Understanding and modelling hydrological and soil erosion processes in burnt forest catchments

Forest fires implications in overland flow and soil erosion have been researched for several years. Therefore, is widely known that fires enhance hydrological and geomorphological activity worldwide as also in Mediterranean areas. Soil burn severity has been widely used to describe the impacts of fire on soils, and has being recognized as a decisive factor controlling post-fire erosion rates. However, there is no unique definition of the term and the relationship between soil burn severity and post-fire hydrological and erosion response has not yet been fully established. Few studies have assessed post-fire erosion over multiple years, and the authors are aware of none which assess runoff. Small amount of studies concerning pre-fire management practices were also found. In the case of soil erosion models, the Revised Universal Soil Loss Equation (RUSLE) and the revised Morgan–Morgan–Finney (MMF) are well-known models, but not much information is available as regards their suitability in predicting post-fire soil erosion in forest soils. The lack of information is even more pronounced as regards post-fire rehabilitation treatments. The aim of the thesis was to perform an extensive research under the post fire hydrologic and erosive response subject. By understanding the effect of burn severity in ecosystems and its implications regarding post fire hydrological and erosive responses worldwide. Test the effect of different pre-fire land management practices (unplowed, downslope plowed and contour plowed) and time-since-fire, in the post fire hydrological and erosive response, between the two most common land uses in Portugal (pine and eucalypt). Assess the performance of two widely-known erosion models (RUSLE and Revised MMF), to predict soil erosion rates during first year following two wildfires of distinctive burn severity. Furthermore, to apply these two models considering different post-fire rehabilitation treatments in an area severely affected by fire. Improve model estimations of post-fire runoff and erosion rates in two different land uses (pine and eucalypt) using the revised MMF. To assess these improvements by comparing estimations and measurements of runoff and erosion, in two recently burned sites, as also with their post fire rehabilitation treatments. Model modifications involved: (1) focusing on intra-annual changes in parameters to incorporate seasonal differences in runoff and erosion; and (2) inclusion of soil water repellency in runoff predictions. Additionally, validate these improvements with the application of the model to other pine and eucalypt sites in Central Portugal. The review and meta-analysis showed that fire occurrence had a significant effect on the hydrological and erosive response. However, this effect was only significantly higher with increasing soil burn severity for inter-rill erosion, and not for runoff. This study furthermore highlighted the incoherencies between existing burn severity classifications, and proposed an unambiguous classification. In the case of the erosion plots with natural rainfall, land use factor affected annual runoff while land management affected both annual runoff and erosion amounts significantly. Time-since-fire had an important effect in erosion amounts among unplowed sites, while for eucalypt sites time affected both annual runoff and erosion amounts. At all studied sites runoff coefficients increase over the four years of monitoring. In the other hand, sediment concentration in the runoff, recorded a decrease during the same period. Reasons for divergence from the classic post-fire recovery model were also explored. Short fire recurrence intervals and forest management practices are viewed as the main reasons for the observed severe and continuing soil degradation. The revised MMF model presented reasonable accuracy in the predictions while the RUSLE clearly overestimated the observed erosion rates. After improvements: the revised model was able to predict first-year post-fire plot-scale runoff and erosion rates for both forest types, these predictions were improved both by the seasonal changes in the model parameters; and by considering the effect of soil water repellency on the runoff, individual seasonal predictions were considered accurate, and the inclusion of the soil water repellency in the model also improved the model at this base. The revised MMF model proved capable of providing a simple set of criteria for management decisions about runoff and erosion mitigation measures in burned areas. The erosion predictions at the validation sites attested both to the robustness of the model and of the calibration parameters, suggesting a potential wider application.

Estudos de síntese e transformação de cromonas e 4-quinolonas

Esta dissertação está dividida em duas partes. Na primeira parte reportam-se métodos de síntese de (E)-3-estirilflavonas e (E)/(Z)-2-aril- 4-cloro-3-estiril-2H-cromenos e estudos de ciclização das (E)-3- estirilflavonas em 5-arilbenzo[c]xantonas. Na segunda parte desenvolveram-se novas rotas de síntese de (E)-2-aril-3-estiril-4- quinolonas e posterior transformação em 5-fenil-12- metilbenzo[c]acridonas e 2,4-diarilfuro[3,2-c]quinolinas. Nesta parte estudou-se também a transformação de 2-aril-4-cloro-1,2-dihidroquinolina- 1,3-dicarbaldeídos em (E)/(Z)-2-aril-4-cloro-3-estiril-1,2- di-hidroquinolina-1-carbaldeídos. A síntese de novos derivados de (E)-3-estirilflavonas, abordada na primeira parte desta dissertação, envolveu estudos de otimização da reação de bromação seguida de ciclização de 3-aril-1-(2- hidroxiaril)propano-1,3-dionas/3-aril-3-hidroxi-1-(2-hidroxiaril)prop-2- en-1-onas em 3-bromoflavonas e o desenvolvimento de uma nova rota de síntese de 3-metilflavonas. As 3-metilflavonas foram sujeitas a bromação e seguidamente transformadas em sais de fosfónio antes de serem utilizadas na síntese de (E)-3-estirilflavonas via reação de Wittig. As 3-bromoflavonas foram também usadas na síntese de (E)-3- estirilflavonas via reação de Heck. A síntese de novos derivados de (E)/(Z)-2-aril-4-cloro-3-estiril-2H-cromenos, via reação de Wittig, envolveu a síntese e formilação de flavanonas. A última transformação reportada na primeira parte desta dissertação é a síntese de 5-arilbenzo[c]xantonas por reação de eletrociclização seguida de oxidação de (E)-3-estirilflavonas. Na segunda parte desta dissertação são estudadas duas vias de síntese de 2-aril-1-metil-4-quinolonas. A primeira via de síntese envolve a síntese de N-(2-acetilfenil)benzamidas, sua ciclização em 4-quinolonas seguida de metilação destas. A segunda via envolve a metilação e ciclização de N-(2-acetilfenil)benzamidas obtendo-se, num só passo, as 2-aril-1-metil-4-quinolonas. Posterior iodação das 2-aril-1-metil-4- quinolonas e subsequente reação de Heck das 2-aril-3-iodo-1-metil-4- quinolonas com estirenos comerciais possibilitaram a síntese de (E)-2- aril-3-estiril-1-metil-4-quinolonas. Estudos de eletrociclização seguidos de oxidação das (E)-2-aril-3-estiril-1-metil-4-quinolonas utilizando uma lâmpada de UV de mercúrio de alta pressão possibilitou a síntese de 5- fenil-12-metilbenzo[c]acridonas, enquanto que o aquecimento em refluxo de 1,2,4-triclorobenzeno deu origem a 2,4-diarilfuro[3,2- c]quinolinas. Nesta segunda parte aborda-se também a síntese de 2-aril-4-cloro-1,2- di-hidroquinolina-1,3-dicarbaldeídos, a partir da formilação de 2-aril- 2,3-di-hidro-4-quinolonas e a sua transformação em (E)/(Z)-2-aril-4- cloro-3-estiril-1,2-di-hidroquinolina-1-carbaldeídos por reação de Wittig. Todos os compostos sintetizados foram caracterizados por espectroscopia de ressonância magnética nuclear de protão e carbono 13C, espectros bidimensionais de correlação heteronuclear (HMBC e HSQC) e, nalguns casos espectros de efeito nuclear Overhauser (NOESY). Os novos produtos foram igualmente caracterizados por espectrometria de massa e sempre que possível análise elementar ou espectrometria de massa de alta resolução.