heat transfeer conduction two three dimensions
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CONDUCCION EN DOS Y TRES DIMENSIONES
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CONDICIONES DE CONTORNO
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BOUNDARY CONDICIONS CONSTANTS
Thus, the quantities Cn, sinh (nX/L) must be the coefficients of the Fourier
sine series for f(x) in the interval 0
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Principle of Superposition
The linearity of the Laplace equation requires that a linear combination of solutions is
itself a solution; this is the principle of superposition. A problem having more than
one non homogeneous boundary condition can be resolved into a set of simpler
problems each with the physical geometry of the original problem and each having
only one non homogeneous boundary condition. The solutions to the simpler
problems can be superposed (at the geometric point being considered) to yield the
solution to the original problem.
EXAMPLE
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NON HOMOGENOUS BOUDARY CONDITIONS
Determine the temperature at the (1/4, 1/4)
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CONDUCTIVE SHAPE FACTOR
The figure represents a heated pipe with a thick layer of insulation. The inner surface of
the insulation is at uniform temperature T1, the outer surface is at uniform temperature To,
and there is a resulting outward heat flux for Ti > To. Constructing uniformly spaced lines
perpendicular to the isotherms results in a group of heat flow lanes. In Fig. there are four
such lanes in the quadrant selected for study, and the other three quadrants would be similar
due to the problem symmetry. If we can determine the rate of heat transfer for a single
lane, then we can easily find the total. Note that there is no heat transfer across one of the
radial lines, such as line a-6, because there is no angular temperature gradient.
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Techniques for freehand plotting include:
1. Identify all known isotherms.
2. Apply symmetry (geometrical and thermal) to reduce the art work.
3. Begin, if possible, in a region where the adiabatics can be uniformly spaced.
4. Begin with a crude network sketch to find the approximate locations of isotherms
and adiabatics.
5. Continuously modify the network by maintaining adiabatic lines normal to
isothermal lines while forming curvilinear squares.
Freehand Plotting
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Electrical Analog
Electrical Analog
NUMERICAL ANALYSIS
Consider a general two-dimensional body as shown in Fig. 3-6. The body
has uniform thickness L in the z-direction and no temperature gradient in
that direction. Choosing an appropriate Ax and Ay, the body is dividedinto a network of rectangles, each containing a single nodal point at
its center. It is convenient to consider the heat transfer as occurring
between nodal points only, these being connected by fictitious rods
acting as conductors resistors for the heat flow. Thermal energy is
considered to be stored at the nodal points only. The horizontal and
vertical conductance are given by
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C t S l ti
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Computer Solution
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R l ti T h i
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Determine the steady state temperatures
at the four interior nodal points of Fig. 3-9.
The nodal equations, obtained with the aid
of (3.14),are
The nodal equations, obtained
Relaxation Technique
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which comprise a set of four linear algebraic equations containing the four
unknown nodal temperatures. The
relaxat ion method of solu t ion proc eeds as fo l low s:
1. Assume (guess) values for the four unknown temperatures. Goodinitial guesses help to minimize the ensuing work.
2. Since the initial guesses will usually be in error, the right side of each
nodal equation will differ from zero; a residual wil l exist due to
inaccu racies in the assumed values. Cons equent ly, we replace the
zeros in equations (I) thr ough (4)w ith RI,R2,R3,and R4,respectively :
3. Set up a unit change table such as Table 3-2, which shows the effectof a one-degree change of temperature at one node upon the residuals.
The fact that a block (overall) unit change has the same effect upon all
residuals is unusual, this being due to the overall problem symmetry.
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4. Calculate the initial residuals for the initially assumed temperatures using the
residual equations (5) through (8).
5. Set up a relaxat ion table such as Table 3-3. Begin with the in i t ia lly
assum ed temperatures and the result ing initial residuals. The left-hand column
records the changes from the initially assumed temperature values.
Notice that the procedure begins by relaxing the largest initial residual (or
perhaps by making a block change, a technique useful when all residuals are of
the same sign).
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the present problem, we should begin by reducing R2 or R3. Arbitrari ly choose R2
and proceed by over-relaxing slightly. At this point the convenience afforded by Table
3-2 becomes evident; this facilitates rapid calculation of the changes in the residuals
without recourse to the equations. Notice that the +20change in T, reduced the
residuals at nodes 1 and 2 but unfortunately increased R3.
The first row in Table 3-3 shows the new residuals and temperatures; the only
temperature changed is underlined. Proceeding, we next relax the largest resulting
residual, this being R3.Following a temperature change of +25 at node 3, we seethatR4=0. This does not necessari ly mean that we have obtained the correcttemperature at node 4,but rather that the set of as yet incorrect temperature
values happens to satisfy eq. (4) exactly. Proceeding, the largest residual is now
R2,which is reduced to 0 by a +5 change in T,. This also reduces all remaining
residuals to zero. A check is made by substituting the temperatures thus obtained
into eqs. (I) through (4);thi s ver i f ies the solution.
GaussSeidel Method
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GaussSeidel Method
To illustrate this very popular method of solution of a set of nodal equations,
return to the figure, and associated temperature nodal equations (1), (2),
(3),and (4).Namin g the s et of equations (3.26a) we have
Next, we rearrange these equations to have the unknown temperature at
each node to appear on one side of the equation alone and with the
coefficient +l. This is done by solving the first equation in (3.16a)for T,, the
second for T2,and so forth, yielding (3.16b).
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Proceeding to solve (3.166)with the Gauss-Seidel method, an initial set of
temperatures T1 throughT4 is assumed. Obviously, reasonablechoices h ere wil l faci l i tate the solu t ion, and the temperatures must
be bounded by 200 C and 500 C. Choosing Tl = 450 C, T2= 350, T3=
250, and T, = 350, all in "C,is a reasonable gu ess. We next in sert
these T2and T4values in the r ight s ide of the f irst equat ion
of (3.16b) and calculate a new estimate of Tl, viz.
Proceeding to calculate new estimates of T2, T3,and T4, always us ing
the newest value avai lable for each temperature, yields (3.I6d).
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At this point we have completed one iteration. To proceed, we next use
the newest temperature values from set (3.16d)together with the
solution set (3.I6b) to calculate the next iteration set, always using
the newest T value available. Thus, to calculate a new T,, defined in
set (3.I6b), we use the T2and T4 values from (3.26d),obtaining
Again, proceeding to calculate new estimates for T2, T,, and T4,
a lways using the newest value available for each temperature,
yields (3.16e).
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The next (third) iteration through the set of equations yields
and the next (fourth) iteration yields
All temperatures are in "C. At this point we question the value of additional
iterations. Usually, temperature values within 5 a few per cent accuracy are
suitable for engineering calculations. If we use m as a superscr ip t todenote the previous iteration and nz + 1 to identify the iteration just
completed, a computer program could use a test such as
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