X-Ray Imaging of SAPO-34 Molecular Sieves at the Nanoscale: Influence of Steaming on the Methanol-to-Hydrocarbons Reaction

The effect of a severe steaming treatment on the physicochemical properties and catalytic performance of H-SAPO-34 molecular sieves during the methanol-to-hydrocarbons (MTH) reaction has been investigated with a combination of scanning transmission X-ray microscopy (STXM), catalytic testing, and bulk characterization techniques, including ammonia temperature programmed desorption and 27Al and 29Si magic angle spinning nuclear magnetic resonance. For this purpose, two samples, namely a calcined and a steamed H-SAPO-34 catalyst powder, have been compared. It has been found that calcined H-SAPO-34 displays a high selectivity towards light olefins, yet shows a poor stability as compared to a zeolite H-ZSM-5 catalyst. Moreover, in situ STXM at the carbon K-edge during the MTH reaction allows construction of nanoscale chemical maps of the hydrocarbon species formed within the H-SAPO-34 aggregates as a function of reaction time and steam post-treatment. It was found that there is an initial preferential formation of coke precursor species within the core of the H-SAPO-34 aggregates. For longer times on stream the formation of the coke precursor species is extended to the outer regions, progressively filling the entire H-SAPO-34 catalyst particle. In contrast, the hydrothermally treated H-SAPO-34 showed similar reaction selectivity, but decreased activity and catalyst stability with respect to its calcined counterpart. These variations in MTH performance are related to a faster and more homogeneous formation of coke precursor species filling up the entire steamed H-SAPO-34 catalyst particle. Finally, the chemical imaging capabilities of the STXM method at the Al and Si K-edge are illustrated by visualizing the silicon islands at the nanoscale before and after steaming H-SAPO-34.

Agents et modèles de l'adaptation publicitaire en agence de communication marketing

L’industrie de la publicité doit se renouveler sans cesse pour suivre la réalité en constante évolution des entreprises et de leurs consommateurs, afin de produire des messages qui toucheront, séduiront, puis convaincront les publics visés. Différents facteurs socioéconomiques, politiques mais également technologiques incitent les annonceurs à orchestrer de vastes campagnes multilingues et multiculturelles, où est présentée une idée unique, conforme à l’identité de la marque, qui sera adaptée dans différents marchés. Il s’agit d’une stratégie très différente de celle de la création de campagnes propres à chaque culture, par des agences locales. Le choix de l’adaptation, motivé par des raisons économiques bien sûr, mais également stratégiques, entraîne une évolution de la perception de l’acte traduisant et de ses acteurs au sein du milieu du marketing et de la publicité. Alors que nous assistons à un rapprochement des industries du marketing et de la traduction, principalement dans les marchés secondaires comme le Québec, ce projet doctoral propose une réflexion traductologique sur la place que peut occuper l’adaptation dans une stratégie en publicité marketing, et sur les différentes fonctions que peut remplir un traducteur intégré à une équipe de spécialistes de la communication. Par ailleurs, de la réception du mandat d’adaptation à l’agence de marketing jusqu’à la diffusion du message dans la culture cible, nous explorons dans notre travail les différentes avenues que peut prendre le processus d’adaptation publicitaire. Cette thèse par articles comprend six publications en traductologie, publiées ou acceptées par des comités scientifiques, qui étudient la question de l’adaptation publicitaire sous un angle traductologique, mais ce travail multidisciplinaire s’inspire aussi des contributions des experts des études sur l’adaptation, la culture ainsi que la communication publicitaire. D’abord, le premier chapitre définit les notions de traduction, d’adaptation et d’appropriation auxquelles nous référerons tout au long de la thèse, et les situe dans le contexte de la communication promotionnelle internationale, notamment. Le deuxième chapitre dresse un portrait pratique et théorique de l’adaptation publicitaire, et porte sur les relations de travail entre le traducteur et les autres professionnels de l’agence. Nous y énumérons notamment les raisons de la progression du marché mondial de l’adaptation, comparativement à celui des multiples créations locales. Ensuite, le chapitre 3 définit les défis variés de l’adaptation publicitaire, et en présente une classification inspirée par la taxonomie de la théorie fonctionnaliste en traductologie, formée de quatre problèmes et deux difficultés traductionnels. Le chapitre 4 présente une réflexion sur les mécanismes intellectuels de l’adaptation publicitaire et sur les différentes lectures que le traducteur doit faire du texte source pour produire un message efficace, respectivement la lecture analytique (rationnelle et raisonnée), puis la lecture empathique, où il anticipe la réaction émotive des cibles. Le cinquième chapitre se concentre sur un aspect de la traduction audiovisuelle presque exclusive à l’industrie publicitaire : la double version, où le traducteur traduit non pas des dialogues apposés à l’image originale, mais plutôt le scénario dans son entièreté, afin de produire un nouveau message vidéo avec des acteurs appartenant à la culture cible. Enfin, notre sixième chapitre est une étude de cas menée en agence de publicité, qui analyse la pratique professionnelle de traducteurs dans leur environnement de travail, les mandats qui leur sont confiés ainsi que les ressources dont ils disposent. Ensemble, ces six chapitres visent à mieux faire connaître la démarche intellectuelle de l’adaptation publicitaire, à comprendre comment différents facteurs influencent le rôle du traducteur au sein d’une agence, à déterminer comment mieux préparer les professionnels de demain à exceller dans le marché très prometteur du marketing international, et à contribuer à l’avancement de la réflexion traductologique par l’étude d’un type de traduction spécialisée qui se démarque par ses pratiques et ses défis aussi intéressants qu’uniques.

The influence of an in-service programme on primary teachers conceptions about practical work

The purpose of this study was to investigate how an in-service programme influenced primary teachers’ conceptions about practical work. Ten elementary teachers participated in a Portuguese city in an one-year professional development programme, which aimed to promote the use of practical activities in classroom. Semi-structured interviews and classroom observations were both used to examine changes in teachers’ conceptions about science teaching and in their classroom pratices. Data also included written artefacts, such as teachers’ written reflections, lesson plans, activity sheets, assessment items and student work samples. Based on the analysis of the data, the changes in teachers’ conceptions were organized into four categories: student and learning, teacher and teaching, science teaching, and teaching context. Throughout their participation in the programme, teachers pointed out several constraints related to planning and implementing practical activities. Results indicate that most teachers were able to overcome their initial difficulties and progressively gained more confidence in using student-centered pratices. However, one year after the end of the programme, teachers reported that their actual practices did not changed significantly, particularly with regard to inquiry-based practical and collaborative activities, which remained absent or rare. Implications for professional development and further research are discussed.

The influence of the rearing period on intramammary infections in Swiss dairy heifers: A cross-sectional study

Healthy replacement heifers are one of the foundations of a healthy dairy herd. Farm management andrearing systems in Switzerland provide a wide variety of factors that could potentially be associated withintramammary infections (IMI) in early lactating dairy heifers. In this study, IMI with minor mastitispathogens such as coagulase-negative staphylococci (CNS), contagious pathogens, and environmentalmajor pathogens were identified. Fifty-four dairy farms were enrolled in the study. A questionnaire wasused to collect herd level data on housing, management and welfare of young stock during farm isitsand interviews with the farmers. Cow-level data such as breed, age at first calving, udder condition andswelling, and calving ease were also recorded. Data was also collected about young stock that spent aperiod of at least 3 months on an external rearing farm or on a seasonal alpine farm. At the quarterlevel, teat conditions such as teat lesions, teat dysfunction, presence of a papilloma and teat lengthwere recorded. Within 24 h after parturition, samples of colostral milk from 1564 quarters (391 heifers)were collected aseptically for bacterial culture. Positive bacteriological culture results were found in 49%of quarter samples. Potential risk factors for IMI were identified at the quarter, animal and herd levelusing multivariable and multilevel logistic regression analysis. At the herd level tie-stalls, and at cow-level the breed category “Brown cattle” were risk factors for IMI caused by contagious major pathogenssuch as Staphylococcus aureus (S. aureus). At the quarter-level, teat swelling and teat lesions were highlyassociated with IMI caused by environmental major pathogens. At the herd level heifer rearing at externalfarms was associated with less IMI caused by major environmental pathogens. Keeping pregnant heifersin a separate group was negatively associated with IMI caused by CNS. The odds of IMI with coagulase-negative staphylococci increased if weaning age was less than 4 months and if concentrates were fed tocalves younger than 2 weeks. This study identified herd, cow- and quarter-level risk factors that may beimportant for IMI prevention in the future.

Agents et modèles de l'adaptation publicitaire en agence de communication marketing

L’industrie de la publicité doit se renouveler sans cesse pour suivre la réalité en constante évolution des entreprises et de leurs consommateurs, afin de produire des messages qui toucheront, séduiront, puis convaincront les publics visés. Différents facteurs socioéconomiques, politiques mais également technologiques incitent les annonceurs à orchestrer de vastes campagnes multilingues et multiculturelles, où est présentée une idée unique, conforme à l’identité de la marque, qui sera adaptée dans différents marchés. Il s’agit d’une stratégie très différente de celle de la création de campagnes propres à chaque culture, par des agences locales. Le choix de l’adaptation, motivé par des raisons économiques bien sûr, mais également stratégiques, entraîne une évolution de la perception de l’acte traduisant et de ses acteurs au sein du milieu du marketing et de la publicité. Alors que nous assistons à un rapprochement des industries du marketing et de la traduction, principalement dans les marchés secondaires comme le Québec, ce projet doctoral propose une réflexion traductologique sur la place que peut occuper l’adaptation dans une stratégie en publicité marketing, et sur les différentes fonctions que peut remplir un traducteur intégré à une équipe de spécialistes de la communication. Par ailleurs, de la réception du mandat d’adaptation à l’agence de marketing jusqu’à la diffusion du message dans la culture cible, nous explorons dans notre travail les différentes avenues que peut prendre le processus d’adaptation publicitaire. Cette thèse par articles comprend six publications en traductologie, publiées ou acceptées par des comités scientifiques, qui étudient la question de l’adaptation publicitaire sous un angle traductologique, mais ce travail multidisciplinaire s’inspire aussi des contributions des experts des études sur l’adaptation, la culture ainsi que la communication publicitaire. D’abord, le premier chapitre définit les notions de traduction, d’adaptation et d’appropriation auxquelles nous référerons tout au long de la thèse, et les situe dans le contexte de la communication promotionnelle internationale, notamment. Le deuxième chapitre dresse un portrait pratique et théorique de l’adaptation publicitaire, et porte sur les relations de travail entre le traducteur et les autres professionnels de l’agence. Nous y énumérons notamment les raisons de la progression du marché mondial de l’adaptation, comparativement à celui des multiples créations locales. Ensuite, le chapitre 3 définit les défis variés de l’adaptation publicitaire, et en présente une classification inspirée par la taxonomie de la théorie fonctionnaliste en traductologie, formée de quatre problèmes et deux difficultés traductionnels. Le chapitre 4 présente une réflexion sur les mécanismes intellectuels de l’adaptation publicitaire et sur les différentes lectures que le traducteur doit faire du texte source pour produire un message efficace, respectivement la lecture analytique (rationnelle et raisonnée), puis la lecture empathique, où il anticipe la réaction émotive des cibles. Le cinquième chapitre se concentre sur un aspect de la traduction audiovisuelle presque exclusive à l’industrie publicitaire : la double version, où le traducteur traduit non pas des dialogues apposés à l’image originale, mais plutôt le scénario dans son entièreté, afin de produire un nouveau message vidéo avec des acteurs appartenant à la culture cible. Enfin, notre sixième chapitre est une étude de cas menée en agence de publicité, qui analyse la pratique professionnelle de traducteurs dans leur environnement de travail, les mandats qui leur sont confiés ainsi que les ressources dont ils disposent. Ensemble, ces six chapitres visent à mieux faire connaître la démarche intellectuelle de l’adaptation publicitaire, à comprendre comment différents facteurs influencent le rôle du traducteur au sein d’une agence, à déterminer comment mieux préparer les professionnels de demain à exceller dans le marché très prometteur du marketing international, et à contribuer à l’avancement de la réflexion traductologique par l’étude d’un type de traduction spécialisée qui se démarque par ses pratiques et ses défis aussi intéressants qu’uniques.

Mean grain size and structure of ODP Hole 140-504B samples

Microstructural investigations of ocean crust samples provide a complementary approach to both marine surveys and laboratory experiments. The recovery of relatively undeformed diabases from Deep Sea Drilling Project (DSDP)/Ocean Drilling Program (ODP) Hole 504B provides a first opportunity to examine a reference section of microstructural features that influence strain localization at depths of 2 km in the ocean crust. Syn- and post-crystallization features in plagioclase and augite crystals have been examined by optical microscopy and secondary and backscattered electron imaging. These features show a strong influence of modal composition and primary textures on early sites of strain localization. Thermal cracking and subsequent alteration intensities and distribution are strongly phase dependent. A consistently higher intragranular fracture density is observed in augite crystals relative to plagioclase. The impact of alteration on the mechanical response of diabases is likely to depend on the primary textural characteristics. Even where extensive augite alteration occurs, the rock remains supported by a framework of weakly altered plagioclase crystals. The Hole 504B diabases from Leg 140 provide a valuable comparison for future studies of more deformed sections likely to be encountered at depth. Advances in constraining the detailed rheology of the ocean crust at spreading centers would benefit from experimental deformation of texturally diverse diabase and gabbro samples.

Sedimentology of surface samples from the Weddell Sea, Antarctica

Mineralogical and granulometric properties of glacial-marine surface sediments of the Weddell Sea and adjoining areas were studied in order to decipher spatial variations of provenance and transport paths of terrigenous detritus from Antarctic sources. The silt fraction shows marked spatial differences in quartz contents. In the sand fractions heavy-mineral assemblages display low mineralogical maturity and are dominated by garnet, green hornblende, and various types of clinopyroxene. Cluster analysis yields distinct heavy-mineral assemblages, which can be attributed to specific source rocks of the Antarctic hinterland. The configuration of modern mineralogical provinces in the near-shore regions reflects the geological variety of the adjacent hinterland. In the distal parts of the study area, sand-sized heavy minerals are good tracers of ice-rafting. Granulometric characteristics and the distribution of heavy-mineral provinces reflect maxima of relative and absolute accumulation of ice-rafted detritus in accordance with major iceberg drift tracks in the course of the Weddell Gyre. Fine-grained and coarse-grained sediment fractions may have different origins. In the central Weddell Sea, coarse ice-rafted detritus basically derives from East Antarctic sources, while the fine-fraction is discharged from weak permanent bottom currents and/or episodic turbidity currents and shows affinities to southern Weddell Sea sources. Winnowing of quartz-rich sediments through intense bottom water formation in the southern Weddell Sea provides muddy suspensions enriched in quartz. The influence of quartz-rich suspensions moving within the Weddell Gyre contour current can be traced as far as the continental slope in the northwestern Weddell Sea. In general, the focusing of mud by currents significantly exceeds the relative and absolute contribution of ice-rafted detritus beyond the shelves of the study area.

(Table 1) Mean grain sizes and standard deviations of gas hydrate samples

Methane hydrates are present in marine seep systems and occur within the gas hydrate stability zone. Very little is known about their crystallite sizes and size distributions because they are notoriously difficult to measure. Crystal size distributions are usually considered as one of the key petrophysical parameters because they influence mechanical properties and possible compositional changes, which may occur with changing environmental conditions. Variations in grain size are relevant for gas substitution in natural hydrates by replacing CH4 with CO2 for the purpose of carbon dioxide sequestration. Here we show that crystallite sizes of gas hydrates from some locations in the Indian Ocean, Gulf of Mexico and Black Sea are in the range of 200-400 µm; larger values were obtained for deeper-buried samples from ODP Leg 204. The crystallite sizes show generally a log-normal distribution and appear to vary sometimes rapidly with location.

Isotopic ratios and concentrations for mineral-associated and particulate organic fractions of sediment core Wilson_Lake samples

The flux of sediment and organic carbon from continents to the coastal ocean is an important factor governing organic burial in coastal sediments, and these systems preserve important records of environmental and biogeochemical conditions during past global change events. Burial of organic materials in coastal systems can be promoted by chemical resilience or through protection by association with mineral surfaces, but the role and influence of these processes on organic records from ancient sediments is poorly known. We studied sediment and organic matter burial as particulate organic matter (POM) and mineral-bound organic matter (MOM) in near-shore marine sediments from the Wilson Lake core (New Jersey, USA) that span the Paleocene-Eocene thermal maximum (PETM), a climatic perturbation 55.9 Myr ago. Our results show that distinct POM and MOM fractions can be isolated from sediments. Both fractions appear to be dominated by terrestrial material, but POM consisted primarily of recently synthesized material whereas MOM included a significant fraction of pre-aged organic matter from soils or ancient sediments. Variation in organic burial through the PETM is associated with changes in inorganic nitrogen burial, clay mineralogy, and clastic grain size that we associate with enhanced continental weathering, erosion and redeposition of ancient kaolinites, and eustatic sea level variation, respectively. These results provide a new perspective on factors governing carbon burial and carbon isotope records in ancient marine margin settings and offer information on rate and phasing of late Paleocene/early Eocene Earth system changes that may constrain interpretations of the cause of the PETM climate change event.

Table 1. Radiocarbon dates from TPC522 and box core surface samples from BC521 and BC523

Recent intensification of wind-driven upwelling of warm upper circumpolar deep water (UCDW) has been linked to accelerated melting of West Antarctic ice shelves and glaciers. To better assess the long term relationship between UCDWupwelling and the stability of theWest Antarctic Ice Sheet, we present a multi-proxy reconstruction of surface and bottom water conditions in Marguerite Bay, West Antarctic Peninsula (WAP), through the Holocene. A combination of sedimentological, diatom and foraminiferal records are, for the first time, presented together to infer a decline in UCDW influence within Marguerite Bay through the early to mid Holocene and the dominance of cyclic forcing in the late Holocene. Extensive glacial melt, limited sea ice and enhanced primary productivity between 9.7 and 7.0 ka BP is considered to be most consistent with persistent incursions of UCDW through Marguerite Trough. From 7.0 ka BP sea ice seasons increased and productivity decreased, suggesting that UCDW influence within Marguerite Bay waned, coincident with the equatorward migration of the Southern Hemisphere Westerly Winds (SWW). UCDW influence continued through the mid Holocene, and by 4.2 ka BP lengthy sea ice seasons persisted within Marguerite Bay. Intermittent melting and reforming of this sea ice within the late Holocene may be indicative of episodic incursions of UCDW into Marguerite Bay during this period. The cyclical changes in the oceanography within Marguerite Bay during the late Holocene is consistent with enhanced sensitively to ENSO forcing as opposed to the SWW-forcing that appears to have dominated the early to mid Holocene. Current measurements of the oceanography of the WAP continental shelf suggest that the system has now returned to the early Holocene-like oceanographic configuration reported here, which in both cases has been associated with rapid deglaciation.

Sedimentation rates calculated on surface sediment samples from different site of the Atlantic and Pacific Oceans (Table 1)

Radiocarbon ages on CaCO3 from deep-sea cores offer constraints on the nature of the CaCO3 dissolution process. The idea is that the toll taken by dissolution on grains within the core top bioturbation zone should be in proportion to their time of residence in this zone. If so, dissolution would shift the mass distribution in favor of younger grains, thereby reducing the mean radiocarbon age for the grain ensemble. We have searched in vain for evidence supporting the existence of such an age reduction. Instead, we find that for water depths of more than 4 km in the tropical Pacific the radiocarbon age increases with the extent of dissolution. We can find no satisfactory steady state explanation and are forced to conclude that this increase must be the result of chemical erosion. The idea is that during the Holocene the rate of dissolution of CaCO3 has exceeded the rain rate of CaCO3. In this circumstance, bioturbation exhumes CaCO3 from the underlying glacial sediment and mixes it with CaCO3 raining from the sea surface.

Radionuclides measured in surface water samples from the South Atlantic

In the nutrient-rich Southern Ocean, Fe is a vital constituent controlling the growth of phytoplankton. Despite much effort, the origin and transport of Fe to the oceans are not well understood. In this study we address the issue with geochemical data and Nd isotopic compositions of suspended particle samples collected from 1997 to 1999 in the South Atlantic Sector of the Southern Ocean. Al, Th, and rare earth element (REE) concentrations as well as 143Nd/144Nd isotopic ratios in acetic acid-leached particle samples representing the lithogenic fraction delineate three major sources: (1) Patagonia and the Antarctic Peninsula provide material with eNd > -4 that is transported toward the east with the polar and subpolar front jets, (2) the south African shelf, although its influence is limited by the circumpolar circulation and wind direction, can account for material with eNd of -12 to -14 adjacent to South Africa, and (3) East Antarctica provides material with eNd of -10 to -15 to the eastern Weddell Sea and adjacent Antarctic Circumpolar Current. For this region we interpret the Nd isotopic evidence in combination with oceanographic/atmospheric constraints as evidence for supply of significant amounts of terrigenous detritus by icebergs.

(Table 1) Sea surface temperature reconstruction for eastern equatorial Pacific surface sediment samples

Significant uncertainties persist in the reconstruction of past sea surface temperatures in the eastern equatorial Pacific, especially regarding the amplitude of the glacial cooling and the details of the post-glacial warming. Here we present the first regional calibration of alkenone unsaturation in surface sediments versus mean annual sea surface temperatures (maSST). Based on 81 new and 48 previously published data points, it is shown that open ocean samples conform to established global regressions of Uk'37 versus maSST and that there is no systematic bias from seasonality in the production or export of alkenones, or from surface ocean nutrient concentrations or salinity. The flattening of the regression at the highest maSSTs is found to be statistically insignificant. For the near-coastal Peru upwelling zone between 11-15°S and 76-79°W, however, we corroborate earlier observations that Uk'37 SST estimates significantly over-estimate maSSTs at many sites. We posit that this is caused either by uncertainties in the determination of maSSTs in this highly dynamic environment, or by biasing of the alkenone paleothermometer toward El Niño events as postulated by Rein et al. (2005).