186,662 research outputs found
Marcelle Nicolle : Charles Nicolle, 1866-1936, (p. 289)
No full textOdier Dollfus Elisabeth. Marcelle Nicolle : Charles Nicolle, 1866-1936, (p. 289). In: Femmes Diplômées, n°60, 1966. p. 165
Giovanni Andréa Lorenzani (Appendice à Christiniana, MÉFR, t. 80, p. 718 et sq.)
No full textBignami-Odier Jeanne. Giovanni Andréa Lorenzani (Appendice à Christiniana, MÉFR, t. 80, p. 718 et sq.). In: Mélanges d'archéologie et d'histoire, tome 81, n°1, 1969. pp. 401-402
Femmes Médecins, t. II, n° 1 (1966). Biographie d’Isabelle Eberhardt, Si Mahmoud Saadi, Femmes Médecins, p. 57
No full textOdier Dollfus Elisabeth. Femmes Médecins, t. II, n° 1 (1966). Biographie d’Isabelle Eberhardt, Si Mahmoud Saadi, Femmes Médecins, p. 57. In: Femmes Diplômées, n°59, 1966. p. 119
Femmes Médecins, t. II, n° 1 (1966), Les premières femmes médecins en Afrique du Nord, G. Montreuil-Straus, Femmes Médecins, p. 65
No full textOdier Dollfus Elisabeth. Femmes Médecins, t. II, n° 1 (1966), Les premières femmes médecins en Afrique du Nord, G. Montreuil-Straus, Femmes Médecins, p. 65. In: Femmes Diplômées, n°59, 1966. p. 119
Turbulent stratified shear flow experiments: Length scale comparison
No full textStratified shear flows are ubiquitous in geophysical systems such as oceanic overflows, wind-driven thermoclines, and atmo- spheric inversion layers. The stability of such flows is governed by the Richardson Number Ri which represents a balance between the stabilizing influence of stratification and the destabilizing influence of shear. For a shear flow with velocity difference U, density difference ∆ρ and characteristic length H, one has Ri = g(∆ρ/ρ)H/U^2 which is often used when detailed information about the flow is not available. A more precise definition is the gradient Richardson Number Rig = N^2/S^2 where the buoyancy frequency N = ((g/ρ)∂ρ/∂z)^{1/2}, the mean strain S = ∂U/∂z in which z is parallel to gravity and suitable ensemble or time averages define the gradients. We explore the stability and mixing properties of a wall-bounded shear flow over a range 0.1< Rig <1 using simultaneous planar measurements of density and velocity fields using Planar Laser-Induced Fluorescence (PLIF) and Particle Image Velocimetry (PIV), respectively. The flow, confined from the top by glass horizontal boundary, is a lighter alcohol-water mixture injected from a nozzle into quiescent heavier salt-water fluid with velocity between 5 and 10 cm/s and with a relative fractional density difference of 0.0026 or 0.0052. The injected flow is turbulent with Taylor Reynolds number between 50 and 100. We compare a set of length scales that characterize the mixing properties of our turbulent stratified shear flow including the Thorpe Length L_T, the Ozmidov Length L_o, the Ellison Length L_E, and turbulent mixing lengths L_m and L_ρ
Femmes médecins
No full textOdier Dollfus Elisabeth. Femmes médecins. In: Diplômées, n°69, 1969. p. 24
Femmes médecins, n° 5, t. V
No full textOdier Dollfus Elisabeth. Femmes médecins, n° 5, t. V. In: Diplômées, n°74, 1970. p. 94
Avenirs, n°s 170-171, janvier-février 1966
No full textOdier Dollfus Elisabeth. Avenirs, n°s 170-171, janvier-février 1966. In: Femmes Diplômées, n°60, 1966. p. 162
Femmes Médecins, n° 4, t. III, septembre-octobre 1967
No full textOdier Dollfus Elisabeth. Femmes Médecins, n° 4, t. III, septembre-octobre 1967. In: Femmes Diplômées, n°66, 1968. p. 75
La Legenda antiqua S. Francisci, texte du ms. 1046 (M. 69) de Pérouse, édité par le P. Ferdinand-M. Delorme. Paris, éditions de la France franciscaine, 1926.
No full textBignami Odier Jeanne. La Legenda antiqua S. Francisci, texte du ms. 1046 (M. 69) de Pérouse, édité par le P. Ferdinand-M. Delorme. Paris, éditions de la France franciscaine, 1926.. In: Bibliothèque de l'école des chartes. 1928, tome 89. pp. 107-108
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