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Sample text
81 states that convection heat transfer results, whether obtained theoretically or experimentally, can be represented in terms of three dimensionless groups instead of seven parameters (h, L, V, k, Cp, It, and p). The convenience is evident. Once the form of the functional dependence of Eq. , negligible viscous dissipation and body forces). Note that the relations of Eqs. 85 are derived without actually solving the system of Eqs. 67. References 3, 7, 12, 15, 16, and 18 cover the above procedure in more detail and also include many different cases.
When simplifying the conservation equation given in a full form, we have to rely on physical intuition or on experimental evidence to judge which terms are negligibly small. 23 Terms may also be shown to be negligibly small by order-of-magnitude estimates [7, 12]. Some classes of flow that result are: Creeping flows: inertia terms are negligible. Forced flows: gravity forces are negligible. Natural convection: gravity forces predominate. Low-speed gas flows: viscous dissipation and compressibility terms are negligible.
Osipova, and A. S. Sukomel, Heat Transfer, Mir Publishers, Moscow, 1977. 19. S. Whitaker, Elementary Heat Transfer Analysis, Pergamon, New York, 1976. CHAPTER 2 THERMOPHYSICAL PROPERTIES Thomas F. Irvine Jr. State University of New York at Stony Brook W h e n organizing a chapter of thermophysical properties with limited space, some difficult decisions have to be made. Since this is a h a n d b o o k for heat transfer practitioners, emphasis has b e e n placed on transport rather than t h e r m o d y n a m i c properties.
