Each flow geometry requires different correlations be used to obtain heat transfer coefficients. Initially, we will look at correlations for fluids flowing in conduits.
Most correlations will take the "Nusselt form":
The correlations that follow are limited to conduit flow without phase change. Different geometries, boiling, and condensation will be covered in later lectures. Frictional heating (viscous dissipation) is not included in these correlations. This should not be a problem, since this phenomena is typically neglected except for highly viscous flows or gases at high mach numbers.
Unless otherwise specified, fluid properties should be evaluated at the "bulk average" temperature -- the arithmetic mean of the inlet and outlet temperatures:
When choosing a correlation, begin by asking:
The historic equation for use in turbulent conduit flow is the Dittus-Boelter Correlation (MSH Eq. 12.32):
Heating and cooling effect the velocity profile of a flowing fluid differently because of the temperature dependence of viscosity. Heating usually makes the fluid near the wall less viscous, so the flow profile becomes more "plug-like." Cooling has the opposite effect, increasing the viscosity near the wall and impeding heat transfer. The effect is most pronounced for viscous flows with large wall -- bulk temperature differences.
Instead of using different exponents for heating and cooling, a direct correction for viscosity can be used. This takes the form of the ratio of the viscosity at the bulk fluid temperature to the viscosity at the wall temperature. The ratio is then raised to the 0.14 power.
Multiplicative correction factors are available to adjust for the entrance/exit consequences of short tubes:
Levenspiel (1998) recommends the following correlation for transition flow. The entrance effect correction may be omitted for "long" conduits.
Many of the laminar flow correlations are set up in terms of the Graetz Number. McCabe et al. define this as
Two correlations are provided for laminar flow, depending on the magnitude of the Graetz number. For Gz<100
Heat usually causes the density of a fluid to change. Less dense fluid tends to rise, while the more dense fluid falls. The result is circulation -- "natural" or "free" convection. This movement raises h values in slow moving fluids near surfaces, but is rarely significant in turbulent flow. Thus, it is necessary to check and compensate for free convection only in laminar flow problems.
The Grashof Number is used to assess the impact of natural convection (MSH Eq. 12.66):
The Grashof Number provides a measure of the significance of natural convection. When the Grashof Number is greater than 1000, heat transfer coefficients should be corrected to reflect the increase due to free circulation. Multiplicative correction factors are available to apply to the Nusselt Number or the heat transfer coefficient (do NOT use both). These are:
References:
R.M. Price
Original: 12/8/99
Modified: 1/2/2001, 1/4/2002, 2/4/2003
Copyright 1999, 2001, 2002, 2003 by R.M. Price -- All Rights Reserved