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The Global ETD Search service is a free service for researchers
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Networked Digital Library of Theses and Dissertations.
Our metadata is collected from universities around the world. If you manage a university/consortium/country archive and want to be added, details can be found on the NDLTD website.
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Showing 81 to 90 of 7317 (0.086 seconds)Spelling suggestions: "subject:"amathematical models."" "subject:"dmathematical models.""
| 81 |
The simulation and analysis of organizational structures as communication queueing systemsVelasco Martinez, Oscar Javier 08 1900 (has links)
No description available.
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| 82 |
Hydrodynamic modeling of shallow basinsMarchand, Philippe, 1972- January 1997 (has links)
A two-dimensional hydrodynamic model is used to simulate the flow field and the concentration distribution of a conservative tracer in shallow basins. A series of numerical test are performed to evaluate different numerical schemes and problems which arise for the use of the Second Moment Method (SMM) in diffusion dominated flows are reported. The results of the basin simulations are compared with experimental data. The model predicts the location and the size of the dead zones, bypassing, recirculation, and local concentrations within the basin. The positioning of the inlet and outlet, and the presence of baffles are important parameters for the location and size of dead zones. The model gives results which are in agreement with the experimental data. The results show that the hydrodynamic model is quite powerful in terms of predicting correctly the residence time distribution for ponds of various dimensions and shapes.
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| 83 |
Finite amplitude waves in a model boundary layerBalagondar, Puttappa Mallappa. January 1981 (has links)
No description available.
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| 84 |
A new dynamic subgrid-scale model for large-eddy simulation of turbulent flowsKim, Won-Wook 12 1900 (has links)
No description available.
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| 85 |
A fluid dynamics model of angiographic injections: possible improvements through the use of drag reducing polymersCarpenter, Walter Alan 12 1900 (has links)
No description available.
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| 86 |
On subgrid combustion modeling for large-eddy simulationsCalhoon, William Henry, Jr. 08 1900 (has links)
No description available.
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| 87 |
Development of an LU-scheme for the solution of hypersonic non-equilibrium flowZoebelein, Till 12 1900 (has links)
No description available.
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| 88 |
Numerical computation of metal/mold boundary heat flux in sand castings using a finite element enthalpy modelMoosbrugger, John C. 05 1900 (has links)
No description available.
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| 89 |
Use of multiple discriminant analysis to evaluate the effects of land use change on the simulated yield of a watershedDeCoursey, Donn Gene 08 1900 (has links)
No description available.
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| 90 |
Comparative complexity of continental divides on five continentsBalakrishnan, Aneesha B. January 2010 (has links)
The main focus of the present study is to identify and integrate the factors affecting the degree of irregularity of five continental divide traces, as expressed by their fractal characteristics measured by the divider method. The factors studied are climate, relief and tectonic environment. The second objective of this study is to determine the relationship between uplift rates and divide trace fractal dimension.
Analysis of the results suggests that the degree of irregularity of continental divide traces at fine scale (approximately 10-70 km of resolution) is strongly affected by both climate and tectonics. It is found that control of the factors is generally weaker at coarse scale (above approximately 70 km of resolution). Generic relief should be ranked below both climate and tectonic environment as a factor affecting the complexity of continental divide traces. In terms of the second objective, the fractal dimension at fine scales follows a weakly inverse relationship with uplift. At coarse scale, there is stronger inverse relationship between uplift rate and fractal dimension. / Introduction -- Methodology -- Geomorphic environment -- Evaluation of results -- Significance of control factors -- Conclusion. / Department of Geological Sciences
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