de SpO2 entre os dois períodos do trabalho de parto, sendo o primeiro subdividido em fases, segundo a dilatação cervical (<=4 cm, 5-7 cm e 8-9 cm). Os valores de SpO2 foram estudados em função do pH da AU ao nascimento ( > ou = 7,20 e <7,20). Considerou-se como normal uma SpO2 > ou = 30,0%. Resultados: as médias da SpO2 fetal no primeiro período do parto foram de 53,0 ± 7,3% e 44,2 ± 6,8%, e no segundo 46,8 ± 7,7% e 38,4 ± 7,1% (pH da AU > ou = 7,20 e <7,20, respectivamente; p<0,01). Quando o primeiro período foi subdividido, as médias de SpO2 (pH de AU > ou = 7,20) foram de 55,1 ± 5,1% (<=4 cm), 52,3 ± 4,6% (5-7 cm) e 51,5 ± 7,2% (8-9 cm); para um pH de AU <7,20 as médias de SpO2 de 46,3 ± 5,1% (<=4 cm), 43,6 ± 6,7% (5-7 cm) e 42,8 ± 5,8% (8-9 cm). Considerando o pH da AU estas diferenças foram significantes (p<0,01). Conclusões: houve um decréscimo significante dos valores de SpO2 fetal durante o trabalho de parto quando utilizada a técnica da oximetria de pulso.

Oximetria fetal de pulso: relação entre a saturação de oxigênio do segundo período do parto e o pH da artéria umbilical ao nascimento

Objetivo: estudar a correlação entre a saturação de oxigênio fetal medida pela oximetria de pulso durante o segundo período do parto e o pH da artéria umbilical ao nascimento. Pacientes e Métodos: a saturação de oxigênio fetal (FSpO2) foi monitorizada pela oximetria de pulso durante o segundo período do trabalho de parto em 64 gestações simples a termo com apresentação de vértice. O sangue dos vasos umbilicais foi obtido imediatamente após o nascimento para subseqüente medida dos gases e do pH venoso e arterial. Todos os fetos mantiveram a FSpO2 > ou = 30% durante o primeiro período do parto, até o início do segundo período. Resultados: a média da FSpO2 durante o segundo período do parto correlacionou-se significantemente com o pH da artéria umbilical ao nascimento (n = 64, r = 0,79, p<0,001). Não houve correlação significante entre a FSpO2 no segundo período do parto e a saturação de oxigênio do sangue da artéria umbilical ao nascimento. Conclusão: a saturação de oxigênio fetal medida pela oximetria de pulso durante o segundo período do trabalho de parto tem uma boa correlação com o pH da artéria umbilical ao nascimento.

Correlação entre Testes para Avaliação da Vitalidade Fetal, pH da Artéria Umbilical e os Resultados Neonatais em Gestações de Alto Risco

Objetivos: analisar a relação entre valores de pH no nascimento, testes de vitalidade fetal e resultados neonatais. Métodos: foram incluídas 1346 pacientes com gestação de alto risco atendidas no Setor de Vitalidade Fetal do HCFMUSP. Para estudo do bem-estar fetal foram realizados exames de cardiotocografia, perfil biofísico fetal e índice de líquido amniótico. Após o parto foram obtidos os seguintes parâmetros dos recém-nascidos: idade gestacional no parto, sexo e peso dos recém-nascidos, índices de Apgar de 1º e 5º minutos, pH da artéria umbilical no nascimento e a ocorrência de óbito neonatal. Para estudo destes resultados neonatais, os casos foram divididos em quatro grupos: G1 (pH <7,05), G2 (pH de 7,05 a 7,14); G3 (pH de 7,15 a 7,19) e G4 (pH > ou = 7,20). Resultados: a cardiotocografia anormal relacionou-se com valores de pH inferiores a 7,20 (p = 0,001). Resultados anormais do perfil biofísico fetal (<=4) foram mais freqüentes à medida que os valores de pH decresceram (p<0,001). Resultados neonatais adversos relacionaram-se à presença de acidose no nascimento, sendo selecionados para o ajuste do modelo de regressão logística. Este modelo revelou que o "odds ratio" referente a cada condição neonatal eleva-se significativamente com o decréscimo do pH no nascimento. Conclusões: observa-se correlação significativa entre valores de pH no nascimento e resultados neonatais, sendo possível estimar o risco neonatal a que é exposto o produto conceptual utilizando-se do pH no nascimento.

Efeito da heparina liofilizada e da líquida sobre a medida do pH do sangue do cordão umbilical

OBJETIVO: avaliar o efeito da heparina liofilizada e da líquida sobre a medida do pH do sangue do cordão umbilical. MÉTODOS: estudo prospectivo que incluiu cento e duas amostras de sangue arterial do cordão umbilical de recém-nascidos no Serviço de Obstetrícia do Hospital Geral de Caxias do Sul. As amostras foram divididas em 51 seringas previamente preparadas com heparina liofilizada (seringa A) e 51 seringas preparadas com heparina líquida (seringa B) no momento da coleta sangüínea. A obtenção das amostras foi realizada por duplo clampeamento do cordão entre pinças, imediatamente após o desprendimento fetal. O pH arterial do sangue obtido foi analisado em no máximo 20 minutos, em analisador de pH da marca AVL OMNI (Viena, Áustria). RESULTADOS: a média dos valores de pH no sangue contido nas seringas dos grupos A e B foi de 7,246±0,086 e 7,244±0,084, respectivamente. A análise estatística demonstrou não haver diferença significante entre os valores de pH entre as amostras de sangue contidas em ambos os conjuntos de seringas. CONCLUSÃO: as duas formas de heparinização de seringas assemelham-se quanto aos efeitos sobre o pH do sangue dos vasos umbilicais, o que permite a escolha daquela de menor custo.

Acidic dissolution of iron oxides and regeneration of a ceramic filter medium

The dewatering of iron ore concentrates requires large capacity in addition to producing a cake with low moisture content. Such large processes are commonly energy intensive and means to lower the specific energy consumption are needed. Ceramic capillary action disc filters incorporate a novel filter medium enabling the harnessing of capillary action, which results in decreased energy consumption in comparison to traditional filtration technologies. As another benefit, the filter medium is mechanically and chemically more durable than, for example, filter cloths and can, thus, withstand harsh operating conditions and possible regeneration better than other types of filter media. In iron ore dewatering, the regeneration of the filter medium is done through a combination of several techniques: (1) backwashing, (2) ultrasonic cleaning, and (3) acid regeneration. Although it is commonly acknowledged that the filter medium is affected by slurry particles and extraneous compounds, published research, especially in the field of dewatering of mineral concentrates, is scarce. Whereas the regenerative effect of backwashing and ultrasound are more or less mechanical, regeneration with acids is based on chemistry. The chemistry behind the acid regeneration is, naturally, dissolution. The dissolution of iron oxide particles has been extensively studied over several decades but those studies may not necessarily be directly applicable in the regeneration of the filter medium which has undergone interactions with the slurry components. The aim of this thesis was to investigate if free particle dissolution indeed correlates with the regeneration of the filter medium. For this purpose, both free particle dissolution and dissolution of surface adhered particles were studied. The focus was on acidic dissolution of iron oxide particles and on the study of the ceramic filter medium used in the dewatering of iron ore concentrates. The free particle dissolution experiments show that the solubility of synthetic fine grained iron oxide particles in oxalic acid could be explained through linear models accounting for the effects of temperature and acid concentration, whereas the dissolution of a natural magnetite is not so easily explained by such models. In addition, the kinetic experiments performed both support and contradict the work of previous authors: the suitable kinetic model here supports previous research suggesting solid state reduction to be the reaction mechanism of hematite dissolution but the formation of a stable iron oxalate is not supported by the results of this research. Several other dissolution mechanisms have also been suggested for iron oxide dissolution in oxalic acid, indicating that the details of oxalate promoted reductive dissolution are not yet agreed and, in this respect, this research offers added value to the community. The results of the regeneration experiments with the ceramic filter media show that oxalic acid is highly effective in removing iron oxide particles from the surface of the filter medium. The dissolution of those particles did not, however, exhibit the expected behaviour, i.e. complete dissolution. The results of this thesis show that although the regeneration of the ceramic filter medium with acids incorporates the dissolution of slurry particles from the surface of the filter medium, the regeneration cannot be assessed purely based upon free particle dissolution. A steady state, dependent on temperature and on the acid concentration, was observed in the dissolution of particles from the surface even though the limit of solubility of free iron oxide particles had not been reached. Both the regeneration capacity and efficiency, with regards to the removal of iron oxide particles, was found to be temperature dependent, but was not affected by the acid concentration. This observation further suggests that the removal of the surface adhered particles does not follow the dissolution of free particles, which do exhibit a dependency on the acid concentration. In addition, changes in the permeability and in the pore structure of the filter medium were still observed after the bulk concentration of dissolved iron had reached a steady state. Consequently, the regeneration of the filter medium continued after the dissolution of particles from the surface had ceased. This observation suggests that internal changes take place at the final stages of regeneration. The regeneration process could, in theory, be divided into two, possibly overlapping, stages: (1) dissolution of surface-adhered particles, and (2) dissolution of extraneous compounds from within the pore structure. In addition to the fundamental knowledge generated during this thesis, tools to assess the effects of parameters on the regeneration of the ceramic filter medium are needed. It has become clear that the same tools used to estimate the dissolution of free particles cannot be used to estimate the regeneration of a filter medium unless only a robust characterisation of the order of regeneration efficiency is needed.

Estudo comparativo entre o teste do pH e do KOH versus escore de Nugent para diagnóstico da vaginose bacteriana em gestantes

OBJETIVO: Aquilatar a prevalência da vaginose bacteriana e comparar a acurácia dos testes do pH e do KOH com o gradiente de Nugent, método padrão-ouro, no diagnóstico da vaginose bacteriana (VB) em gestantes assintomáticas e sintomáticas de baixo risco. MÉTODOS: Foi realizado um estudo de corte transversal em 321 grávidas, com idade gestacional entre 14ª e 26ª semanas, 218 assintomáticas e 103 com queixa de secreção vaginal sugestiva de vaginose bacteriana. Todas as gestantes foram avaliadas pelos critérios de Nugent e submetidas à pHmetria vaginal e ao teste do KOH a 10%. O coeficiente de Kappa foi utilizado para avaliar os métodos quanto à concordância diagnóstica. RESULTADO: A maioria das gestantes era adolescente (média etária 21,0±5,6 anos), nulípara e parda. A prevalência da vaginose bacteriana foi de 33,3% pelo método de pH e KOH e de 35,5% pelo Nugent. Entre as grávidas assintomáticas, foi observada ótima concordância dos métodos, com 72,5% delas apresentando resultados negativos para ambos os métodos, o que resultou em um elevado coeficiente de Kappa (k=0,82). No grupo de gestantes sintomáticas, houve 49,5% de positividade para ambos os métodos diagnósticos, demonstrando ótima concordância (k=0,74). CONCLUSÃO: A prevalência da vaginose bacteriana foi elevada tanto pelo método de pH e KOH quanto pelo Nugent. O método do pH e KOH é tão capaz em diagnosticar a vaginose bacteriana quanto os critérios de Nugent.