Particle fluxes of the bathypelagic sediment trap CVOO-3 in the eastern tropical North Atlantic for the period December 2009 until May 2011

Particle fluxes at the Cape Verde Ocean Observatory (CVOO) in the eastern tropical North Atlantic for the period December 2009 until May 2011 are discussed based on bathypelagic sediment trap time-series data collected at 1290 and 3439 m water depth. The typically oligotrophic particle flux pattern with weak seasonality is modified by the appearance of a highly productive and low oxygen (minimum concentration below 2 µmol kg**-1 at 40 m depth) anticyclonic modewater eddy (ACME) in winter 2010. The eddy passage was accompanied by unusually high mass fluxes of up to 151 mg m**-2 d**-1, lasting from December 2009 to May 2010. Distinct biogenic silica (BSi) and organic carbon flux peaks of ~15 and 13.3 mg m**-2 d**-1, respectively, were observed in February-March 2010 when the eddy approached the CVOO. The flux of the lithogenic component, mostly mineral dust, was well correlated with that of organic carbon, in particular in the deep trap samples, suggesting a tight coupling. The lithogenic ballasting obviously resulted in high particle settling rates and, thus, a fast transfer of epi-/meso-pelagic signatures to the bathypelagic traps. We suspect that the two- to three-fold increase in particle fluxes with depth as well as the tight coupling of mineral dust and organic carbon in the deep trap samples might be explained by particle focusing processes within the deeper part of the eddy. Molar C : N ratios of organic matter during the ACME passage were around 18 and 25 for the upper and lower trap samples, respectively. This suggests that some productivity under nutrient (nitrate) limitation occurred in the euphotic zone of the eddy in the beginning of 2010 or that a local nitrogen recycling took place. The d15N record showed a decrease from 5.21 to 3.11 per mil from January to March 2010, while the organic carbon and nitrogen fluxes increased. The causes of enhanced sedimentation from the eddy in February/March 2010 remain elusive, but nutrient depletion and/or an increased availability of dust as a ballast mineral for organic-rich aggregates might have contributed. Rapid remineralisation of sinking organic-rich particles could have contributed to oxygen depletion at shallow depth. Although the eddy formed in the West African coastal area in summer 2009, no indications of coastal flux signatures (e.g. from diatoms) were found in the sediment trap samples, confirming the assumption that the suboxia developed within the eddy en route. However, we could not detect biomarkers indicative of the presence of anammox (anaerobic ammonia oxidation) bacteria or green sulfur bacteria thriving in photic zone suboxia/hypoxia, i.e. ladderane fatty acids and isorenieratene derivatives, respectively. This could indicate that suboxic conditions in the eddy had recently developed and/or the respective bacterial stocks had not yet reached detection thresholds. Another explanation is that the fast-sinking organic-rich particles produced in the surface layer did not interact with bacteria from the suboxic zone below. Carbonate fluxes dropped from -52 to 21.4 mg m**-2 d**-1 from January to February 2010, respectively, mainly due to reduced contribution of shallow-dwelling planktonic foraminifera and pteropods. The deep-dwelling foraminifera Globorotalia menardii, however, showed a major flux peak in February 2010, most probably due to the suboxia/hypoxia. The low oxygen conditions forced at least some zooplankton to reduce diel vertical migration. Reduced "flux feeding" by zooplankton in the epipelagic could have contributed to the enhanced fluxes of organic materials to the bathypelagic traps during the eddy passage. Further studies are required on eddy-induced particle production and preservation processes and particle focusing.

Under-ice export flux measurements by short-term drifting sediment traps at 27 stations in the Arctic Ocean during summer 1995, 1997, and 2012

A critical question regarding the organic carbon cycle in the Arctic Ocean is whether the decline in ice extent and thickness and the associated increase in solar irradiance in the upper ocean will result in increased primary production and particulate organic carbon (POC) export. To assess spatial and temporal variability in POC export, under-ice export fluxes were measured with short-term sediment traps in the northern Laptev Sea in July-August-September 1995, north of the Fram Strait in July 1997, and in the Central Arctic in August-September 2012. Sediment traps were deployed at 2-5 m and 20-25 m under ice for periods ranging from 8.5 to 71 h. In addition to POC fluxes, total particulate matter, chlorophyll a, biogenic particulate silica, phytoplankton, and zooplankton fecal pellet fluxes were measured to evaluate the amount and composition of the material exported in the upper Arctic Ocean. Whereas elevated export fluxes observed on and near the Laptev Sea shelf were likely the combined result of high primary production, resuspension, and release of particulate matter from melting ice, low export fluxes above the central basins despite increased light availability during the record minimum ice extent of 2012 suggest that POC export was limited by nutrient supply during summer. These results suggest that the ongoing decline in ice cover affects export fluxes differently on Arctic shelves and over the deep Arctic Ocean and that POC export is likely to remain low above the central basins unless additional nutrients are supplied to surface waters.

In vitro and in vivo evaluation of lyophilized bioprosthetic valve

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Modelagem dinâmica e simulação computacional de poços de petróleo verticais e direcionais com elevação por bombeio mecânico

LINS, Filipe C. A. et al. Modelagem dinâmica e simulação computacional de poços de petróleo verticais e direcionais com elevação por bombeio mecânico. In: CONGRESSO BRASILEIRO DE PESQUISA E DESENVOLVIMENTO EM PETRÓLEO E GÁS, 5. 2009, Fortaleza, CE. Anais... Fortaleza: CBPDPetro, 2009.

Oil Flow Rate Measurements Using 198au And Total Count Technique

In industrial plants, oil and oil compounds are usually transported by closed pipelines with circular cross-section. The use of radiotracers in oil transport and processing industrial facilities allows calibrating flowmeters, measuring mean residence time in cracking columns, locate points of obstruction or leak in underground ducts, as well as investigating flow behavior or industrial processes such as in distillation towers. Inspection techniques using radiotracers are non-destructive, simple, economic and highly accurate. Among them, Total Count, which uses a small amount of radiotracer with known activity, is acknowledged as an absolute technique for flow rate measurement. A viscous fluid transport system, composed by four PVC pipelines with 13m length (12m horizontal and 1m vertical) and ½, ¾, 1 and 2-inch gauges, respectively, interconnected by maneuvering valves was designed and assembled in order to conduct the research. This system was used to simulate different flow conditions of petroleum compounds and for experimental studies of flow profile in the horizontal and upward directions. As 198Au presents a single photopeak (411,8 keV), it was the radioisotope chosen for oil labeling, in small amounts (6 ml) or around 200 kBq activity, and it was injected in the oil transport lines. A NaI scintillation detector 2”x 2”, with well-defined geometry, was used to measure total activity, determine the calibration factor F and, positioned after a homogenization distance and interconnected to a standardized electronic set of nuclear instrumentation modules (NIM), to detect the radioactive cloud.

Contrôle adaptatif d'un bioréacteur cardiaque par algorithme génétique

Un bon fonctionnement du coeur humain est primordial pour maintenir une bonne qualité de vie. Cependant, lorsque le coeur est défaillant, certaines interventions chirurgicales s’avèrent nécessaires pour prolonger l’espérance de vie. Dans le cadre d’un projet multidisciplinaire reliant le génie mécanique avec le domaine biomédical, notre équipe travaille sur la fabrication de valves cardiaques conçues entièrement par génie tissulaire. Pour y parvenir, il est important d’obtenir des propriétés mécaniques optimales pour les tissus biologiques. Afin d’obtenir ces propriétés mécaniques, un outil important a été fabriqué lors d’une étude antérieure : le bioréacteur cardiaque. Le bioréacteur cardiaque permet de reproduire l’environnement physiologique du coeur, notamment les conditions de débit et de pression. Il est crucial de bien contrôler ces conditions, car celles-ci jouent un rôle important lors du conditionnement des substituts valvulaires. Toutefois, il est complexe de contrôler simultanément ces deux conditions de manière efficace. C’est pourquoi notre équipe s’est concentrée sur le développement d’une nouvelle stratégie de contrôle afin que le bioréacteur puisse reproduire le plus fidèlement possible l’environnement physiologique. Plusieurs techniques de contrôle ont été essayés jusqu’à maintenant. Par contre, leur précision était généralement limitée. Une nouvelle approche a donc été envisagée et est présentée dans ce mémoire. Cette nouvelle approche pour le contrôle du bioréacteur est basée sur un type d’algorithme bien connu mais encore très peu utilisé en contrôle : les algorithmes génétiques. Cette approche prometteuse nous a permis de produire des résultats dépassant tous ceux obtenus jusqu’à maintenant pour l’une des deux conditions, soit le débit physiologique.

Nucleic Acid Diagnostics using Isotachophoresis and Isothermal Amplification

Thesis (Ph.D.)--University of Washington, 2016-08

Microturbinas em redes de abastecimento de água

Nos dias de hoje a sociedade exige níveis qualitativos de vida cada vez mais elevados, o que torna prioritária a conceção de sistemas eficientes, não poluidores, económicos e diversificados que permitam uma gestão integrada e racionalizada de recursos tão escasso como é o da água e da energia. Em sistemas de abastecimento de água, o uso de válvulas redutoras de pressão (VRP) visa a uniformização e controlo de pressões, promovendo uma perda de carga localizada que dissipa a energia hidráulica presente através da redução dos valores de pressão a jusante. Estas são fundamentais no controlo e redução de pressão. A utilização de microturbinas é uma alternativa sustentável para o controle de pressão e, simultaneamente, para a produção de energia elétrica. Trata-se de um método de mitigação para controlar as perdas referidas convergindo no âmbito da eficiência energética. Na perspetiva de promover um aproveitamento de energia nas redes de abastecimento de água, o presente trabalho sugere a substituição de válvulas redutoras de pressão (VRP) por microturbinas. Desse modo, apresenta-se um método automático de seleção de (i) local para implementação e (ii) projeto de microturbinas para sistemas de abastecimento de água. Para a modelação do funcionamento dos sistemas hidráulicos recorre-se ao simulador hidráulico EPANET. Esta ferramenta possibilita avaliação de caudais e pressões em todos os pontos da rede durante um determinado intervalo de tempo. A metodologia desenvolvida permite selecionar o local ideal no sistema hidráulico através de uma análise de cada secção conduta-nó escolhendo-se a melhor opção baseada na produção de energia. Depois da localização procede-se à seleção do tipo de turbina (Kaplan, Francis, Pelton e Cross-flow) que vai depender das características do sistema hidráulico. Na etapa seguinte apresenta-se os resultados obtidos pela turbina nomeadamente a produção de energia elétrica anual, o investimento necessário, o tempo de retorno e a rentabilização ao final de um período de 25 anos. Na última etapa da metodologia, de forma avaliar o comportamento do sistema final, realiza-se uma nova simulação da rede mas tendo em conta a introdução da microturbina no local. Apresentam-se alguns casos de estudo que validam a ferramenta desenvolvida. A metodologia desenvolvida é comparada com um caso de estudo real. Em ambos os exemplos simulados a metodologia aplicada permite obter soluções com ganhos energéticos significativos associados ao sistema. Apenas num dos exemplos se observaram que a implementação da microturbina no sistema hidráulico não seria economicamente rentável.

Agrandissement des feuillets mitraux en insuffisance aortique : un mécanisme actif pouvant prévenir l’insuffisance mitrale dans le ventricule dilaté

L’insuffisance mitrale (IM) fonctionnelle est une complication fréquente des cardiopathies, causée par la dilatation du ventricule gauche (VG) qui empêche la valve de se fermer. L’insuffisance aortique (IA) est une condition associée à des valves mitrales (VM) inhabituellement grandes, et relativement peu d’IM malgré des VG très dilatés. Cet élargissement de la VM a le potentiel de prévenir l’IM dans les VG dilatés. Les mécanismes sont cependant peu compris : il n’est pas clair s’il s’agit d’une croissance active ou d’un étirement passif des feuillets. Également, le timing de l’adaptation valvulaire n’est pas connu. Notre hypothèse est que l’agrandissement de la valve mitrale en IA est un phénomène actif avec réactivation des mécanismes de croissance embryonnaire. Cent-onze rats ont été divisés en deux groupes : IA (perforation aortique) et contrôle. Les animaux ont été sacrifiés à 48 h, 1 semaine et 3 mois après la création du modèle. Des échocardiographies ont évalué la sévérité de l’IA, la présence d’IM et les dimensions du VG. Les valves ont été prélevées pour analyses microscopiques et moléculaires. La création de l’insuffisance aortique a entrainé une dilatation et une hypertrophie du VG. Malgré cette dilatation rapide du VG, aucun animal n’a développé de l’IM fonctionnelle. À l’échographie, le feuillet antérieur mitral était significativement plus long dans les groupes IA. Par microscopie, les feuillets étaient plus épais dés la première semaine. L’IA était associée à une surexpression de collagène α-SMA (un marqueur de myofibroblastes), TGF-β1 et MMP-2 dans le tissu valvulaire dès la première semaine. Les valves exposées à l’IA étaient également positives pour ces différents facteurs dés les premiers jours. L’agrandissement de la VM est un phénomène actif qui survient rapidement après la création de l’IA, en parallèle de la dilatation du VG. La stimulation de cette croissance dans d’autres pathologies pourrait contribuer à prévenir l’IM fonctionnelle.