Int. Comm. Hat
Pergamon
Mass Transfec Vol. 28, No. 6. pp. 847-856, 2001 Copyright 0 2001 Elsevier Sctence Ltd Printed m the USA All rights reserved 0735.1933/01/$-see front matter
PII: SO7351933(01)00288-3
NUMERICAL METHOD FOR HYPERBOLIC INVERSE HEAT CONDUCTION
PROBLEMS
H.T.Chen, S.Y. Peng,P.C.Yang National Cheng Kung University Department of Mechanical Engineering Tainan, Taiwan 701, R.O.C. L.C. Fang Chinese Military Academy Fengshan, Kaohsiung Taiwan 830. R.O.C.
by K. Suzuki and S. Nishio)
(Communicated ABSTRACT
The Laplace transform technrque and control volume method III conjunction \vlth the hyperbolic shape function and least-squares scheme are applied to estimate the unknown surface condltlons of one-dImensIonal hyperbolic Inverse heat conduction problems In the present study. the expressIon of the unknown surface condltlons IS not given a prIorI To obtam the more accurate estimates. the whole time domam IS dlvlded mto several anal!.sls sub-time Intervals .4fterward. the unknown surface condltlons In each analysis Interval are estimated To evidence the accuracy of the present method. a comparison betn-ten the present estlmatlons and exact results IS made Results show that good estlmatlons on the unknown surface condltlons can be obtained from the transient temperature recordings onI> at one selected locatlon even for the cases with measurement errors 0 2001 Elsevier Science Ltd Introduction The Inverse lnltlal
condltlons
InsIde
the material
measurements surface known
problems
lnvolvmg
the estlmatlon
as well as thermal
propertles
of a body
are
condltlons
have
various
fxst
fltted
appllcatlons and
then
may be estunated
from these
short the
period
of time
circumstances.
thermal
wa\c
methods
ha\ c been developed
will
become
the
or for ver!
curve-fltted
with
the
dominant
To
date.
finite
condltlons
These temperature
various
and
measurements
near
or
temperatures
quantltles
unkno\vn It IS ~211
heat flow absolute
propagation
of the parabolic 847
fields
for the transient
10~ temperatures
theory
for the analysis
physlcal
down
of surface
from measured
In engmeerlng
unknown
that the classIcal Fourier’s model can break
extremcl! Under
thermal
analytlcal znverse
In an
zero
[I ]
velocity
of
the
and
numerlcal
heat conductlon
848
H.T. Chen et al.
problem
(IHCP)
temperatures
mvolvtng
mslde
the
csttmation
the material knowledge,
there
IHCP
non-Fourter
heat
observed
on the
from Refs. [6. 71 that there
and tnteractlon problems
feature
surface
condtttons Fourrer’s
IS no report
of such
flux
tn the
model
can exist
tn the numertcal
Thus the hyperboltc
of
based on the classical
best of the authors’ based
Vol. 28, No. 6
the sharp
solutton
IHCP IS more
from
model
a study open
of the
[2-j]
To the
for the hyperbolic
literatures
drsconttnutty.
difficult
measured
It can
reflection
hvperboltc
heat
to be solved
be
feature
conductton
than the paraboltc
IHCP It can be found
Ref
by the frntte-difference an optimum
approsrmatton
combtnatlon
numerical
solutton
transform
techntque
of the ttme
one-dimenstonal
m
errors
concept
dtmenstonal
IHCP
Chen
the Laplace
transform function
present
study
applies
concept
to estimate
present
to
using
the
size
applied
the
same
the unknown
or uncertainty
the hyperbolic technique surface
In conJunction
on the estimation
of the unknown
surface
condtttons
of the
surface wrthout
scheme
the hybrid
wtth
appltcatton
problems
with
a
III two-
in conJunctron
of
wtth a Thus.
the
a sequential-In-time
of the present
measurements,
control
temperature
heat conductron
condittons
of the temperature
stmtlar
method
exists
of the Laplace
the unknown
surface
volume
there
temperatures
the
and Ltn [6. 71 have ever developed
to analyze
method
to estimate
unknown
and the control
for error
measured
[j]
the ttme dertvattve
In general,
the hybrtd
method
et al.
estimate
technique
shape
errors
Chen
data
errors
and the mesh [4] applied
IHCP
Recently.
sequenttal-tn-ttme
the error
step
and the fintte-difference
temperature
measurement
can lead to large
Thus Chen and Chang
measurement
suitable
[3] that for “notsy”
problem
the effect 1s also
Owmg
to
of measurement
tnvesttgated
in the
analysis Mathematical Formulation The hyperboltc
be written
heat
equation
wtth
constant
thermal
properttes
can
as [I, 61:
8T’ ~-+-=~(g2 where
conductton
x’ and t’ respectively
ttme assumed
to be constant.
i?T’
d’T*
at*
ax**
denote
the spatial
a is the thermal
(1) coordinate diffusivtty.
and time Formally,
r ts a relaxatton the sttuation
for r
Vol. 28, No. 6
-
0 leads
HYPERBOLIC INVERSE HEAT CONDUCTION
to tnstantaneous
dtffusron
with the classical
thermal
For convcntcnce
of numertcal
defined
as
where
c = (dry”
dlmenslonless
at infinite
dtffuston
1s the
the followtng
propagation
speed
form ofEq. (I) can be written
with the drmenstonless
boundary T= F,(t)
d’T T-Y
condttlons or
of
Q, = --
discrete
temperature
thermocouple = I.
measurements
temperature
the
htstory
practtcal
osctllations Tr
owing
obtained
the dtrect
applications,
number
of the
small
random
can be expressed
w represents
0 05 tn the present
the averaged study
condttlons
the addltronal
ttme
history t,
discrete
informatron taken
IS denoted
of
from the
by T,“‘“. m
measurement
times
The
as
at x=x,
Thus,
errors
(7)
profiles
often
the simulated
to the exact
exhibit
data
value
from
m = 1.
,M
random
of measurements the solutton
of
as Tr=
where
(3)
(6)
can be expressed
measured
errors
t,
(3
The temperature
at x =x,
actual
to measurement
by adding
problem
the
the
= 0
T= T,(t) In
Thus.
at s=l
dtmenstonless
T,(t)
are
at x=0
= F,(t) f% IX=”
F,(t) or F,(t).
specific
wave
mtttal
IS required
A4 denotes
cornctdes
parameters
thermal
and dlmenstonless
g(O,x)
functtons
at the successtve
. Ad.where
dtmenstonless
the unknown
the
I. o
aT 0
T(O.x)=O.
dtmenstonless
,n 05x<
-= 3X
To estimate
whtch
as
+,r3T -x=
dt’
velocity
849
theory
analysts,
d’-r
propagation
PROBLEMS
random
The polynomtal
T:=(I error
+a),
and IS assumed
function
IS often
to be within
used to approximate
(8) -0.05
to
these
850
H.T. Chen et al.
measured
temperatures
standard respect
del,ratrons
usmg
the
least-squares
of the measured
to the exact
Vol. 28, No. 6
scheme
temperatures
[S]
cr,,,r and
and calculated
CT,~ are
temperatures
transform
of Eqs
(3)-(j)
A4
0, = i!:(s)
dT -_=O dx .Y IS the Laplace
1’ =s’+
transform
T(x,s)
2s and
=
It IS easy to obtarn
cT(x,
at x = 0
(11)
at x=1
parameter.
The
(1-a
parameter
1’ and
T are defined as
t)e-“dt
the drscretrzed
T!_,- 2cosh(he)?,
form of Eqs
(lo)-(
+?*,, = 0 i
T, = F,(s)
or
12) as
i=l.2,
(13)
.n
;I -T
-AiL=F2(s)
(14)
21
T”_,= T”+I where
n denotes
the number
The rearrangement
where
drmensronless Gaussran
nodal
elrmlnatron
are applred
to invert
temperatures algorrthm
divided
Into some
the followrng
( 7 ; IS an n xl
matrix,
In the
and the numerical
analysrs
functron ranges.
and inversron
equation
representmg (f}
IS an II xl of Laplace
the
unknown
matrix.
The
transform
[9]
domarn
F,(t) or F,(t), where
vector-matrix
matrix
s domain
T to that rn the physrcal
To fit the unknown
(13
of nodes
of Eqs. (Id)-( 16) gives
IS an nxn
[k]
(9)
IS
T = F,(s)or
where
~rth
data [8]
m = 1, The Laplace
the
the whole
t, IS the rnrtial
time
domarn
measurement
t, It St, is time
In other
Vol. 28, No. 6
words,
HYPERBOLIC INVERSE HEAT CONDUCTION PROBLEMS
a sequential-in-time
conditions
Owing
procedure
IS introduced
to the application
IS not alwa! s the initial
time
of the Laplace
Assume
that time
2.
interval
F,(t) or F:(t) on each
approximated
analysis
by a polynomial
and can be e\rpressed
series
transform
the dimensionless
At, IS At, = Ct; - t,, )/M The discrete .M
to estimate
coordinate
t,
t, It
of time before
the unknown
851
surface
in the present
stud!-.
measurement
time
t,, step
IS t,,, = t,, + m At,. m = I.
< t,_,_,,
I = 0. N-2. 2(N-2).
performing
the inverse
can be
calculation
as N
F,(t)
xC,t'-'
=
F,(t) = .$)z$-’
or
where
C, IS the unknown
N denotes
the degree
squares
of
the
temperature E(C!,C,,
coefficient
and is estimated
of the polynomial
The least-squares
technrque
between
measurements
taken
using
the least-squares
method
series
mmimization
deviations
117)
t-1
,=I
the
from
IS applied
calculated
the
to minimize
temperatures
thermocouple
the sum of the and
The error
curve-fitted
m the estimates
,C,)
(18) o-1
is to be
minimized
measurements. value
The estimated
of E( C,,C,,
procedures
T,‘:, IS obtamcd
,C,)
for estimating
from
values
the
of C,,
IS minimum
J
=
curve-fitted 1, 2,
The detailed
C, can refer
to Ref
profile
of
, N, are determined
description
of the
temperature until
the
computational
[7]
Results and Discussion The present
numerical
results
are obtained
N = 8, n = I I and B = 0 1 The initial Example First.
I:
Dtrichlet
the Dirichlet
boundary boundary
guess
by using
of {C,,C,,.
t, = 1, t, = 8. At, = 1, M = I, ,C,)
is { I, I,
1)
condttron
condition
IS considered
0(0, t) = sin(t)
as:
(I’))
852
H.T. Chen et al.
Table
1 shows
the estrmatton
at x, = 0 5 and obtained
from
1 0 wrth
of Table
I
non-Fourrer
heat
model
for0
the paruboltc
respect
to u,,
flux
It can be seen
the estimated
1 t 1
of the surface temperature T(0. t) usrng = 0 and
tr
results
This rmpltes
IHCP
slrghtly for
the present from
that the hyperbolic
Thus discrepancy
rn the solutron
1 also shows
T-method
and IS 0 0072 for the Qr -method
of the hyperbolrc
0 008 ts 0 0219 for the T-method
and IS 0.021
the present
behavior
cstrmates
exhrbtt
stable
Comparison
1(0.6527)1
I(0 6499)l
value
for the
for varrous
estrmates
obtained
In the
from
the
for short
trmes
wrth the exact
results
dtfficult
to solve
than
of the Jump drscontrnurtv. heat conductton
problem
[6,
= 0 0075 IS 0 014 for the
at x, = 1 w& respect to b,r Qr-method
This
cr,r values
TABLE I of T(0, t) for Example
1(0.6538)1
present
results
IS more
o,r at x,= 0 5 wnh respect to cr,r The u,,
The
estimates
agreement
IHCP
T- and Qr-methods
~,,,r = 0 are Itsted
can be to the exrstence
71 Table
I
f 0
the exact
T = 0 are rn good
and rnteractron
that
that
devrate
reflectton
I
o,,
the classrcal Fourrer heat flux model ( s = 0) for
parentheses
However.
Vol. 28, No. 6
1
\(0.6505)1
rmplres
=
that
Example
853
HYPERBOLIC INVERSE HEAT CONDUCTION PROBLEMS
Vol. 28, No. 6
Neumann
2:
The unknown
boundary
boundary
condition
condition
of the second aT
--
example
IS assumed
as
= sm( t)
(20)
ax <=” It can be seen loom Table 2 that the present exact
for I i
solution
surface
Ho\\ever.
than those
using
estimates
t S 7 even though
the estimated the T-method
results Results
Thus
method
approslmatlon
ImplIes
the sensor usmg
The
Mixed
mixed
applied
the accuracy
to estimate
the
to be more
accurate
ocT. at x5 = 0 5 with respect to g’mT The Gus value
at
that
can
the
present
hybrid
temperatures
unknown
provide
with the measurement
the
good
error
2
condition
condition
of the
method
TABLE 2 of T(0, t) forExample
in this
example
-- ZT = Isx x:0 To improve
seem
and IS 0 09 I for the Q, -
boundary
boundary
with the
= 0 0054 IS 0 0 17 for the T-method
even for the measured
3:
that
agree
1s far from the estimated
and IS 0 0086 for the T-method
Comparison
Example
locatlon
the Q,--method
also show
= 0 0055 IS 0 0139 for the Q,-method x5 = I \h~rhrespect to 6,,
usmg T- and Q, -methods
present surface
IS assumed
as
T(0, t)
estimates, temperature
(21) N = 3, N = 4 and T(0,
t) using
N = 5 are
the T-method,
854
H.T. Chen et al.
as shown m Table 3 Table
3 shows
that
increasing
of N
However,
In the
expected
beyond
observed
that
result
IN = 8 A suitable the
estimates
I shows
FIN
present
value
estimates
show
that
the
Other
different
such as (C,,C,,. agree
estimated
results
the estimated the
value
values
present
hybrid
method
sets
of the mltlal
well
with
are not
of the lnltlal
has
guesses
good
the estimates
using
shown
manuscript
m this
guesses
.,08}
{C,,C,,...,C,)={
on the estimates
The
T(0.
I. 1.
foregoing
IS not slgnlflcant
be
exact
and
the
I and FIN
good
Results
the
result
Table
to predict
, 0 5) and {O 8. 0.8,
It can
with
and
is not
4-6
exact
o’mr = 0
accuracy
are applied
range
the
with
estimates
agreement
t) between
for N = 5, x, = 0 5, At, = 0 5 and
of
In the
In good
of T(0,
can be Improved
improvement
of N seems
N = 5 are
comparison
.,C,} = (0 5, 0 5.
estimates
that the effect
the
for
Vol. 28, No. 6
1
rellabllrty t) for N = 8,
show
, I}
that their Thus.
statement
their shows
for the present
method.
Comparison
TABLE 3 of T(0, t) for Example
and various
N values
using
3, crmr=O, x, = 0 5
the T-method
Conclusions The accurate estimates for the Inverse hyperbolic heat conduction problems are obtained by ustng a hybnd application of the Laplace transform technique and the control volume method m conjunction with a hyperbolic shape function
The main difficulty in solvmg the Lnverse hyperbohc heat conduction
problems 1s that there emst the phenomena of jump discontinuity,
reflection and interaction. It is seen
from three different examples that the stab&y and accuracy of the es&mated results for various boundary
HYPERBOLIC INVERSE HEAT CONDUCTION PROBLEMS
Vol. 28, No. 6
conditions are good to compare with the exact result. Hence, the proposed numerical method IS efficient and applicable for solvmg the inverse hyperbolic heat conduction problems
FIG. I Comparison of T(0, t) Between the Present Estimates and Exact Results for Example 3,N=5. x, = 0 5 and b,,,r = 0
Nomenclature
e
distance
Qi
temperature
T
dimensionless
temperature
t!
dimensionless
final time
dimensionless
measurement
4
between
two neighboring
nodes
gradient in the transform
domain
time step
I
measurement
X,
location References
1
W W Yuan and S C Lee. J Heat Transfer
2
M N
3
J Taler.
4
H T Chen and S.M
Gzisik.
Heat Conduction.
Heat and Mass Transfer Chang,
Int
Chap
I1 1, 178 (1989)
14 Wylie,
New York (1993)
3 I, 105 (1996) J Heat Mass
Transfer
33, 621 (1990)
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856
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5
H T Chen.
6
H.T Chen and J Y Lm, Int
7
H.T Chen and J Y Lm, Int. J Heat Mass Transfer
8
JP Holman and WI GaJda. Jr McGraw-Hill, New York (19X9)
9.
G. HomgandU.
S Y Lln and L.C
H1rdes.J
J
Fang,
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Int. J. Heat Mass Transfer
Heat Mass Transfer
Comput
36.2891 (1993). 37, 153 (1994).
ExperImental
Appl.
Math
44, 1455 (2001)
Methods
for
Engineers.
p
37
IO. 113 (1984)
Received June I, 2001