148 research outputs found

    Optical in situ size determination of single lanthanide-ion doped oxide nanoparticles

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    International audienceWe show that the size of a lanthanide-ion doped nanoparticle can be accurately determined from its luminosity. The optically determined size distribution is in very good agreement with the distribution obtained from transmission electron microscopy. These data confirm that single nanoparticles are visualized in microscopy experiments. Nanoparticles as small as 13 nm are detectable with integration times of 500 ms. (c) 2006 American Institute of Physics

    TLS- and inventory-based Magnitude – Frequency relationship for rockfall in Montserrat and Castellfollit de la Roca

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    Hazard scenarios are defined by a representative event of a certain magnitude, which corresponds to a frequency of occurrence or annual probability. In rockfall, scenario magnitude is identified by the total volume detached. Therefore, in diffuse hazard assessment it is crucial to fit this relationship magnitude/frequency, called McF, where cumulated frequency is quoted in spatial & temporal terms. Inventories are the classical source of data to deal with this objective. Last decade, TLS or digital photogrammetry monitoring came to offer a complementary approach. The samples obtained by the two methods have a specific coverage and each has its own lack of information that can be compensated together.Peer ReviewedPostprint (published version

    Caractérisation de tissu osseux et de biomatériaux pour la régénération osseuse sur gros volume.

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    L’objectif de cette Ă©tude est de dĂ©velopper un processus expĂ©rimental de rĂ©gĂ©nĂ©ration de tissus osseux de grand volume. Une premiĂšre Ă©tape vise Ă  produire du matĂ©riau osseux Ă  partir de lambeau de pĂ©rioste vascularisĂ© et Ă  le caractĂ©riser grĂące a des essais d’indentation. Ensuite, nous dĂ©veloppons un process impliquant un biomatĂ©riau poreux et biodĂ©gradable utilisĂ© comme rĂ©ceptacle de cellules mĂ©senchymateuses. Dans les deux cas, le nouveau matĂ©riau obtenu est Ă©tudiĂ© grĂące Ă  des tests mĂ©caniques et biologiques

    Rockfall Magnitude-Frequency Relationship Based on Multi-Source Data from Monitoring and Inventory

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    Quantitative hazard analysis of rockfalls is a fundamental tool for sustainable risk management, even more so in places where the preservation of natural heritage and people's safety must find the right balance. The first step consists in determining the magnitude-frequency relationship, which corresponds to the apparently simple question: how big and how often will a rockfall be detached from anywhere in the cliff? However, there is usually only scarce data on past activity from which to derive a quantitative answer. Methods are proposed to optimize the exploitation of multi-source inventories, introducing sampling extent as a main attribute for the analysis. This work explores the maximum possible synergy between data sources as different as traditional inventories of observed events and current remote sensing techniques. Both information sources may converge, providing complementary results in the magnitude-frequency relationship, taking advantage of each strength that overcomes the correspondent weakness. Results allow characterizing rockfall detachment hazardous conditions and reveal many of the underlying conditioning factors, which are analyzed in this paper. High variability of the hazard over time and space has been found, with strong dependencies on influential external factors. Therefore, it will be necessary to give the appropriate reading to the magnitude-frequency scenarios, depending on the application of risk management tools (e.g., hazard zoning, quantitative risk analysis, or actions that bring us closer to its forecast). In this sense, some criteria and proxies for hazard assessment are proposed in the paper

    La longue séquence de Marchésieux: reconstitution de paléoenvironnements marins durant le premier cycle glaciaire de l'hémisphÚre nord

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    International audienceA l'échelle des cinq derniers millions d'années, les enregistrements paléoclimatiques restitués par les sédiments océaniques illustrent le contrÎle des paramÚtres orbitaux (précession, obliquité et excentricité) sur le climat global. La tendance au refroidissement qui accompagne la fin du NéogÚne est ainsi marquée, vers -2,4 Ma, par le développement rapide des calottes de glace de l'hémisphÚre nord (Shackleton et al., 1984). Alors que l'histoire du climat global restituée par les enregistrements océaniques est sans cesse précisée, les données concernant l'évolution des environnements continentaux et cÎtiers au cours de ces changements restent essentiellement fragmentaires. Le forage effectué à Marchésieux (Manche; Normandie) a permis de réaliser une étude pluridisciplinaire de la signature de ce premier cycle glaciaire de l'hémisphÚre nord (Prétiglien). Les premiers résultats stratigraphiques, paléoenvironnementaux (eustatisme, température, paléobathymétrie) sont présentés
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