Résumé : (i) La pertinence du thème est attestée par la richesse de la littérature internationale qui lui est consacrée. 11 convient au demeurant de noter la présence de publications de l'IFREMER dans ce même domaine. Les principaux acquis procèdent généralement d'approches descriptives, permettant de disposer à ce jour d'un inventaire quasi exhaustif des différents outils de gestion classiquement mis en oeuvre. D'ores et déjà il apparaît que la question de la transférabilité de mesures de gestion (e.g QIT, Licence, PME...) soulève plusieurs interrogations: cohérence juridique, acceptabilité, contrôle, coûts, efficience... Mais surtout, poser l'étude de la régulation en termes d'analyse du comportement d'un système élargit le champ des investigations au delà du domaine habituel de l'halieutique. C'est cette complexification de la problématique qui a principalement nourri la réflexion du groupe. (ii) En plus des travaux scientifiques produits sous ce thème, l'IFREMER, du fait de ses missions, se doit de répondre aux diverses sollicitations d'avis et d'expertise; pour ce qui concerne les ressources halieutiques cette charge incombe au Département RH. En outre, celui-ci a été amené à assurer un ensemble de tâches récursives (échantillonnage, statistiques de pêche et autres collectes de données) fortement consommatrices de temps, de moyens et contraignant à la dispersion géographique. Enfin, en tant qu'acteur du système de gestion, l'IFREMER s'est trouvé soumis à une certaine réserve quant à l'évaluation du système lui même, y compris son éventuelle remise en cause, ainsi qu'à des clauses limitatives pour l'exploitation et la valorisation des données. Aujourd'hui, près de 80 % de l'activité du Département sont dévolus à la réalisation d'études destinées à fournir des avis en réponse aux demandes émanant par exemple du CIEM, du CSTP, des COREMODE, des divers Comités Professionnels, des Etats Régionaux de la Ressource, et à s'impliquer dans des dossiers tels que les SMVM, le système de gestion en Méditerranée, les POP, les Plans Sectoriels, les conflits d'espace spécifiques (extraction de granulats, aquaculture) (1). La nature et la diversité de ces questions reflètent: -le statut d'interlocuteur privilégié de l'IFREMER; -la complexification des interactions pour l'accès ou l'usage des ressources marines; -la position centrale du thème de la régulation. [OCR NON CONTRÔLE]

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/1992/rapport-4235.pdf
http://archimer.ifremer.fr/doc/00000/4235/

Éditeur(s) : HAL CCSD PubMed
Résumé : International audience
To investigate thermal response, hydration behaviour and performance over flatwater kayaking races in tropical conditions (36.8°C and 68 % rh). Five internationally-ranked subjects participated in the 2012 Surfski Ocean Racing World Cup in Guadeloupe to the “Ze Caribbean Race 2012” [i.e., a 35-km downwind race]. Core temperature (T°C) and heart rate (HR) were measured using portable telemetry units whereas water intake was deduced from backpacks absorption. The kayakers were asked to rate both their comfort sensation and thermal sensation on a scale before and after the race. The performance was related to an increase in T°C, high HR and low water intake (WI); and (2) high values of final T°C were related to high pre T°C and greater increases in T°C being obtained with low pre T°C and (3) WI being related to high pre T°C. The present study demonstrated that the fastest kayakers were those able to paddle at the highest intensities, increasing their T°C and drinking little water without any interference from thermal sensations. Water intake was positively related to pre-race T°C, which reinforces the importance of beginning surfski races with a low T°C. This study demonstrated that well-trained kayakers drinking ad libitum were able to anticipate their intensity/heat storage ratio to prevent heat illness and severe dehydration and maintain high performance.
ISSN: 0860-021X

hal-01137286
https://hal.univ-antilles.fr/hal-01137286

Éditeur(s) : HAL CCSD GeoScienceWorld
Résumé : International audience
Due to their "iron-loving" properties, platinum-group elements (PGE) are expected to be stored in the Earth's core. Although very low, at a few parts per billion, PGE concentrations measured in mantle-derived rocks are too high to be in chemical equilibrium with the core. The "late veneer" model offers the best explanation for this paradox-it postulates that a flux of primitive meteorites hit the early Earth after core formation had ceased. However, the inferred PGE composition of the hypothetical primitive mantle exhibits slight positive excesses of Ru, Rh, and Pd compared to the canonical chondritic signature. Such deviations have trigger debate about the composition of the late veneer and the extent of reworking of PGE signatures by igneous processes within the Earth's mantle.
ISSN: 1811-5209

hal-00411483
https://hal.archives-ouvertes.fr/hal-00411483
DOI : 10.2113/GSELEMENTS.4.4.247

Éditeur(s) : HAL CCSD University of Uludag
Résumé : International audience
We tested whether the silicone swim caps (SC) worn by young swimmers in a tropical climate negatively influence aerobic performance. Nine trained pre-adolescents [11.8 (± 0.8) years] swam randomized 800-m trials (water: 32.9°C, outdoors: shade, 29.2 ± 0.2 °C, 74 ± 0.3 % rh) with a SC or a nude head (NH). Performance times and heart rate (HR) were monitored continuously. Rectal temperature (T rec) was measured before and after trials. The rating of perceived exertion (RPE) was assessed. Stroke frequency (SF), stroke length (SL) and stroke index (SI) were measured every 50-m. The SC trial was significantly longer than NH (799 ± 16 and 781 ± 16 seconds, respectively). Mean delta T rec was significantly greater in SC (0.2 ± 0.1°C vs.-0.1 ± 0.1°C in SC vs. NH), mean SI was significantly different in SC versus NH (1.83 ± 0.07 vs 1.73 ± 0.06); but RPE and mean HR, SF and SL showed no change. We conclude that a silicone swim cap worn in tropical environment significantly decreased 800-m crawl performance without affecting HR or RPE. Silicone swim caps worn by young swimmers in a tropical environment may also have negative effects on training capacity.
ISSN: 1303-2968

hal-01137570
https://hal.univ-antilles.fr/hal-01137570
https://hal.univ-antilles.fr/hal-01137570/document
https://hal.univ-antilles.fr/hal-01137570/file/Hue%2C%20Galy%20-%202012%20-%20The%20effect%20of%20a%20silicone%20swim%20cap%20on%20swimming%20performance%20in%20tropical%20conditions%20in%20pre-adolescents.pdf

Éditeur(s) : HAL CCSD
Résumé : National audience
Le standard d’eau de rivière naturelle SLRS-5 (NRC-CNRC) est uneréférence de contrôle qualité en analyse d’eau de routine pour la communautéinternationale. Dix laboratoires français étudiant les élémentsmajeurs et en trace dans les solutions naturelles (groupe de travail del’atelier du CNRS « Isotrace ») valident leurs mesures avec les 19 élémentscertifiés par le producteur. Or, d’autres éléments non certifiés sontrégulièrement analysés par ces laboratoires qui ont comparé et compilé2 années de leurs mesures sur ce standard d’eau. La plupart desmesures sont réalisées par ICP-MS (Inductively Coupled Plasma Mass-Spectrometry).Dans un premier temps, il a été vérifié que les résultats obtenus étaientcohérents pour les éléments certifiés par le producteur. Ainsi Ba présenteune valeur compilée de 14,2 1,4 g/l (330 mesures issues de 9laboratoires participants) en accord avec la valeur certifiée de 14 0,5g/l.Ensuite, des valeurs moyennes et leurs incertitudes associées sont proposéespour des éléments non certifiés par NRC-CNRC tels que le siliciumet 35 éléments en trace (terres rares, Ag, B, Bi, Cs, Ga, Ge, Li, Nb,P, Rb, Rh, Re, S, Sc, Sn, Th, Ti, Tl,W, Y et Zr). Le rapport isotopique deSr est aussi proposé à partir de mesures par TIMS (Thermo IonisationMass Spectrometry).Il apparaît que les mesures individuelles et compilées varient dequelques ng/l à 2400 g/l avec des incertitudes associées comprisesentre 2 et 240%. Les fortes incertitudes associées ne sont pas proportionnellesaux concentrations puisque certaines mesures s’accordent mêmeà de faibles teneurs tels que Bi (0,9 0,3 ng/l valeur compilée). Danscertains cas, un ou deux laboratoires ont caractérisé l’élément impliquantmoins de mesures et une incertitude associée plus élevée quelleque soit la concentration en l’élément. C’est le cas, par exemple, de Ge(0,015 0,014 g/l valeur compilée) caracterisé par seulement 2 laboratoires(34 mesures) et de P (8,19 3,40 g/l) issu de 8 mesuresd’un seul laboratoire. Les terres rares et onze autres éléments (B, Bi,Cs, Li, Rb, Si, Th, Ti, Tl, Y et Zr) ont été déterminés par au moins 3laboratoires différents et apportent des informations complémentairesessentielles à l’utilisation
24 ème Réunion des sciences de la Terre 2014
Pau, France

insu-01080879
https://hal-insu.archives-ouvertes.fr/insu-01080879

Éditeur(s) : HAL CCSD Springer Verlag
Résumé : International audience
Cobalt-bearing pyrite (0.5-2.0 wt.% Co) is abnormally abundant (up to 35 vol.% of the total volume of the sulfide phase) in some eastern Pyrenean peridotite massifs, compared to pieces of subcontinental mantle studied so far for sulfides. Pyrite occurs as vermicular intergrowths inside pentlandite and/or chalcopyrite or as coarser, blocky grains in the intergranular pores of host peridotites. Those different pyrites are characterized by different platinum-group element systematics (measured by laser ablation microprobe and ICP-MS). Vermicular pyrite intergrown with pentlandite displays Os-, Ir-, Ru- and Rh-enriched chondrite normalized PGE patterns of Monosulfide solid solution (Mss). In contrast, coarse-grained intergranular ("blocky") pyrites, are PGE-poor. Chalcophile trace elements (i.e. Zn, Pb, Ag, Au) that are not usually concentrated in mantle-derived sulfides were commonly detected. By contrast, selenium contents are generally low, yielding thus pyrite with high S/Se ratio (> 10(5)), consistent with a sedimentary sulfur source. Pyrite microtextures and chalcophile trace element contents support a process of assimilation of crustal sulfur from the metamorphosed sedimentary country rocks. These latter generated highly reactive CO2-S fluids, which were injected into structural discontinuities of the lherzolitic bodies. Sulfur has reacted at T = 300-550A degrees C with pre-existing, mantle-derived, metal-rich sulfide assemblages (pentlandite-chalcopyrite). Addition of crustal sulfur did produce Mss which, on cooling, exsolved the Os-rich pyrite in addition to pentlandite. The coarse-grained pyrite types have crystallized directly from S-rich fluids.
ISSN: 0010-7999

hal-00617425
https://hal.archives-ouvertes.fr/hal-00617425
DOI : 10.1007/s00710-010-0138-2

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Highly siderophile element concentrations (HSE: Re and platinum-group elements (PGE)) are presented for gabbros, gabbroic eclogites and basaltic eclogites from the high-pressure Zermatt-Saas ophiolite terrain, Switzerland. Rhenium and PGE (Os, Ir, Ru, Rh, Pt, Pd) abundances in gabbro- and eclogite-hosted sulphides, and Re-Os isotopes and elemental concentrations in silicate phases are also reported. This work, therefore, provides whole rock and mineral-scale insights into the PGE budget of gabbroic oceanic crust and the effects of subduction metamorphism on gabbroic and basaltic crust. Chondrite-normalised PGE patterns for the gabbros are similar to published mid-ocean ridge basalts (MORB), but show less inter-element fractionation. Mean Pt and Pd contents of 360 and 530 pg/g, respectively, are broadly comparable to MORB, but gabbros have somewhat higher abundances of Os, Ir and Ru (mean: 64, 57 and 108 pg/g). Transformation to eclogite has not significantly changed the concentrations of the PGE, except Pd which is severely depleted in gabbroic eclogites relative to gabbros (similar to 75% loss). In contrast, basaltic eclogites display significant depletion of Pt (>= 60%), Pd (>85%) and Re (50-60%) compared with published MORB, while Os, Ir and Ru abundances are broadly comparable. Thus, these data suggest that only Pt, Pd and Re, and not Os, Ir and Ru, may be significantly fluxed into the mantle wedge from mafic oceanic crust. Re-Os model ages for gabbroic and gabbroic eclogite minerals are close to age estimates for igneous crystallisation and high-pressure metamorphism, respectively, hence the HSE budgets can be related to both igneous and metamorphic behaviour. The gabbroic budget of Os, Ir, Ru and Pd (but not Pt) is dominated by sulphide, which typically hosts >90% of the Os, whereas silicates account for most of the Re (with up to 75% in plagioclase alone). Sulphides in gabbroic eclogites tend to host a smaller proportion of the total Os (10-90%) while silicates are important hosts, probably reflecting Os inheritance from precursor phases. Garnet contains very high Re concentrations and may account for >50% of Re in some samples. The depletion of Pd in gabbroic eclogites appears linked, at least in part, to the loss of Ni-rich sulphide. Both basaltic and gabbroic oceanic crust have elevated Pt/Os ratios, but Pt/Re ratios are not sufficiently high to generate the coupled Os-186-Os-187 enrichments observed in some mantle melts, even without Pt loss from basaltic crust. However, the apparent mobility of Pt and Re in slab fluids provides an alternative mechanism for the generation of Pt- and Re-rich mantle material, recently proposed as a potential source of Os-187-Os-186 enrichment.
ISSN: 0016-7037

hal-00420072
https://hal.archives-ouvertes.fr/hal-00420072
DOI : 10.1016/j.gca.2008.11.036

Éditeur(s) : HAL CCSD University of Uludag
Résumé : International audience
We tested whether the silicone swim caps (SC) worn by young swimmers in a tropical climate negatively influence aerobic performance. Nine trained pre-adolescents [11.8 (± 0.8) years] swam randomized 800-m trials (water: 32.9°C, outdoors: shade, 29.2 ± 0.2 °C, 74 ± 0.3 % rh) with a SC or a nude head (NH). Performance times and heart rate (HR) were monitored continuously. Rectal temperature (T rec) was measured before and after trials. The rating of perceived exertion (RPE) was assessed. Stroke frequency (SF), stroke length (SL) and stroke index (SI) were measured every 50-m. The SC trial was significantly longer than NH (799 ± 16 and 781 ± 16 seconds, respectively). Mean delta T rec was significantly greater in SC (0.2 ± 0.1°C vs.-0.1 ± 0.1°C in SC vs. NH), mean SI was significantly different in SC versus NH (1.83 ± 0.07 vs 1.73 ± 0.06); but RPE and mean HR, SF and SL showed no change. We conclude that a silicone swim cap worn in tropical environment significantly decreased 800-m crawl performance without affecting HR or RPE. Silicone swim caps worn by young swimmers in a tropical environment may also have negative effects on training capacity.
ISSN: 1303-2968

hal-01143533
https://hal.univ-antilles.fr/hal-01143533

Éditeur(s) : HAL CCSD Berlin: A. Asher & Co.
Résumé : International audience
In this work, we compare IASI-retrieved vertical water vapour profiles and related precipitable water over a complex region, namely the Rhine Valley area, during the pre-operational period of IASI exploitation (June?August 2007). Both IASI water vapour mixing ratio profiles and integrated water vapour content are retrieved from L1C radiances spectra using two techniques and compared with water vapour related observations acquired during the Convective and Orographically-induced Precipitation Study (COPS) field campaign that took place in this area at that time (i.e. lidars, radiosoundings and a global positioning system - GPS - station network). This work addresses the issue of IASI vertical spatial resolution and its capability to detect two-layer water vapour structures such as those observed in a mountainous area and which play an important role in convective initiation or inhibition. We found that this capability mostly relies on the type of a-priori background vector (climatology or space-time colocated ECMWF analysis), which is used within the retrieval scheme. Systematic comparison of water vapour products derived from 71 IASI spectra confirms that IASI can retrieve water vapour amounts in 2 km width layers, in the lower troposphere, with an accuracy of approximately 10%.
ISSN: 0369-1845

hal-00923710
https://hal.archives-ouvertes.fr/hal-00923710
https://hal.archives-ouvertes.fr/hal-00923710/document
https://hal.archives-ouvertes.fr/hal-00923710/file/masiello.pdf
DOI : 10.1127/0941-2948/2013/0430

Éditeur(s) : HAL CCSD
Résumé : For operational forecasts anticipate convective inhibition processes is as important than convective initiation processes. Based on the 15th July 2007 case study this work shows how the morning shallow convection over the Vosges is inhibited while it develops over the Black Forest. This case occurs during IOP 8b of the Convective and Orographically-Induced Precipitation Study (COPS). This international field campaign took place during the summer of 2007 over the Vosges, the Rhine Valley and the Black-Forest. The aim of this intensive observation campaign was to study various phases of convection and convective environment and improve quantitative precipitation forecasts. Thanks to GPS tomography data the study show the differences of low-level water-vapor variability between Vosges and Black-Forest. The analysis of ground based and airborne lidar data suggests the importance of dry air layers advected from the south and the influence of the mountains and diurnal cycle of mountain breeze which interfere strongly with these layers preventing the dry air to reach the eastern side of the mountain and the Black Forest. This dynamics is confirmed by models, wind profiler and radiosounding data. So we show how the inhibition of the convection over the Vosges during this case study can be explained with the water vapor variability due to advection and local boundary layer processes.
31st ICAM (International Conference on Alpine Meteorology)
Aviemore, United Kingdom

hal-00668829
https://hal.archives-ouvertes.fr/hal-00668829