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.

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.

Homogeneous and heterogenised new gold C-scorpionate complexes as catalysts for cyclohexane oxidation

Gold(III) complexes of type [AuCl2{eta(2)-RC(R'pz)(3)}]Cl [R = R' = H (1), R = CH2OH, R' = H (2) and R = H, R' = 3,5-Me-2(3), pz = pyrazol-1-yl] were supported on carbon materials (activated carbon, carbon xerogel and carbon nanotubes) and used for the oxidation of cyclohexane to cyclohexanol and cyclohexanone, with aqueous H2O2, under mild conditions.

Imunohistoquímica no diagnóstico da glomerulonefrite membranosa: estudo comparativo de binómios cromogênio + coloração de contraste

A glomerulonefrite membranosa faz parte das doenças glomerulares que provocam glomerulonefrite crônica, apresentando-se como uma das causas da doença renal terminal. As técnicas de imunofluorescência são o gold standard no estudo imunológico desta patologia em biópsia renal, através da deteção de imunocomplexos (e.g. IgG e C3) e do seu padrão de distribuição granular característico. No entanto, a imunofluorescência não permite uma contextualização histológica e os fluorocromos utilizados possuem um reduzido tempo de atividade, ao contrário das técnicas imunoenzimáticas que utilizam cromogénios coloridos precipitados que permitem a obtenção de uma marcação permanente e a sua contextualização histológica por via da utilização de eficientes colorações de contraste. Com a finalidade de contribuir para a qualidade do diagnóstico da glomerulonefrite membranosa, em biópsias renais, procurou-se, com esta pesquisa, identificar uma técnica imunoenzimática, através da conjugação entre diferentes cromogênios e colorações de contraste, que permita a deteção de depósitos de IgG e C3, com padrão granular. Foram constituídos diferentes binômios cromogênio + coloração, com os cromogênios 3,3›- Diaminobenzidine Tetrahydrochloride e 3-Amino-9-ethylcarbazole e as colorações Periodic Acid Schiff, Periodic Acid Methenamine Silver e Hematoxilina. Foram utilizadas 72 secções de tecido provenientes de seis de casos de biópsias renais com diagnóstico de glomerulonefrite membranosa, fixados em formalina a 10% e incluídos em parafina. A recolha de dados foi realizada por observação microscópica com preenchimento de uma grelha de classificação dos parâmetros: preservação da morfologia, intensidade da marcação específica, quantidade relativa de estruturas marcadas, marcação inespecífica/fundo, contraste e padrão da marcação, que permitiu a classificação dos binómios estudados num score quantitativo de 0-100 pontos. O binômio que apresentou melhores resultados foi 3-Amino-9-ethylcarbazole + Hematoxilina (score 71,81) e o binômio 3,3›- Diaminobenzidine Tetrahydrochloride+Periodic Acid Methenamine Silver (score 7,81), apresentou os piores resultados. O resultado do teste Kruskal-Wallis indica-nos a presença de diferenças estatísticas entre os binómios em estudo (p=0,000). A Hematoxilina pode ser considerada a coloração mais eficaz, pois cumpriu a sua função de auxiliar e facilitar a observação do tipo de padrão com os dois cromogênios utilizados. O cromogênio 3-Amino-9-ethylcarbazole apresentou resultados semelhantes aos produzidos pelo 3,3›-Diaminobenzidine Tetrahydrochloride, no entanto, permitiu identificar em todos os casos o padrão granular de imunomarcação, ao contrário do que aconteceu com este último.

Classificação GOLD e sintomas respiratórios em idosos: estudo GERIA

A Europa assiste ao envelhecimento da população, onde a doença respiratória assume relevância. Com o aumento da idade, da exposição à poluição ambiental e do tabagismo, a prevalência da Doença Pulmonar Obstrutiva Crónica (DPOC) tende a ser elevada, nomeadamente na população idosa. A idade avançada poderá associar-se com uma menor percepção de sintomas, pelo que a espirometria será útil nesta faixa etária. Objetivo do estudo - Descrever o resultado da espirometria com prova de broncodilatação, de acordo com os critérios GOLD e prevalência de sintomas respiratórios dos idosos residentes num lar de Lisboa.