determination of continuous relaxation spectrum based on
TRANSCRIPT
© 2017 The Korean Society of Rheology and Springer 115
Korea-Australia Rheology Journal, 29(2), 115-127 (May 2017)DOI: 10.1007/s13367-017-0013-3
www.springer.com/13367
pISSN 1226-119X eISSN 2093-7660
Determination of continuous relaxation spectrum based on the Fuoss-Kirkwood relation
and logarithmic orthogonal power-series approximation
Sang Hun Lee1, Jung-Eun Bae
2 and Kwang Soo Cho
1,*1Department of Polymer Science and Engineering, School of Applied Chemical Engineering,
Kyungpook National University, Daegu 41566, Republic of Korea2Research Center, LG Household & Health Care, Daejeon 34114, Republic of Korea
(Received January 13, 2017; final revision received March 2, 2017; accepted March 27, 2017)
In this study, we suggest a new algorithm for inferring continuous spectrum from dynamic moduli data. Thealgorithm is based on the Fuoss-Kirkwood relation (Fuoss and Kirkwood, 1941) and logarithmic power-series approximation. The Fuoss-Kirkwood relation denotes the existence of the uniqueness of continuousspectrum. If we know the exact equation of dynamic moduli, then continuous spectrum can be inferreduniquely. We used the Chebyshev polynomials of the first kind to approximate dynamic moduli data in dou-ble-logarithmic scale. After the approximation, a spectrum equation can be derived by use of the complexdecomposition method and the Fuoss-Kirkwood relation. We tested our algorithm to both simulated andexperimental data of dynamic moduli and compared our result with those obtained from other methods suchas the fixed-point iteration (Cho and Park, 2013) and cubic Hermite spline (Stadler and Bailly, 2009).
Keywords: continuous relaxation spectrum, linear viscoelasticity, Chebyshev polynomials, Fuoss-Kirkwood
relation, power-series approximation
1. Introduction
In the theory of linear viscoelasticity, relaxation spec-
trum is one of the most important viscoelastic functions. It
is because most of other viscoelastic functions can be cal-
culated from relaxation spectrum and it helps us to under-
stand relaxation mechanisms of materials.
One of such efforts is to find the molecular weight scal-
ing for rheological parameters. Bae and Cho (2015) showed
that quadratic mixing rule is suitable to predict relaxation
modulus for polymer blends. They used continuous relax-
ation spectra to calculate relaxation moduli of mono-
disperse polymers and their blends. Furthermore, they
showed that continuous relaxation spectrum can be used
for the interconversion of linear viscoelastic data which
are measured by the optical measurements of Brownian
particles in the viscoelastic medium (Mason and Weitz,
1995).
However, relaxation spectrum is a hypothetical quantity
which cannot be measured directly. It should be calculated
from other measurable viscoelastic functions. Further-
more, it is a representative ill-posed problem in rheology.
It is because errors in experimental data are apt to be mag-
nified in determined relaxation spectrum (Honerkamp,
1989). It implies that relaxation spectrum has better res-
olution to errors than those of other measurable viscoelas-
tic functions. In the viewpoint of developing molecular
models, this property can be applied to verify their accu-
racy as an acid test.
There are two types of relaxation spectra: discrete and
continuous relaxation spectra (Ferry, 1980). Discrete relax-
ation spectrum is made up of finite relaxation times and
the corresponding relaxation strengths (Baumgärtel and
Winter, 1989). Continuous relaxation spectrum is the
extended version of discrete relaxation spectrum. It con-
tains the infinitesimal contributions of infinite relaxation
times.
There has been a doubt about the uniqueness of relax-
ation spectrum because of the ill-posedness. Malkin and
Masalova (2001) reported that discrete relaxation spec-
trum cannot be determined uniquely. It is because discrete
relaxation spectrum can be differed by any number of
relaxation times.
However, the physically correct meaning of relaxation
spectrum is a continuous function from vanishing times to
a certain terminal relaxation time (Stadler and Bailly,
2009). It denotes that there should be existing only one
continuous relaxation spectrum from the perspective of
physics. This was proven by Fuoss and Kirkwood (1941).
They derived the mathematical relation (the FK relation)
between continuous relaxation spectrum and loss modulus
using inverse Fourier transform and convolution theorem.
There have been a number of noteworthy algorithms
developed by researchers. Baumgärtel and Winter (1989)
developed an algorithm called “IRIS”. IRIS calculates the
“parsimonious” discrete relaxation spectrum based on
nonlinear regression. Cho (2010) suggested an algorithm
determining discrete relaxation spectrum based on the
wavelet transform. It provides a way of determining the*Corresponding author; E-mail: [email protected]
Sang Hun Lee, Jung-Eun Bae and Kwang Soo Cho
116 Korea-Australia Rheology J., 29(2), 2017
number of relaxation times as well as the arrangement of
the relaxation times.
Although it can be a convenient way to determine con-
tinuous relaxation spectrum using the FK relation, it must
be considered both the radius of convergence and branch
cut problem. It is because the FK relation is made up of
complex variable and it is hard to know the exact equation
of loss modulus (Davies and Anderssen, 1997). Instead,
most of the researchers focused on the development of
algorithms using the least-square method of continuous
relaxation spectrum itself.
Honerkamp and Weese (1993) developed an algorithm
based on Tikhonov regularization with nonlinear regres-
sion (NLRG). Although regularization method allows to
select the best fit of given experimental data and prevents
over-fitting the data, NLRG smoothens edges of deter-
mined continuous relaxation spectrum unnecessarily. Roths
et al. (2000) suggested a revised algorithm of Honerkamp
and Weese (1993) with preserving edges of continuous
relaxation spectrum. However, determined continuous
relaxation spectrum shows discontinuous slope which may
be assumed an artifact in double-logarithmic scale. Stadler
and Bailly (2009) developed an iterative algorithm based
on the cubic Hermite spline with regularization method
(CHS). Although CHS shows the remarkable result with
experimental data of PBd-430k (Stadler and van Ruym-
beke 2010), it requires several hours to maximize the pre-
cision of determined continuous relaxation spectrum. Cho
and Park (2013) developed a remarkable iterative algo-
rithm with fast computation time with a precision called
fixed-point iteration (FPI). McDougall et al. (2014) exam-
ined algorithms of CHS, NLRG, and FPI on the same data.
They showed that three algorithms give nearly identical
continuous relaxation spectra. This supports the unique-
ness of determined continuous relaxation spectra from
these algorithms indirectly.
On the other hand, some algorithms are based on the
least-square approximation of dynamic moduli. Cho (2013)
suggested an algorithm based on the power series approx-
imation of dynamic moduli data. The method converts the
coefficients of dynamic moduli to those of continuous
relaxation spectrum. As mentioned above, Bae and Cho
(2015) developed an iterative algorithm based on cubic B-
spline with Levenverg-Marquardt method (BLM). BLM
can be applicable not only to dynamic moduli but also to
the Laplace transform of relaxation modulus by changing
its kernel function.
It has been appeared recently application of the FK rela-
tion to determine continuous relaxation spectrum. Anders-
sen et al. (2015) suggested a derivative-based algorithm
using the FK relation and Gureyev iteration. They derived
ordinary differential equation from the FK relation. How-
ever, the algorithm contains multiple convolution proce-
dures, it demands a number of computation time to calculate
thousands of numerical integrations.
In this study, we suggest a new algorithm for determin-
ing continuous relaxation spectrum from dynamic moduli.
Similar with the algorithm of Anderssen et al. (2015), this
method is based on the FK relation and series approxi-
mation. However, this method is not an iterative method.
If the coefficients of dynamic moduli are calculated by
power series approximation, then the continuous relax-
ation spectrum is readily determined. It is only affected by
the precision of curve fitting result to the accuracy of
determined continuous relaxation spectrum. In other words,
the better fit of dynamic moduli, the more precise contin-
uous relaxation spectrum will be determined. This algo-
rithm was tested for simulated data and experimental data
in order to verify the capability of this algorithm.
2. Theoretical Background
2.1. Relaxation spectrumStress relaxation is measuring the stress response of
materials under the certain unit step exertion of strain.
There have been efforts to explain stress relaxation mech-
anisms of materials quantitatively by the models of spring
and dashpot (Ferry, 1980). Generalized Maxwell model is
the most representative one of such models. It consists of
a parallel connection of a finite number of Maxwell mod-
els with different relaxation times and its corresponding
relaxation strengths. Relaxation modulus of the model can
be expressed as the following equation with M relaxation
times.
(1)
where λk and hk are the relaxation time and strength of kth
Maxwell component, respectively. Eq. (1) implies that a
group of relaxation times and corresponding strengths has
a distribution of discrete form. This distribution is called
discrete relaxation spectrum.
If the number of Maxwell elements in Eq. (1) is
increased without limit, then the distribution will be a con-
tinuous function with infinitesimal contributions of each
relaxation time. Therefore, Eq. (1) can be written in the
form of integral equation as follows:
(2)
where H(λ) is continuous relaxation spectrum.
Complex modulus is defined as
(3)
where denotes the Laplace transform of relaxation
modulus, i is the imaginary unit such that , and ω is
the angular frequency.
Dynamic moduli are the real and imaginary parts of
G t( ) = k 1=
M
∑ hk expt
λk
-----–⎝ ⎠⎛ ⎞
G t( ) = ∞–
∞
∫ H λ( )expt
λ---–⎝ ⎠
⎛ ⎞d logλ
G*ω( ) = sG̃ s( )
s=iω = iωG̃ iω( )
G̃ s( )1–
Determination of continuous relaxation spectrum based on the Fuoss-Kirkwood relation and logarithmic orthogonal.....
Korea-Australia Rheology J., 29(2), 2017 117
complex modulus such that
(4)
where and are storage and loss moduli,
respectively. Storage and loss moduli can be expressed in
terms of continuous relaxation spectrum with the help of
Eqs. (2)-(4) as follows:
;
. (5)
Eqs. (2) and (5) denote that H(λ) allows us to intercon-
vert between dynamic moduli and relaxation modulus.
However, it is difficult to measure relaxation modulus
precisely due to the hardware limitation of exerting unit
step function of strain to the specimen. It is impossible to
reproduce initial part of the unit step strain by machine.
Most of researchers prefer to measure dynamic moduli
from oscillatory experiment.
2.2. The Fuoss-Kirkwood relationFuoss and Kirkwood (1941) derived the valuable rela-
tion between continuous relaxation spectrum and loss
modulus. Davies and Anderssen (1997) generalized defi-
nition of the FK relation to storage modulus as follows:
(6)
where Re[…] and Im[…] are equal to the real and imag-
inary parts of complex function, respectively.
Eq. (6) can be derived from Eq. (5) with the convolution
theorem of the Fourier transform. Eq. (6) implies the exis-
tence of the uniqueness of continuous relaxation spectrum.
It is because Fourier transform pairs are uniquely defined
for any continuous function (Boas, 2006).
However, Davies et al. (2016) suggested that the correct
expression of the FK relation has to be the following
equation.
(7)
where ε is an arbitrary real number and 0 < ε << 1.
Note that Eq. (7) includes limit process in contrast to Eq.
(6). Simple replacement of ω by iω gives sometimes use-
less results. As an example, consider loss modulus of the
Maxwell model.
. (8)
Applying Eq. (6) to Eq. (8) gives
. (9)
However, applying Eq. (7) to (8) gives
. (10)
Note that
; . (11)
Then Eq. (10) becomes
. (12)
By the definition of the Dirac delta function, λω is 1.
Then Eq. (12) can be written as
. (13)
Eq. (13) confirms that the relaxation spectrum of Max-
well model with modulus of unity is the Dirac delta func-
tion of λ = 1/ω. It satisfies the physical meaning of
relaxation spectrum. As mentioned in section 2.1, contin-
uous spectrum consists of infinitesimal contributions of
infinite relaxation times. However, simple substitution of
Eq. (6) often happens to give the same result of Eq. (7) for
some functions such as the extended Cole-Cole model
suggested by Marin and Graessley (1977). In spite of that,
we will employ Eq. (7) in developing an algorithm accord-
ing to the correct expression of the FK relation.
2.3. Ill-posedness of inferring relaxation spectrumIt is well-known that inferring relaxation spectrum from
dynamic moduli data is an ill-posed problem (Honerkamp
1989). It is because errors in experimental data are apt to
be magnified in determined relaxation spectrum. Cho
(2016) explained this problem with mathematics using the
FK relation. They showed how the error effect appears by
adding a sinusoidal perturbation to both exact functions of
relaxation spectrum and modulus. We shall show the ill-
posedness briefly in a graphic manner.
Consider that continuous relaxation spectrum is given
by
, (14)
(15)
where H0(λ) is exact spectrum and HE(λ) represents the
perturbed spectrum. In order to make a difference between
H0(λ) and HE(λ), we added 30% of statistical random
errors to H0(λ) which is represented as δH in Eq. (14).
G*ω( ) = G′ ω( ) + iG″ ω( )
G′ ω( ) G″ ω( )
G′ ω( ) = ∞–
∞
∫λ2ω
2
1 λ2ω
2+
-------------------H λ( )d logλ
G″ ω( ) = ∞–
∞
∫λω
1 λ2ω
2+
-------------------H λ( )d logλ
H1
ω-----
⎝ ⎠⎛ ⎞ =
2
π---Re G″ iω( )[ ] =
2
π---Im G′ iω( )[ ]
H1
ω----
⎝ ⎠⎛ ⎞ =
ε 0→lim
2
π---Re G″ iω ε+( )[ ] =
ε 0→lim
2
π---Im G′ iω ε+( )[ ]
G″ ω( ) = λω
1 λ2ω
2+
-------------------
Re G″ iω( )[ ] = 0
ε 0→lim
2
π---Re G″ iω ε+( )[ ] =
ε 0→lim
2
π---Re
iλω λε+
1 iλω λε+( )2+----------------------------------
= ε 0→lim
2
π---
λε
λε( )2 λω 1–( )2+--------------------------------------
⎩ ⎭⎨ ⎬⎧ ⎫ λε( )2 λω( )2 1+ +
λε( )2 λω 1+( )2+---------------------------------------
⎩ ⎭⎨ ⎬⎧ ⎫
δ x( ) = 1
π---
ε 0→lim
ε
ε2
x2
+--------------
ε 0→lim
λε( )2 λω( )2 1+ +
λε( )2 λω 1+( )2+--------------------------------------- =
λω( )2 1+
λω 1+( )2---------------------
ε 0→lim
2
π---Re G″ iω ε+( )[ ] =
2 λω( )2 2+
λω 1+( )2-------------------------δ λω 1–( )
ε 0→lim
2
π---Re G″ iω ε+( )[ ] = δ
1
ω---- λ–⎝ ⎠
⎛ ⎞
HE λ( ) = H0 λ( ) + δH
H0 λ( ) = 0.1
log10λ( )2 0.01+[ ]2
-------------------------------------------
Sang Hun Lee, Jung-Eun Bae and Kwang Soo Cho
118 Korea-Australia Rheology J., 29(2), 2017
This is shown in Fig. 1a.
Figure 1b confirms that calculated dynamic moduli from
each of continuous relaxation spectra are almost same. It
is because when we calculate dynamic moduli from HE(λ)
by the numerical integration of Eq. (5), errors in HE(λ) are
being suppressed (Atkinson and Han, 2001). It is assumed
that relaxation spectrum has a higher resolution to errors
than those of dynamic moduli.
3. Development of Algorithm
3.1. Main algorithmIn order to employ Eq. (7) for inferring continuous relax-
ation spectrum, we need an analytical equation to express
dynamic moduli. In general, dynamic moduli vary in log-
arithmic scale as frequency varies in logarithmic scale. It
is plausible to approximate dynamic moduli data in dou-
ble-logarithmic scale by polynomials. Because dynamic
moduli have shapes of simple function in double-logarith-
mic scale. Furthermore, the Weierstrass theorem reads that
any continuous function defined on a closed interval can
be uniformly approximated by polynomials (Atkinson and
Han, 2001).
Since dynamic moduli are assumed as continuous ones,
it is suitable that dynamic moduli data of a finite range of
frequency can be expressed by
(16)
where coefficients {gk} are real numbers, N is polynomial
order, and {Tk(ξ)} is the Chebyshev polynomials of the
first kind. ξ is the Chebyshev domain which is defined by
with (17)
where ν is logω, νmin and νmax are the minimum and max-
imum values of the frequency range, respectively.
Note that ξ is always in . In order to fit
dynamic moduli data by Eq. (16), frequency domain of
logarithmic scale should be changed to ξ by using Eq.
(17). Furthermore, the recursive formula allows us to cal-
culate higher order of {Tk(ξ)} by the definition as follows
(Mason and Handscomb, 2003):
.
(18)
The Chebyshev polynomials of the first kind are one of
orthogonal polynomials. Although curve fitting of the data
by simple polynomials has a unique global minimum of
the sum of square errors, N > 15 usually gives rise to a
numerical problem. If frequency range is tens of decades,
such numerical problem should be solved by using orthog-
onal polynomials. It is because orthogonal polynomials
are more stable for regression than simple polynomials
irrespective of N.
In order to derive the real and imaginary parts of Eq.
(16), we should define the complex logarithm of iω + ε as
follows:
. (19)
Applying the limit process of ε gives
. (20)
Equation (20) confirms that the substitution of logω by
log(iω + ε) with the limit process of ε is equal to the sub-
stitution of ν by ν + iπ/2. Then, the complex version of
Chebyshev domain can be expressed as
(21)
where
. (22)
f ν( ) exp k 0=
N
∑ gkTk ξ( )⎩ ⎭⎨ ⎬⎧ ⎫
≈
ξ = 2ν νmax– νmin–
νmax νmin–---------------------------------- νmin ν νmax≤ ≤
1– ξ 1≤ ≤
T0 ξ( ) = 1
T1 ξ( ) = ξ
�
Tk 1+ ξ( ) = 2ξTk ξ( ) − Tk 1– ξ( )
log iω ε+( ) = log ω2
ε2
+( ) + i arctanω
ε----
ε 0→lim log iω ε+( )[ ] = ν + i
π
2---
ξν ν→ +iπ /2
= 2 ν +iπ /2( ) νmax– νmin–
νmax νmin–------------------------------------------------------
= ξ + iφ
φ = π
νmax νmin–-----------------------
Fig. 1. (Color online) (a) Original spectrum, H0(λ) and perturbed
spectrum, HE(λ). (b) Calculated dynamic moduli from both con-
tinuous relaxation spectra of H0(λ) and HE(λ). Symbols and lines
denote ones which are related to H0(λ) and HE(λ), respectively.
Determination of continuous relaxation spectrum based on the Fuoss-Kirkwood relation and logarithmic orthogonal.....
Korea-Australia Rheology J., 29(2), 2017 119
It can be noticed that is equal to
from Eq. (21). If we substitute ν and ξ of Eq. (16) respec-
tively by and , then Eq. (16) becomes
. (23)
It is difficult to decompose Eq. (23) directly into the real
and imaginary parts. Because we should decompose
of each polynomial order. However, it can be
solved if we define the complex version of Eq. (18). Here,
we shall introduce some useful notations for the real and
imaginary parts of .
;
(24)
where one and two primes denote the real and imaginary
parts of , respectively. Substitution of ξ by
to Eq. (18) gives
.
(25)
Since {gk} are real numbers, the use of Euler’s formula
gives
, (26)
. (27)
Therefore, continuous relaxation spectrum from storage
modulus is
. (28)
On the other hand, continuous relaxation spectrum from
loss modulus is
. (29)
Note that the sign of H(−ν) is affected by the trigono-
metric function of the imaginary part. If the sign of trig-
onometric function is negative, then it is needed to add n
to the imaginary part in order to avoid negative signs of
H(−ν) (Zorn, 1999).
3.2. Verification of main algorithmWe shall use simulated dynamic moduli data to verify
the capability of the main algorithm. Model spectrum is
needed to find out whether the algorithm can determine
the exact spectrum. It is because we do not know the exact
continuous relaxation spectrum of experimental data.
Consider the following model spectrum which was sug-
gested by Baumgärtel and Winter (1992):
. (30)
This spectrum is known to be effective in describing
polydisperse polymer melts (Cho, 2013). We choose the
values of the parameters as H1 = 6.276 × 104 Pa, H2 =
1.27 × 105 Pa, λc = 2.481 s, λmax = 2.564 × 104 s, n1 = 0.25,
and n2 = −0.5. We shall call Eq. (30) as BSW spectrum.
We also choose the double-logarithmic distribution
model as follows:
(31)
where H3 = 1.4737 Pa, H4 = 10−3 H3, λ1 = 1.8328 × 10−2 s,
λ2 = 106λ1, and ω1 = ω2 = 1.5092 rad s–1. It has two peaks
of different heights and a local minimum valley between
them. Eq. (31) was subjected as a model spectrum by Cho
and Park (2013) because this model spectrum gives
severer test to algorithms than the model spectrum of Eq.
ξ ξ iφ+→ ν ν→ +iπ /2
ν +iπ /2 ξ + iφ
f ν iπ
2---+⎝ ⎠
⎛ ⎞ = exp k 0=
N
∑ gkTk ξ + iφ( )⎩ ⎭⎨ ⎬⎧ ⎫
Tk ξ + iφ( ){ }
Tk ξ + iφ( ){ }
Tk′ ξ( ){ } Re Tk ξ + iφ( ){ }[ ]≡ Tk″ ξ( ){ } Im Tk ξ + iφ( ){ }[ ]≡( )
Tk ξ + iφ( ){ }ξ + iφ
T0′ ξ( ) = 1; T0″ ξ( ) = 0
T1″ ξ( ) = ξ; T1″ ξ( ) = φ
Tk 1+ ′ ξ( ) = 2ξTk′ ξ( ) − 2φTk″ ξ( ) Tk 1– ′ ξ( )– ;
Tk 1+ ″ ξ( ) = 2ξTk″ ξ( ) + 2φTk′ ξ( ) Tk 1– ″ ξ( )–
Re f ν iπ
2---+⎝ ⎠
⎛ ⎞ = exp k 0=
N
∑ gkTk′ ξ( )⎩ ⎭⎨ ⎬⎧ ⎫
cos k 0=
N
∑ gkTk″ ξ( )⎩ ⎭⎨ ⎬⎧ ⎫
Im f ν iπ
2---+⎝ ⎠
⎛ ⎞ = exp k 0=
N
∑ gkTk′ ξ( )⎩ ⎭⎨ ⎬⎧ ⎫
sin k 0=
N
∑ gkTk″ ξ( )⎩ ⎭⎨ ⎬⎧ ⎫
H ν–( ) = 2
π---exp
k 0=
N
∑ gkTk′ ξ( )⎩ ⎭⎨ ⎬⎧ ⎫
sin k 0=
N
∑ gkTk″ ξ( )⎩ ⎭⎨ ⎬⎧ ⎫
H ν–( ) = 2
π---exp
k 0=
N
∑ gkTk′ ξ( )⎩ ⎭⎨ ⎬⎧ ⎫
cos k 0=
N
∑ gkTk″ ξ( )⎩ ⎭⎨ ⎬⎧ ⎫
H λ( ) = H1
λ
λc
------⎝ ⎠⎛ ⎞
n1
+ H2
λ
λc
------⎝ ⎠⎛ ⎞
n2
⎩ ⎭⎨ ⎬⎧ ⎫
expλ
λmax
-----------⎝ ⎠⎛ ⎞–
⎩ ⎭⎨ ⎬⎧ ⎫
H λ( ) = H3 exp1
ω1
------– log10
λ
λ1
------⎝ ⎠⎛ ⎞
2
⎩ ⎭⎨ ⎬⎧ ⎫
+ H4 exp1
ω2
------– log10
λ
λ2
------⎝ ⎠⎛ ⎞
2
⎩ ⎭⎨ ⎬⎧ ⎫
Fig. 2. (Color online) Regression results of dynamic moduli
data: Dynamic moduli data were calculated from (a) BSW and
(b) DP model spectra by the numerical integration. Symbols are
dynamic moduli data. Lines are regression curves.
Sang Hun Lee, Jung-Eun Bae and Kwang Soo Cho
120 Korea-Australia Rheology J., 29(2), 2017
(30). We shall call Eq. (31) as double peak spectrum (DP).
With the help of Eq. (5), dynamic moduli can be calcu-
lated from the numerical integration from both BSW and
DP spectra.
Figure 2 shows results of regression for dynamic moduli
data which is generated from both model spectra. It can be
noticed that the results of regression by Eq. (16) fit well
with their original data. Note that results of regression in
different N were omitted for both model spectra. It is
because they become nearly same when N > 13.
Figure 3 shows determined spectra from loss modulus
data of both model spectra. We chose N = 6 for BSW and
N = 13 for DP spectra. Two vertical dash-dot lines denote
the effective range of relaxation time, which is determined
mathematically from the given range of the data. It was
proven by Davies and Anderssen (1997). According to
their research, the effective range of the determined relax-
ation time should have the interval such as
(32)
where ωmin and ωmax are the minimum and maximum fre-
quencies of the modulus data, respectively. Eq. (32)
implies that the effective range of relaxation time is nar-
rower than the range of frequency of the modulus data.
We shall indicate the Davies-Anderssen interval [Eq. (32)]
as vertical lines in the figures of calculated spectrum.
Figure 3a shows that the determined spectrum is similar
to the original BSW spectrum. On the other hand, Fig. 3b
shows the severe fluctuation of the determined spectrum
for DP spectrum. It can be explained by the Runge’s phe-
nomenon which occurs in polynomial interpolation. It
seems that the fluctuation is occurring due to the use of
high order polynomials more than the data requires. Even
though the Chebyshev polynomials are more stable than
simple polynomials for regression, it does not guarantee
that the Chebyshev polynomials are independent on
Runge’s phenomenon especially for higher N. Further-
more, the loss modulus data have a sudden change of
slopes in a narrow range of frequency, which is analogous
to the local minimum valley of the spectrum. This can be
the reason that N should be larger than required for the
plausible result of regression.
In order to solve this problem, we should use lower
order polynomials. However, higher order polynomials are
needed to fit the experimental data which have a broad
range of frequency. Consequently, we should consider
some modifications of the main algorithm to satisfy these
requirements.
3.3. Point-wise calculationIn order to satisfy the requirements as mentioned in the
previous section, it can be a solution to use low order
polynomials in a partitioned range of frequency. However,
there is not an absolute benchmark to solve an ambiguity
of dividing experimental data into several partitions.
Hence, we shall introduce a modified version of the main
algorithm, which does not need to consider the ambiguity.
We shall call this algorithm as the point-wise calculation.
Consider the following definition of each partition for
experimental data as
with (33)
where {νp} are frequency points of the whole range of the
data, Δν is half of the width of each Ip, and Ndata is the
number of frequency points in the whole range of fre-
quency. We shall call the number of collected data points
in each Ip as Nsamp.
Eq. (33) implies that every frequency point of the data
becomes the center of each Ip. In other words, the number
of divided partitions is same with Ndata. Then, the dynamic
moduli data in each Ip can be expressed by
(34)
where denote the coefficients of the pth partition.
Therefore, calculated spectrum at νp from storage mod-
ulus is
eπ /2–
ωmin( ) 1–------------------ λ
eπ /2
ωmax( ) 1–-------------------≤ ≤
Ip = ν νp|νp– Δν– ν νp≤ ≤ Δν+{ } p = 1, 2, ..., Ndata
f ν νp–( ) = exp k 0=
N
∑ gk
p( )Tk ξ ξp–( )
⎩ ⎭⎨ ⎬⎧ ⎫
gk
p( ){ }
Fig. 3. (Color online) Comparison of original and determined
relaxation spectra from loss modulus data by the main algo-
rithm: (a) BSW and (b) DP model spectra. Symbols are deter-
mined spectra. Lines are original spectra. Dash-dot vertical lines
indicate the effective range of determined relaxation spectra.
Determination of continuous relaxation spectrum based on the Fuoss-Kirkwood relation and logarithmic orthogonal.....
Korea-Australia Rheology J., 29(2), 2017 121
.
(35)
On the other hand, calculated spectrum at νp from loss
modulus is
.
(36)
Note that every Ip has the same N and Nsamp.
Figure 4 illustrates the algorithm of the point-wise cal-
culation in a graphic manner. It is expected that the point-
wise calculation allows us to approximate dynamic mod-
uli data with lower order polynomials without loss of the
precision. As mentioned in section 1, the accuracy of
determined continuous relaxation spectrum is only
affected by the precision of regression for dynamic moduli
data.
4. Results and Discussion
4.1. Comparison of determined relaxation spectrafrom storage and loss moduli
According to Eq. (7), continuous relaxation spectrum
can be calculated either from storage and loss moduli.
Theoretically, both spectra should be the same. However,
it is usual that the both spectra are very similar but dif-
ferent (Cho, 2013).
In order to represent a difference of determined spectra
and its original model spectrum, we defined the sum of
square errors of determined spectrum as follows:
(37)
where HN(λ) and HExact(λ) denote the determined spectrum
by the point-wise calculation and its original model spec-
trum, respectively.
Figure 5 shows results of determined spectra from stor-
age and loss moduli by the point-wise calculation for both
model spectra. Figure 5a confirms that both determined
spectra from storage and loss moduli are nearly identical
to the original BSW spectrum. However, Fig. 5b shows
the deviation between determined spectra from storage
and loss moduli for DP spectrum. This also can be noticed
by the of each determined spectrum in Table 1. has
smaller value in the determined spectrum from loss mod-
ulus than that of determined spectrum from storage mod-
ulus. Although both determined spectra from storage and
loss moduli are more plausible than the result of Fig. 3b,
it is clear that the determined spectrum from loss modulus
is more acceptable than that from storage modulus.
This can be explained by the difference of shapes
between storage and loss moduli data. The shape of loss
modulus is more similar to the shape of original spectrum
H νp–( ) = 2
π---exp
k 0=
N
∑ gk
p( )Tk′ ξ ξp–( )
⎩ ⎭⎨ ⎬⎧ ⎫
sin k 0=
N
∑ gk
p( )Tk″ ξ ξp–( )
⎩ ⎭⎨ ⎬⎧ ⎫
H νp–( ) = 2
π---exp
k 0=
N
∑ gk
p( )Tk′ ξ ξp–( )
⎩ ⎭⎨ ⎬⎧ ⎫
cos k 0=
N
∑ gk
p( )Tk″ ξ ξp–( )
⎩ ⎭⎨ ⎬⎧ ⎫
χH
2 =
1
Ndata
---------- k 0=
Ndata
∑ 1HN λ( )
HExact λ( )--------------------–⎝ ⎠
⎛ ⎞2
χH
2χH
2
Fig. 4. (Color online) Schematic illustration of the point-wise
calculation which consists of (i) determination of coefficients
from the regression for the experimental data of the pth partition;
(ii) calculation of the spectrum at the pth frequency point using
Eqs. (35) or (36); (iii) repetition of the same procedure over the
whole frequency points.Fig. 5. (Color online) Comparison of determined relaxation
spectra from storage and loss moduli by the point-wise calcu-
lation: (a) BSW and (b) DP model spectra. The dash-dot vertical
lines are Eq. (32).
Sang Hun Lee, Jung-Eun Bae and Kwang Soo Cho
122 Korea-Australia Rheology J., 29(2), 2017
than that of storage modulus. Even though we calculated
continuous relaxation spectrum by the use of lower order
polynomials, this difference cannot be filled completely.
In addition, it is worthy to consider that relaxation spec-
trum has higher resolution to the errors than those of
dynamic moduli. Small regression errors are magnified in
determined spectrum. Therefore, we will use only loss
modulus data for continued sections.
4.2. Effects of calculation conditionsThere are two parameters in the algorithm of the point-
wise calculation, which are the order of polynomials, N
and the number of collected data points in the partition,
Nsamp. In order to check the effect of parameters of the
point-wise calculation, we assigned different sets of N and
Nsamp.
Figure 6 shows results of determined spectra in different
sets of N for both model spectra. We fixed Nsamp = 8 for
BSW model and Nsamp = 15 for DP model spectra. How-
ever, Fig. 7 shows results of determined spectra in differ-
ent sets of Nsamp for both model spectra. In contrast to Fig.
6, we fixed N = 8 and N = 14 for BSW and DP model
spectra, respectively.
It seems that determined spectra are not different
between results with different sets of N and Nsamp for BSW
model spectrum in both Fig. 6a and Fig. 7a. However, Fig.
6b and Fig. 7b show the same tendency that local mini-
mum valley of determined spectrum is more plausible
Table 1. of determined relaxation spectra from storage and
loss moduli data by the point-wise calculation.
BSW Model DP Model
From From
7.5869 × 10−4 1.8685 × 101
1.0271 × 10−4 8.1319 × 10−3
χH
2
χH
2χH
2
G′ ω( ) G′ ω( )G″ ω( ) G″ ω( )
Fig. 6. (Color online) Comparison of determined relaxation
spectra in different sets of N and original spectra: (a) BSW and
(b) DP model spectra. Nsamp was fixed at 8 and 15 for each model
spectrum, respectively. The dash-dot vertical lines are Eq. (32).
Fig. 7. (Color online) Comparison of determined relaxation
spectra in different sets of Nsamp and original spectra: (a) BSW
and (b) DP model spectra. N was fixed at 7th and 14th for each
model spectrum, respectively. The dash-dot vertical lines are Eq.
(32).
Table 2. of determined relaxation spectra in differentsets of N and Nsamp by the point-wise calculation.
BSW Model
N Nsamp Nsamp N
2
8
2.4846 × 10−2 14
7
8.1674 × 10−5
5 1.2034 × 10−4 11 6.8829 × 10−5
7 5.4804 × 10−5 8 5.4804 × 10−5
DP Model
N Nsamp Nsamp N
9
15
1.8475 × 10−2 23
14
2.6892 × 100
11 8.1319 × 10−3 19 1.9507 × 10−2
14 1.3008 × 10−3 15 1.3008 × 10−3
χH
2
χH
2χH
2
χH
2χH
2
Determination of continuous relaxation spectrum based on the Fuoss-Kirkwood relation and logarithmic orthogonal.....
Korea-Australia Rheology J., 29(2), 2017 123
with the set of N + 1 = Nsamp than the other sets for DP
model spectrum. Table 2 shows of determined spectra
in each set of N and Nsamp. of N + 1 = Nsamp is the most
smallest value in the Table 2. This implies that the
N + 1 = Nsamp condition is the best condition for describing
the loss modulus data of DP model spectrum. It is because
dynamic moduli data do not contain errors.
Although we included the determined spectrum with
N + 1 = Nsamp condition for comparison of other deter-
mined spectra with different conditions, the result is not
meaningful for the real application of the point-wise cal-
culation due to experimental errors. It is because the con-
dition of N + 1 = Nsamp cannot exclude the experimental
error in the data by the regression.
4.3. Error effectIn the previous sections, we dealt with simulated data
which are free from any errors. However, real experimen-
tal data have errors which are originated from various rea-
sons. In order to mimic experimental data, we added 5%
of statistical random errors to the simulated dynamic mod-
uli data from the BSW model spectrum. We generated 100
sets of error-contaminated data in order to investigate
error effect on spectrum calculation.
Figure 8 shows the average of the spectra calculated
from the 100 sets of error-contaminated data. The vertical
lines behind individual symbols represent the range of the
spectrum values at the corresponding relaxation times.
The error-contaminated data consist of 36 data points and
Nsamp is fixed by 22. Figure 8a is the result from N = 8 and
Fig. 8b from N = 5. Because of the error in data, lower
order of polynomial seems to provide better result than
higher order. As shown in Fig. 8, the vertical lines of N =
5 is shorter than those of N = 8. The errors in raw data
result in rapid variation around the exact values of data,
which is called waviness. Higher order polynomial is sen-
sitive to describe the rapidly varying data while lower
order polynomial gives slowly varying curve. This
explains why higher order polynomial is inferior to lower
order polynomial in fitting dynamic data with errors
although higher order polynomial is better than lower
order polynomial in fitting dynamic data without errors.
On the other hand, Fig. 9 compares the effect of Nsamp
with fixing the order of polynomial, N = 5. The lengths of
the vertical lines are reduced by the increase of Nsamp. The
effect of Nsamp can be explained by the fact that the more
data gives the better regression result.
Table 3 summarizes the results of both Fig. 8 and Fig. 9
in terms of . Note that is calculated from the aver-
aged spectrum. The evaluation by gives the same with
that by the length of vertical lines. The same effects of N
and Nsamp are found for the error-contaminated data from
the DP spectrum. Because of duplication, we omitted the
result from the DP spectrum.
χH
2
χH
2
χH
2χH
2
χH
2
Fig. 8. (Color online) Comparison of determined BSW spectra
for different sets of N with 5% of statistical random errors: (a) N
= 8th and (b) 5th. Nsamp was fixed at 22. The dash-dot vertical lines
are Eq. (32).
Fig. 9. (Color online) Comparison of determined BSW spectra
for different sets of Nsamp with 5% of statistical random errors for
BSW model spectrum: (a) Nsamp = 14 and (b) 22. N was fixed at
5th. The dash-dot vertical lines are Eq. (32).
Sang Hun Lee, Jung-Eun Bae and Kwang Soo Cho
124 Korea-Australia Rheology J., 29(2), 2017
We found the optimized N and Nsamp for the 5% error-
contaminated data from both the BSW and DP spectra.
Figure 10 shows the optimized results from the two model
spectra, which are calculated by the point-wise calculation
as before. Figure 10a shows the BSW spectrum can be
inferred overcoming the effect of errors in the raw data.
On the other hand, Fig. 10b shows that the error bars in
spectrum (vertical lines behind the symbols) are signifi-
cantly high at the both ends of the boundary of relaxation
time as well as in the valley. Furthermore, the average
spectrum deviates significantly from the original DP spec-
trum at the same regimes of relaxation time. Hence, Fig.
10 implies that the DP model spectrum is a more severe
test than the BSW model spectrum. Furthermore, 5% error
is much higher than the error levels expected for usual
experimental data (Bae and Cho, 2015). It is interesting
that the BSW spectrum is more similar to inferred spectra
from usual experimental data of polymers than the DP
spectrum (Baumgärtel and Winter, 1992; Stadler and van
Ruymbeke, 2010). Since the DP spectrum is a severe test,
most researchers test their algorithms with the DP spec-
trum (Bae and Cho, 2015; Cho and Park, 2013; Honer-
kamp and Weese, 1993; Stadler and Bailly, 2009).
4.4. Analysis on truncation errorIn the previous section, we investigated the effect of
experimental error by using the simulated data which sta-
tistical errors are added. However, since our algorithm is
based on polynomial approximation, the spectrum calcu-
lation contains inevitably truncation error. Therefore, it is
demanded to analyze the truncation errors in order to clar-
ify the errors in the spectrum calculated from the point-
wise calculation. The error analysis will be made by use
of the remainder theorem.
We can define that the loss modulus data can be expressed
exactly with the infinite series of Eq. (34) as follows:
. (38)
However, since we use finite order of polynomial, the
remainder theorem of Taylor expansion gives
(39)
where
, (40)
; . (41)
PN(ξ) and RN(ξ) denote the truncated series with a finite
order of N and the remainder term of series expansion,
respectively. Therefore, the exact equation of continuous
relaxation spectrum becomes
(42)
where
; , (43)
; . (44)
Note that , , , and are the real functions
of . Application of the addition formula of trigono-
metric function to Eq. (42) gives
(45)
where
. (46)
denotes the determined spectrum by the trun-
cated series. It is convenient for the analysis of the effect
G″ ν νp–( ) = exp k 0=
∞
∑ gkTk ξ ξp–( )⎩ ⎭⎨ ⎬⎧ ⎫
G″ ν νp–( ) = GN″ ν νp–( )exp RN ξ ξp–( ){ }
GN″ ν νp–( ) = exp PN ξ ξp–( ){ }
PN ξ( ) = k 0=
N
∑ gkTk ξ( ) RN ξ( ) = logG″ ν( )GN″ ν( )-----------------
⎩ ⎭⎨ ⎬⎧ ⎫
H νp–( ) = 2
π---exp PN′ RN′+( )cos PN″ RN″+( )
PN′ = Re PN ξ iφ+( )[ ] PN″ = Im PN ξ iφ+( )[ ]
RN′ = Re RN ξ iφ+( )[ ] RN″ = Im RN ξ iφ+( )[ ]
PN′ PN″ RN′ RN″ξ ξp–
H νp–( ) = HN νp–( )exp RN′( ) cosRN″ sin RN″ tan PN″–( )
HN νp–( ) = 2
π---exp PN′( )cos PN″
HN νp–( )
Table 3. of determined relaxation spectra in differentsets of N and Nsamp with 5% of statistical random errors bythe point-wise calculation.
BSW Model
N Nsamp Nsamp N
822
8.3301 × 10−1 145
1.9126 × 10−2
5 1.5848 × 10−2
22 1.5848 × 10−2
χH
2
χH
2χH
2
Fig. 10. (Color online) Optimized results of determined spectra
with 5% of statistical random errors for both model spectra: (a)
BSW and (b) DP model spectra. The dash-dot vertical lines are
Eq. (32).
Determination of continuous relaxation spectrum based on the Fuoss-Kirkwood relation and logarithmic orthogonal.....
Korea-Australia Rheology J., 29(2), 2017 125
of truncation error to define the relative difference
between and as
. (47)
With the help of Eqs. (45) and (46), Eq. (47) can be
rewritten by
. (48)
If is a good approximation then the truncation
error is bounded by a small positive number, say
δ << 1: for all n. Then the following inequality
is the immediate consequence:
; . (49)
Then, Eq. (48) becomes
. (50)
Consider the modulus data as the one contaminated
errors which can be expressed by
(51)
where εv is the relative error at the frequency of ν = logω.
Then Eq. (39) can be modified as follows
. (52)
Note that can be regarded as the experimental data
of loss modulus (or error-contaminated simulated data).
Since , the error term of Eq. (52) can be expressed
by
(53)
where
. (54)
If we extend the meaning of the upper bound, δ as the
following:
. (55)
We can use Eq. (50) as the estimator of the total error.
Then we can estimate δ at each frequency as follows
. (56)
Figure 11 shows the and for the inferred
spectra of Fig. 10 which contain statistical errors as well
as truncation ones. To compare and eas-
ily, they are normalized by their mean values. Although all
the points of and are not superposed,
overall shapes are similar to each other. Figure 11 indi-
cates again that the DP model spectrum is a more severe
test than the BSW model spectrum. It is observed that
lower consistency between and is found
in Fig. 11b than in Fig. 11a. The error analysis confirms
that the accuracy of approximating loss modulus data is
the most important factor for the determination of accurate
spectrum.
4.5. Application to experimental dataIn order to test our algorithm, we used loss modulus data
of poly(1,3-butadiene) 430k (PBd 430 K) which were
measured by Stadler and van Ruymbeke (2010). The data
have a wide frequency range of 14 decades. The Mw of
polybutadiene is about 450,000 g/mol. The data is shown
H νp–( ) HN νp–( )
δH νp–( ) = 1HN νp–( )H νp–( )-------------------–
δH νp–( ) = 11
exp RN′( ) cosRN″ sin RN″ tan PN″–( )------------------------------------------------------------------------------------–
PN ν( )RN ν( )
RN ν( ) <δ
RN′ δ< RN″ δ<
δH νp–( ) 11
eδ
cosδ sinδ tanPN″–( )----------------------------------------------------–≈ ΦH νp–( )≡
Gε″ ν( ) = G″ ν( ) 1 εv+( )
Gε″ ν( ) = GN″ ν( )exp RN ξ( ){ } 1 εv+( )
Gε″
εv <1<
1 εv+( )exp RN ξ( ){ } = exp RN ξ( ){ }
RN ξ( ) RN ξ( ) + log 1 εv+( )≡
RN ξ( ) + log 1 εv+( ) <δ <<1
δ logGN″ ν( )Gε″ ν( )-----------------
⎩ ⎭⎨ ⎬⎧ ⎫
≈
ΦH νp–( ) δH νp–( )
ΦH νp–( ) δH νp–( )
ΦH νp–( ) δH νp–( )
ΦH νp–( ) δH νp–( )
Fig. 11. (Color online) Comparison of δH(−νp) and ΦH(−νp) for
the results of Fig. 10: (a) BWS and (b) DP model spectra. Values
on all vertical axis are normalized by its mean values.
Fig. 12. (Color online) Loss modulus data of PBd 430k (Stadler
and van Ruymbeke 2010). Symbol and line indicate the original
data and the result of regression, respectively.
Sang Hun Lee, Jung-Eun Bae and Kwang Soo Cho
126 Korea-Australia Rheology J., 29(2), 2017
with the regression result in Fig. 12.
Since we do not know the exact spectrum of real exper-
imental data, we compared our result with those obtained
from other algorithms such as fixed-point iteration method
by Cho and Park (2013) and cubic Hermite spline method
by Stadler and Bailly (2009). We chose Nsamp = 130 and N
= 6 for the calculation. The comparison is shown in Fig.
13. It confirms that our algorithm gives a spectrum nearly
identical to those from the fixed-point iteration and cubic
Hermite spline methods within the effective range. Hence,
our algorithm is at least equivalent to the previous algo-
rithms. Although the two previous algorithms are mainly
based on least-square method, our algorithm is based on
mathematically exact equation, the FK relation. Hence, it
can be said that our method is superior to the previous
algorithms from the mathematical viewpoint.
5. Conclusions
We suggested a new algorithm called the point-wise cal-
culation for inferring continuous relaxation spectrum from
dynamic moduli data. The algorithm of the point-wise cal-
culation is based on the analytical equation of double log-
arithmic orthogonal polynomials and the FK relation.
We confirmed the algorithm of the point-wise calcula-
tion works well with both simulated and experimental
data. The success of the point-wise calculation mainly
originates from the use of Eq. (16) which is flexible in
curve fitting of loss modulus data with the precision.
We analyzed the error of determined spectrum using the
remainder theorem. The error analysis denotes that the
regression accuracy of loss modulus data is the most
important factor for determining continuous relaxation
spectrum in the algorithm of the point-wise calculation.
Acknowledgment
This work (2013R1A1A2055232) was supported by
Mid-Career Researcher Program through NRF grant funded
by the MEST.
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