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Design and Optimization of Thermal Systems Episode 1 Part 8 doc
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Modeling of Thermal Systems 147
a set of simultaneous ordinary differential equations arise. For instance, the temperatures T1, T2, T3,z, Tn of n components of a given system are governed by a
system of equations of the form
dT
d FTT T T,
dT
d F T T ,T
n
1
2
T
T
T
1123
212 3
(, ,, , )
( ,
, , )
(, , , , ) 123
"
T ,
dT
d F T T T T,
n
n
n n
T
T T
(3.15)
where the F’s are functions of the temperatures and thus couple the equations.
These equations can be solved numerically to yield the temperatures of the various components as functions of time T (see Example 2.6).
Partial differential equations are obtained for distributed models. Thus, Equation (3.4) is the applicable energy equation for three-dimensional, steady conduction in a material with constant properties. Similarly, one-dimensional transient
conduction in a wall, which is large in the other two dimensions, is governed by
the equation
R
T
C T
x
k T
x
t
t t
t
t
t
¤
¦
¥
³
µ
´ (3.16)
if the material properties are taken as variable. For constant properties, the equation becomes
t
t t
t
T T
T x
A 2
2
(3.17)
where A k/RC is the thermal diffusivity. Similarly, equations for two- and threedimensional cases may be written. For convective transport, the energy equation
is written for a two-dimensional, constant property, transient problem, with negligible viscous dissipation and pressure work, as
R
T
C T
u
T
x
v
T
y
k T
x
T
y p
t
t
t
t
t
t
¤
¦
¥
³
µ
´ t
t
t
t
¤
¦
¥
2
2
2
2
³
µ
´
(3.18)
where Cp is the specific heat of the fluid at constant pressure and u and v are the
velocity components in the x and y directions, respectively. Partial differential
148 Design and Optimization of Thermal Systems
equations that govern most practical thermal systems are amenable to a solution
by analytical methods in very few cases and numerical methods are generally
necessary. Finite-difference and finite-element methods are the most commonly
employed techniques for partial differential equations. Ordinary differential
equations can often be solved analytically, particularly if the equation is linear.
The integral formulation is based on an integral statement of the conservation
laws and may be applied to a small finite region, from which the finite-element
and finite volume methods are derived, or to the entire domain. For instance,
conduction in a given region is governed by the integral equation
R
T
C T dV k T
n p dS q dV VS V
t
t t
t ``` ¯¯ ¯ (3.19)
where V is the volume of the region, A is its surface area, q``` is an energy source
per unit volume in the region, and n is the outward drawn normal to the surface.
This integral equation states that the rate of net energy generated in the region
plus the rate of net heat conducted in the region at the surfaces equals the rate of
increase in stored thermal energy in the region. Similar equations may be derived
for convection in a given domain. Radiative transport often leads to integral
equations because energy is absorbed over the volume of a participating fluid or
material. In addition, the total radiative transport, in general, involves integrals
over the area, wavelength, and solid angle. Figure 3.13 shows a few examples of
integral and differential formulations for the mathematical modeling of thermal
systems.
Further Simplification of Governing Equations
After the governing equations are assembled, along with the relevant boundary
conditions, employing the various approximations and idealizations outlined
here, further simplification can sometimes be obtained by a consideration of the
various terms in the equations to determine if any of them are negligible. This
is generally based on a nondimensionalization of the governing equations and
evaluation of the governing parameters, as given earlier in Equation (3.6). For
instance, cooling of an infinite heated rod moving continuously at speed U along
the axial direction x [Figure 1.10(d) and Figure 3.6(a)] is governed by the dimensionless equation
t
t `
t
t Q
T
Q Pe Q
X
2 (3.20)
where 2 is the Laplacian operator in cylindrical coordinates, nondimensionalized by the rod diameter D, and the Peclet number Pe is given by Pe UD/A.
The dimensionless temperature Q is defined as Q T/Tref, where the reference
temperature Tref may be the temperature at x 0. Also, dimensionless time T` is