51. Solve Example IIIa.3.13 by direct derivation. For this purpose, consider the elemental control volume inside the boundary layer as shown in the figure. Write a steady state energy balance for this control volume by considering the net con- vection in the flow direction, net conduction perpendicular to the flow direction, and viscous work. Convection dy dx Conduction ↑ Viscous work
51. Solve Example IIIa.3.13 by direct derivation. For this purpose, consider the elemental control volume inside the boundary layer as shown in the figure. Write a steady state energy balance for this control volume by considering the net con- vection in the flow direction, net conduction perpendicular to the flow direction, and viscous work. Convection dy dx Conduction ↑ Viscous work
Elements Of Electromagnetics
7th Edition
ISBN:9780190698614
Author:Sadiku, Matthew N. O.
Publisher:Sadiku, Matthew N. O.
ChapterMA: Math Assessment
Section: Chapter Questions
Problem 1.1MA
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REFERENCE: FROM BOOK - ENGINEERING THERMOFLUIDS, M. MASSOUD

Transcribed Image Text:51. Solve Example III..3.13 by direct derivation. For this purpose, consider the
elemental control volume inside the boundary layer as shown in the figure. Write
a steady state energy balance for this control volume by considering the net con-
vection in the flow direction, net conduction perpendicular to the flow direction,
and viscous work.
Convection
dy
dx
Conduction
TViscous work

Transcribed Image Text:Example IIIa.3.13. Find the governing equation for steady state incompressible
flow over a flat plate.
Solution: Starting with Equation IIIa.3.23, the first term in the left-hand side and
the fourth term in the right-hand side are canceled due to the steady and incom-
pressible fluid assumptions, respectively. The equation then reduces to:
pv Vu° =V · (kỹT)-V ğ; +ġ* ++V ·B
If the effect of all body forces is also negligible, there is no internal heat genera-
tion, and we ignore contribution by thermal radiation then we get:
pv.Vu = V · (kỹT)+O
Substituting for u in terms of temperature, developing terms, substituting for vis-
cous-dissipation function, and considering only two-dimensional flow, the equa-
tion becomes:
v( av, əv
ду
ƏT
Vx
+V,
ax
ду
c( dr
ду
dx
In the boundary layer, variation in V, in the x-direction is much less than variation
in V, in the y-direction and the first term in the second parenthesis can be ne-
glected. Also neglecting dV,/dy and temperature variations in the x-direction, the
above equation simplifies to:
ƏT
ƏT
Vx
+V
dx
ду
vav,
-= -
y
dy?
c dy
Ignoring viscous dissipation, the above equation further simplifies to:
a?T
dy
ƏT
+V.
Ша.3.23-1
ax
ду
Note the striking resemblance between Equations IIIa.3.20-1 (in the absence of the
pressure gradient term) and IIIa.3.23-1.
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