Identification of tsunami-induced deposits using numerical modeling and rock magnetism techniques: A study case of the 1755 Lisbon tsunami in Algarve, Portugal

Storm- and tsunami-deposits are generated by similar depositional mechanisms making their discrimination hard to establish using classic sedimentologic methods. Here we propose an original approach to identify tsunami-induced deposits by combining numerical simulation and rock magnetism. To test our method, we investigate the tsunami deposit of the Boca do Rio estuary generated by the 1755 earthquake in Lisbon which is well described in the literature. We first test the 1755 tsunami scenario using a numerical inundation model to provide physical parameters for the tsunami wave. Then we use concentration (MS. SIRM) and grain size (chi(ARM), ARM, B1/2, ARM/SIRM) sensitive magnetic proxies coupled with SEM microscopy to unravel the magnetic mineralogy of the tsunami-induced deposit and its associated depositional mechanisms. In order to study the connection between the tsunami deposit and the different sedimentologic units present in the estuary, magnetic data were processed by multivariate statistical analyses. Our numerical simulation show a large inundation of the estuary with flow depths varying from 0.5 to 6 m and run up of similar to 7 m. Magnetic data show a dominance of paramagnetic minerals (quartz) mixed with lesser amount of ferromagnetic minerals, namely titanomagnetite and titanohematite both of a detrital origin and reworked from the underlying units. Multivariate statistical analyses indicate a better connection between the tsunami-induced deposit and a mixture of Units C and D. All these results point to a scenario where the energy released by the tsunami wave was strong enough to overtop and erode important amount of sand from the littoral dune and mixed it with reworked materials from underlying layers at least 1 m in depth. The method tested here represents an original and promising tool to identify tsunami-induced deposits in similar embayed beach environments.

Identification of tsunami-induced deposits using numerical modeling and rock magnetism techniques: A study case of the 1755 Lisbon tsunami in Algarve, Portugal

Storm- and tsunami-deposits are generated by similar depositional mechanisms making their discrimination hard to establish using classic sedimentologic methods. Here we propose an original approach to identify tsunami-induced deposits by combining numerical simulation and rock magnetism. To test our method, we investigate the tsunami deposit of the Boca do Rio estuary generated by the 1755 earthquake in Lisbon which is well described in the literature. We first test the 1755 tsunami scenario using a numerical inundation model to provide physical parameters for the tsunami wave. Then we use concentration (MS. SIRM) and grain size (chi(ARM), ARM, B1/2, ARM/SIRM) sensitive magnetic proxies coupled with SEM microscopy to unravel the magnetic mineralogy of the tsunami-induced deposit and its associated depositional mechanisms. In order to study the connection between the tsunami deposit and the different sedimentologic units present in the estuary, magnetic data were processed by multivariate statistical analyses. Our numerical simulation show a large inundation of the estuary with flow depths varying from 0.5 to 6 m and run up of similar to 7 m. Magnetic data show a dominance of paramagnetic minerals (quartz) mixed with lesser amount of ferromagnetic minerals, namely titanomagnetite and titanohematite both of a detrital origin and reworked from the underlying units. Multivariate statistical analyses indicate a better connection between the tsunami-induced deposit and a mixture of Units C and D. All these results point to a scenario where the energy released by the tsunami wave was strong enough to overtop and erode important amount of sand from the littoral dune and mixed it with reworked materials from underlying layers at least 1 m in depth. The method tested here represents an original and promising tool to identify tsunami-induced deposits in similar embayed beach environments.

Exposição ocupacional a formaldeído: avaliação da exposição e efeitos genotóxicos

O formaldeído (FA) foi classificado, em 2004, pela International Agency for Cancer Research como agente cancerígeno. Este agente químico ocupa a 25ª posição em toda a produção química dos Estados Unidos da América, com mais de 5 milhões de toneladas produzidas por ano. Devido à sua importância económica e uso diversificado, muitos indivíduos estão expostos profissionalmente a FA. Com o estudo desenvolvido pretendeu‑se avaliar a exposição a FA em dois contextos ocupacionais distintos – na produção de FA e resinas e em laboratórios de anatomia patológica (AP) e relacionar com eventuais efeitos para a saúde, comparando a frequência de micronúcleos (MN) em linfócitos do sangue periférico e em células esfoliadas da mucosa bucal dos trabalhadores expostos a FA com indivíduos não expostos (controlos). Como amostra foram estudados 80 trabalhadores ocupacionalmente expostos a FA: 30 trabalhadores da fábrica de produção de FA e resinas e 50 trabalhadores de 10 laboratórios de AP. Foi constituído um grupo controlo de 85 indivíduos com atividades profissionais que não envolviam a exposição a formaldeído ou qualquer outro agente químico com propriedades genotóxicas. Aplicaram‑se duas metodologias distintas de avaliação ambiental do FA com o objetivo de conhecer a exposição profissional. Compararam‑se os resultados obtidos com os valores limite para a exposição média ponderada (TLV‑TWA=0,75 ppm) e para a concentração máxima (VLE‑CM=0,3 ppm). A totalidade dos laboratórios apresentou resultados superiores ao valor de referência existente para a concentração máxima. Nenhum dos resultados obtidos para a exposição média ponderada foi superior ao valor de referência. O exame macroscópico obteve os valores das concentrações máximas mais elevadas em 90% dos laboratórios. Os valores de MN foram mais elevados nos indivíduos expostos a FA comparativamente com os controlos. No caso dos MN nos linfócitos, a média foi de 3,96 nos expostos e de 0,81 nos não expostos. Os MN nas células esfoliadas da boca apresentaram uma média de 0,96 nos expostos e de 0,16 nos controlos. Os resultados obtidos nesta acção de biomonitorização podem revelar‑se particularmente úteis para as organizações responsáveis em definir os níveis aceitáveis para a exposição humana a FA. ABSTRACT: Since 2004, formaldehyde (FA) has been classified by the International Agency for Cancer Research as a carcinogen. The FA ranks 25th in the overall United States chemical production, with more than 5 million tons produced each year. Due to its economic importance and varied use, many individuals are exposed to FA at their occupational settings. This study aimed to assess the exposure to FA in two occupational settings – FA production factory and pathology anatomy (PA) laboratories – and relate it to possible health effects by comparing frequency of micronuclei (MN) in peripheral blood lymphocytes and exfoliated cells from the oral mucosa of workers exposed to FA with individuals not exposed to this agent (controls). This study was performed in 80 workers occupationally exposed to FA: 30 workers of the FA factory and 50 workers in 10 PA laboratories. The control group comprised 85 subjects without exposure. We have applied two different methodologies for environmental monitoring of FA. The results were compared with the reference to the exposure weighted average (TLV‑TWA = 0.75 ppm) and ceiling concentration (VLE‑MC = 0.3 ppm). All laboratories had results higher than the reference value to CM (1.41 ppm). None of the results obtained for the TWA exposure (0.16 ppm) were higher than the reference value. Macroscopic examination obtained the highest values of CM in 90% of laboratories. MN values were higher in individuals exposed to FA as compared to controls. As for MN in lymphocytes, the average was 3.96 in exposed compared with 0.81 in the unexposed. The MN in exfoliated cells of the buccal mucosa had an average of 0.96 in exposed, compared with 0.16 in controls. The results of this biomonitoring can be particularly useful to organizations responsible for defining acceptable levels for human exposure to FA.

Identification of tsunami-induced deposits using numerical modeling and rock magnetism techniques: Astudy case of the 1755 Lisbon tsunami in Algarve, Portugal (vol 182, pg 187, 2010)

Storm- and tsunami-deposits are generated by similar depositional mechanisms making their discrimination hard to establish using classic sedimentologic methods. Here we propose an original approach to identify tsunami-induced deposits by combining numerical simulation and rock magnetism. To test our method, we investigate the tsunami deposit of the Boca do Rio estuary generated by the 1755 earthquake in Lisbon which is well described in the literature. We first test the 1755 tsunami scenario using a numerical inundation model to provide physical parameters for the tsunami wave. Then we use concentration (MS. SIRM) and grain size (chi(ARM), ARM, B1/2, ARM/SIRM) sensitive magnetic proxies coupled with SEM microscopy to unravel the magnetic mineralogy of the tsunami-induced deposit and its associated depositional mechanisms. In order to study the connection between the tsunami deposit and the different sedimentologic units present in the estuary, magnetic data were processed by multivariate statistical analyses. Our numerical simulation show a large inundation of the estuary with flow depths varying from 0.5 to 6 m and run up of similar to 7 m. Magnetic data show a dominance of paramagnetic minerals (quartz) mixed with lesser amount of ferromagnetic minerals, namely titanomagnetite and titanohematite both of a detrital origin and reworked from the underlying units. Multivariate statistical analyses indicate a better connection between the tsunami-induced deposit and a mixture of Units C and D. All these results point to a scenario where the energy released by the tsunami wave was strong enough to overtop and erode important amount of sand from the littoral dune and mixed it with reworked materials from underlying layers at least 1 m in depth. The method tested here represents an original and promising tool to identify tsunami-induced deposits in similar embayed beach environments.

Meios de comunicação como instrumentos de inserção da comunidade cabo-verdiana na sociedade de acolhimento: o caso da área metropolitana de Lisboa

Dissertação apresentada à Escola Superior de Comunicação Social como parte dos requisitos para obtenção de grau de mestre em Jornalismo.

Sistema de visão para aterragem automática de UAV

Dissertação para obtenção do grau de Mestre em Engenharia Electrotécnica Ramo de Automação e Electrónica Industrial