Determinação e aplicações dos frutooligossacarídeos de Yacon (Smallanthus sonchifolius)

Torna-se cada vez mais importante fortalecer o vínculo entre o setor agrário, as universidades e o setor industrial. Através de estudos científicos pode-se aprimorar a produção agrícola, valorizar comercialmente os produtos manufaturados e permitir usos biotecnológicos anteriormente indisponíveis. Este trabalho ambicionou gerar dados que incentivassem e permitissem o suporte técnico-científico adequado ao pequeno e médio agricultor do litoral da Grande-Florianópolis, no estado de Santa Catarina (Brasil) viabilizando a exploração comercial das raízes de yacon (Smallanthus sonchifolius). Primeiro, o enfoque agronómico que objetivou ofertar dados científicos da adequação climática do plantio de yacon na região do litoral de Florianópolis (SC) com a finalidade de otimizar a produção e rentabilizá-la. Por cromatografia líquida de alta eficiência foram quantificados os valores de frutooligossacarídeos (fração de interesse, alimento funcional com efeito prebiótico), frutose, glucose e sacarose e avaliaram-se os efeitos diretos dos fatores climáticos na produção fazendo uso da análise multivariada para sua interpretação. Os resultados mostram que a produção de FOS não consegue atingir valores similares aos de outras regiões onde o yacon é explorado economicamente. Igualmente a produção de FOS parece ter uma grande dependência do clima, especialmente da amplitude térmica e da chuva. O segundo enfoque foi a possibilidade de exploração comercial, através de secagem em estufa. O processo de secagem, especialmente em amostras produzidas em condições climatológicas mais drásticas induzem modificações provocadas pela reacção de Maillard, como foi verificado por estudos de GCxGC-Tof-Ms e ESI-MS. O terceiro enfoque foi biotecnológico e consistiu em aproveitar frutooligossacarídeos comerciais para utilizá-los como matriz polimérica para produção de estruturas em escala nano e micrométrica através da eletropulverização. Foram observadas, nesta etapa, os aspetos morfológicos e as características das partículas formadas e a sua capacidade de servir como veículo transportador de compostos com características anti-oxidantes.

Analysis of the organic matter associated to sea salt : definition of potential molecular markers based on the volatile composition and presence of glycosidic derivatives and polysaccharides

Sea salt is a natural product obtained from the evaporation of seawater in saltpans due to the combined effect of wind and sunlight. Nowadays, there is a growing interest for protection and re-valorisation of saltpans intrinsically associated to the quality of sea salt that can be evaluated by its physico-chemical properties. These man-made systems can be located in different geographical areas presenting different environmental surroundings. During the crystallization process, organic compounds coming from these surroundings can be incorporated into sea salt crystals, influencing their final composition. The organic matter associated to sea salt arises from three main sources: algae, surrounding bacterial community, and anthropogenic activity. Based on the hypothesis that sea salt contains associated organic compounds that can be used as markers of the product, including saltpans surrounding environment, the aim of this PhD thesis was to identify these compounds. With this purpose, this work comprised: 1) a deep characterisation of the volatile composition of sea salt by headspace solid phase microextraction combined with comprehensive two-dimensional gas chromatography time-of-flight mass spectrometry (HS-SPME/GCGC–ToFMS) methodology, in search of potential sea salt volatile markers; 2) the development of a methodology to isolate the polymeric material potentially present in sea salt, in amounts that allow its characterisation in terms of polysaccharides and protein; and 3) to explore the possible presence of triacylglycerides. The high chromatographic resolution and sensitivity of GC×GC–ToFMS enabled the separation and identification of a higher number of volatile compounds from sea salt, about three folds, compared to unidimentional chromatography (GC–qMS). The chromatographic contour plots obtained revealed the complexity of marine salt volatile composition and confirmed the relevance of GC×GC–ToFMS for this type of analysis. The structured bidimentional chromatographic profile arising from 1D volatility and 2D polarity was demonstrated, allowing more reliable identifications. Results obtained for analysis of salt from two locations in Aveiro and harvested over three years suggest the loss of volatile compounds along the time of storage of the salt. From Atlantic Ocean salts of seven different geographical origins, all produced in 2007, it was possible to identify a sub-set of ten compounds present in all salts, namely 6-methyl-5-hepten-2-one, 2,2,6-trimethylcyclohexanone, isophorone, ketoisophorone, β-ionone-5,6-epoxide, dihydroactinidiolide, 6,10,14-trimethyl-2-pentadecanone, 3-hydroxy-2,4,4-trimethylpentyl 2-methylpropanoate, 2,4,4-trimethylpentane-1,3-diyl bis(2-methylpropanoate), and 2-ethyl-1-hexanol. These ten compounds were considered potential volatile markers of sea salt. Seven of these compounds are carotenoid-derived compounds, and the other three may result from the integration of compounds from anthropogenic activity as metabolites of marine organisms. The present PhD work also allowed the isolation and characterisation, for the first time, of polymeric material from sea salt, using 16 Atlantic Ocean salts. A dialysis-based methodology was developed to isolate the polymeric material from sea salt in amounts that allowed its characterisation. The median content of polymeric material isolated from the 16 salts was 144 mg per kg of salt, e.g. 0.014% (w/w). Mid-infrared spectroscopy and thermogravimetry revealed the main occurrence of sulfated polysaccharides, as well as the presence of protein in the polymeric material from sea salt. Sea salt polysaccharides were found to be rich in uronic acid residues (21 mol%), glucose (18), galactose (16), and fucose (13). Sulfate content represented a median of 45 mol%, being the median content of sulfated polysaccharides 461 mg/g of polymeric material, which accounted for 66 mg/kg of dry salt. Glycosidic linkage composition indicates that the main sugar residues that could carry one or more sulfate groups were identified as fucose and galactose. This fact allowed to infer that the polysaccharides from sea salt arise mainly from algae, due to their abundance and composition. The amino acid profile of the polymeric material from the 16 Atlantic Ocean salts showed as main residues, as medians, alanine (25 mol%), leucine (14), and valine (14), which are hydrophobic, being the median protein content 35 mg/g, i.e. 4,9 mg per kg of dry salt. Beside the occurrence of hydrophobic volatile compounds in sea salt, hydrophobic non-volatile compounds were also detected. Triacylglycerides were obtained from sea salt by soxhlet extraction with n-hexane. Fatty acid composition revealed palmitic acid as the major residue (43 mol%), followed by stearic (13), linolenic (13), oleic (12), and linoleic (9). Sea salt triacylglycerides median content was 1.5 mg per kg of dry salt. Both protein and triacylglycerides seem to arise from macro and microalgae, phytoplankton and cyanobacteria, due to their abundance and composition. Despite the variability resulting from saltpans surrounding environment, this PhD thesis allowed the identification of a sea salt characteristic organic compounds profile based on volatile compounds, polysaccharides, protein, and triacylglycerides.

Metais em águas e sedimentos da plataforma dos Açores

A presente tese tem por objetivo principal contribuir para o conhecimento da geoquímica sedimentar da zona oceânica da crista da Terceira e montanhas submarinas a sul (região entre 29-39ºN e 27-32ºW), integrando também a caraterização dos metais e nutrientes na coluna de água e propondo concentrações para servirem de referência nesta região do Atlântico Central. Para o efeito foram realizadas amostragens na coluna de água em sete locais e de sedimento em cinco locais, durante a campanha oceanográfica designada por EMEPC/AÇORES/G3/2007 a bordo do navio SV Kommandor Jack, no âmbito do projeto da Estrutura de Missão para a Extensão da Plataforma Continental (EMEPC). Os perfis de CTD da coluna de água na região estudada revelam a presença de massas de água distintas: a Western North Atlantic Central Water (WNACW), a Eastern North Atlantic Central Water tropical (ENACWt), a Eastern North Atlantic Central Water polar (ENACWp), a Mediterranean Overflow Water (MOW), a Deep Mediterranean Water (DMW) e a North Eastern Atlantic Deep Water (NEADW). Observou-se nos perfis de temperatura e salinidade, referentes aos primeiros 200 m da coluna de água, um gradiente meridional negativo entre as estações localizadas na crista da Terceira e as estações localizadas mais a sul. Observou-se nas águas superficiais valores de oxigénio dissolvido de 93% e de pH de 8,1, assim como que as concentrações dos nutrientes NOx, PO4 e SiO2 variam de acordo com a atividade biológica, tendo-se registado concentrações medianas mais baixas, respetivamente de 6,5, 0,23 e 1,3 mol L-1, que aumentam com a profundidade devido à ausência de produção primária (respetivamente 31, 1,4 e 22 mol L-1). As concentrações de NH4 e de SO4 não variam significativamente nas massas de água, sendo os valores medianos mínimos e máximos de 0,69 a 0,79 mol L-1 para o NH4 e de 30 a 32 mol L-1 para o SO4. São propostas concentrações de referência para as massas de água, para os elementos cobre, cádmio, chumbo e arsénio. Os perfis de sedimento analisados permitem distinguir os sedimentos na crista da Terceira (core A) dos restantes (cores B a E). A grande variabilidade textural encontrada no core A, que contrasta com os outros cores analisados, deve-se a importantes contribuições terrígenas, originadas pela erosão sub-aérea e pela atividade vulcânica das ilhas próximas. iv resumo (continuação) A análise mineralógica, efetuada à fração areia e à fração fina (< 63 μm), confirma que os sedimentos do core A derivam de rochas vulcânicas formadas maioritariamente por piroxenas, olivinas, anfíbolas, biotite, alterites e ainda calcite, plagióclase e magnetite, tendo-se identificado ao microscópio a glauconite e o vidro vulcânico. De acordo com a composição química destes minerais o core A apresenta valores mais elevados de Al, Fe, K, P, Mg, Si, Na, Zn, V, Cr e Mn relativamente aos cores B a E. Os cores B a E apresentam grandes quantidades de calcite (>80%) formada maioritariamente por foraminíferos e nanoplâncton calcário (cocolitóforos). A fração areia confirma a composição maioritariamente carbonatada com grande abundância de material biogénico formado por oozes de foraminíferos (planctónicos e bentónicos) com raras espículas de espongiários e restos de conchas. Os cores B a E apresentam valores muito mais elevados que o core A para os elementos Ca e Sr. Os resultados para o Al, Fe, K, P, Si, Na, As, Cu, Ni, Zn, V, Cr, Li, Pb, Cd e Co presentes nos locais B, C, D e E sugerem que estes cores são comparáveis aos sedimentos de fundo carbonatados. Propõe-se concentrações de referência para a região do Atlântico compreendida entre 29-39ºN e 27-32ºW considerando a primeira camada colhida em cada core. Para o core A as concentrações são normalizadas a 5% de Al e CaCO3, enquanto que para os cores B a E são normalizadas a 2% de Al e CaCO3. Assim as concentrações de referência para o core A são: As – 18 mg kg-1, Cr – 91 mg kg-1, Cu – 127 mg kg-1, Ni – 84 mg kg-1, Pb – 41 mg kg-1, Hg – 41 ng g-1 e Zn – 482 mg kg-1. Para os cores B a E as concentrações de referência são: As – 3 mg kg-1, Cr – 10 mg kg-1, Cu – 36 mg kg-1 Ni – 12 mg kg -1, Hg – 3 ng g-1 e Zn – 20 mg kg-1. Para os restantes metais as concentrações de referência para o core A são: Al – 9%, Si – 25%, Fe – 6%, Ca – 13%, K – 2%, Mg – 2%, Na – 3%, P – 0,4%, Sr – 900 mg kg-1, Li – 10 mg kg-1, Mn – 1200 mg kg-1, Ba – 700 mg kg-1 e V – 140 mg kg-1. Para os cores B a E as concentrações de referência são: Al – 0,9%, Si – 2%, Fe – 0,2%, Ca – 95%, K – 0,3%, Mg – 0,4%, Na – 0,3%, P – 0,04%, Sr – 2600 mg kg-1, Li – 5 mg kg-1, Mn – 240 mg kg-1, Ba – 345 mg kg-1, Co – 2 mg kg-1 e V – 6 mg kg-1. Os resultados da presente tese constituem um contributo para a caraterização geoquímica da região e podem servir de referência à monitorização futura do mar dos Açores e montes submarinos a sul.

Sustainable viticulture in Bairrada appellation: vineyard and harvest year effects on grapes oenological potential

The sustainable viticulture of a region passes, among other aspects, for maximizing the varieties potential minimizing subsequent interventions during winemaking, which should contribute to the production of quality wines maintaining their typicity and rationalizing costs. The detailed knowledge of each Appellation specificities, namely vineyard parcel (soil type and topographical peculiarities) and harvest climatic conditions is crucial for sustainability in this sector. Thus, in line with this current trend, the starting point for the development of this PhD thesis was to evaluate the oenological potential of different varieties cultivated throughout Bairrada Appellation (Portugal). During maturation several changes in grape varieties occur, namely berries become sweeter, less acidic, and they develop flavour, aroma and colour properties. The development of these characteristics is essential to define grapes oenological potential, i.e. to estimate the possibility of their usage to produce specific wines. A three years sampling plan was designed to evaluate the effect of harvest year and parcel characteristics on V. vinifera cv. Arinto, Bical, Sauvignon Blanc, Baga, Castelão, Touriga Nacional, and Sousão grapes composition. For each variety, 3 parcels with different characteristics were selected. Several physicochemical parameters were evaluated, during maturation: berry weight, pH, titratable acidity, sugar and phenolic contents, antiradical activity, and volatile composition (free fraction). Special attention was devoted to grapes at technologic maturity, since, besides these parameters, glycosidically-linked fraction was also considered. By using the results obtained at technologic maturity, a comprehensive approach was applied to identify the significance of harvest and parcel characteristics effects on each variety composition. Considering all the parameters under study, it may be highlighted some significant differences. According to the obtained results determined during maturation, it was possible to conclude that Arinto, Bical and Sauvignon Blanc grapes from parcels with clay-sandy and clay-calcareous soils have higher phenolic content and antiradical activity. Otherwise, Sauvignon Blanc presented similar volatile composition for grapes cultivated in the 3 parcels, while Arinto and Bical exhibited higher volatile content in grapes from claysandy and clay-calcareous soils. For Baga, Castelão and Touriga Nacional red varieties, grapes with higher phenolic content, antiradical activity, and volatile content were obtained from clayey and clay-calcareous soils. Furthermore, for Touriga Nacional, parcels altitude seems also to modulate grapes composition. Beyond parcel effect, harvest year conditions also influence grapes composition: 2011 harvest was related with lower phenolic and volatile contents, as well as lower antiradical activity.For grapes collected at technologic maturity, analysis of variance-simultaneous component analysis (ASCA) was applied combining all the parameters under study, in order to assess the influence of harvest and parcel characteristics on each variety oenological potential. The results obtained using this comprehensive approach is closely related with those observed during maturation and revealed that harvest was the main factor that influenced grapes composition (53% to 68% of the total data set variance) followed by parcel characteristics, explaining ca. 15-19% of the total data set variance. The oenological potential of each variety may be different from one parcel to another, i.e., clay-sandy and clay-calcareous related-environments seem to favour Arinto and Bical white grapes composition, but for the red varieties, grapes composition was favoured by clayey and clay-calcareous soils. Besides, also higher altitude seems to favour Touriga Nacional grapes composition. Sauvignon Blanc seems to be a variety well adapted to the different parcel characteristics. In order to go forward in the valuation of these varieties, the aroma properties of 6 monovarietal wines were studied based on an aroma network-approach, linking molecular data related to volatile composition and aroma data about the key odor active molecules. This approach allowed to identify different wine aroma properties and to infer about the consumer’s sensory perception. It was found that aroma properties differ from one wine variety to another: while Arinto and Sauvignon Blanc wine exhibited higher tree fruity, sweety and flowery aromas, related essentially with ester compounds and C13 norisoprenoids, the opposite was obtained for Bical wine, corroborating the aroma sensory perceptions of the trained panel. Sauvignon Blanc also exhibited higher toasted aromas (related with thiols, mainly with 2-methyl-3-furanthiol). Touriga Nacional red wine exhibited higher tree, tropical, and berry fruits notes (sensory described as sweet fruits), toasted and flowery aromas, while these are similar for the other red wines under study. Besides Portuguese Bairrada wines, this aroma network approach is a tool that can be used to explain the aroma properties of wines worldwide. The grape and wine data generated under the present PhD thesis, in the context of Bairrada Appellation, shows the unique character of each variety, and may be used by growers and wine producers as a support for decisionmaking based on objective criteria, increasing the sustainability in this sector. For instance, it is possible to take advantage of the natural resources and produce products with different characteristics obtained from the same variety, minimizing costs during the winemaking process.

Regional and urban air quality modelling under a climate change scenario

The better understanding of the interactions between climate change and air quality is an emerging priority for research and policy. Climate change will bring changes in the climate system, which will affect the concentration and dispersion of air pollutants. The main objective of the current study is to assess the impacts of climate change on air quality in 2050 over Portugal and Porto urban area. First, an evaluation and characterization of the air quality over mainland Portugal was performed for the period between 2002 and 2012. The results show that NO2, PM10 and O3 are the critical pollutants in Portugal. Also, the influence of meteorology on O3, NO2 and PM10 levels was investigate in the national main urban areas (Porto and Lisboa) and was verified that O3 has a statistically significant relationship with temperature in most of the components. The results also indicate that emission control strategies are primary regulators for NO2 and PM10 levels. After, understanding the national air quality problems and the influence that meteorology had in the historical air quality levels, the air quality modelling system WRF-CAMx was tested and the required inputs for the simulations were prepared to fulfil the main goal of this work. For the required air quality modelling inputs, an Emission Projections under RCP scenarios (EmiPro-RCP) model was developed to assist the estimation of future emission inventories for GHG and common air pollutants. Also, the current emissions were estimated for Portugal with a higher detailed disaggregation to improve the performance of the air quality simulations. The air quality modelling system WRF/CAMx was tested and evaluated over Portugal and Porto urban area and the results point out that is an adequate tool for the analysis of air quality under climate change. For this purpose, regional simulations of air quality during historical period and future (2045-2050) were conducted with CAMx version 6.0 to evaluate the impacts of simulated future climate and anthropogenic emission projections on air quality over the study area. The climate and the emission projections were produced under the RCP8.5 scenario. The results from the simulations point out, that if the anthropogenic emissions keep the same in 2050, the concentrations of NO2, PM10 and O3 will increase in Portugal. When, besides the climate change effects, is consider the projected anthropogenic emissions the annual mean concentrations of NO2 decrease significantly in Portugal and Porto urban area, and on the contrary the annual mean PM10 concentrations increases in Portugal and decrease in Porto urban area. The O3 results are mainly caused by the reduction of ozone precursors, getting the higher reductions in urban areas and increases in the surrounding areas. All the analysis performed for both simulations for Porto urban area support that, for PM10 and O3, there will be an increase in the occurrence of extreme values, surpassing the annual legislated parameters and having more daily exceedances. This study constitutes an innovative scientific tool to help in future air quality management in order to mitigate future climate change impacts on air quality.