Hydraulics of skimming flows on stepped chutes: The effects of inflow conditions?

Modern stepped spillways are typically designed for large discharge capacities corresponding to a skimming flow regime for which flow resistance is predominantly form drag. The writer demonstrates that the inflow conditions have some effect on the skimming flow properties. Boundary layer calculations show that the flow properties at inception of free-surface aeration are substantially different with pressurized intake. The re-analysis of experimental results highlights that the equivalent Darcy friction factor is f similar to 0.2 in average on uncontrolled stepped Chute and f similar to 0.1 on stepped chute with pressurized intake. A simple design chart is presented to estimate the residual flow velocity, and the agreement of the calculations with experimental results is deemed satisfactory for preliminary design.

Dam break wave of thixotropic fluid

Thixotropy is the characteristic of a fluid to form a gelled structure over time when it is not subjected to shearing, and to liquefy when agitated. Thixotropic fluids are commonly used in the construction industry (e.g., liquid concrete and drilling fluids), and related applications include some forms of mud flows and debris flows. This paper describes a basic study of dam break wave with thixotropic fluid. Theoretical considerations were developed based upon a kinematic wave approximation of the Saint-Venant equations down a prismatic sloping channel. A very simple thixotropic model, which predicts the basic theological trends of such fluids, was used. It describes the instantaneous state of fluid structure by a single parameter. The analytical solution of the basic flow motion and theology equations predicts three basic flow regimes depending upon the fluid properties and flow conditions, including the initial degree of jamming of the fluid (related to its time of restructuration at rest). These findings were successfully compared with systematic bentonite suspension experiments. The present work is the first theoretical analysis combining the basic principles of unsteady flow motion with a thixotropic fluid model and systematic laboratory experiments.

Submerged and unsubmerged natural hydraulic jumps in a bedrock step-pool mountain channel (Fig. 1 Classical hydraulic jump with partially developed inflow conditions)

Fig. 1. Classical hydraulic jump with partially developed inflow conditions. F1 = 13.6, V1 = 4.7 m/s, B = 0.25 m, h = 0.020 mm, d1 = 0.012 mm, Q = 14 L/s. Photo courtesy of Dr. Hubert Chanson. published in: Geomorphology Volume 82, Issues 1-2, 6 December 2006, Pages 146-159 The Hydrology and Geomorphology of Bedrock Rivers doi:10.1016/j.geomorph.2005.09.024 Submerged and unsubmerged natural hydraulic jumps in a bedrock step-pool mountain channel Brett L. Vallé and Gregory B. Pasternacka

An experimental study of the jet of a boat propeller

An experimental study of the velocity and concentration (scalar) fields of a propeller is presented. Field and laboratory measurements were undertaken. The former were up to 50 diameters downstream. Important findings were that the mean velocity and scalar fields quickly become Gaussian while further downstream they both become irregular sometimes approaching approximately linear profiles. Propeller turbulence causes rapid mixing giving an initial concentration dilution factor of 1/20,000 after fifty propeller diameters. Some preliminary comparisons with field measurements of an actual boat in a natural waterway are made. Considerably more work is needed to gain a full understanding of the complex problem of propeller mixing.

Experimental Measurements of Velocity and Pressure Distribution on a Large Broad-Crested Weir

Basic experiments were conducted in a near full-scale broad-crested weir. Detailed velocity and pressure measurements were performed for two configurations. The results showed the rapid flow distribution at the upstream end of the weir, while an overhanging crest design may affect the flow field. The study showed further that large vortical structures might be observed immediately upstream of the weir and impact adversely on the overflow.

La musique acousmatique et le documentaire : vers un art sonore informatif

Ce mémoire rend compte de la création du « documentaire acousmatique » Littorale, une œuvre musicale à visée informative, élaborée au moyen de prises de son in situ, d’extraits d’archives sonores et des témoignages de sept informateurs. En tissant des liens entre les deux disciplines médiatiques que sont la composition acousmatique et le documentaire, l’œuvre retrace l’histoire d’un impressionnant corpus de chants folkloriques récoltés en 1918 par l’ethnologue Marius Barbeau, dans les villages côtiers de Sainte-Anne-des-Monts et Tourelle, Haute-Gaspésie. La démarche de composition s’élabore ainsi en trois axes communicants : la mise en lumière de liens préexistants mais sous-exploités entre le documentaire et l’acousmatique, la recherche de terrain entourant le répertoire de chansons et sa résurgence dans la population actuelle de la Haute-Gaspésie, ainsi que la composition des trois mouvements musicaux constituant Littorale. À travers l’investigation d’enjeux identitaires qui découlent de la redécouverte du répertoire et la mise en lumière de certains flous historiques qui y sont reliés, cet alliage de deux genres médiatiques vise l’émergence d’une démarche de composition informative et socialement pertinente.

A.A. Milne - When We Were Very Young : cycle éclectique de chansons pour enfants, chanté par des enfants

Les fichiers qui accompagnent mon document on été réalisés avec les logiciels Microsoft Word et Finale.

Le roman de Guillaume d'Orange de la tradition cyclique à la mise en prose

Mémoire numérisé par la Direction des bibliothèques de l'Université de Montréal.

La bioéthique, l’art et le syndrome des ovaires polykystiques: propos impressionniste visant à réhabiliter les corps tabous et les ovaires blâmés

Essai / Essay