Ford tagavara osade Hinnakiri mud. T

kuv., 10 x 14 cm

Ford tagavara osade hinnakiri mud. Y ja C

kuv., 14 x 21 cm

Ford tagavara osade hinnakiri mud. 1928-1938

kuv., 21 x 27 cm

Ford tagavara osade hinnakiri mud. A & AA

kuv., 10 x 15 cm

Ford tagavara osade hinnakiri mud. T

kuv., 10 x 15 cm

Ford tagavara osade hinnakiri mud. A & AA

kuv., 10 x 15 cm

Ford tagavara osade hinnakiri V-8 ja 4-sil. MUD. 1928-1932

kuv., 10 x 15 cm

Ford tagavara osade hinnakiri 4 ja 8-sil. MUD. 1932-1933

kuv., 10 x 15 cm

Ford tagavara osade hinnakiri mud. T

kuv., 10 x 14 cm

Numerical study of wedge supported oblique shock wave-oblique detonation wave transitions

The results of a numerical study of premixed Hydrogen-air flows ignition by an oblique shock wave (OSW) stabilized by a wedge are presented, in situations when initial and boundary conditions are such that transition between the initial OSW and an oblique detonation wave (ODW) is observed. More precisely, the objectives of the paper are: (i) to identify the different possible structures of the transition region that exist between the initial OSW and the resulting ODW and (ii) to evidence the effect on the ODW of an abrupt decrease of the wedge angle in such a way that the final part of the wedge surface becomes parallel to the initial flow. For such a geometrical configuration and for the initial and boundary conditions considered, the overdriven detonation supported by the initial wedge angle is found to relax towards a Chapman-Jouguet detonation in the region where the wedge surface is parallel to the initial flow. Computations are performed using an adaptive, unstructured grid, finite volume computer code previously developed for the sake of the computations of high speed, compressible flows of reactive gas mixtures. Physico-chemical properties are functions of the local mixture composition, temperature and pressure, and they are computed using the CHEMKIN-II subroutines.

Vitamin D3-induced calcemic and phosphatemic responses in the freshwater mud eel Amphipnous cuchia maintained in different calcium environments

Vitamin D3 (100 ng 100 g body weight-l day-l) was administered intraperitoneally (ip) to the freshwater mud eel Amphipnous cuchia kept in artificial freshwater, calcium-free freshwater, low-calcium freshwater (0.2 mmol/l CaCl2) or calcium-rich freshwater (13.4 mmol/l CaCl2) for 15 days. Analyses of serum calcium and phosphate levels were performed on days 1, 3, 5, 10 and 15 after the beginning of the experiment (six eels from each group at each interval). Administration of vitamin D3 elevated the serum calcium [maximum elevation occurred at day 10 in artificial freshwater (vehicle: 10.55 ± 0.298, vitamin D: 13.90 ± 0.324), low-calcium freshwater (vehicle: 11.17 ± 0.220, vitamin D: 12.98 ± 0.297) and calcium-rich freshwater (vehicle: 11.24 ± 0.373, vitamin D: 14.24 ± 0.208) whereas it occurred at day 5 (vehicle: 8.42 ± 0.253, vitamin D: 11.07 ± 0.328) in calcium-free freshwater] and phosphate levels [maximum elevation at day 15 in artificial freshwater (vehicle: 4.39 ± 0.105, vitamin D: 5.37 ± 0.121), calcium-free freshwater (vehicle: 4.25 ± 0.193, vitamin D: 5.12 ± 0.181), low-calcium freshwater (vehicle: 3.93 ± 0.199, vitamin D: 5.28 ± 0.164) and calcium-rich freshwater (vehicle: 3.77 ± 0.125, vitamin D: 5.46 ± 0.151)] of the fish maintained in the above mentioned environmental media, but the responses were more pronounced in the fish kept in calcium-rich media

Sedimentology and stratigraphy of the Lower Silurian Grimsby formation, in subsurface, Lake Erie and Southwestern Ontario

Since the first offshore Lake Erie well was drilled in 1941, the Grimsby and Thorold formations of the Cataract Group have been economically important to the oil and gas industry of Ontario. The Cataract Group provides a significant amount of Ontario's gas production primarily from wells located on Lake Erie. The Grimsby - Thorold formations are the result of nearshore estuarine processes influenced by tides on a prograding shelf and are composed of subtidal channel complexes, discrete tidal channels, mud flats and non-marine deposits. Deposition was related to a regressive - transgressive cycle associated with eustatic sea level changes caused by the melting and resurgence of continental glaciation centred in Africa in the Late Ordovician/Early Silurian. Grimsby deposition began during a regression with the deposition of subtidal channel complexes incised into the marine deposits of the Cabot Head Formation. The presence of mud drapes and mud couplets suggest that these deposits were influenced by tides. These deposits dominate the lower half of the Grimsby. Deposition continued with a change from these subtidal channel complexes to laterally migrating, discrete, shallow tidal channels and mud flats. These were in turn overlain by the non-marine deposits of the Thorold Formation. Grimsby - Thorold deposition ended with a major transgression replacing siliciclastic deposition with primarily carbonate deposition. Sediment was sourced from the east and southeast and associated with a continuation of the Taconic Orogeny into the Early Silurian. The fluvial head of the estuary prograded from a shoreline that was located in western New York and western Pennsylvania running NNE-SSW and then turning NW-SE and paralleling the present day Lake Erie shoreline. iii The facies attributed to the Grimsby - Thorold formations can be ascribed to the three zones within the tripartite zonation suggested by Dalrymple et ale (1992) for estuaries, that is, a marine-dominated facies, a mixed energy facies, and a facies that is dominated by fluvial processes. Also, sediments within the Grimsby - Thorold are commonly fining upwards sequences which are common in estuarine settings whereas deltaic deposits are normally composed of coarsening upwards sequences in a vertical wedge shape with coarser material near the head. The only coarsening observed was in the Thorold Formation and attributed to non-marine deposition by palynological evidence. The presence of a lag deposit at the base of the sediments of the Grimsby Thorold formations suggests that they were incised into the Cabot Head Formation. Further, the thickness of Early Silurian sediments located between the top of the Queenston Formation, where Early Silurian sedimentation began, to the top of the Reynales - Irondequoit formation are constant whether the Grimsby - Thorold formations are present or not. Also, cross-sections using a sand body located in the Cabot Head Formation for correlation further imply that the Grimsby Formation has been incised into the previous deposits of the Cabot Head.

Les pratiques rhétoriques associées à une stratégie de wedge politics : une analyse du débat public portant sur le projet de loi C-391

Ce mémoire étudie le phénomène de wedge politics sous un angle communicationnel, en proposant d’identifier et décrire les principales pratiques rhétoriques associées au déploiement d’une stratégie de wedge politics par les nombreux acteurs du débat public sur le projet de loi C-391, intitulé Loi modifiant le Code criminel et la Loi sur les armes à feu (abrogation du registre des armes d’épaule). La posture rhétorique que nous adoptons se traduit par une démarche méthodologique et des analyses imbriquées en quatre étapes: 1) l’élaboration d’une mise en perspective historique relativement élargie du débat public entourant le projet de loi C-391, 2) la recension des principaux acteurs et des discours qu’ils ont produits à un moment fort de ce débat, entre mai 2009 et mai 2011, 3) une première analyse et description générale de la dynamique rhétorique entre les acteurs du débat pendant cette période, et enfin, 4) une analyse systématique des discours échangés entre le 1er août 2010 et le 22 septembre 2010 nous permettant d’identifier et de décrire les principales pratiques rhétoriques employées par les acteurs. Les dix pratiques que nous avons relevées sont: l’appel à l’action, le scapegoating, le ciblage, la personnalisation du débat, le blâme, la dérision, l’attribution d’intentions malveillantes, la menace de représailles de la part des électeurs, l’exploitation des clivages et le contraste. En conclusion, nous discutons en quoi ces pratiques rhétoriques peuvent contribuer à l’atteinte des objectifs d’une stratégie de wedge politics.