Fluid MechanicsAcademic Press, 2010 M01 20 - 904 páginas Fluid mechanics, the study of how fluids behave and interact under various forces and in various applied situations—whether in the liquid or gaseous state or both—is introduced and comprehensively covered in this widely adopted text. Fluid Mechanics, Fourth Edition is the leading advanced general text on fluid mechanics.
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Dentro del libro
Resultados 1-5 de 63
Página xiii
... Density in Atmosphere and Ocean .............. 605 3. Equations of Motion ............................................. 607 4. Approximate Equations for a Thin Layer on a Rotating Sphere........ 610 5. Geostrophic Flow ......
... Density in Atmosphere and Ocean .............. 605 3. Equations of Motion ............................................. 607 4. Approximate Equations for a Thin Layer on a Rotating Sphere........ 610 5. Geostrophic Flow ......
Página xv
... Atmospheric Pressure ................... A3. Properties of Dry Air at Atmospheric Pressure ...................... A4. Properties of Standard Atmosphere ................................ Appendix B Curvilinear Coordinates B1. Cylindrical ...
... Atmospheric Pressure ................... A3. Properties of Dry Air at Atmospheric Pressure ...................... A4. Properties of Standard Atmosphere ................................ Appendix B Curvilinear Coordinates B1. Cylindrical ...
Página xxv
... atmosphere during the course of writing and production of the book. Lastly, I am grateful to Amjad Khan, the late Amir Khan, and the late Omkarnath Thakur for their music, which made working after midnight no chore at all. I recommend ...
... atmosphere during the course of writing and production of the book. Lastly, I am grateful to Amjad Khan, the late Amir Khan, and the late Omkarnath Thakur for their music, which made working after midnight no chore at all. I recommend ...
Página 1
... Atmosphere . . 22 Exercises. . . . . . . . . . . . . . . . . . . . . . . . 22 Literature Cited ... atmosphere and in the ocean, why a layer of fluid heated from below breaks up into cellular patterns, why a tennis ball hit with “top spin ...
... Atmosphere . . 22 Exercises. . . . . . . . . . . . . . . . . . . . . . . . 22 Literature Cited ... atmosphere and in the ocean, why a layer of fluid heated from below breaks up into cellular patterns, why a tennis ball hit with “top spin ...
Página 5
... atmospheric air is ≈5 × 10−8 m. In special situations, however, the mean free path of the molecules can be quite large and the continuum approach breaks down. In the upper altitudes of the atmosphere, for example, the mean free path ...
... atmospheric air is ≈5 × 10−8 m. In special situations, however, the mean free path of the molecules can be quite large and the continuum approach breaks down. In the upper altitudes of the atmosphere, for example, the mean free path ...
Contenido
1 | |
25 | |
53 | |
81 | |
139 | |
Irrotational Flow | 165 |
Gravity Waves | 213 |
Dynamic Similarity | 279 |
Turbulence | 537 |
Geophysical Fluid Dynamics | 603 |
Aerodynamics | 679 |
Compressible Flow | 713 |
Introduction to Biofluid
Mechanics | 765 |
Some Properties of
Common Fluids | 841 |
Curvilinear Coordinates | 845 |
Founders of
Modern Fluid Dynamics | 851 |
Laminar Flow | 295 |
Boundary Layers and Related
Topics | 339 |
Computational Fluid
Dynamics | 411 |
Instability | 467 |
Visual Resources | 855 |
Index | 857 |
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Términos y frases comunes
approximation assumed atmosphere average becomes blood body boundary conditions boundary layer called Chapter circulation components Consider constant continuity coordinates cylinder decreases defined density depends derivative determined developed direction discussed distribution drag dynamics effects element energy equal equation example expressed field Figure finite flow fluid follows force function given gives gravity heat horizontal important increases initial instability integral irrotational length limit linear mass mean Mechanics method momentum motion moving normal Note obtain particle plane plate positive potential pressure problem propagation region relation represents requires result Reynolds number rotation scale shear shock shown shows side similarity solution speed steady streamlines stress surface surface tension temperature tensor theory tube turbulent unit variables vector velocity viscous volume vortex vorticity wall wave written zero