962 resultados para Iraí reservoir


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Deflections of jets discharged into a reservoir with a free surface are investigated numerically. The jets are known to deflect towards either side of the free surface or the bottom, whose direction is not determined uniquely in some experimental conditions, i.e. there are multiple stable states realizable in the same condition. The origin of the multiple stable states is explored by utilizing homotopy transformations in which the top boundary of the reservoir is transformed from a rigid to a free boundary and also the location of the outlet throat is continuously moved from mid-height to the top. We depicted bifurcation diagrams of the flow compiling the data of numerical simulations, from which we identified the origin as an imperfect pitchfork bifurcation, and obtained an insight into the mechanism for the direction to be determined. The parameter region where such multiple stable states are possible is also delimited. © 2011 The Japan Society of Fluid Mechanics and IOP Publishing Ltd.

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Acknowledgments Support for this work came from the SAFARI consortium which was funded by Bayern Gas, ConocoPhillips, Dana Petroleum, Dong Energy, Eni Norge, GDF Suez, Idemitsu, Lundin, Noreco, OMV, Repsol, Rocksource, RWE, Statoil, Suncor, Total, PDO, VNG and the Norwegian Petroleum Directorate (NPD). This manuscript has benefited from discussion with Bruce Ainsworth, Rachel Nanson and Christian Haug Eide. Boyan Vakarelov and Richard Davis Jr. are thanked for their constructive reviews and valuable comments that helped to improve the manuscript.

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

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Between May 1920 and March 1923, there were seventy-three houses belonging to the County Cork establishment burnt down by IRA and anti-treaty forces. More houses were destroyed by this method in Cork than in any other Irish county in the same timeframe. The establishment were targeted by the IRA for their political, military and social persuasions that were essentially in opposition to the nationalist movement. The motivations behind these burnings is examined, the main reasons being reprisals for actions taken by Crown forces, military reasons, loyalty of house owners to the British government and agrarianism. The geographical distribution of these burnings is also provided to reveal how active individual IRA brigades were that operated within the county. Though there were few areas of the county left unaffected by the occurrence of arson attacks, there were higher concentrations of burnings in some areas. The house burnings in County Cork did not conform to the national pattern of house burnings and the reasons for this are explored. This study argues that the presence of Crown forces in Cork and their implementation of an official reprisal policy in January 1921 escalated military conflict, and arson attacks became a key tactic utilised by IRA forces in response to this policy. The aftermath of house burnings for members of the establishment is revealed through the various compensation committees that were formed after both the War of Independence and Civil War. Key sources for this study included personal papers of both the establishment and military figures, IRA witness statements, local and national newspapers, the 1901 and 1911 Irish Censuses, Colonial Office Papers, compensation claims filed with the British government and Irish Free State, and others from archives throughout Ireland and the United Kingdom.

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

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The feasibility of monitoring fluid flow subsurface processes that result in density changes, using the iGrav superconducting gravimeter, is investigated. Practical targets include steam-assisted gravity drainage (SAGD) bitumen depletion and water pumping from aquifers, for which there is currently a void in low-impact, inexpensive monitoring techniques. This study demonstrates that the iGrav has the potential to be applied to multi-scale and diverse reservoirs. Gravity and gravity gradient signals are forward modeled for a real SAGD reservoir at two time steps, and for surface-fed and groundwater-fed aquifer pumping models, to estimate signal strength and directional dependency of water flow. Time-lapse gravimetry on small-scale reservoirs exhibits two obstacles, namely, a µgal sensitivity requirement and high noise levels in the vicinity of the reservoir. In this study, both limitations are overcome by proposing (i) a portable superconducting gravimeter, and (ii) a pair of instruments under various baseline geometries. This results in improved spatial resolution for locating depletion zones, as well as the cancellation of noise common in both instruments. Results indicate that a pair of iGrav superconducting gravimeters meet the sensitivity requirements and the spatial focusing desired to monitor SAGD bitumen migration at the reservoir scales. For SAGD reservoirs, the well pair separation, reservoir depth, and survey sampling determine the resolvability of individual well pair depletion patterns during the steam chamber rising phase, and general reservoir depletion patterns during the steam chamber spreading phase. Results show that monitoring water table elevation changes due to pumping and tracking whether groundwater or surface water is being extracted are feasible.