Still One-Dimensional but More Complicated Heat Transfer from Extended Surfaces Heat flow Heat flux: Heat flow:
q′x′ = h ⋅ (Ts − T∞ ) Q′′ = h ⋅ A ⋅ (Ts − T∞ ) Heat transfer surface area
Fluid flow
Heat flow
Th
Extended surfaces
Tb (base temperature) Ts (surface temperature) T∞ Q′′ = h ⋅ A1 ⋅ (Tb − T∞ ) + h ⋅ A2 ⋅ (Ts − T∞ ) Base area (A1) Fluid flow Extended surface area (A2)
1
T∞ , h
Fin with uniform cross-section Thickness =t Width = w
Conduction
Tb
Ac (cross-section)
Heat flow Length = L
Convection
Tb T(L)
0
x
L
General Analysis dAs qx
dqconv Ac(x)
qf
qx+dx dx z
y x
2
q x = q x + dx + dq x + dx dT dx dq dT d dT = q x + x = −k ⋅ Ac ⋅ − k ⋅ Ac ⋅ ⋅ dx dx dx dx dx
q x = −k ⋅ Ac ⋅ q x + dx
d dT Ac ⋅ ⋅ dx dx dx = h ⋅ dAs ⋅ (T − T∞ )
dqconv = −k ⋅ dqconv
d dT h dAs ⋅ (T − T∞ ) = 0 Ac ⋅ − ⋅ dx dx k dx or d 2T 1 dAc dT 1 h dAs + ⋅ ⋅ − ⋅ ⋅ ⋅ (T − T∞ ) = 0 dx 2 Ac dx dx Ac k dx
Fin Performance Fin effectiveness: The ratio of the fin heat transfer rate to the heat transfer rate that would exist without the fin. Heat flow out of the fin
εf =
qf
h ⋅ Ac ,b ⋅ (Tb − T∞ ) Heat flow without the fin
To be practical
εf >2
Fin cross-sectional area at the base
3
Fin efficiency:
ηf =
qf qmax, f
=
qf
h ⋅ A f ⋅ (Tb − T∞ ) Surface area of the fin
Overall surface efficiency:
ηo =
qt qmax,t
=
Total heat flow with the fin
qt h ⋅ At ⋅ (Tb − T∞ ) Total surface area
Total heat flow: qt = h ⋅ Ab ⋅ (Tb − T∞ ) + h ⋅ A f ⋅η f ⋅ (Tb − T∞ ) At = Ab + A f
ηo = 1 −
Af At
⋅ (1 − η f )
4
Transient Heat Transfer (The Uniform Temperature Assumption)
h
T
T∞
T∞
dT mC p ⋅ = h ⋅ A ⋅ (T∞ − T ) dt
∂T ∂ 2T ρC p ⋅ =k 2 ∂t ∂x
or
Biot Number Definition - 1 q”x Ts,1 Ts,2
L T∞ x x=L
x=0
q ′x′ = k ⋅
Ts ,1 − Ts , 2 L
= h ⋅ (Ts , 2 − T∞ )
1
Biot Number Definition - 2 q ′x′ = k ⋅
Ts ,1 − Ts , 2 L Ts ,1 − Ts , 2 Ts , 2 − T∞ Bi =
= h ⋅ (Ts , 2 − T∞ ) =
h⋅L k
h⋅L k
Critical Biot Number: Bi < 0.1
Non-uniform Temperature T
h T∞
T∞
k 1 R h⋅L L Bi = = = conduction ks 1h Rconvection
2
Typical Values of the Convection Heat Transfer Coefficient (h) Process Free convection Gases Liquids Forced convection Gases Liquids Convection with phase change Boiling or condensation
h (W.m-2.K-1) 2-25 50-1000 25-250 100-20,000
2500-100,000
Determination of h (1) External flow
Double-pipe arrangement
Internal flow
Pipe
Channel
3
Determination of h (2) Forced convection is due to fluid movement which enhances heat transfer. Conduction only Fluid temperature T∞ Convection
m ⋅ C p ⋅T travels at a Velocity Hot object
Determination of h (3) Conduction: Thermal conductivity of the fluid (k) * Thermal diffusivity:
α = k (m2.s-1) ρ ⋅ C p
Density of the fluid (ρ)
Convection: Velocity and its distribution (u or V) Viscosity of the fluid (µ) * Kinematic viscosity: υ = µ
ρ
(m2.s-1)
Density of the fluid (ρ) Specific heat capacity of the fluid (Cp)
4
Determination of h (4) (Dimensionless Groups) Heat transfer: Biot number (Bi) Reynolds number (Re) Prandtl number (Pr) Nusselt number (Nu) Fourier number (Fo)
Film temperature :
T film =
Ts + T∞ 2
Mass transfer: Sherwood number (Sh) Schmidt number (Sc)
Determination of h (5) (Construction of the Correlations)
Rate of ‘reaction’
Nu =
h⋅L kf
Reactant A
Re =
ρ ⋅u ⋅ L µ
Reactant B
Pr =
υ α
Nu = c ⋅ Re m ⋅ Pr n
5
The Loop Tbulk fluid Tsurface
Physical properties
Dimensionless parameters Re, Pr etc
Another estimate? Do you really know that?
Nu ⋅ k f
h= L/L kfluid Nu
Find the correlation for Nu
6
Transient Conduction (Finite difference method) One dimensional (at x-direction):
∂T ∂T ρ ⋅Cp ⋅ =k⋅ 2 ∂t ∂x 2
Th
Steady state
At t > 0
Tl
Initial temperature (t = 0) To
Initial and Boundary Conditions Initial condition:
t = 0 ,T ( x ) = To , x ∈ [0 , L ]
Th
Steady state
Boundary condition:
∂T = hh ⋅ (Th − T (t ,0 )) ∂x ∂T t > 0 , x = L ,− k = hl ⋅ (T (t , L ) − Tl ) ∂x t > 0 , x = 0 ,− k
x=0
To
Tl
x=L
1
When heat transfer coefficients are very large (+∞) Th
Steady state
Tl
t ≥ 0 , x = 0,T = Th t ≥ 0 , x = L ,T = Tl
Finite Difference Approach ∂T ∂ 2T =k⋅ 2 ρ ⋅Cp ⋅ ∂t ∂x T p+1 2
3
p
∂T ∆T T p +1 − T p ≈ = ∂t ∆t ∆t
1
t=0
∆t
t
2
T − Ti ∆T ∂T = i +1 ≈ ∆x i + 0.5 ∆x ∂x i + 0.5 p
1
T
2
p
p
p
3 i-1
i
i+1
T − Ti −1 ∆T ∂T = i ≈ ∆x i −0.5 ∆x ∂x i −0.5 p
x=L
∆x
x=0 p
p
p
∆T ∆T p − 2 ∂ T 2 ≈ ∆x i + 0.5 ∆x i −0.5 ∆x ∂x i Ti +p1 − Ti p Ti p − Ti −p1 − ∆ ∆x x = ∆x Ti +p1 − 2Ti p + Ti −p1 = (∆x )2 p
Explicit Method p +1
T − Ti ∂T ≈ i ∆t ∂t i p
p
p
3
p +1
T − Ti ∂T ≈ ρC p i ρC p ∂t i ∆t p
Ti
Ti
p +1
p +1
− Ti
p
Ti +p1 − 2Ti p + Ti −p1 k⋅ (∆x )2
p
α ⋅ ∆t
(∆x )
2
(
⋅ Ti +p1 − 2Ti p + Ti −p1
)
2 ⋅ α ⋅ ∆t p p p 1 − ⋅ Ti ⋅ + + T T i +1 i −1 2 2 (∆x ) (∆x )
α ⋅ ∆t
(
)
4
Other Boundary Conditions Steady state
Th
∂T = hh ⋅ (Th − T (t ,0 )) ∂x ∂T t > 0 , x = L ,−k =0 ∂x t > 0 , x = 0 ,− k
To
Adiabatic
Adiabatic
x=0
x=L
Exact Equation ∂T ∂ 2T =k⋅ 2 ρ ⋅Cp ⋅ ∂t ∂x
Approximate Equation Ti
p +1
2 ⋅ α ⋅ ∆t p p p 1 − ⋅T ⋅ + + T T (∆x )2 i +1 i −1 (∆x )2 i
α ⋅ ∆t
(
)
1
Approximate Equation Ti
2 ⋅ α ⋅ ∆t p p p 1 − ⋅T ⋅ + + T T (∆x )2 i +1 i −1 (∆x )2 i
α ⋅ ∆t
p +1
(
)
Setting this One could then deduce a ∆t once α and ∆x are given
Ti
p +1
α ⋅ ∆t
(∆x )
2
0?
2 ⋅ α ⋅ ∆t 1 − =0 2 (∆x )
(
⋅ Ti +p1 + Ti −p1
)
An Example An medium (solid), which has uniform initial temperature of 50°C and a length of 0.5m, has its one side suddenly exposed to a fast flowing heating medium (fluid) having very large h (giving a constant surface temperature Ts = 150°C). The density of the solid is 8933 kg.m-3, specific heat capacity is 385 J.kg-1.K-1, thermal conductivity is 401 W.m-1.K-1. Show the temperature profile as heating progresses.
2
Convective Heat (& Mass) Transfer – Fundamentals 1 (at interface between two mediums) x
Solid
The heat flux along x-direction:
q′x′
=
− ks ⋅
∂T ∂T = −k f ⋅ ∂x s ∂x
Ts
h Fluid
f
T∞
∂T = h ⋅ (Ts − T∞ ) − ks ⋅ ∂x s
kf ⋅ h=−
∂T ∂x
f
(Ts − T∞ )
Average heat transfer coefficient
q′′
u∞, T∞
dAs As, Ts ‘Total’ heat flow (W.m-2): Local heat flux (W.m-2):
q′′ = h ⋅ (Ts − T∞
q )
Local heat transfer coef (W.m-2.K-1) Average heat transfer coef (W.m-2.K-1)
= ∫ h ⋅ (Ts − T∞ ) ⋅ dAs As
Constant surf temp
h ⋅ dA s A∫ s ⋅ (T − T ) ⋅ A ≈ s ∞ s As
1
Average heat transfer coefficient (flat plate)
q′′
u∞, T∞
As, Ts x
dx Plate length L Average heat transfer coef (W.m-2.K-1):
‘Total’ heat flow (W.m-2):
q
L
= h ⋅ L ⋅ (Ts − T∞ )
h=
∫ h ⋅ dx 0
L
Mass transfer (flat plate)
N ′′
u∞, cA,∞
(local mass flux, kg.m-3.m-2.s-1)
As, cA,s x
dx Plate length L Average mass transfer coef (m.s-1):
N ′A′ = hm ⋅ (c A, s − c A,∞ )
N A = hm ⋅ As ⋅ (c A, s − c A,∞ ) hm =
L
∫h
m
⋅ dx
0
L
2
Convection Boundary Layers (Velocity and temperature) Velocity Profile Temperature Profile Temperature
T∞
u∞
y
Velocity
δT
Heat Flux
δV
Ts
x Solid or Liquid Surface
Heated Plate
Convection Boundary Layers (Velocity and concentration) Velocity Profile Concentration Profile Concentration
cA,∞
u∞
y
Velocity
Mass Flux
δV
δC cA,s
x Solid or Liquid Surface
3
Heat and mass transfer coefficients kf ⋅ h=−
∂T ∂y
DA ⋅ y =0
hm = −
(Ts − T∞ )
(c
A, s
∂c A ∂y
y =0
− c A ,∞ )
y
h or hm
x Stationary medium
Laminar to Turbulent Flow (Transition) Velocity Profile Velocity Profile
u∞
y
Re x ,c = −
ρ ⋅ u∞ ⋅ xc = 5 ×105 µ
u∞
Turbulent region Buffer layer
δV
x
xc Laminar
Turbulent
Laminar sublayer
Transition Solid or Liquid Surface
4
Convective Heat (& Mass) Transfer – Fundamentals 1 (at interface between two mediums) x
Solid
The heat flux along x-direction:
q′x′
=
− ks ⋅
∂T ∂T = −k f ⋅ ∂x s ∂x
Ts
h Fluid
f
T∞
∂T = h ⋅ (Ts − T∞ ) − ks ⋅ ∂x s
kf ⋅ h=−
∂T ∂x
f
(Ts − T∞ )
Average heat transfer coefficient (flat plate)
q′′
u∞, T∞
As, Ts x
dx Plate length L
‘Total’ heat flow (W.m-2):
q
Average heat transfer coef (W.m-2.K-1):
L
= h ⋅ L ⋅ (Ts − T∞ )
h=
∫ h ⋅ dx 0
L
1
Mass transfer (flat plate)
N ′′
u∞, cA,∞
(local mass flux, kg.m-3.m-2.s-1)
As, cA,s x
dx Plate length L Average mass transfer coef (m.s-1):
N ′A′ = hm ⋅ (c A, s − c A,∞ )
L
N A = hm ⋅ As ⋅ (c A, s − c A,∞ ) hm =
∫h
m
⋅ dx
0
L
Heat and mass transfer coefficients kf ⋅ h=−
∂T ∂y
DA ⋅ y =0
(Ts − T∞ )
hm = −
(c
A, s
∂c A ∂y
y =0
− c A ,∞ )
y
h or hm
x Stationary medium
2
Laminar to Turbulent Flow (Transition) Velocity Profile Velocity Profile
Re x ,c =
u∞
y
ρ ⋅ u∞ ⋅ xc = 5 ×105 µ
u∞
Turbulent region Buffer layer
δV
x
xc Laminar
Turbulent
Laminar sublayer
Transition Solid or Liquid Surface
Convective Heat (& Mass) Transfer – Fundamentals 2 (h and hm determination) Conduction (heat): Thermal conductivity of the fluid (k) *Thermal diffusivity (α) (m2.s-1) Density of the fluid (ρ) Temperature gradient Diffusion (mass): *Mass diffusivity (D) (m2.s-1) Density of the fluid (ρ) Concentration gradient Convection: Velocity and its distribution (u or V) Viscosity of the fluid (µ) * Kinematic viscosity (υ) (m2.s-1) Density of the fluid (ρ) Specific heat capacity of the fluid (Cp)
h(W .m −2 .K −1 )
hm (m.s −1 )
Temperature and concentration difference
3
Determination of h Heat transfer: Biot number (Bi) Reynolds number (Re) Prandtl number (Pr) Nusselt number (Nu) Fourier number (Fo)
Film temperature :
T film =
Ts + T∞ 2
Film concentration :
Mass transfer: Sherwood number (Sh) Schmidt number (Sc)
c A, film =
c A, s + c A, ∞ 2
Determination of h Rate of ‘reaction’
Nu =
h⋅L kf
Reactant A
Re =
ρ ⋅u ⋅ L µ
Reactant B
Pr =
υ α
Nu = c ⋅ Re m ⋅ Pr n Sh = c ⋅ Re m ⋅ Sc n
4
The Working Loop Tbulk fluid Tsurface
Physical properties
Dimensionless parameters Re, Pr etc
Another estimate? Do you really know that?
Nu ⋅ k f
h= L/L kfluid Nu
Find the correlation for Nu
5
Convective Heat (& Mass) Transfer – Fundamentals 3 (Internal flows - momentum)
Re =
Wall Uniform Entry Flow Velocity u∞
δv
Fully developed region
xfd,h Fully developed
r
ro
Entry flow region
x
ρ ⋅ um ⋅ d µ
Hydrodynamic
Laminar to Turbulence Transition Re c ≈ 2300
Flow Becomes Fully Turbulent Re > 4000
Laminar Entry Length x fd ,h d
≈ 0.05 Re
Hydraulic Diameter
dh =
4 Ac P
Turbulent Entry Length 10 ≤
x fd ,h d
≤ 60
1
(Internal flows - energy)
Re =
ρ ⋅ um ⋅ d µ
Temperature profile Wall temperature Uniform Entry Temperature Tin
δT
ro
Thermal entry region
r
Fully developed region
xfd,t x Fully developed
Thermal
Laminar Thermal Entry Length x fd ,t ≈ 0.05 Re⋅ Pr
Turbulent Entry Length x fd ,t d
≈ 10
Fully developed thermal region
Comparison When Pr > 1,
x fd ,h < x fd ,t
When Pr < 1,
x fd ,h > x fd ,t
When Pr >100,
x fd ,h << x fd ,t
∂ Ts ( x ) − T (r , x ) =0 ∂x Ts ( x ) − Tm ( x )
2