Heat and Mass Transfer Balamurgan Notes
Transcript of Heat and Mass Transfer Balamurgan Notes
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BBALAMUGUND
ANSENIORLECTURER PAN
IMALAR ENGGCOLLEGECHEN
NAI
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36. What is
meant
by Newtonianheating or
coolingprocess?
The process inwhich the
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internalresistance is
assumed asnegligible
in comparisonwith its surface
resistance is
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known asNewtonian
heatingor cooling
process.37. What is
meant by
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Lumped heat
analysis?
In a Newtonianheating or
cooling processthe temperature
throughoutthesolid is
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consideredto be uniform at
a given time.Such an
analysisis called Lumpe
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d heat capacityanalysis.
38. Whatis meant by
Semi-infinitesolids?
In a semiinfinite solid, at
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any instant oftime, there is
always a pointwherethe effect
of heating orcooling at one
of its
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boundaries isnot felt at all.
Atthis point thetemperature
remainsunchanged. In
semi infinite
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solids, the biotnumber value is
.39. What is
meantby infinite
solid?
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A solid whichextends itself
infinitely in alldirections of
space is knownasinfinite solid.
In infinite
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solids, the biotnumber value is
in between 0.1and100..1001.0
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40. Define Biot
number.
It is defined asthe ratio of
internalconductive
resistance tothe
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surface convective resistance.ceresisconvectiveSurfacecere
sisconductive Internal Bi
tantan
=k hL B
ci
=
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41. What is
the significance
ofBiot Number?
B
BALAMUGUND
ANSENIOR
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LECTURER PAN
IMALAR ENGG
COLLEGECHEN
NAI
Biot number is
used to findLumped heat
analysis, Semi
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infinite solidsand Infinite
solids42. Explain
the significanceof Fourier
number.
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It is defined asthe ratio of
characteristicbody
dimension totemperature wa
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ve penetrationdepth in time.timeindepthn penetratiowav
eeTemperatur ensionbody sticCharacterinumber Fourier
dim=
It signifies thedegree
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thermal
conductivity?
1. Moisture. 2.Density of
material. 3.Pressure. 4.
Temperature.5.
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Structure ofmaterial.
44. Explainthe significance
of thermaldiffusivity.
The physicalsignificance of
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thermaldiffusivity is
that it tells ushow
fast heat is propagated or it dif
fuses through a
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0.3m thick. If the
temperatures of
the inner and outer
surface aremaintained at 50C
and 30Crespectively.
Calculate the heatlossthrough one
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square meter area.
Find also the
temperature at an
interior pointof the wall 24cm
distance from theouter wall.
(Ans : 46.67w/m2
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, 34C)
2.A steam pipe
200mm OD
is covered with25mm thich layer
of insulationmaterial with an
average thermalconductivity of
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0.08W/mK. The
temperature of the
pipesurface is
400C and that ofthe outer surface
of insulation is50C. Find the loss
of heat from a
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length of 10m of
the pipe line.(Ans: 7.88kW)
B
BALAMUGUND
ANSENIOR
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LECTURER PAN
IMALAR ENGG
COLLEGECHEN
NAI3.Computethe heat loss per
square meter ofthe surface area
of furnace wall25cmthick. The
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inner and outer
surface
temperatures are
400C and 40Crespectively. The
variation of thethermal
conductivity inW/mK with
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temperature in C is
given by the
following
equation: k =0.002T - 10
-6T2
(Ans: 575 W/ m
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2
)4.The temperature
distribution in along cylindrical
tube at a certaininstant is given by
T= 800 + 1000r
5000r2
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. Find (1) The
rate of heat flow
at the inside
and outsidesurface per m
length. (2) Therate of heat
storage per mlength. (3)
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Therate of change
of temperature
with time at the
inner and outersurfaces. Take
the following data ID = 60cm, O
D = 1m, k = 58
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W/mK, = 0.00
4m2
/h.(Ans: 219kW,
730kW, -511kW,-72C/h)
5.An
aluminium spher
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e weighing 7kg a
nd initially
at a temperature
of 260Cis suddenly
immersed in afluid at 10C. If h =
50W/m2
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K, compute the
time requiredto
cool the sphere to
90C.3
/2707mkg
=
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, c = 9000 J/kgK,
k = 204 W/mC.
(Ans: 1580sec)
UNITIICONVECTIO
N HEAT
TRANSFER
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to the bulk motion
of thefluid
particles; through
the molecularconduction within
the fluid itself alsocontributes
tosome extent. If this motion is mai
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nly due to the den
sity variations ass
ociated with tempe
rature gradientswithin the fluid,
the mode of heattransfer is said to
be due to
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freeor
natural convectio
n
. On the otherhand if this fluid
motion isprincipally
produced bysomesuperimposed
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velocity field like
fan or blower, the
energy transport is
said to be due toforced convection
. B
BALAMUGUNDANSENIOR
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LECTURER PAN
IMALAR ENGG
COLLEGECHEN
NAIConvection
BoundaryLayers:Velocity B
oundary Layer
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: Consider the
flow of fluid over
a flat plate as
shown in thefigure. The fluid
approaches theplate in x direction
with uniformvelocity u
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. The fluid particlesin the fluid layer
adjacent to thesurface get zero
velocity. Thismotionlesslayer
acts to retart the
motion of particles
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in the adjoining
fluid layer as a
result of
friction betweenthe particles of
these twoadjoining fluid
layers at twodifferent
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velocities.
Thisfluid layer
then acts to retart
the motion ofparticles of next
fluid layer and soon, until
adistancey =
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from the surface
reaches, where
these effects
become negligibleand the
fluid velocity ureaches the free
stream velocity u.
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as a result of
frictional effects
between thefluid
layers, the localfluid velocity u
will vary from x=0, y = 0 to y =
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.The region of the
flow over the
surface bounded
by
in which theeffects of
viscous shearingforces caused by
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fluid viscosity are
observed, is called
velocity boundary
layer or hydrodynamic
boundary layer.The thickness of
boundary layer
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is
generallydefined
as a distance from
the surface atwhich local
velocity u = 0.99of free
streamvelocity u.
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The retardation of
fluid motion in
the boundary
layer is due to theshear stresses
acting in oppositedirection with
increasing thedistance y from
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the surface
shear stress
decreases, the
local velocity uincreases until
approaches u
. With increasing
thedistance from
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the leading edge,
the effect of
viscosity
penetrates furtherinto the free stream
and boundarylayer thickness
grows.
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Thermal boundar
y Layer:
If the fluid
flowing on asurface has a
different temperature than the
surface, thethermal boundary
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aconstant
temperature Ts.
The fluid particles
in adjacent layerto the plate get the
same temperaturethat of surface. T
he particles exchange heat energy
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with particles in a
djoining fluid
layers and so on.
As a result, thetemperature
gradients aredeveloped inthe
fluid layers and atemperature
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profile is
developed in the
fluid flow, which
ranges from Ts atthe surface to
fluid temperatureT
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sufficiently far
from the surface
in y direction.