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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Página 14
... follows that the heat transferred per unit mass per unit temperature change in a constant volume process is ( dQdT ) = ( ∂e∂T ) =Cv. v v This shows that Cv dT represents the heat transfer per unit mass in a reversible constant volume ...
... follows that the heat transferred per unit mass per unit temperature change in a constant volume process is ( dQdT ) = ( ∂e∂T ) =Cv. v v This shows that Cv dT represents the heat transfer per unit mass in a reversible constant volume ...
Página 17
... follows that the temperature and density change during an isentropic process from state 1 to state 2 according to T 1 T2 = ( p1p2 ) (γ−1)/γ and ρ1 ρ2 = ( p1p2 ) 1/γ (isentropic) (1.26) See Exercise 8. For a perfect gas, simple ...
... follows that the temperature and density change during an isentropic process from state 1 to state 2 according to T 1 T2 = ( p1p2 ) (γ−1)/γ and ρ1 ρ2 = ( p1p2 ) 1/γ (isentropic) (1.26) See Exercise 8. For a perfect gas, simple ...
Página 18
... follows that a statically stable atmosphere is one in which the density decreases with height faster than in an adiabatic atmosphere. It is easy to determine the rate of decrease of 18 Introduction 10. Static Equilibrium of a ...
... follows that a statically stable atmosphere is one in which the density decreases with height faster than in an adiabatic atmosphere. It is easy to determine the rate of decrease of 18 Introduction 10. Static Equilibrium of a ...
Página 20
... follows that the actual temperature T and the potential temperature θ are related by T = θ ( pps ) (γ−1)/γ . (1.31) Taking the logarithm and differentiating, we obtain T dz = θ dz + γ p dz. Substituting dp/dz = −ρg and p = ρRT, we ...
... follows that the actual temperature T and the potential temperature θ are related by T = θ ( pps ) (γ−1)/γ . (1.31) Taking the logarithm and differentiating, we obtain T dz = θ dz + γ p dz. Substituting dp/dz = −ρg and p = ρRT, we ...
Página 33
... ) to find the normal and shear stresses on the given surface. An alternative method is described in what follows. For simplicity, consider a two-dimensional case, for which the known 6. Force on a Surface 33 6. Force on a Surface.
... ) to find the normal and shear stresses on the given surface. An alternative method is described in what follows. For simplicity, consider a two-dimensional case, for which the known 6. Force on a Surface 33 6. Force on a Surface.
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