OK. For the thermal boundary layer problems that I outlined previously, the boundary layer equations (for the so-called "thermal entrance region" of the heated section) are as follows:
[tex]\overline{v}\frac{\partial T}{\partial x}=α\frac{\partial^2T}{\partial y^2}[/tex]
for the inviscid flow case and
[tex]\left(\frac{8\overline{v}}{D}\right)y\frac{\partial T}{\partial x}=α\frac{\partial^2T}{\partial y^2}[/tex]
for the viscous flow case, where α is the thermal diffusivity.
Boundary and initial conditions on these problems are as follows:
[itex]T=T_0[/itex] at y = 0, x < 0
[itex]T=T_1[/itex] at y = 0, x > 0
[itex]T=T_0[/itex] at y → ∞, all x
[itex]T=T_0[/itex] at x < 0, all y
The solution to these equations for both cases can be found in Transport Phenomena by Bird, Stewart, and Lightfoot. From these solutions, the local heat flux at the wall for each of these cases is given by:
[tex]q(x)=\frac{k(T_1-T_0)}{δ(x)}[/tex]
where δ can be recognized as the effective boundary layer thickness. This is given by:
[itex]\frac{δ(x)}{D}=0.806\left(\frac{αx}{\overline{v}D^2}\right)^{1/3}[/itex] for the viscous flow case and by
[itex]\frac{δ(x)}{D}=1.77\left(\frac{αx}{\overline{v}D^2}\right)^{1/2}[/itex] for the inviscid case.
These equations are valid for [itex]\left(\frac{αx}{\overline{v}D^2}\right)[/itex] less than 0.01. Why don't you plot them up on a log-log plot and see what you get. Even though the slope is higher for the inviscid case than for the viscous case, the viscous case starts out higher at low values of x. The only real difference between the viscous and the inviscid cases with respect to the cause of the difference in boundary layer growth rate is the nature of the velocity profile near the boundary, where in the inviscid case, the fluid velocity is constant, while, in the viscous case, the velocity is zero at the wall, and increases linearly with distance from the wall (far from the center of the tube).