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Littérature scientifique sur le sujet « Mont de La Saxe »

Auteur : Grafiati

Publié le 9 mars 2023

Mis à jour le 10 mars 2023

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Articles de revues sur le sujet "Mont de La Saxe"

Giordan, D., A. Manconi, P. Allasia et D. Bertolo. « Brief Communication : On the rapid and efficient monitoring results dissemination in landslide emergency scenarios : the Mont de La Saxe case study ». Natural Hazards and Earth System Sciences 15, n^o 9 (10 septembre 2015) : 2009–17. http://dx.doi.org/10.5194/nhess-15-2009-2015.

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Abstract. Straightforward communication of monitoring results is of major importance in emergency scenarios relevant to large slope instabilities. Here we describe the communication strategy developed for the Mont de La Saxe rockslide threatening La Palud and Entrèves hamlets in the Courmayeur municipality (Aosta Valley, Italy). Starting from the definition of actions and needs of the landslide management team, including scientists, technicians, civil protection operators, decision makers, and politicians, we show that sharing and disseminating ad hoc information simplifies the understanding of the landslide evolution, as well as the correct communication of the level of criticality.

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Giordan, D., A. Manconi, P. Allasia et D. Bertolo. « Brief Communication : On the rapid and efficient monitoring results dissemination in landslide emergency scenarios : the Mont de La Saxe case study ». Natural Hazards and Earth System Sciences Discussions 3, n^o 4 (21 avril 2015) : 2757–75. http://dx.doi.org/10.5194/nhessd-3-2757-2015.

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Abstract. Straightforward communication of monitoring results is of major importance in emergency scenarios relevant to large slope instabilities. Here we describe the communication strategy developed for the Mont de La Saxe case study, a large rockslide threatening La Palud and Entrèves hamlets in the Courmayeur municipality (Aosta Valley, Italy). Starting from the definition of actions and needs of the Landslide Management Team, including scientists, technicians, civil protection operators, decision makers, and politicians, we show that sharing and disseminating ad hoc information simplifies the understanding of the landslide evolution, as well as the correct communication of the level of criticality.

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Crepaldi, Stefano, Ye Zhao, Muriel Lavy, Gianpiero Amanzio, Enrico Suozzi et Marina De Maio. « Landslide analysis by multi-temporal terrestrial laser scanning (TLS) data : the Mont de la Saxe landslide ». Rendiconti online della Società Geologica Italiana 35 (avril 2015) : 92–95. http://dx.doi.org/10.3301/rol.2015.72.

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Roncella, R., G. Forlani, M. Fornari et F. Diotri. « Landslide monitoring by fixed-base terrestrial stereo-photogrammetry ». ISPRS Annals of Photogrammetry, Remote Sensing and Spatial Information Sciences II-5 (28 mai 2014) : 297–304. http://dx.doi.org/10.5194/isprsannals-ii-5-297-2014.

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Photogrammetry has been used since long to periodically control the evolution of landslides; however, true monitoring is reserved to robotic total stations and ground based InSAR systems, capable of high frequency, high accurate 24h/day response. This paper presents the first results of a fixed terrestrial stereo photogrammetric system developed to monitor shape changes of the scene. The system is made of two reflex cameras, each contained in a sealed box with a control computer that periodically acquires an image and send it to a host computer; once an image pair is received from the two cameras, the DSM of the scene is generated by image correlation and made available for archiving or analysis. The system has been installed and is being tested on the Mont de la Saxe landslide, where several monitoring system are active. Some instability of the camera attitude has been noticed and is corrected with an automated procedure. First comparisons with InSAR data show a good agreement.

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Dakovic, Aleksandra, Zivko Sekulic, Georg Rottinghaus, Srdjan Matijasevic, Sonja Milicevic et Ana Stojanovic. « Montmorillonite modified with copper ions : Efficient adsorbent for aflatoxin B1 ». Veterinarski glasnik 62, n^o 1-2 (2008) : 35–42. http://dx.doi.org/10.2298/vetgl0802035d.

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In this paper, the results of preparation of material for adsorption of aflatoxin B1, based on modification of montmorillonite with copper ions (Cu-MONT), are presented. The bentonite clay from Sokolac deposit (Sipovo, Bosnia) was used as the starting raw material. After modification of concentrate of montmorillonite (MONT) with copper, the content of copper in Cu-MONT, was 2.65%. It was shown that MONT, as well as the Cu-MONT were efficient in adsorption of aflatoxin B1, at different mass ratios of adsorbent : toxin, and at different pH values. It was determined that for MONT, at the mass ratio adsorbent : toxin = 5000 : 1, aflatoxin B1 adsorption index was 100% at pH 3, 98% at pH 7 and 96% at pH 9. For Cu-MONT, at the same mass ratio, the following aflatoxin B1 adsorption indexes were achieved: 98% at pH 3, 98% at pH 7 and 96% at pH 9. No differences in adsorption of this toxin by both montmorillonites with decreasing the mass ratio of adsorbent : toxin (250 : 1) were observed. That means that ion exchange of inorganic cations in montmorillonite with copper ions did not cause any changes in aflatoxin B1 adsorption, at pH 3, as well as at pH 7 and 9. It was also noticed that adsorption of aflatoxin B1 by MONT and Cu-MONT was not pH dependent.

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Recq, Maurice, Isabelle Le Roy, Philippe Charvis, Jean Goslin et Daniel Brefort. « Structure profonde du mont Ross d'après la réfraction sismique (îles Kerguelen, océan Indien austral) ». Canadian Journal of Earth Sciences 31, n^o 12 (1 décembre 1994) : 1806–21. http://dx.doi.org/10.1139/e94-161.

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Mont Ross is the main volcanic feature of the Kerguelen Archipelago (terres Australes et Antarctiques françaises). This newly formed volcano buildup over 2 Ma provides us with an outstanding model of volcanism occurring on an intraplate structure already aged 40 Ma. Mont Ross is the subaerial part of a plutonic complex located in Galliéni Peninsula. From seismic refraction studies, P-wave velocities within the upper crust range downward from 5.35 km/s at sea level to 6.60 km/s at a depth of 11 km. These are definitely higher than those encountered within surrounding basalts known as plateau basalts. These high velocities reveal, at first glance, an origin and composition of the basement of Mont Ross far distinct from those of tholeiitic or transitional lava flows generated near spreading centres. By comparison with plutonic ring complexes, it is reasonable to state that monzonite and syenite are the basic materials of the basement. Seismic velocities (6.85 to 7.30–7.35 km/s) and related Poisson ratio (σ = 0.30) within lower crust are consistent with gabbros as prominent material. The thickness of the lower crust below Mont Ross (6–7 km) is roughly the same as that below the archipelago. Gabbros are exposed around several plutonic ring complexes spread over the archipelago. The transition to mantle might be modelled by a 2 km thick transition zone, with high velocity gradient, already noticed below the archipelago. Velocities of 7.30–7.35 km/s at the base of the crust below Mont Ross do not preclude contamination of the lower crust by mantle material. Both gravity and seismic data substantiate the occurrence of high density (velocity) within the upper crust below Mont Ross. Isostatic compensation of Mont Ross is rather achieved by a flexural deflection of the lithosphere than by an Airy-type model. The structures of Mont Ross and Hawaiian volcanoes bear analogies likely related to their intraplate genesis.

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Waskitaningsih, Novida. « Teritorialisasi Pengembangan Ekonomi di Wilayah Val De Saone, Lyon, Perancis Sebagai Implikasi Diciptakannya Undang-Undang Chevenement ». JURNAL PEMBANGUNAN WILAYAH & ; KOTA 8, n^o 2 (15 juin 2012) : 204. http://dx.doi.org/10.14710/pwk.v8i2.11572.

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Cooperation between regions in France (intercommunalité) has been known since 1890. Laws bringing abig influence on the development of cooperation between regions is The Chevènement Act 1999. This lawpermits the implementation of territorialisation of economic development by Urban Community(Communauté Urbaine) of Grand Lyon in Val de Saône, Lyon. We examine how the territorialisationprocess of economic development in Val de Saône as the implication of the creation of The ChevènementAct. As a result, we found that the territorialisation is a kind of adaptation to the Chevènement Actenforcement related to the authority of Urban Community of Grand Lyon and Association betweenregions of Saône Mont d’Or (Syndicat de Communes Saône Mont d’Or) in economic development in Valde Saône. Territorialisation is characterized by the consensus and the signing of the developmentcontract concerning the role division between Urban Community of Grand Lyon, which has a newauthority in intervening the economic development in local and metropolitan level, and AssociationBetween Regions of Saône Mont d’Or, which has the same authority in intervening the economicdevelopment in local level of Val de Saône.Keywords : Urban Community of Grand Lyon, Association Between Regions Saône Mont d’Or,Chevènement Act 1999, economic development, teritorialisation

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Sollman, Philip. « Dichodontium opacifolium Dix. in Christ. and Dichodontium brasiliense Broth. are both identical with Chrysoblastella chilensis (Mont.) Reim. » Bryophyte Diversity and Evolution 17, n^o 1 (31 décembre 1999) : 21. http://dx.doi.org/10.11646/bde.17.1.7.

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Sun, Guangyin, Jiankun Zhang, Wei Meng et Liping Wang. « Optimization of preparation of montmorillonite nanometer zero-valent iron and the degradation of amoxicillin by response surface methodology ». Water Supply 20, n^o 8 (18 septembre 2020) : 3625–35. http://dx.doi.org/10.2166/ws.2020.227.

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Abstract Three-factor and three-level tests were carried out by Box–Behnken response surface methodology, with amoxicillin as the target pollutant, nanometer zero-valent iron (nZVI) materials loaded with montmorillonite prepared by liquid phase reduction method and the concentration of FeSO4 and NaBH4 and montmorillonite dosage as influencing factors. It revealed that the interaction between FeSO4 concentration and NaBH4 concentration had a significant effect on the preparation of montmorillonite-loaded nanometer zero-valent iron material, playing a key role in the removal of amoxicillin, and the effect of FeSO4 concentration was even more significant. In addition, the shape, structure and characteristic groups of the prepared materials were analyzed by means of scanning electron microscopy (SEM), Fourier transform infrared spectroscopy (FTIR), X-ray diffraction (XRD), etc. The nanometer zero-valent iron loaded with montmorillonite can effectively slow down the nZVI agglomeration effect and improve the effect of material degradation of pollutants. For the same concentration of amoxicillin wastewater, the removal rate of amoxicillin wastewater, after 1 h reaction, is as follows: Mont/nZVI > nZVI > Mont. The optimal conditions for the reaction are: pH is 3, the initial concentration is 60 mg/L, and the dosage is 2 g/L. The higher the temperature, the more amoxicillin is degraded by Mont/nZVI.

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Kawai, Yohei, Yuji Narita, Aika Yamawaki-Ogata, Akihiko Usui et Kimihiro Komori. « Montelukast, a Cysteinyl Leukotriene Receptor 1 Antagonist, Induces M2 Macrophage Polarization and Inhibits Murine Aortic Aneurysm Formation ». BioMed Research International 2019 (27 mai 2019) : 1–11. http://dx.doi.org/10.1155/2019/9104680.

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Background. The pathogenesis of abdominal aortic aneurysm (AAA) is characterized by atherosclerosis with chronic inflammation in the aortic wall. Montelukast is a selective cys-LT 1 receptor antagonist that can suppress atherosclerotic diseases. We evaluated the in vitro properties of montelukast and its in vivo activities in an angiotensin II–infused apolipoprotein E–deficient (apoE−/−) AAA mouse model. Methods. The mouse monocyte/macrophage cell line J774A.1 was used in vitro. M1 macrophages were treated with montelukast, and gene expressions of inflammatory cytokines were measured. Macrophages were cultured with montelukast, then gene expressions of arginase-1 and IL (interleukin)-10 were assessed by quantitative polymerase chain reaction, arginase-1 was measured by fluorescence-activated cell sorting, and IL-10 concentration was analyzed by enzyme-linked immunosorbent assay. In vivo, one group (Mont, n=7) received oral montelukast (10 mg/kg/day) for 28 days, and the other group (Saline, n=7) was given normal Saline as a control for the same period. Aortic diameters, activities of matrix metalloproteinases (MMPs), cytokine concentrations, and the number of M2 macrophages were analyzed. Results. Relative to control, montelukast significantly suppressed gene expressions of MMP-2, MMP-9, and IL-1β, induced gene expressions of arginase-1 and IL-10, enhanced the expression of the arginase-1 cell surface protein, and increased the protein concentration of IL-10. In vivo, montelukast significantly decreased aortic expansion (Saline vs Mont; 2.44 ± 0.15 mm vs 1.59 ± 0.20 mm, P<.01), reduced MMP-2 activity (Saline vs Mont; 1240 μM vs 755 μM, P<.05), and induced infiltration of M2 macrophages (Saline vs Mont; 7.51 % vs 14.7 %, P<.05). Conclusion. Montelukast induces M2 macrophage polarization and prevents AAA formation in apoE−/− mice.

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Thèses sur le sujet "Mont de La Saxe"

ALBERTI, STEFANO. « Geological analysis and numerical modelling of La Saxe landslide (Courmayeur) to improve understanding of geomorphological and geotechnical mechanisms and of the potential landslide evolution ». Doctoral thesis, Università degli Studi di Milano-Bicocca, 2019. http://hdl.handle.net/10281/241657.

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Le frane a lento scorrimento sono solitamente caratterizzate da tassi di spostamento da estramente lento, i.e. mm/anno a lento, i.e. centimetri/anno. Si sviluppano frequentemente in rocce metamorfiche foliate, e la deformazione è prevalentemente localizzata lungo una zona di taglio principale. Le caratteristiche mineralogiche, granulometriche e tessiturali di queste zone controllano sia il comportamento della frana che la sua possibile evoluzione. In questa tesi sono stati investigati sia il comportamento che l'evoluzione della zona di taglio, attraverso prove di laboratorio convenzionali (taglio diretto, le prove uniassiali e triassiali) e non convenzionali (ring shear apparatus). Le successive analisi hanno permesso di considerare sia la degradazione dal punto di vista mineralogico, che meccanico, valutando il ruolo di entrambe nella transizione da lenta a rapida (fenomeni di creep). Le prove sono state condotte su campioni provenienti dalla frana del Mont de La Saxe (MLS, Valle d'Aosta, Italia). La frana ha un volume stimato di circa 8x106 m3 e si estende tra 1,400 e 1,870 m a.s.l., su un'area di 150,000 m2. Questa frana interessa le frazioni di Entréves e di La Palud (Courmayeur), nonchè l'autostrada ed il tunnel del Monte Bianco che collega l'Italia alla Francia. Un altro caso studio comparitivo (Chervaz, Valle d'Aosta, Italia) è stato selezionato per effettuare i test di laboraorio, variando le litologie analizzate (scisti serpentinitici con elevata presenza di fillosilicati). La zona di taglio di MLS contiene sia fillosilicati (almeno il 20%) che grafite (circa il 10%) in grado di controllare le proprietà di attrito. Inoltre, la riduzione della granulometria è stata osservata durante il test con il ring shear apparatus insieme all’allineamento preferenziale delle particelle. Sono state derivate le caratteristiche di attrito e viscosità, come l'incremento di spostamento tangenziale prima dello stato stazionario e il comportamento di creep terziario. Il monitoraggio della frana di Mont de La Saxe è iniziato nel 2009 e negli anni seguenti è stato via via perfezionato. Il sistema di monitoraggio – ad oggi - è composto sia da strumentazione superficiale (e.g. GB-InSAR,…) che di strumentazione di monitoraggio installata in profondità (inclinometri, piezometri e DMS). Un monitoraggio così ampio è - probabilmente - un caso unico nelle Alpi. È stato osservato un chiaro comportamento stagionale, in particolare durante lo scioglimento delle nevi quando la frana mostra un massiccio incremento degli spostamenti (ad esempio, 2012, 2013 e soprattutto 2014). Inoltre, è stata investigata anche la frana del Ruinon (Valtellina, Italia) considerando la disponibilità di dati a lungo termine (dal 2006). È stata quindi condotta un'analisi statistica dei dati di monitoraggio, caratterizzando il comportamento della frana nel tempo e proponendo un nuovo approccio per definire le soglie di Early Warning. Infine, dopo la campagna sperimentale e la profonda analisi dei dati di monitoraggio, è stato sviluppato un modello matematico, basato sull’approccio proposto da Perzyna, in cui l’incrudimento subisce un processo di degradazione. I parametri del materiale sono stati calibrati sia con i risultati sperimentali precedentemente ottenuti e con i dati di monitoraggio. Le simulazioni numeriche attraverso questo modello danno l'evoluzione delle variabili cinematiche (spostamento, velocità e accelerazione) durante i risultati sperimentali. I risultati ottenuti in questa tesi contribuiscono alle nuove conoscenze relative allo sviluppo e all'evoluzione delle zone di taglio e forniscono anche una migliore comprensione di questi meccanismi combinando i test innovativi sviluppati con i dati sul campo in grado di sviluppare un modello per la previsione degli spostamenti delle frane. Infine, lo studio fornisce anche un nuovo approccio per definire le soglie di Early Warning.
Rockslides are characterized by slow to extremely slow displacement rates in their initial phases or for their entire evolution. They frequently occur in foliated metamorphic rocks. Field and monitoring evidence show that deformation is predominantly localized along a shear zone. Mineralogic, grain size and fabric characteristics of the shear zone control its behavior and the possible evolution of the rockslide from a slow creeping to a fast moving one. In this thesis we investigate the shear zone behavior and evolution through conventional (direct shear, standard uniaxial compression and triaxial test) and unconventional laboratory testing (with an ring shear apparatus). We try to merge mineralogic data with material degradation and their role in the transition from slow to fast evolution due to creep phenomena, the change in material behavior with shear displacement and velocity. The tests were carried out on samples collected from boreholes through cataclastic shear zones within the Mont de La Saxe (MLS) rockslide, Valle d’Aosta region, Italy, at the extreme termination of a Deep-seated Gravitational Slope Deformations. The rockslide volume is of about 8x106 m3, and it extends between 1,400 and 1,870 m a.s.l., over area of 150,000 m2. This landslide is located close to Entréves and La Palud (Courmayeur municipality) villages and to the Mont Blanc highway that connects Italy to France through a tunnel. Laboratory tests were also performed on samples from the Chervaz rockslide (Valle d’Aosta region) located in a different rock suite (e.g. serpentine schist with phyllosilicates). The MLS shear zone contained both phyllosilicates (at least 20%) and graphite minerals (about 10%) which can control frictional properties. Furthermore, grain size reduction has been observed during slow ring shear testing together with particles rearrangement. Frictional and viscous characteristics, such as the tangential displacement increment before the steady state and the tertiary creep behavior, have been derived. The long-term monitoring of this instability started on 2009 and during the following years has been improved. The monitoring system is composed by ground surface (GB-InSAR, optical targets, TLS surveys, GPS network) and deep-seated equipment (inclinometers, piezometers and DMS probes). Such an extensive monitoring is – probably – a unique case in the Alps. A clear seasonal behavior has been observed, especially during snow-melt season when the rockslide shows a massive increment of displacements (e.g. 2012, 2013 and especially 2014). An addition a case study was selected, the Ruinon rockslide (upper Valtellina, Italian Alps) because of the long-term available dataset (since 2006). A statistical analysis of monitoring data has been completed, in order to characterize to behavior of the rockslides through time and to propose a new approach to define Early Warning displacement rate thresholds. Finally, after the experimental campaign and the deep analysis of monitoring data, a mathematical model, based on the Perzyna’s delayed plasticity theory, in which the hardening rule considers the degradation process, has been developed. The material parameters were calibrated on the experimental results previously obtained and using the monitoring data. The numerical simulations through this model give the evolution of the kinematic variables (displacement, velocity and acceleration) during the experimental results. The results contribute new knowledge regarding the shear zone development and evolution and also provide an improved understanding of these mechanisms by developing one of the first high quality data sets that combines new laboratory tests and field data able to develop a model in order the landslide forecasting. Finally, the study provides a new approach to define Early Warning displacement rate thresholds for slope failures.

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Düselder, Heike. « Der Tod in Oldenburg : sozial- und kulturgeschichtliche Untersuchungen zu Lebenswelten im 17. und 18. Jahrhundert / ». Hannover : Verl. Hahnsche Buchhandlung, 1999. http://catalogue.bnf.fr/ark:/12148/cb38841669j.

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Stumpf, Jonathan M. « The last best fish will conservation and consensus save Montana's Arctic Grayling ? / ». [Missoula, Mont.] : The University of Montana, 2008. http://etd.lib.umt.edu/theses/available/etd-12182008-103630/unrestricted/STUMPF_JONATHAN_PROJECT.pdf.

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Thesis (M.A.) -- University of Montana, 2008.
Title from author supplied metadata. Description based on contents viewed on June 22, 2009. ETD number: etd-12182008-103630. Includes bibliographical references.

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Tessier, Marc. « Dynamique des communautes vegetales sur un marais sale : importance de suaeda maritima (baie du mont-saint-michel) ». Rennes 1, 1999. http://www.theses.fr/1999REN10115.

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Suaeda maritima est une halophyte relativement tolerante a la salinite. De plus, la periode de germination coincide avec une periode ou la salinite du sediment est basse. Ainsi, le taux de germination observe sur le terrain est proche de 100%, si bien que le stock de graines persistant est nul. D'autres facteurs abiotiques tels que l'action des marees, l'immersion jouent ensuite un role significatif en determinant les conditions d'etablissement et de survie des jeunes plants. Enfin, les facteurs abiotiques ont des consequences sur la reproduction de suaeda maritima. Les facteurs biotiques auront egalement une influence sur la dynamique de cette espece. Ainsi, suaeda maritima repond a l'augmentation de la densite par des modifications morphologiques tendant a reduire les individus a une simple tige feuillee non ramifiee. Il en resulte une diminution du succes reproducteur au niveau individuel. Au niveau des relations interspecifiques, suaeda maritima apparait comme une espece peu competitive par rapport aux perennes. Lorsque la canopee de ces deux especes est dense, elle limite le developpement des jeunes germinations de suaeda maritima. En outre, une matrice lache de puccinellia maritima peut a l'inverse proteger les jeunes germinations de suaeda maritima de l'effet des vagues et limiter la mortalite suite a la dessiccation du sediment. Suite a la suppression de la vegetation dans des communautes a puccinellia maritima et halimione portulacoides, suaeda maritima est l'espece dominante. Le suivi des effectifs, de la biomasse et du recouvrement de cette espece a permis de voir qu'elle repond tres rapidement aux perturbations. Neanmoins, elle est progressivement eliminee par exclusion competitive. Suite a des apports artificiels d'azote, suaeda maritima est favorise seulement avec des doses tres elevees. Les apports d'azote d'origine marine mesures ne sont pas en mesure de favoriser suaeda maritima. Sur le bas, le moyen et le haut marais, les depressions sont apparues, a l'instar des perturbations, comme responsables d'une certaines variabilite environnementale spatio-temporelle favorable au maintien de suaeda maritima et de la diversite vegetales.

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VIVIER, JEAN-PAUL. « Influence du paturage sur la disponibilite de l'azote pour l'exportation dans un marais sale (baie du mont-saint-michel) ». Rennes 1, 1997. http://www.theses.fr/1997REN10048.

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Dans le cadre d'une etude pluridisciplinaire sur les marais sales de la baie du mont saint-michel et leur role sur la qualite des eaux cotieres, l'objectif de notre travail etait de montrer quelle etait l'influence du paturage ovin sur la disponibilite de l'azote, facteur limitant la productivite, pour l'exportation vers le milieu marin. A partir d'une approche indirecte axee sur la production et le devenir de l'azote produit sur un marais sale non pature, un marais pature et des zones exclues du paturage, nous avons tente de comprendre l'influence du paturage sur le fonctionnement du marais sale. Sous paturage, la production et la disponibilite de l'azote particulaire provenant de la vegetation sont faibles. Les potentialites d'exportation sont donc moindres meme si une partie importante de l'azote ingeree est restituee sous forme d'urine et de feces. La disponibilite de l'azote mineral est dependante de l'elevation du marais. Nous avons mis en evidence deux types de fonctionnement du marais selon sa maturation: un fonctionnement terrestre caracterise par un taux de renouvellement de l'azote organique dans le sol (azote mineralise sur azote total) lent et un fonctionnement marin caracterise par un taux de renouvellement rapide. Nos resultats suggerent que les potentialites d'exportation sont augmentees lorsque ce taux est eleve. La forte pression de paturage diminue la production de l'azote mineral et accelere indirectement la maturation du sol. En d'autres termes, le paturage intensif reduit les potentialites d'exportation de l'azote mineral. Si le paturage diminue les potentialites d'exportation de l'azote, a long terme, celui-ci par son action sur la structure et la composition des communautes vegetales permet le maintien du caractere maritime du marais sale et donc les echanges avec le milieu marin

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Doherty, Kevin Eric. « Sage-grouse and energy development integrating science with conservation planning to reduce impacts / ». [Missoula, Mont.] : The University of Montana, 2008. http://etd.lib.umt.edu/theses/available/etd-03262009-132629/unrestricted/doherty.pdf.

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Delpech, Louis. « Frantzösische Musicanten. Musique et musiciens français en Basse-Saxe et en Saxe (1666-1733) ». Thesis, Poitiers, 2015. http://www.theses.fr/2015POIT5004.

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Alors que de nombreux travaux ont déjà mis en lumière la circulation de musiciens et de genres musicaux italiens au Nord des Alpes durant les XVIIe et XVIIIe siècles, la musique française est encore largement perçue, pour reprendre l'expression de Rousseau, comme « indéchiffrable pour toute autre nation ». Reconduisant le paradigme d'un isolement musical de la France au sein d'une Europe baroque tout acquise à la musique italienne, l'historiographie a eu tendance à sous-estimer le rôle des transferts musicaux depuis la France dans la vie musicale européenne, et singulièrement allemande. Plusieurs phénomènes témoignent pourtant d'une intensification des échanges musicaux entre la France et les territoires germaniques du Saint Empire autour de 1700 : l'embauche de musiciens français dans plusieurs cours d'Allemagne, la diffusion et la copie de sources imprimées de musique française, l'exécution d'œuvres françaises ou d'inspiration française dans les grands centres musicaux de l'espace germanique, ainsi que la formation d'un discours théorique de langue allemande sur la musique française constituent autant de modalités essentielles de la circulation des hommes, des œuvres, des savoirs et des pratiques musicales dans l'Europe moderne. La Basse-Saxe et la Saxe offrent deux cas d'étude exemplaires où la migration des musiciens français, qui fait d'abord l'objet d'une analyse prosopographique à travers une reconstruction des réseaux et des trajectoires individuelles, peut ensuite être mise en parallèle avec la circulation de nombreuses sources musicales transmettant des œuvres du répertoire français. Au carrefour de la musicologie et de l'histoire sociale des migrations, ce travail vise ainsi à éclairer les différentes facettes d'un transfert culturel, en restituant à ce concept une chair humaine dont il est trop souvent privé
Many studies have highlighted the spread of Italian musicians and musical genres across the Alps during the 17th and 18th centuries, but French music remains time and again perceived as « undecipherable for any other nation », as Rousseau once put it. The historiography has long held fast to the idea of an isolated France within a European musical market shaped by the pervasive diffusion of Italian music, thus overlooking the role played by French music and musicians on the European and indeed the German musical scene. However, a few facts strongly indicate that musical exchanges between France and certain German territories of the Holy Roman Empire were becoming increasingly important around 1700 : several courts hired French bands, scores of French music were copied and disseminated throughout Germany, musical works genuinely French or emulating French models were performed in all major musical centers, and a coherent discourse on French music was further articulated in German theoretical production. Those facts are essential to our understanding of the mobility of people, works, ideas and practices in the Early-Modern Europe. Lower-Saxony and Saxony provide two case studies in order to show how the migration of French musicians, subjected to a prosopographical investigation that points out social networks and individual odysseys, can be connected to the dissemination of actual sources of French music. Bringing together musicology and social history of migrations, this study examines different aspects of a cultural transfer and ultimately reveals that human flesh is always part of it

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Petschel, Dorit. « Sächsische Aussenpolitik unter Friedrich August I. : zwischen Rétablissement, Rheinbund und Restauration / ». Köln : Böhlau Verl, 2000. http://catalogue.bnf.fr/ark:/12148/cb38861906w.

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Buschmann, Mirko. « Zwischen Bündnis und Integration : Sachsens militärpolitischer Eintritt in den Norddeutschen Bund 1866/67 / ». Köln : Böhlau, 2004. http://catalogue.bnf.fr/ark:/12148/cb39160732k.

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Keller, Katrin. « Kleinstädte in Kursachsen : Wandlungen einer Städtelandschaft zwischen Dressigjährigem Krieg und Industrialisierung / ». Köln : Böhlau, 2001. http://catalogue.bnf.fr/ark:/12148/cb39076491r.

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Livres sur le sujet "Mont de La Saxe"

Wulf, Walter. Saxe romane. [La Pierre-qui-Vire, Yonne] : Zodiaque, 1996.

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Saxe, Adrian Anthony. Adrian Saxe. [Kansas City, Mo.] : University of Missouri-Kansas City Gallery of Art, 1987.

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Bois, Jean-Pierre. Maurice de Saxe. [Paris] : Fayard, 1992.

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Kʻartʻvelebis sulieri saxe. Tʻbilisi : Akolasia, 2010.

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Dippel, Horst, et Werner Heun, dir. Saxe-Meiningen – Württemberg / Addenda. Berlin, New York : Walter de Gruyter – K. G. Saur, 2008. http://dx.doi.org/10.1515/9783598440762.

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Hulot, Frédéric. Le Maréchal de Saxe. Paris : Pygmalion, 1989.

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Le rêve de Saxe. Paris : Editions Ramsay, 1986.

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Balanyà, Jaume. Mont-serrat. [Spain] : Triangle Postals, 2002.

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Maupassant, Guy de. Mont-Oriol. Ottawa : eBooksLib, 2009.

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Viscogliosi, Fabio. Mont Blanc. Paris : Stock, 2011.

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Chapitres de livres sur le sujet "Mont de La Saxe"

Amanzio, Gianpiero, Ashwani Kumar Tiwari, Muriel Lavy et Marina De Maio. « Integration of Terrestrial Laser Scanning and GIS Analysis for Multi-temporal Landslide Monitoring : A Case Study of the Mont de La Saxe (Aosta Valley, NW Italy) ». Dans Landslides : Theory, Practice and Modelling, 267–82. Cham : Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-77377-3_12.

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Tau, Ramiro. « Martínez Mont, Luis ». Dans The Palgrave Biographical Encyclopedia of Psychology in Latin America, 1–3. Cham : Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-38726-6_589-1.

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Glaser, Horst Albert. « Thronprätendent in Kurland Maurice de Saxe ». Dans Abenteurer als Helden der Literatur, 95–105. Stuttgart : J.B. Metzler, 2002. http://dx.doi.org/10.1007/978-3-476-02877-8_8.

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Pargoire, Jules. « II. Mont Saint-Auxence ». Dans Revue de l’Orient Chrétien (1896-1946), sous la direction de René Graffin, 15–31. Piscataway, NJ, USA : Gorgias Press, 2010. http://dx.doi.org/10.31826/9781463220716-003.

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Pargoire, Jules. « II. Mont Saint-Auxence ». Dans Revue de l’Orient Chrétien (1896-1946), sous la direction de René Graffin, 426–58. Piscataway, NJ, USA : Gorgias Press, 2010. http://dx.doi.org/10.31826/9781463220716-023.

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Rüber-Schütte, Elisabeth. « Les stucs de Saxe-Anhalt, recherches nouvelles ». Dans Bibliothèque de l'Antiquité Tardive, 339–48. Turnhout : Brepols Publishers, 2006. http://dx.doi.org/10.1484/m.bat-eb.3.153.

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Mellein, Richard, et KLL. « Maupassant, Guy de : Mont-Oriol ». Dans Kindlers Literatur Lexikon (KLL), 1–2. Stuttgart : J.B. Metzler, 2020. http://dx.doi.org/10.1007/978-3-476-05728-0_13115-1.

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Stille, Alexander. « Makeover for Mont-Saint-Michel ». Dans A Museum Studies Approach to Heritage, 259–64. Abingdon, Oxon ; New York, NY : Routledge, 2018. | Series : Leicester readers in museum studies : Routledge, 2018. http://dx.doi.org/10.4324/9781315668505-21.

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Biard, Joël. « Albert de Saxe et les sophismes de l’infini ». Dans Sophisms in Medieval Logic and Grammar, 288–303. Dordrecht : Springer Netherlands, 1993. http://dx.doi.org/10.1007/978-94-011-1767-8_16.

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Massey, Joseph. « Adelaide of Saxe-Meiningen : The Childless Queen Mother ». Dans Queenship and Power, 89–110. Cham : Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-12829-5_6.

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Actes de conférences sur le sujet "Mont de La Saxe"

Bang, Hyunwoo, et Yunsil Heo. « Mont ». Dans SA '11 : SIGGRAPH Asia 2011. New York, NY, USA : ACM, 2011. http://dx.doi.org/10.1145/2077355.2425790.

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Puzovic, Nikola. « Mont-Blanc ». Dans the 9th conference. New York, New York, USA : ACM Press, 2012. http://dx.doi.org/10.1145/2212908.2212961.

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Kryeziu, Driton R., Bojan Bratuž, Alojz Nastran et Binak Beqaj. « 3 MONT - System for Energy Saving in Building ». Dans University for Business and Technology International Conference. Pristina, Kosovo : University for Business and Technology, 2012. http://dx.doi.org/10.33107/ubt-ic.2012.6.

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Bastien, Pierre, Vincent Ross et Olivier Hernandez. « New imaging polarimeter for the Mont Megantic Observatory ». Dans Astronomical Telescopes and Instrumentation, sous la direction de Silvano Fineschi. SPIE, 2003. http://dx.doi.org/10.1117/12.458900.

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Morin, Antoine, Olivier J. Caron, Robert-André Daigneault, Alexis Robitaille et William W. Shilts. « NEW INSIGHTS INTO THE DEGLACIATION OF MONT MEGANTIC ». Dans GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-358159.

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« Population Dynamics of Pseudomonad fluorescent Isolate Pf-122 In Formula in Different Save Containers ». Dans 5th International Seminar of Research Month 2020. Galaxy Science, 2021. http://dx.doi.org/10.11594/nstp.2021.0933.

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Bonnot-Courtois, Chantal, et J. Le Rhun. « Evolution des fonds aux abords du Mont-Saint-Michel ». Dans Journées Nationales Génie Côtier - Génie Civil. Editions Paralia, 1996. http://dx.doi.org/10.5150/jngcgc.1996.027-b.

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Shingai, Masashi, Akiyoshi Iida et Akisato Mizuno. « Numerical Study on Securing Evacuation Environment Under Fire at an Inclined Tunnel Part ». Dans ASME/JSME 2007 5th Joint Fluids Engineering Conference. ASMEDC, 2007. http://dx.doi.org/10.1115/fedsm2007-37605.

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We have experienced severe fire accidents in tunnels, such as in the Mont Blanc Tunnel or Tauern Tunnel. These accidents triggered a series of studies for securing safe environments in case of tunnel fire. Plenty of research has been done so far, experimentally or numerically, on the phenomena of tunnel fire, and the behavior of smoke and heat has been discussed for the flat part of the tunnel. At the inclined part, however, the analysis is not sufficient, and it is necessary to be studied. The authors estimated the behavior of heat and smoke by fire at an inclined tunnel part by means of a 3-D numerical analysis. The analysis was done utilizing a freeware, named “FrontFlow/red” developed by a group at Tokyo University. The simulation results give a detailed flow field as well as heat and smoke distribution, which can be used to establish tunnel facilities as ventilation systems and their control, so that safe environments can be attained. It is also available to decide the interval of cross passages for evacuation.

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Gerhorst, Frank, Martin Wirth et Kai Kuhlbach. « Application of Monte-Carlo-Simulation and Most Probable Limit State on Gasoline DI Combustion System Optimization ». Dans SAE 2010 World Congress & Exhibition. 400 Commonwealth Drive, Warrendale, PA, United States : SAE International, 2010. http://dx.doi.org/10.4271/2010-01-0712.

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Cayocca, Florence, Morgan Dussauze, Pierre Le Hir, Philippe Bassoullet et Hervé Jestin. « Modélisation hydro-sédimentaire de la baie du Mont Saint-Michel ». Dans Journées Nationales Génie Côtier - Génie Civil. Editions Paralia, 2006. http://dx.doi.org/10.5150/jngcgc.2006.016-c.

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Rapports d'organisations sur le sujet "Mont de La Saxe"

St-Onge, M. R., et S. B. Lucas. Geology, Mont Albert-Low, Québec. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/128009.

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Cloutier, M., et P. Corbeil. Géologie du Quaternaire, Mont Alexandre, Québec. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/130048.

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Homan, Kara, Michel Ayer et Bogdana Rus. Mount Vernon Parks and Schools Safe Connection Routes Plan. University of Iowa, mai 2007. http://dx.doi.org/10.17077/7iqp-i3b8.

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Van Kranendonk, M. J. Geology, Mont Jacques-Rousseau, Québec-Newfoundland (Labrador). Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/183959.

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Santhya, K. G. Making pregnancy safe for women in Rajasthan : Targeting the most vulnerable. Population Council, 2009. http://dx.doi.org/10.31899/pgy15.1004.

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Gagnon, Y. D., et R. A. Jamieson. Geology of the Mont Albert region, Gaspe Peninsula, Quebec. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1985. http://dx.doi.org/10.4095/120205.

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Adams, J. A precursory sub-event to the Mont-Laurier earthquake. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1995. http://dx.doi.org/10.4095/315315.

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Dumont, R., et J. Potvin. Residual total magnetic field, 22C/09 - Mont-Joli, Quebec. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2005. http://dx.doi.org/10.4095/220912.

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Dumont, R., et J. Potvin. Residual total magnetic field, 22 A/11 - Mont Alexandre, Quebec. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2004. http://dx.doi.org/10.4095/215932.

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Dumont, R., et J. Potvin. Residual total magnetic field, 22 H/04 - Mont Louis, Quebec. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2004. http://dx.doi.org/10.4095/215942.

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