944 resultados para horizons d’attente
Resumo:
If you stand on the edge of a river you are likely to see the otherside. From a narrow stream in the countryside to broad urban bodies of water, one of the conditions of rivers in Europe is the relative narrowness and ease to cross. Other rivers, such as Rio de la Plata are very far from this condition, with a width of 48 km at the merging of delta del Paraná and 219 km where it meets the sea. This
condition had a great significance in the way Buenos Aires was perceived and the way it developed
historically. A boundless flat land confronted with a boundless flat river is a very particular condition
that invites each person to frame their own view. The riverfront is therefore the fringe and horizon
of the city. As a horizon it is the link with others, with the outside, with faraway lands, and for some
even the reminder of home. These areas, in their harbor condition, are the fringe of the city; they
are working areas, contested spaces, open for speculation and social conflict.
In this paper I intend to explore a series of different perceptions of the river from the land and the
land from the river as the riverfront evolved from a fortified defense system through to the
combination of a commercial harbor, airport and populated public spaces. For this purpose I will
investigate the writings of travelers, urban designers and policy makers who were instrumental in
the transformation of the riverfront.
Resumo:
Since 1999, the rapid, inexpensive and non-destructive use of Th/K and Th/U ratios from spectral gamma ray measurements have been used as a proxy for changes in palaeo-hinterland weathering. This model is tested here by analysis of in situ palaeoweathering horizons where clay mineral contents are well-known. A residual palaeoweathered horizon of Palaeogene laterite (developed on basalt) has been logged at 14 locations across N. Ireland using spectral gamma ray detectors. The results are compared to published elemental and mineralogical data. While the model of K and U loss during the early stages of weathering to smectite and kaolinite is supported, the formation (during progressively more advanced weathering) of gibbsite and iron oxides has reversed the predicted pattern and caused U and Th retention in the weathering profile. The severity (duration, humidity) of weathering and palaeoweathering may be estimated using Th/K ratios as a proxy. The use of Th/U ratios is more problematic should detrital gibbsite (or similar clays) or iron oxides be detected. Mineralogical analysis is needed in order to evaluate the hosts for K, U and Th: nonetheless, the spectral gamma ray machine offers a real-time, inexpensive and effective tool for the preliminary or conjunctive assessment of degrees of weathering or palaeoweathering.
Resumo:
Ticks as vectors of several notorious zoonotic pathogens, represent an important and increasing threat for human, animal health in Europe. Recent application of new technology revealed the complexity of the tick microbiome that might impact upon its vectorial capacity. Appreciation of these complex systems is expanding our vision of tick-borne pathogens leading us to evolve a more integrated view that embraces the “pathobiome” representing the pathogenic agent integrated within its abiotic and biotic environments. In this review, we will explore how this new vision will revolutionize our understanding of tick-borne diseases. We will discuss the implications in terms of research approach for the future in order to efficiently prevent and control the threat posed by ticks.
Resumo:
Périodicité : Mensuel
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1912/06 (A1,N3).
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1913/06 (A2,N10).
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1912/02 (A1,N1).
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1913/03 (A2,N8).
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1912-1913.
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1912/10 (A1,N4).
Resumo:
L’historien n’écrit pas de nulle part. Ancré dans son présent et participant à la société, il en épouse – ou critique – les projets, les utopies et les grands récits. Nous proposons dans ce travail d’approfondir cet ancrage à travers une histoire croisée et comparée des expériences du temps de deux historiens français (Michel de Certeau, François Furet) et d’un historien-sociologue québécois (Fernand Dumont). Notre objectif est double : il s’agit d’établir, dans un premier temps, les correspondances entre leurs expériences lors de deux tournants, celui des années 1960 et celui des années 1970. Tout en prenant en compte les contextes des auteurs à l’étude, nous élargirons l’échelle d’analyse afin de cerner la contemporanéité d’expériences du temps qui ne se réduisent pas aux seuls cadres nationaux. Nous pourrons ainsi établir les coordonnées des régimes d’historicité à chaque tournant en contribuant à préciser les différentes combinaisons des modes futuristes et présentistes en jeu. Dans un deuxième temps, nous explorerons les liens entre historiographie et régime d’historicité afin de mettre en évidence les jonctions entre les considérations épistémologiques et l’horizon d’attente des historiens à l’étude. En abordant plus spécifiquement la question du rôle de l’historien dans sa société, nous jaugeons les transformations parallèles de son expérience du temps et de ses pratiques historiographiques. Le passage de l’expérience d’une Histoire en marche au tournant de 1960 à celle d’une histoire bloquée au tournant de 1970 affecte considérablement la place et le statut de l’historien. D’éminent passeur du temps à l’écoute du sens du progrès, l’historien voit son statut contesté et marginalisé, ce qui ne veut pas dire que son rôle est moins important. Qu’il débusque des alternatives passées ou court-circuite des téléologies, il est chargé de maintenir coûte que coûte ouverts les horizons du temps. Nous verrons spécifiquement le sens que prenait cette tâche à un moment où la possibilité d’une « société nouvelle », après Mai 68, pointait à l’horizon des contemporains.