Résumé : Dans le cadre de la promotion de systèmes de culture alternatifs à moindres intrants chimiques, des études sur l'introduction de plantes de service ayant vocation à réduire l'usage des pesticides et engrais azotés mobilisent un effort de recherche considérable. Dans le cadre de la production bananière pour laquelle la nuisibilité causée par les nématodes phytoparasites constitue l'une des principales contraintes, une des principales alternatives à l'utilisation de nématicides chimiques repose sur l'usage raisonné en rotation ou en association culturale de plantes de service à propriétés nématorégulatrices. Parmi les espèces candidates, celles du genre Crota/aria spp. ont largement été étudiées en raison de leur aptitude à contrôler les nématodes phytoparasites. Une méta-analyse révèle cependant que même si de nombreux auteurs s'accordent à reconnaître les propriétés allélopathiques des plantes de cette espèce, ils sont également enclins à reconnaître la forte variabilité d'expression de ces propriétés vis-à-vis du contrôle des nématodes selon les situations expérimentées. L'objectif de ce travail repose sur la compréhension du déterminisme biochimique des exsudats. La stratégie expérimentale mise en oeuvre a consisté à tester en conditions contrôlées le comportement biochimique des exsudats racinaires de deux espèces de crotalaires (C retusa, C spectabilis) et d'une espèce sensible, le bananier dessert (Musa spp.) en fonction i) de conditions biotiques variées -i.e. présence ou non de nématodes (Radopholus similis et Meloidogyne arenariaï, et présence ou non de mycorhizes-, ii) de conditions abiotiques contrastées -i.e. utilisation d'un sol naturel vs. substrat neutre, ajout ou non d'engrais chimique. La méthodologie innovante des «plantes à traire » (Brevet INRA) a été requise pour pouvoir travailler sur les exsudats racinaires des plantes conditionnées plutôt que sur des Iixiviats, comme réalisé dans des expérimentations antérieures.Les résultats obtenus en spectrophométrie visible montrent que la modification des conditions abiotiques affecte de manière importante les profils biochimiques des plantes étudiées. En présence du nématode 1..·1. arenaria les profils biochimiques des deux crotalaires sont également modifiés. Des biotests réalisés à l'aide des exsudats racinaires conditionnés au préalable par les modifications biotiques ont permis de démontrer l'effet nématostatique des crotalaires. Des analyses biochimiques en Ge-MS mettent en évidence de manière plus précise des molécules actives mises en jeu sous différentes modalités biotiques et abiotiques. Ces recherches, de portée générique, permettront de mieux comprendre les conditions de l'environnement qui régulent les profils biochimiques des exsudats racinaires des crotalaires et par extension, seront applicables aux recherches menées sur d'autres plantes de service candidates. Ceci aidera, à terme, à définir les conditions environnementales à réunir, pour orienter de manière optimale les effets allélopathiques dans une perspective de nématorégulation naturelle
As part of the promotion of alternative cropping systems at lower chemical inputs, studies on the introduction of cover crops designed to reduce the use of pesticides and nitrogen fertilizers mobilize a considerable research effort. Under banana production for which the hannfu1ness caused by plant-parasitic-nematodes is one ofthe main constraints, one of the main alternatives to the use ofchemical nematicides is based on the rational use in rotation or intercropping of cover rI crops to proteet crops from plant-parasitic-nematodes, Among the candidate species, the species from the genus of Crota/aria spp. have been widely studied because of their ability to control plant parasitic-nematodes. A meta-analysis reveals that although many authors agree allelopathic properties of these species, they are also likely to recognize the high variability of expression of these properties vis-àvis the control of nematodes according to the situations experieaced.. The objective of this woIk is focnsed on the onderstanding of the biochemical determinism of mot exudates onder environment biotic and abiotic variations. The experimental strategy was 10 test onder controlled conditions the biochemical behavior of mot exudates of two species of crotalarias (C retusa, C. spectabilis) and a susceptible species, the dessert banana crop (Musa spp.) with i) modification ofbiotic conditions -ie presence or absence of nematodes iMeloidogyne arenaria and Radopho/us similis), and presence or absence of mycorrhiza-ii) contrasting abiotic conditions -ie using a natural soil vs. neutral substrate, whether to add fertilizer. The innovative methodology of "milking plants" (patent INRA) was required in order to work on the root exudates of plants packed rather thanleachate, as done in previous experiments. The results obtained show that 'visible spectrophotometry changing abiotic conditions affect significantly the biochemical profiles of the studied plants. In the presence of nematode M. arenaria biochemical profiles of both crotalarias are also changed. Bioassays conducted using mot exudates conditioned in advance by biotic changes have demonstrated the effect of nématostatique crotalarias. Biochemical Ge-MS demonstrate more clearly active molecules that are involved in varions biotic and abiotic conditions. This research, generic scope, to better understand the environmental conditions that regulate biochemical profiles of mot exudates crotalarias and by extension, will apply to research on other plants service candidates. This will ultimately define the environmental conditions to meet, to guide optimal allelopathic effects from the perspective ofnatural nématorégulation

http://www.theses.fr/2012AGUY0561/document

Éditeur(s) : AIHP-GEODE : Archéologie Industrielle, Histoire, Patrimoine/Géographie- Développement Environnement de la Caraïbe
Extrait de : "Rimed gran moun. Plantes et usages au fil du temps" : séminaire, le 15 décembre 2012. Université des Antilles et de la Guyane
Description : Après avoir souligné toute la complexité du mot "précurseur", Jacques Dumont présente quelques auteurs de références qu'il considère comme "précurseurs" de la publication en botanique. A partir de cette présentation, il s'interroge sur les types d'usages des plantes aux Antilles. Usage traditionnel ou thérapeutique ? Pour Jacques Dumont la réponse se trouve dans la bibliographie des auteurs "précurseurs". Après un arrêt sur les enjeux épistémologiques de la botanique, il s'interroge sur la prise en charge actuelle de la santé en se demandant, quel type de médecine domine.

Droits : CC-BY-NC-ND - Attribution - Pas d'utilisation commerciale - Pas de modification
Permalien : http://www.manioc.org/fichiers/V13004
V13004

Éditeur(s) : HAL CCSD
Résumé : International audience
Cet article prolonge le débat introduit dans l'article précédent de la rubrique « Innovations obsjectivées ». Il s'agit ici de discuter un certain nombre de thèmes autour de enseigner et apprendre afin que les apprentissages en sport collectif à l'école deviennent plus efficaces. A cet effet, nous allons examiner successivement comment les élèves apprennent, comment les professeurs enseignent et aussi comment enseigner pour que les élèves apprennent et retiennent. Dans une dernière partie, une discussion est menée autour de la question de l'égal accès de toutes et tous aux fondamentaux de la culture scolaire et sportive. Mots clés : sport collectif, connaissance, enseigner, apprendre, réussite Le développement des technologies et, en particulier, l'avènement de la société de l'information ont augmenté les possibilités d'accès des individus à l'information et au savoir. Mais, en même temps, tous ces phénomènes entraînent une modification des compétences à acquérir pour le travail ou les loisirs. La société du futur sera donc une société cognitive est-il souvent affirmé (Commission européenne, 1995) et c'est dans cette perspective que se place le rôle central de l'éducation et la formation. L'éducation physique et sportive a plus que jamais une place prépondérante à jouer dans une société où la sédentarité devient une menace. Aussi, dans cette deuxième partie, nous allons discuter un certain nombre de thèmes autour d'enseigner et apprendre afin que les apprentissages en sport collectif à l'école deviennent plus efficaces. A cet effet, nous allons examiner successivement comment les élèves apprennent, comment les professeurs enseignent et aussi comment enseigner pour que les élèves apprennent et retiennent. Enfin une discussion sera menée autour de la question de l'égal accès de toutes et tous aux fondamentaux de la culture scolaire et sportive.
eJRIEPS

hal-01620910
https://hal.univ-antilles.fr/hal-01620910
https://hal.univ-antilles.fr/hal-01620910/document
https://hal.univ-antilles.fr/hal-01620910/file/7.%20eJR%2040%20Gr%C3%A9haigne%20et%20al.%202.pdf

Éditeur(s) : EDP Sciences
Résumé : Lessons for the future from two development projects in aquaculture in the French overseas territories. Numerous research and development projects have been launched since the seventies in the French overseas territories. Their aim was to foster new activities in agriculture based on local productions for local markets, notably in the French West Indies (FWI). In this paper we analyze two development projects on the rearing of giant freshwater prawn, one in the FWI and the other in French Guyana, over twenty years after their launching. The purpose of these compared studies is twofold: first to try to understand why a set of relevant technical innovations ended in failure 15 years later; second to identify recommendations in terms of methodology in order to diminish risks of mistakes or failure for future projects. To reach this goal we followed two approaches. A first analysis is based on a set of three criteria: social acceptability, legitimacy and time planning. The second analysis, justified by the subjective need for an explanatory tool, is based on the actor-network theory. The results show that beyond the levels of political support and financial investment and support the three key criteria for success are: (i) reactivity of the decision-makers, notably when markets change, (ii) quality of leadership transfer between the launching phase and the stabilized phase, and (iii) capacity of the decision-makers to take into account the concrete consequences of the various scenarios. Regarding this third criterion, our analysis suggests that the scenario of full technical success needs to be explored, notably in terms of economic sustainability. The integration of these two types of analyses into an ex-ante frame should contribute to reducing risks of failure in similar development projects.
De nombreux projets d’aquaculture ont été menés depuis les années 1970 dans les territoires et départements français d’outre-mer. L’objectif était de diversifier l’agriculture avec des productions destinées au marché local comme aux Antilles, ou à l’exportation comme en Guyane. L’étude s’intéresse au bilan de deux projets d’élevage de la crevette tropicale d’eau douce aux Antilles et en Guyane, plus de vingt ans après leur lancement. L’objectif est de comprendre comment des innovations technologiques pertinentes ont conduit à deux échecs sur le moyen terme et de tirer des recommandations de méthode afin de réduire les risques d’erreurs ultérieures. Pour cela, deux cadres d’analyse sont mobilisés : le premier s’appuie sur les concepts de temporalité, légitimité et acceptabilité ; le second, motivé par la recherche subjective de cadres explicatifs, emprunte la vision de la théorie de l’acteur-réseau. Les trois déterminants majeurs du succès ou de l’échec se révèlent être la réactivité des responsables face aux problèmes d’adaptation à l’évolution des marchés, la qualité du transfert du leadership lors du passage de la phase de lancement à la phase de croisière et enfin la capacité de prendre en compte dès le départ les conséquences des scénarios d’évolution du projet, y compris la réussite technique. Une capacité d’intégration de ces types d’analyse, dans un cadre ex ante, devrait permettre de réduire les risques d’échec dans des projets de développement similaires à venir.
Natures Sciences et Sociétés (1240-1307) (EDP Sciences), 2013-12 , Vol. 21 , N. 4 , P. 400-415

Droits : NSS-Dialogues, EDP Sciences 2014
http://archimer.ifremer.fr/doc/00187/29784/28242.pdf
DOI:10.1051/nss/2014004
http://archimer.ifremer.fr/doc/00187/29784/

Résumé : La navigation côtière a pris, depuis quelques années, un développement considérable dans notre marine militaire et attiré l'attention des officiers sur des questions de navigation laissées depuis longtemps dans l'oubli. La connaissance de la côte, de ses ports, de la manière d'y naviguer, l'étude du pilotage des côtes de France, en un mot, a succédé, chez beaucoup de nos camarades, à l'étude du régime général des vents ou des routes de circumnavigation, legs intéressant de la marine à voiles et des voyages réguliers en Nouvelle-Calédonie.

Droits : 1894 Imprimerie Nationale, Paris
http://archimer.ifremer.fr/doc/00032/14310/11590.pdf
http://archimer.ifremer.fr/doc/00032/14310/

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Introduction Les Maldives sont peuplées depuis plus de 2500 ans et leur nom viendrait du mot malodheep signifiant « guirlande » en sanskrit (Risk and Sluka, 2000). L’archipel compte en effet 26 atolls géographiques, classés en 19 atolls administratifs, qui s’étirent sur près de 800 km du nord au sud et 130 km d’est en ouest (figure 1). Les 1 200 îles répertoriées constituent une surface émergée totale de 297 km2 dont seulement 38 % sont habités par les 270 100 habitants que comptait le pays e...
Maldives

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.862
http://journals.openedition.org/etudescaribeennes/862

Éditeur(s) : HAL CCSD Springer Verlag
Résumé : GPS velocities and seismicity across the Betic-Rif Arc structural domains (Morocco and Iberia) provide a basis to evaluate present-day seismotectonic processes between different deformation belts. The results show asymmetric movements in the complex Alboran system accommodating the convergence between the African (Nubian) and Eurasian plates. While the Betic Mountains are attached to Iberia, moving toward the southeast with respect to Africa, the Rif is divided into three blocks with distinct displacements relative to Nubia: (1) the Tangier block moving southeastward, (2) the Central Rif block moving SSW, and (3) the Oriental Rif block undergoing clockwise rotation. GPS-derived motions decrease in rate from the Rif nappes complex to the foreland.
ISSN: 0010-7999

hal-00411144
https://hal.archives-ouvertes.fr/hal-00411144
DOI : 10.1016/j.crte.2008.02.003

Éditeur(s) : HAL CCSD American Geophysical Union (AGU)
Résumé : International audience
[1] The Pyrenees, north of the North Pyrenean fault, display a complex structure involving a succession of peridotite massifs, basement massifs, and mid-Cretaceous to Late Cretaceous basins located in a narrow domain, which was affected by a mid-Cretaceous, preorogenic, high-temperature, low-pressure metamorphism. The Late Cretaceous basins were interpreted either as pull-apart basins formed during transcurrent motion of Iberia relative to Eurasia or as remnants of a larger extensional basin. Recent models support that peridotite massifs result from the exhumation of the mantle during this preorogenic event. The northern boundary of the Agly basement massif shows evidence of ductile deformation of the basal formations of the Agly sedimentary cover. Macroscopic and microscopic kinematics indicators consistent with asymmetry of crystallographic fabrics suggest normal sense of shear and thus suggest detachment, at least partial, of the Mesozoic cover from its basement. Triassic to Early Cretaceous limestones are mylonitic and consistently shows a foliation, a NS- to NE-trending lineation, shear criteria suggesting top-to-the-north shearing and locally boudinage. At the microscopic scale, mylonites are characterized by a very fine grain size, frequently <10 µm. They contain larger, partially recrystallized calcite parent grains and undeformed quartz grains with calcite fringes crystallized in pressure shadows. In these mylonites, calcite systematically shows a weak but well-defined crystallographic-preferred orientations, suggesting HT dislocation creep combined to diffusion creep and possibly grain boundary sliding in the finest fraction of the mylonites. Paleotemperatures determined using Raman spectrometry suggest synkinematic temperature conditions in the range 340-390°C, in good agreement with observed microstructures and calcite CPO. The mylonitic fabric in Mesozoic limestones is folded by EW-trending Pyrenean folds north of the Agly basement massif, attesting that this fabric formed before the Pyrenean orogeny. These data consistently support preorogenic extension under medium-temperature conditions of the northern Agly massif and likely of the massif itself. Since simultaneously (~100 Ma) a mid-Cretaceous basin opened south of the basement massif, we suggest a model of preorogenic exhumation of the Agly massif in response to the regional extension associated to the rotation of Iberia. This model may explain the exhumation of the North Pyrenean massifs during a single preorogenic event that allowed the opening of extensional basins and the exhumation of the lithospheric mantle. All these structures being subsequently reworked during the Pyrenean orogeny.
ISSN: 0278-7407

hal-00852833
https://hal.archives-ouvertes.fr/hal-00852833
DOI : 10.1002/tect.20015

Éditeur(s) : HAL CCSD Oxford University Press (OUP)
Résumé : International audience
A temporary network of 10 broad-band seismic stations has been installed in French Polynesia for the Polynesian Lithosphere and Upper Mantle Experiment (PLUME). All the seismic stations were installed either on volcanic islands or on atolls of the various archipelagos of French Polynesia in a manner which complements the geographic coverage provided by the regional permanent stations. The primary aim of PLUME is to image the upper mantle structures related to plate motion and hotspot activity. However, because of its proximity to all sites, the ocean is responsible for a high level of noise in the seismic data and we show that these data can also be used to analyse ocean wave activity. The power spectral density (PSD) analyses of the seismic data recorded in French Polynesia show clear peaks in the 0.05– 0.10 Hz band (periods between 10 and 20 s), which corresponds to swell frequencies. Clear peaks in this frequency band are also observed in infrasonic data recorded on Tahiti. Ground motion analysis shows that the swell-related seismic noise (SRSN) is linearly polarized in the horizontal plane and its amplitude decreases rapidly with the distance from the shore. The microseismic and the infrasonic 'noise' amplitudes show very similar variations from station to station and both are strongly correlated with the swell amplitudes predicted by the National Oceanic and Atmospheric Administration (NOAA), wind-forced, 'WaveWatch' models. The swell direction can be estimated from SRSN polarization analysis but this has to be done with care since, for some cases, the ground motions are strongly controlled by the islands' anisometric shapes and by swell refraction processes. We find cases, however, such as Tahiti or roughly circular Tuamotu atolls, where the azimuth of the swell is in good agreement with the seismic estimates. We, therefore, demonstrate that the SRSN and the infrasonic signal observed in French Polynesia can be used in such cases as a proxy for swell amplitude and azimuth. From the continuous analysis of the data recorded in 2003 at the permanent seismic station PPTL in Tahiti, transfer functions have been obtained. This could provide a way to quantify the swell activity during the last two decades and, therefore, assist in the investigation of climate changes.
ISSN: 0956-540X

hal-01388809
http://hal.univ-reunion.fr/hal-01388809
http://hal.univ-reunion.fr/hal-01388809/document
http://hal.univ-reunion.fr/hal-01388809/file/Barruol_swell_GJI2006.pdf
DOI : 10.1111/j.1365-246X.2006.02871.x

Éditeur(s) : HAL CCSD American Geophysical Union (AGU)
Résumé : International audience
Subduction of a narrow slab of oceanic lithosphere beneath a tightly curved orogenic arc requires the presence of at least one lithospheric scale tear fault. While the Calabrian subduction beneath southern Italy is considered to be the type example of this geodynamic setting, the geometry, kinematics and surface expression of the associated lateral, slab tear fault offshore eastern Sicily remain controversial. Results from a new marine geophysical survey conducted in the Ionian Sea, using high-resolution bathymetry and seismic profiling reveal active faulting at the seafloor within a 140 km long, two-branched fault system near Alfeo Seamount. The previously unidentified 60 km long NW trending North Alfeo Fault system shows primarily strike-slip kinematics as indicated by the morphology and steep-dipping transpressional and transtensional faults. Available earthquake focal mechanisms indicate dextral strike-slip motion along this fault segment. The 80 km long SSE trending South Alfeo fault system is expressed by one or two steeply dipping normal faults, bounding the western side of a 500+ m thick, 5 km wide, elongate, syntectonic Plio-Quaternary sedimentary basin. Both branches of the fault system are mechanically capable of generating magnitude 6–7 earthquakes like those that struck eastern Sicily in 1169, 1542, and 1693.
ISSN: 0278-7407

insu-01256887
https://hal-insu.archives-ouvertes.fr/insu-01256887
https://hal-insu.archives-ouvertes.fr/insu-01256887/document
https://hal-insu.archives-ouvertes.fr/insu-01256887/file/GutscherEtal_2015_Tectonics.pdf
DOI : 10.1002/2015TC003898

Éditeur(s) : HAL CCSD Wiley-Blackwell
Résumé : International audience
In the Oman ophiolite, the large scale Makhibiyah shear zone, in Wadi Tayin massif was generated with no or little relative motion between the two adjacent blocks, in contrast with what is reported from otherwise similar shear zones in deep crust and upper mantle. This shear zone is asymmetrical with, along one margin an asthenospheric mantle (similar to 1200 degrees C) and along the adjacent margin, a lithospheric mantle (similar to 1000 degrees C). Within the hotter side and with increasing shear strain, horizontal flow lines smoothly swing towards the shear zone direction before abutting against the wall of the lithosphere side. Profuse mafic melts issued from the hotter mantle are frozen in the shear zone by cooling along this lithospheric wall. Tectonic and magmatic activities are entirely localized within the asthenospheric compartment. Mantle flow lines were rotated, during their channelling along this NW-SE shear zone, in the NW and SE opposite directions. Depending on whether the flow lines are deviated NW or SE, dextral or sinistral shear sense is recorded in the shear band mylonitic peridotites. This demonstrates that the shear zone was not generated by strike-slip motion, a conclusion supported by regional observations.
ISSN: 0954-4879

hal-00411334
https://hal.archives-ouvertes.fr/hal-00411334
DOI : 10.1111/j.1365-3121.2008.00806.x

Éditeur(s) : HAL CCSD Oxford University Press (OUP)
Résumé : International audience
We analyse temporal variations of gravity measured in southern Taiwan since November 2006 at 10 sites using absolute gravimeters and, since November 2008, at 70 sites using a relative gravimeter. We describe and apply methods to interpret the gravity changes in terms of local hydrological processes and vertical ground motions. The effect of land water is computed from local rainfall data and a model of rain accumulation and discharge in the ground. The effect of the vertical motions of the ground is estimated using time-series of permanent Global Positioning System (GPS) stations and the theoretical gravity to height ratio of −2 μGal cm−1. Unexpectedly, Morakot typhoon (2009 August), the strongest typhoon in Taiwan in 50 yr, was responsible for the highest gravity changes. Morakot triggered numerous large landslides and debris flow deposits. Their thicknesses are estimated from the gravity changes (up to ∼280 μGal) along with field observations and satellite images.
ISSN: 0956-540X

hal-00768216
https://hal.archives-ouvertes.fr/hal-00768216
DOI : 10.1093/gji/ggs019

Éditeur(s) : Université de Bretagne Occidentale
Résumé : Study of mineral suspended particulate matter (SPM) is essential to understand ecosystem dynamics. SPM influences light penetration which is closely related to primary production and carries pollutants and nutrients within the water masses. This work aims to study near-surface mineral SPM dynamics in the English Channel using two complementary methods: remote-sensing by satellites and numerical modelling. Firstly, MODIS and MERIS satellite images processed by the IFREMER semi-analytical algorithm and describing non-algal SPM, are analysed to build three statistical models which are able to estimate near-surface SPM using simple variables, e.g., tidal coefficient, significant wave height and mean chlorophyll-a concentration. Secondly, the three-dimensional hydrosedimentary model ROMS (Regional Ocean Modeling System) is applied in the English Channel. It considers tidal forcing along open boundaries, wind stress at the sea-surface, wave-current interactions in the bottom boundary layer and realistic heterogeneous bottom sediments. Results of the more sophisticated statistical model is also used to impose SPM concentrations at open boundaries. Sensitivity tests on SPM boundary conditions show the importance of prescribing realistic sediment concentrations to improve the model predictions. Biological influences on mineral SPM are also tested using settling velocity and critical shear stress for erosion which vary with seasons. Both statistical and numerical models highlight and locate respective influences of tide, waves and biology on mineral SPM. Numerical predictions indicate that near-surface SPM is mainly composed of silts (>70%). Near-surface suspended silts come largely from seabed resuspension alongshore in the Eastern Channel and from the open boundaries of our limited-area coastal model at the West of Cotentin Peninsula and offshore. Near-surface SPM variations are investigated at semi-diurnal, neap-spring tidal cycle time scales and during a wave event. Finally, dynamics of sediments in the turbidity maximum zone around the Isle of Wight is examined depending on hydrodynamical conditions in order to distinguish the role played by advection and local erosion/settling processes in this area. Keywords: Suspended particulate matter, satellite, remote-sensing, modelling, English Channel, sediments, turbidity, tide, wave
L'étude des matières en suspension (MES) minérales est essentielle pour comprendre le fonctionnement des écosystèmes en Manche : les MES influencent la pénétration de la lumière dans la colonne d'eau, paramètre clé pour la production biologique, et sont susceptibles de transporter des polluants et nutriments. Lors de ce travail, la dynamique des MES minérales de surface en Manche est étudiée à l'aide de deux méthodes complémentaires : l'observation par satellite et la modélisation numérique tridimensionnelle. Dans un premier temps, les images satellite MODIS et MERIS, traitées par l'algorithme semi-analytique développé par l'IFREMER et représentant les MES non-algales de surface, sont analysées afin d'élaborer trois modèles statistiques permettant d'estimer la MES de surface en fonction de variables basiques telles que le coefficient de marée, la hauteur significative des vagues et la concentration moyenne en chlorophylle-a. Dans un deuxième temps, le modèle hydrosédimentaire multiclasse tridimensionnel ROMS (Regional Ocean Modeling System) est implémenté en Manche. Il prend en considération le forçage par la marée aux frontières ouvertes, la contrainte exercée par le vent à la surface de la mer, l'interaction houle-courant en couche limite de fond et l’hétérogénéité spatiale réaliste du lit sédimentaire. Les résultats du modèle statistique le plus sophistiqué sont également utilisés pour forcer la concentration en MES aux frontières ouvertes du domaine de calcul. Des tests de sensibilité sur les conditions limites montrent l'importance de considérer de manière réaliste les sédiments entrant en Manche par les frontières ouvertes lors de la modélisation numérique. L'influence de la biologie sur les MES minérales est testée en utilisant une formulation de la vitesse de chute et de la contrainte critique d'érosion variant saisonnièrement. Grâce à ces deux outils associés, les influences respectives de la marée, de la houle et de la biologie sur les MES minérales sont mises en avant et localisées en Manche. Le modèle numérique prédit que les MES de surface sont composées principalement de silts (>70%). Les silts en suspension en surface proviennent majoritairement du lit sédimentaire près des côtes en Manche orientale et des frontières ouvertes du domaine de calcul à l'ouest de la presqu'île du Cotentin et au large en Manche centrale et orientale. Les variations des MES de surface sont ensuite étudiées aux échelles des cycles de marée semi-diurnes, vive-eau/morte-eau et autour d'un épisode de houles. Enfin, l'évolution de la concentration de sédiments dans la zone de forte turbidité autour de l'île de Wight peut être analysée suivant les conditions hydrodynamiques afin d'évaluer les rôles respectifs des processus locaux d'érosion/dépot et d'advection dans la génération de ces turbidités remarquables. Mots-clés : Matière en suspension, télédétection, satellite, modélisation, Manche, sédiments, turbidité, marée, houle

Droits : 2013 UBO
http://archimer.ifremer.fr/doc/00157/26783/24884.pdf
http://archimer.ifremer.fr/doc/00157/26783/

Éditeur(s) : HAL CCSD Springer-Verlag
Résumé : We provide evidence for a plume-like upwelling beneath the Eifel hotspot, Western Germany, by using teleseismic shear-wave splitting to resolve the anisotropy associated with upwelling flow that is spreading laterally into the asthenosphere. The variation in fast-polarization azimuth we find across the Eifel hotspot is explained by a model of slowly upwelling material that is horizontally being deflected or sheared in a parabolic asthenospheric flow (PAF) pattern toward west-southwest, a direction that correlates with Eurasian absolute plate motion. We suggest that the lack of an age progression for Eifel volcanism, which is expected for a fixed-upwelling model, is a result of (1) sporadic volcanism due to a low excess plume temperature and/or varying crustal stresses that periodically relax and facilitate eruption, and (2) complex upwelling flow pathways and/or Late Tertiary changes in the slow Eurasian plate motion. The success of the PAF model in fitting the data is remarkable given the small number of parameters (four) and the consistency with the plate motion direction determined from geology and/or geodesy. This suggests that a predictable mantle-anisotropy pattern may exist also for other hotspots driven by plume-like upwellings, and that splitting can be a useful diagnostic to differentiate between plume-like and alternative sources for mantle hotspots.
Mantle plumes - a multidisciplinary approach

hal-00407986
https://hal.archives-ouvertes.fr/hal-00407986
DOI : 10.1007/978-3-540-68046-8

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
A network of continuous GPS stations has been installed in NW Iran since 2005 to complement the survey GPS network already existing in the region. We present the 1999-2009 GPS-derived velocity field for this region based on the continuous and survey-mode observations. The results confirm a right lateral slip of 7 +/- 1 mm/yr for the North Tabriz fault, in agreement with previous studies. This rate is consistent with earthquakes of magnitude 7-7.3 and recurrence times of 250-300 yr. The higher spatial coverage of the new network shows that deformation is localized in the vicinity of the Chalderan, south Gailatu-Siah Cheshmeh-Khoy fault and the North Tabriz fault. However the eastern end of the North Tabriz fault appears to cross Mount Bozgush rather than following its southern foothills. This new velocity field does not indicate the 8 mm/yr of NNE-SSW extension suggested earlier for the region, but rather shows lower extension of 1-2 +/- 1 mm/yr across the eastern segment of the North Tabriz fault and the Talesh. To the west, the Chalderan and the western North Tabriz fault segment act like pure strike slip faults without significant extension or compression. The denser network in the Rudbar earthquake region (Ms 7.3, 1992) shows no significant motion across the fault, suggesting that the recurrence time of earthquakes like the Rudbar event must be very long. The lack of substantial compressive strain and the sharp azimuth change of the velocity vectors in the transition zone from Arabia to Lesser Caucasus motion imply that processes other than "extrusion", possibly related to old subduction or delamination, contribute to active deformation.
ISSN: 0012-821X

hal-00617666
https://hal.archives-ouvertes.fr/hal-00617666
DOI : 10.1016/j.epsl.2011.04.029

Éditeur(s) : HAL CCSD
Résumé : International audience
Human spatial motions determine geographic social contacts that influence the way an information is spread on a population or a community. As mobility is a transverse dimension to social practices it is important to better understand its role. With the Eternal-Return model we propose, we simulate an artificial world populated by heterogeneous agents who differ in their mobility. We have chosen a multi-agent framework perspective for this simulation. We endow the agents with simple rules on how to move around the space and how to establish proximity-contacts. This allows to distinguish different kinds of mobile agents, from sedentary ones to travelers. To summarize the dynamics induced by mobility over time, we define the mobility-based Social Proximity Network as being the network of all distinct contacts between agents. Its properties give insight in the process of information spreading. We conduct simulations to understand how an information can be broadcast when agent-nodes are in motion.
IEEE/ACM International Conference on Advances in Social Networks Analysis and Mining
Niagara falls, Canada

hal-00874344
https://hal.archives-ouvertes.fr/hal-00874344

Éditeur(s) : HAL CCSD
Résumé : International audience
The aim of this study is to suggest two automated techniques able to help medical staff to detect earlier than usual some diseases using wireless sensor networks (WSNs). In this context, a patient is equipped with physical sensors (for temperature, pressure, ..). This WSN will perform some computations and will run an alarm when a disease is suspected. The first technique uses a population protocol to handle data exchanged between motes and provides an efficient algorithm to suggest that a disease is diagnosed on a patient. The algorithm is distributed, i.e., the decision may be done by any mote dealing with the disease detection. The second technique uses a token algorithm where, some motes, denoted as masters. Each of them is in charge of deciding if a specific disease occurs. This technique is not totally distributed but enhances the network efficiency regarding to the energy consumption, the time execution and the number of exchanged messages.
Proceedings of The Ninth IEEE International Symposium on Networking Computing and Applications
Cambridge, MA, United States

hal-00519599
https://hal.archives-ouvertes.fr/hal-00519599

Éditeur(s) : Amer Geophysical Union
Résumé : On November 21, 2004, a magnitude 6.3 earthquake occurred offshore, 10 km south of Les Saintes archipelago in Guadeloupe (French West Indies). There were more than 30000 aftershocks recorded in the following two years, most of them at shallow depth near the islands of the archipelago. The main shock and its main aftershock of February 14, 2005 (M-w = 5.8) ruptured a NE-dipping normal fault (Roseau fault), mapped and identified as active from high-resolution bathymetric data a few years before. This fault belongs to an arc-parallel en echelon fault system that follows the inner edge of the northern part of the Lesser Antilles arc, accommodating the sinistral component of oblique convergence between the North American and Caribbean plates. The distribution of aftershocks and damage (destruction and landslides) are consistent with the main fault plane location and attitude. The slip model of the main shock, obtained by inverting jointly global broadband and local strong motion records, is characterized by two main slip zones located 5 to 10 km to the SE and NW of the hypocenter. The main shock is shown to have increased the Coulomb stress at the tips of the ruptured plane by more than 4 bars where most of the aftershocks occurred, implying that failures on fault system were mainly promoted by static stress changes. The earthquake also had an effect on volcanic activity since the Boiling Lake in Dominica drained twice, probably as a result of the extensional strain induced by the earthquake and its main aftershock.
Journal Of Geophysical Research-solid Earth (0148-0227) (Amer Geophysical Union), 2011-10 , Vol. 116 , N. B10301 , P. 1-25

Droits : Copyright 2011 by the American Geophysical Union.
http://archimer.ifremer.fr/doc/00200/31099/29511.pdf
DOI:10.1029/2011JB008310
http://archimer.ifremer.fr/doc/00200/31099/

Éditeur(s) : HAL CCSD American Geophysical Union
Résumé : International audience
We report measurements of long-period P wave polarization (P pol) in Australia and Tahiti made by combining modeling of the polarization deviation and harmonic analysis. The analysis of the deviation of the horizontal polarization of the P wave as a function of event back azimuth may be used to obtain information about (1) sensor misorientation, (2) dipping discontinuities, (3) seismic anisotropy, and (4) velocity heterogeneities beneath a seismic station. The results from harmonic analysis and a grid search using Snell's law suggest the presence of a dipping seismic discontinuity beneath stations CTAO and CAN in Australia. These results are consistent with published receiver function studies for these stations. The P pol fast axis orientation is close to the N–S absolute plate motion direction at station TAU (Tasmania), which may be due to plate-motion-driven alignment of olivine crystals in the asthenosphere. Interestingly, measurements of SKS splitting at Tahiti (French Polynesia) show an apparent isotropy, whereas an inversion of P pol observations at PPTL seismic station located in Tahiti suggests the presence of two anisotropic layers. The fast axis azimuth is oriented E–W in the upper layer, and it is close to the NW–SE orientation in the lower layer. Since P pol orientations are used for real-time earthquake locations, especially in poorly instrumented areas such as the South Pacific, we show that the bias from anisotropy and sensor misorientation determined here can be corrected to improve the location accuracy, which yields fundamental data for rapid location necessary for effective tsunami warning.
ISSN: 2169-9313

hal-01389113
http://hal.univ-reunion.fr/hal-01389113
http://hal.univ-reunion.fr/hal-01389113/document
http://hal.univ-reunion.fr/hal-01389113/file/Fontaine_Ppol_JGR2009.pdf
DOI : 10.1029/2008JB005709

Éditeur(s) : Université des Antilles et de la Guyane
Extrait de : Les rencontres culturelles de la BU 2013-2014. Université des Antilles et de la Guyane
Description : Patrick Odent-Allet rappelle en quelques phrases le parcours littéraire de Daniel Boukman, avant d'effectuer la présentation de l'ouvrage "Liwa lajan". Après un mot de Daniel Boukman, Georges-Henri Léontin effectue une rapide présentation de l'écrivain, puis se concentre sur une comparaison entre les travaux d'Aristophane et ceux de Daniel Boukman. Un parallèle se justifiant par le fait que "Liwa lajan" est une adaptation créole du "Plutus" de l'auteur grec Aristophane.
Siècle(s) traité(s) : 21
Droits : CC-BY-NC-ND - Attribution - Pas d'utilisation commerciale - Pas de modification
Permalien : http://www.manioc.org/fichiers/V14072
V14072