Deep weathering of calcareous sedimentary rock and the redistribution of iron and manganese in soil and saprolite

Iron and Mn redistribute in soil and saprolite during weathering. The geological weathering fronts ofcalcareous sedimentary rock were investigated by examining the bulk density, porosity, and distribution ofCa, Fe, and Mn. Core samples were taken ofsoil, saprolite, and bedrock material from both summit (HHMS-4B) and sideslope (HHMS-5A) positions on an interbedded Nolichucky shale and Maryville limestone landform in Solid Waste Storage Area 6 (SWSA-6). This is a low-level radioactive solids waste disposal site on the Dept. ofEnergy (DOE) Oak Ridge Reservation in Roane County Tennessee. This work was initiated because data about the properties of highly weathered sedimentary rock on this site were limited. The core samples were analyzed for pH, calcium carbonate equivalence (CCE), hydroxylamine-extractable (HA) Mn, and dithionite-citrate (CBD)-extractable Fe and Mn. Low pH values occurred from the soil surface down to the depth of the oxidized and leached saprolite in both cores. The CCE and HA-extractable Mn results were also influenced by the weathering that has occurred in these zones. Extractable Mn oxide was higher at a lower depth in the oxidized and leached saprolite compared with the Fe oxide, which was higher in the overlying soil solum. Amounts of Mn oxides were higher in the sideslope core (HHMS-5A) than in the summit core (HHMS-4B). Iron was more abundant in the deeper weathered summit core, but the highest value, 39.4 g kg-1, was found at 1.8 to 2.4 m in the sideslope core. The zone encompassing the oxidized and partially leached saprolite down to the unoxidized and unleached bedrock had higher densities and larger quantities of CaCO3 than the soil solum and oxidized and leached saprolite. The overlying soil and oxidized and leached saprolite had lower pH and CCE values and were higher in Fe and Mn oxides than the oxidized and unleached saprolite. The distribution of Fe and Mn is important when evaluating soil and saprolite for hazardous waste disposal site assessment.

Room-temperature ionic liquids as replacements for organic solvents in multiphase bioprocess operations

Organic solvents are widely used in a range of multiphase bioprocess operations including the liquid-liquid extraction of antibiotics and two-phase biotransformation reactions. There are, however, considerable problems associated with the safe handling of these solvents which relate to their toxic and flammable nature. In this work we have shown for the first time that room-temperature ionic liquids, such as 1-butyl-3-methylimidazolium hexafluorophosphate, [bmim][PF6], can be successfully used in place of conventional solvents for the liquid-liquid extraction of erythromycin-A and for the Rhodococcus R312 catalyzed biotransformation of 1,3-dicyanobenzene (1,3-DCB) in a liquid-liquid, two-phase system. Extraction of erythromycin with either butyl acetate or [bmim][PF6] showed that values of the equilibrium partition coefficient, K, up to 20-25 could be obtained for both extractants. The variation of K with the extraction pH was also similar in the pH range 5-9 though differed significantly at higher pH values. Biotransformation of 1,3-DCB in both water-toluene and water-[bmim][PF6] systems showed similar profiles for the conversion of 1,3-DCB initially to 3-cyanobenzamide and then 3-cyanobenzoic acid. The initial rate of 3-cyanobenzamide production in the water-[bmim][PF6] system was somewhat lower, however, due to the reduced rate of 1,3-DCB mass transfer from the more viscous [bmim] [PF,] phase. it was also shown that the specific activity of the biocatalyst in the water-[bmim][PF6] system was almost an order of magnitude greater than in the water-toluene system which suggests that the rate of 3-cyanobenzamide production was limited by substrate mass transfer rather than the activity of the biocatalyst. (C) 2000 John Wiley & Sons, Inc.

Solid-bound, proton-driven, fluorescent ‘off–on–off’ switches based on PET (photoinduced electron transfer)

Anthracene-based, H+-driven, ‘off–on–off’ fluorescent PET (photoinduced electron transfer) switches are immobilized on organic and inorganic polymeric solids in the form of Tentagel® and silica, respectively. The environment of the organic bead displaces apparent switching thresholds towards lower pH values whereas the Si–O- groups of silica electrostatically cause the opposite effect. These switches are ternary logic gate tags, one of which can be particularly useful in strengthening molecular computational identification (MCID) of small solid objects.

Verification of McCabe's Delta L Law for Growth of Lysozyme Crystals by Hanging Drop Method

Lysozyme is a naturally occurring enzyme in egg white and has high commercial importance due to its antimicrobial properties. The main objective of this work was to study the growth rate of lysozyme crystals isolated from egg for the first 72 hours and verify the results with McCabe’s constant crystal growth theory. Hanging drop crystallization method was used to form high purity lysozyme crystals from the embryonic stage. To this end, this work differs from an earlier work of Forsythe et al., who used seed crystals in the size range of 10 µm - 40 µm for face growth measurements at different pH values. The maximum crystal size recorded in the present work was 392.86 µm, which is within the typical size range of 50 µm - 500 µm for which constant crystal growth is expected to hold according to McCabe’s ?L law. Electron micrographs (SEM) revealed the structure and dimensions of the crystals while SDS-Page was used to measure the purity of the crystals. The SEM results showed that that lysozyme growth rate was linear and agreed with McCabe’s constant growth theory, producing a growth rate of 1.77 x 10-3 µm .s-1

Adsorption and photocatalytic bleaching of acid orange 7 on P25 titania

The observed adsorption of acid orange 7, AO7(-), on P25 titania over a range of pH values (pH 2-8) gives a good fit to data generated using a charge distribution, multisite complexation, i.e. CD-MUSIC, model, modified for aggregated dye adsorption. For this system the model predicts that both the apparent dark Langmuir adsorption constant. K-L, and the number of adsorption sites, n(o), increase with decreasing pH, and are negligible above pH 6. At pH 2 the CD-MUSIC model predicts the fraction of singly co-ordinated sites occupied by the dye,f(AO7), is ca. 32% under the in situ monitoring experimental conditions used in this work to study the photocatalytic bleaching of AO7(-) under UV light illumination ([TiO2] = 20 mgdm(-3); [AO7(-)](total) = 4.86 x 10(-5) M). Although AO7(-) adsorption on P25 titania is insignificant above pH 6 and increases almost linearly and markedly below this pH, the measured initial rate of bleaching of AO7(-), photocatalysed by titania using UV appears to only increase modestly (

Modelling and fixed bed column adsorption of Cr(VI) onto orthophosphoric acid-activated lignin

The advantage of using an available and abundant residual biomass, such as lignin, as a raw material for activated carbons is that it provides additional economical interest to the technical studies. In the current investigation, a more complete understanding of adsorption of Cr(VI) from aqueous systems onto H PO -acid activated lignin has been achieved via microcolumns, which were operated under various process conditions. The practice of using microcolumn is appropriate for defining the adsorption parameters and for screening a large number of potential adsorbents. The effects of solution pH (2-8), initial metal ion concentration (0.483-1.981 mmol·L ), flow rate (1.0-3.1 cm ·min ), ionic strength (0.01-0.30 mmol·L ) and adsorbent mass (0.11-0.465 g) on Cr(VI) adsorption were studied by assessing the microcolumn breakthrough curve. The microcolumn data were fitted by the Thomas model, the modified Dose model and the BDST model. As expected, the adsorption capacity increased with initial Cr(VI) concentration. High linear flow rates, pH values and ionic strength led to early breakthrough of Cr(VI). The model constants obtained in this study can be used for the design of pilot scale adsorption process. © 2012 Chemical Industry and Engineering Society of China (CIESC) and Chemical Industry Press (CIP).

Phenol degradation by powdered metal ion modified titanium dioxide photocatalysts

Conventional water purification and disinfection generally involve potentially hazardous substances, some of which known to be carcinogenic in nature. Titanium dioxide photocatalytic processes provide an effective route to destroy hazardous organic contaminants. This present work explores the possibility of the removal of organic pollutants (phenol) by the application of TiO2 based photocatalysts. The production of series of metal ions doped or undoped TiO2 were carried out via a sol–gel method and a wet impregnation method. Undoped TiO2 and Cu doped TiO2 showed considerable phenol degradation. The efficiency of photocatalytic reaction largely depends on the photocatalysts and the methods of preparation the photocatalysts. The doping of Fe, Mn, and humic acid at 1.0 M% via sol–gel methods were detrimental for phenol degradation. The inhibitory effect of initial phenol concentration on initial phenol degradation rate reveals that photocatalytic decomposition of phenol follows pseudo zero order reaction kinetics. A concentration of > 1 g/L TiO2 and Cu doped TiO2 is required for the effective degradation of 50 mg/L of phenol at neutral pH. The rise in OH- at a higher pH values provides more hydroxyl radicals which are beneficial of phenol degradation. However, the competition among phenoxide ion, Cl- and OH- for the limited number of reactive sites on TiO2 will be a negative influence in the generation of hydroxyl radical. The dependence of phenol degradation rate on the light intensity was observed, which also implies that direct sunlight can be a substitute for the UV lamps and that photocatalytic treatment of organic pollutants using this technique shows some promise.

Antimony bioavailability in mine soils

Five British former mining and smelting sites were investigated and found to have levels of total Sb of up to 700 mg kg(-1), indicating high levels of contamination which could be potentially harmful. However, this level of Sb was found to be biologically unavailable over a wide range of pH values, indicating that Sb is relatively unreactive and immobile in the surface layers of the soil, remaining where it is deposited rather than leaching into lower horizons and contaminating ground water. Sb, sparingly soluble in water, was unavailable to the bacterial biosensors tested. The bioluminescence responses were correlated to levels of co-contaminants such as arsenic and copper, rather than to Sb concentrations. This suggests that soil contamination by Sb due to mining and smelting operations is not a severe risk to the environment or human health provided that it is present as immobile species and contaminated sites are not used for purposes which increase the threat of exposure to identified receptors. Co-contaminants such as arsenic and copper are more bioavailable and may therefore be seen as a more significant risk.

A single-component multidrug transporter of the major facilitator superfamily is part of a network that protects Escherichia coli from bile salt stress

Resistance to high concentrations of bile salts in the human intestinal tract is vital for the survival of enteric bacteria such as Escherichia coli. Although the tripartite AcrAB-TolC efflux system plays a significant role in this resistance, it is purported that other efflux pumps must also be involved. We provide evidence from a comprehensive suite of experiments performed at two different pH values (7.2 and 6.0) that reflect pH conditions that E. coli may encounter in human gut that MdtM, a single-component multidrug resistance transporter of the major facilitator superfamily, functions in bile salt resistance in E. coli by catalysing secondary active transport of bile salts out of the cell cytoplasm. Furthermore, assays performed on a chromosomal ΔacrB mutant transformed with multicopy plasmid encoding MdtM suggested a functional synergism between the single-component MdtM transporter and the tripartite AcrAB-TolC system that results in a multiplicative effect on resistance. Substrate binding experiments performed on purified MdtM demonstrated that the transporter binds to cholate and deoxycholate with micromolar affinity, and transport assays performed on inverted vesicles confirmed the capacity of MdtM to catalyse electrogenic bile salt/H(+) antiport.

Biosensor based toxicity dissection of tannery and associated environmental samples

Kenyan tannery and associated environmental samples were selected for ecotoxicological assessment. A tool-kit of techniques was developed, including whole-cell biosensor and chemical assays. A luminescence based bacterial biosensor (Escherichia coli HB101 pUCD607) (via a multi-copy plasmid) was used for toxicity assessment. Samples were manipulated prior to biosensor interrogation to identify the nature of the toxic contaminants. Untreated samples (before any manipulations) showed a strong toxic effect at the discharge point in comparison to other sampling points. Sparging was used to identify toxicity associated with volatile organics. The toxicity of contaminants, removed by treatment with activated charcoal was identified for all the sampling points except for those upstream of effluent discharges. Filtration identified toxicity associated with suspended solids. Changes in availability of toxic contaminants due to pH adjustment of most samples from the tannery effluent treatment pits were also associated with the extreme pH values (4.0 and 8.0). The approach used has highlighted the complexicity of toxic pollutants in effluent from the tanning industry and the dissection of toxicity points to possible remediation strategies for effluents from the tanning industry.

Mechanism of Alizarin Red S and Methylene Blue Biosorption onto Olive Stone: Isotherm study in Single and Binary Systems

The biosorption process of anionic dye Alizarin Red S (ARS) and cationic dye methylene blue (MB) as a function of contact time, initial concentration and solution pH onto olive stone (OS) biomass has been investigated. Equilibrium biosorption isotherms in single and binary systems and kinetics in batch mode were also examined. The kinetic data of the two dyes were better described by the pseudo second-order model. At low concentration, ARS dye appeared to follow a two-step diffusion process, while MB dye followed a three-step diffusion process. The biosorption experimental data for ARS and MB dyes were well suited to the Redlich-Peterson isotherm. The maximum biosorption of ARS dye, qmax = 16.10 mg/g, was obtained at pH 3.28 and the maximum biosorption of MB dye, qmax = 13.20 mg/g, was observed at basic pH values. In the binary system, it was indicated that the MB dye diffuses firstly inside the biosorbent particle and occupies the biosorption sites forming a monodentate complex and then the ARS dye enters and can only bind to untaken sites; forms a tridentate complex with OS active sites.

Matérias-primas da plataforma do Mondego para cerâmica

O presente trabalho divulga os resultados dos estudos levados a efeito nas matérias-primas argilosas que se integram tipologicamente na argila comum, ocorrentes na designada Plataforma do Mondego, Centro de Portugal, na região entre Miranda do Corvo, a SW, e Tábua, a NE. Para tal realizou-se a cartografia superficial dos sedimentos continentais do Cretácico e do Terciário, aí preservados, estabeleceram-se as colunas sedimentares, a nível regional e a nível local, nas áreas de maior potencial reconhecido e, caracterizaram-se as matérias-primas argilosas amostradas, em termos de composição, textura e aptidão cerâmica, objectivando a definição das zonas das jazidas com maior interesse industrial. A informação obtida e compilada, relativa ao caulino e ao feldspato é também apresentada, com vista a uma percepção da potencialidade destas matériasprimas cerâmicas ocorrentes na área. O estudo de caracterização dos materiais argilosos investigados teve como base 53 amostras obtidas em seis regiões da Plataforma do Mondego aqui definidas por motivo de organização do trabalho, segundo os critérios geográfico e geotectónico. As formações de Côja e de Campelo, do Terciário, constituem as unidades onde ocorrem litótipos produtivos, em termos de matéria-prima para a Cerâmica de Barro Vermelho ou Cerâmica de Construção. Relativamente às características texturais e composicionais, em síntese, apresentam-se os factos relevantes seguintes: A matéria-prima argilosa existente na área estudada materializa, granulometricamente, na maioria das amostras, silte, caindo os níveis amostrados com maior percentagem de argila, no domínio do silte argiloso. O défice em fracção argila implica limitações quanto à possibilidade de diversificação de produtos cerâmicos fabricados com estas matérias-primas tal-qual. Os diferentes métodos analíticos utilizados na caracterização mineralógica dos materiais amostrados confirmaram uma composição em termos dos minerais argilosos, consistindo de ilite/mica (em geral, o mais abundante), caulinite e esmectite, interestratificados e clorite. Os minerais não argilosos são quartzo (predominante), feldspato (sobretudo potássico) e hematite, com uma representação baixa. A mineralogia da fracção inferior a 2μm das amostras, não difere das amostras totais, salvo no teor mais elevado dos minerais argilosos e acentuada redução dos minerais não argilosos. Os resultados da análise química por fluorescência de raios X das amostras integrais correlacionam-se com as características mineralógicas observadas através das técnicas analíticas utilizadas. No respeitante às propriedades e comportamento cerâmico verifica-se: Os parâmetros relacionados com a plasticidade indicam que parte das pastas elaboradas com estes materiais argilosos têm uma trabalhabilidade aceitável, mas existem problemas de conformação e acentuada retracção num número significativo de amostras, devido à elevada plasticidade da maioria das amostras. A extrusão é satisfatória a óptima. A RMF e a retracção em seco assumem valores, respectivamente, moderados a baixos e moderados, embora seja necessário ter em conta o procedimento de extrusão dos provetes, sem dispositivo de vácuo. Todas as amostras foram sujeitas a cozedura a 900ºC, e um conjunto seleccionado foi cozido a 1000ºC e a 1100ºC. As fases mineralógicas ocorrentes após cozeduras a 900ºC e 1100ºC foram identificadas num conjunto de amostras, tendo-se evidenciado a coerência dessas fases, com a mineralogia das amostras em seco. Após cozedura a 900ºC, os valores de RMF das amostras satisfazem geralmente os valores mínimos, exigidos para o fabrico de tijolo, abobadilha e, com alguma frequência, de telha, como já se verificava com os valores daquela propriedade em seco. Os valores de retracção seco-cozido são em geral, modestos. A capacidade de absorção de água é maioritariamente elevada. A formação de vidro, sobretudo, condiciona o comportamento destas propriedades por cozedura dos provetes a 1000ºC e a 1100ºC. A coloração predominante em cru das matérias-primas argilosas amostradas é amarelo acastanhado a castanho avermelhado. Após cozedura a 900ºC, há um acentuado escurecimento e incremento no grau de vermelho. As cozeduras a 1000ºC e 1100ºC promovem escurecimento gradual, com ligeira influência na cor. O comportamento dos provetes após as cozeduras cerâmicas revelou-se homogéneo a cada uma das respectivas temperaturas, não se registando também defeitos significativos, nem eflorescências. A análise das amostras em termos composicionais e tecnológicos permitiu destacar as principais características e aspectos distintivos das matériasprimas, nas diferentes regiões definidas objectivando as diferentes potencialidades cerâmicas. Nesta abordagem comparativa foram consideradas só as amostras dos campos silte e silte arenoso, por serem aquelas com maior interesse para a Cerâmica de Construção. Nas colunas sedimentares das regiões de Tábua e Santa Quitéria constata-se a ocorrência de dois ritmos de sedimentação, que embora assumam características específicas em cada região, têm aspectos composicionais e tecnológicos em comum, traduzindo melhor aptidão cerâmica os ritmos inferiores. A conjugação da cartografia realizada com os estudos laboratoriais permite concluir que as regiões de Tábua e de Santa Quitéria serão as que têm maior potencial por explorar, em matéria-prima para Cerâmica de Construção, apesar da primeira já ser intensamente explorada. Na região de Tábua, as amostras têm como fases mineralógicas principais ilite e quartzo na mesma proporção média (35%) e caulinite (média=19%) que regista enriquecimento significativo na fracção argila (média=38%). As argilas desta região registam a cor em cru mais vermelha e pH mais ácido observados. O ritmo de sedimentação inferior, com esmectite e interestratificados e ligeiramente menos quartzoso, apresenta melhores propriedades cerâmicas. A composição mineralógica média das amostras da região de Santa Quitéria é próxima daquela da região de Tábua, mas menos caulinítica, em especial na sequência inferior, na qual o teor médio de caulinite na fracção argila (7%) é o mais baixo observado. Na região de Côja – Arganil, a actividade extractiva é significativa na bacia de Côja. Aqui, a exploração de novas áreas potenciais é condicionada pela cobertura conglomerática e por estruturas tectónicas e não tectónicas relacionadas com comportamento plástico. Na restante área desta região, os recursos argilosos são penalizados por material areno-conglomerático. As amostras desta região distinguem-se das restantes a nível textural pela maior fracção areia e mineralogicamente pela presença de clorite, teor reduzido de caulinite e elevado de feldspato. As potencialidades em barro vermelho na região de Sanguinheda não serão significativas, pois a Formação de Côja é predominantemente arcósica e a Formação de Campelo pouco espessa e conglomerática. As argilas com melhor aptidão cerâmica foram amostradas na região de Miranda do Corvo – Lousã. Na composição, estas amostras são as que contêm maior fracção de argila, maior teor de ilite e caulinite e menor de argilas expansivas. Registam os melhores valores nas características tecnológicas, nomeadamente a RMF e absorção de água. A consistência dos grupos amostrais e ritmos definidos em termos composicionais e tecnológicos é corroborada pelas técnicas de análise estatística multivariada aplicadas, que os identificam. As condições de amostragem na região de Tábua, permitiram a elaboração de uma coluna tipológica, na qual, a partir de uma caracterização expedita de amostras é possível identificar a sua afinidade com os ritmos argilosos definidos e, consequentemente, a sua situação na coluna sedimentar regional e aptidão cerâmica. A cartografia dos recursos argilosos potenciais, elaborada à escala 1:25.000, constitui um dos objectivos principais deste trabalho e nela constam unidades litológicas, nas quais são diferenciadas unidades argilosas tendo também em consideração a tipologia e guias mineralógicos resultantes da caracterização das amostras. As características composicionais destas unidades denotam diferente aptidão cerâmica e, portanto, permitem salientar as zonas com maior interesse económico.

Gene expression in understanding mechanisms of toxicity in amphibians

De uma forma geral os anfíbios são conhecidos como organismos que apresentam uma grande sensibilidade a vários tipos de contaminantes. Contudo existem casos, como o de Pelophylax perezi (rã-verde), em que estes organismos habitam áreas extremamente contaminadas. Este facto verifica-se na mina de urânio desactivada, da Cunha Baixa (Viseu, centro de Portugal), em que uma população destas rãs habita na lagoa de efluente ácido mineiro (M). Estudos ecotoxicológicos anteriores com estes organismos revelaram apenas efeitos de toxicidade ténues levantando algumas questões. Com o objectivo de elucidar quais os mecanismos que permitem a P. perezi permanecer neste local, sem sofrer aparentemente efeitos perniciosos, encetamos este trabalho. Numa primeira abordagem, avaliámos o sistema de defesa antioxidante de rãs adultas, bem como o conteúdo em metais de alguns órgãos. Desta forma verificámos alterações enzimáticas, principalmente no pulmão e acumulação de metais nos vários órgãos. Posteriormente foi realizado um estudo de expressão genética diferencial, também em organismos adultos e desta feita foram sugeridos alguns mecanismos de protecção basal que estarão por detrás da capacidade de suportar este ambiente extremamente contaminado. Numa etapa seguinte abordámos os efeitos em fases larvares, fazendo inicialmente uma exposição in situ, a vários efluentes, caracteristicamente diferentes, do complexo mineiro. Avaliámos o crescimento, a acumulação de metais e a actividade de alguns biomarcadores de stress oxidativo. Como resultado pudemos constatar que nas fases larvares para além de alguma mortalidade existe acumulação de metais bem como algumas alterações a nível de biomarcadores de stress oxidativo. Numa última abordagem realizamos uma exposição crónica dos girinos a efluente da mina com diversos níveis de pH para distinguir os efeitos da toxicidade do pH, dos efeitos da toxicidade pelo conteúdo de metais. Para tal avaliámos novamente biomarcadores de stress oxidativo, crescimento, acumulação de metais e efectuamos ainda um estudo de expressão genética diferencial. Esta última aproximação permitiu verificar que a toxicidade do efluente resulta primariamente do pH ácido, assumindo a contaminação por metais um papel secundário. Contudo o crescimento dos girinos de P. perezi apresenta-se estimulado por pHs mais baixos. São apontados ainda alguns mecanismos, em girinos, para lidar com o stress causado pela contaminação por metais.De uma forma geral pôde-se constatar que quer anfíbios adultos quer girinos expostos ao efluente apresentam valores altos de metais acumulados. Os biomarcadores de stress oxidativo na sua maioria não apresentaram respostas coerentes mediante as várias exposições. Este trabalho apresentase como um contributo importante para a ecotoxicologia de anfíbios, aumentando os níveis actuais de conhecimento sobre o efeito de contaminação proveniente de efluentes mineiros, sugerindo ainda mecanismos de resistência quer em larvas, quer para adultos.

Integration of geochemical and biological modifications in mining areas: waters, sediments and diatoms

The development of mining activities over thousands of years in the region of Aljustrel is nowadays visible as a vast area of ore tailings, slag and host rocks of sulphides mineralization. The generation of acidic waters by the alteration of pyritic minerals - Acid Mine Drainage (AMD) - causes a significant impact on the river system both in the south of the village (Rib ª. Água Forte) and in the north of it (Rib ª. Água Azeda and Barranco do Farrobo), which is reflected in extremely low pH values (< 3) and high concentrations of As, Cd, Cu, Fe, Mn, Pb, Zn and sulphates. This study aimed to assess the environmental impacts extent, integrating geochemical (surface waters and stream sediments) and biological (diatoms) parameters. Three groups of sites were defined, based on sediments and water analysis, which integration with diatom data showed the same association of groups: Group 1- impacted, with acidic pH (1.9-5.1), high metal contents (0.4-1975 mg L-1) and Fe-Mg-sulphate waters, being metals more bioavailable in waters in cationic form (Me2+); mineralogically the sediments were characterized by phyllosilicates and sulphates/oxy-hydroxysulphate phases, easily solubilized, retaining a high amount of metals when precipitated; dominant taxon was Pinnularia aljustrelica (a new species); Group 2- slightly impacted, weak acid to neutral pH (5.0-6.8), metal contents not so high (0.2-25 mg L-1) and Fe-Mg-sulphate to Mg-chloride waters; dominant taxa were Brachysira neglectissima and Achnanthidium minutissimum; Group 3- unimpacted, alkaline pH (7.0-8.4), low metal contents (0-7 mg L-1) with Mg-chloride waters. In this group, metals were associated to the primary phases (e.g. sulphides), not so easily available; the existence of high chloride contents explained the presence of typical taxa of brackish/marine (e.g. Entomoneis paludosa) waters. Taxonomical aspects of the diatoms were studied (discovery of a new species: Pinnularia aljustrelica Luis, Almeida et Ector sp. nov.), as well as morphometric (size decrease of diatoms valves, as well as the appearance of deformed valves of Eunotia exigua in Group 1 and A. minutissimum in Group 2) and physiological (effective to assess the effects of metals/acidity in the photosynthetic efficiency through PAM Fluorometry) aspects. A study was carried out in an artificial river system (microcosm) that aimed to mimic Aljustrel’s extreme conditions in controlled laboratory conditions. The chronic effects of Fe, SO42- and acidity in field biofilms, inoculated in the artificial rivers, were evaluated as well as their contribution to the communities’ tolerance to metal toxicity, through acute tests with two metals (Cu and Zn). In general, the effects caused by low pH values and high concentrations of Fe and SO42- were reflected at the community level by the decrease in diversity, the predominance of acidophilic species, the decrease in photosynthetic efficiency and the increase of enzymatic (e.g. catalase, superoxide dismutase) and non-enzymatic activities (e.g. total glutathione and total phytochelatins). However, it was possible to verify that acidity performed a protective effect in the communities, upon Cu and Zn addition. A comparative study between Aljustrel mining area and New Brunswick mining area was carried out, both with similar mining and geological conditions, reflected in similar diatom communities in both mines, but in very different geographic and climatic areas.

Effects of environmental factors on the toxicity of pesticides to zebrafish embryos

During the last century mean global temperatures have been increasing. According to the predictions, the temperature change is expected to exceed 1.5ºC in this century and the warming is likely to continue. Freshwater ecosystems are among the most sensitive mainly due to changes in the hydrologic cycle and consequently changes in several physico-chemical parameters (e.g. pH, dissolved oxygen). Alterations in environmental parameters of freshwater systems are likely to affect distribution, morphology, physiology and richness of a wide range of species leading to important changes in ecosystem biodiversity and function. Moreover, they can also work as co-stressors in environments where organisms have already to cope with chemical contamination (such as pesticides), increasing the environmental risk due to potential interactions. Therefore, the objective of this work was to evaluate the effects of climate change related environmental parameters on the toxicity of pesticides to zebrafish embryos. The following environmental factors were studied: pH (3.0-12.0), dissolved oxygen level (0-8 mg/L) and UV radiation (0-500 mW/m2). The pesticides studied were the carbamate insecticide carbaryl and the benzimidazole fungicide carbendazim. Stressors were firstly tested separately in order to derive concentration- or intensity-response curves to further study the effects of binary combinations (environmental factors x pesticides) by applying mixture models. Characterization of zebrafish embryos response to environmental stress revealed that pH effects were fully established after 24 h of exposure and survival was only affected at pH values below 5 and above 10. Low oxygen levels also affected embryos development at concentrations below 4 mg/L (delay, heart rate decrease and edema), and at concentrations below 0.5 mg/L the survival was drastically reduced. Continuous exposure to UV radiation showed a strong time-dependent impact on embryos survival leading to 100% of mortality after 72 hours of exposure. The toxicity of pesticides carbaryl and carbendazim was characterized at several levels of biological organization including developmental, biochemical and behavioural allowing a mechanistic understanding of the effects and highlighting the usefulness of behavioural responses (locomotion) as a sensitive endpoint in ecotoxicology. Once the individual concentration response relationship of each stressor was established, a combined toxicity study was conducted to evaluate the effects of pH on the toxicity of carbaryl. We have shown that pH can modify the toxicity of the pesticide carbaryl. The conceptual model concentration addition allowed a precise prediction of the toxicity of the jointeffects of acid pH and carbaryl. Nevertheless, for alkaline condition both concepts failed in predicting the effects. Deviations to the model were however easy to explain as high pH values favour the hydrolysis of carbaryl with the consequent formation of the more toxic degradation product 1- naphtol. Although in the present study such explanatory process was easy to establish, for many other combinations the “interactive” nature is not so evident. In the context of the climate change few scenarios predict such increase in the pH of aquatic systems, however this was a first approach focused in the lethal effects only. In a second tier assessment effects at sublethal level would be sought and it is expectable that more subtle pH changes (more realistic in terms of climate changes scenarios) may have an effect at physiological and biochemical levels with possible long term consequences for the population fitness.