Combined effect of heat source, porosity and thermal radiation on mixed convection flow in a vertical annulus An exact solution Engineering Science and Technology, an International Journal xxx (2017)[.]
Trang 1Full Length Article
Combined effect of heat source, porosity and thermal radiation on mixed
convection flow in a vertical annulus: An exact solution
Michael O Oni
Department of Mathematics, Ahmadu Bello University, Zaria, Nigeria
a r t i c l e i n f o
Article history:
Received 18 September 2016
Revised 5 December 2016
Accepted 25 December 2016
Available online xxxx
Keywords:
Heat source
Thermal radiation
Mixed convection
Vertical annulus
Porous material
Exact solution
a b s t r a c t This paper examines the effect of heat source, thermal radiation and porosity on mixed convection flow in
a vertical annulus filled with porous material The inner surface of outer cylinder is assumed to be the heated surface Closed-form expression for temperature, velocity, Nusselt number, skin-friction and mass flow rate are obtained in terms of Bessel’s function and modified Bessel’s function of first and second kind Based on depicted graphs, fluid temperature and Nusselt number increase with increase in radiation parameter and heat source parameter while velocity as well as skin-friction decreases with increase in radiation parameter and heat source parameter at the surfaces of the cylinder
Ó 2017 Karabuk University Publishing services by Elsevier B.V This is an open access article under the CC
BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/)
1 Introduction
Over the years, owing to the fact that cylinders have been used
in nuclear waste disposal, energy extortion in catalytic beds and
undergrounds, convective heat transfer about cylindrical
geome-tries has begun to attract the attention of many researchers since
some fluids are good emitter and absorber of thermal radiation,
it is of interest to study the effect of heat source on temperature
distributions and heat transfer when the fluid is capable of
emit-ting and absorbing thermal radiation This can be attributed to
the fact that heat transfer by thermal radiation is becoming of
greater importance when we are concerned with space
applica-tions (space journey) and higher operating temperatures
Several investigations have been carried out on problem of heat
transfer by radiation as an important application of space and
tem-perature related problems Greif et al.[1]obtained an exact
solu-tion for the problem of laminar convective flow in a vertical
heated channel in the optically thin limit They concluded that in
the optically thin limit, the fluid does not absorb its own emitted
radiation which means that there is no self-absorption but the fluid
does absorb radiation emitted by the boundaries Viskanta [2]
investigated the forced convective flow in a horizontal channel
permeated by uniform vertical magnetic field taking radiation into
account In his work, he studied the effects of magnetic field and radiation on the temperature distribution and the rate of heat transfer in the flow and found that the effect of magnetic field is
to decrease fluid velocity Later Gupta and Gupta[3]studied the effect of radiation on the combined free and forced convection of
an electrically conducting fluid flowing inside an open-ended ver-tical channel in the presence of a uniform transverse magnetic field for the case of optically thin limit They found that radiation tends
to increase the rate of heat transfer of the fluid there by reducing the effect of natural convection
Later, Hossain and Takhar[4]analyzed the effect of radiation using the Rosseland diffusion approximation which leads to non-similar solution for the forced and free convection of an optically dense viscous incompressible fluid past a heated vertical plate with uniform free stream and uniform surface temperature, while Hos-sain et al.[5]studied the effect of radiation on free convection from
a porous vertical plates
The role of thermal radiation is of major importance in the design of many advanced energy convection systems operating at high temperature and due to increase in science and technology, radiative heat transfer becomes very important in nuclear power plants, gas turbines and various propulsion devices for aircraft, missiles and space vehicles[6–10]
In cylindrical geometry, the studies of heat generation and ther-mal radiation have been studied by several authors Chamkha[11]
analyzed the heat and mass transfer of a MHD flow over a moving
http://dx.doi.org/10.1016/j.jestch.2016.12.009
2215-0986/Ó 2017 Karabuk University Publishing services by Elsevier B.V.
This is an open access article under the CC BY-NC-ND license ( http://creativecommons.org/licenses/by-nc-nd/4.0/ ).
E-mail address: Michaeloni29@yahoo.com
Contents lists available atScienceDirect Engineering Science and Technology,
an International Journal
j o u r n a l h o m e p a g e : w w w e l s e v i e r c o m / l o c a t e / j e s t c h
Please cite this article in press as: M.O Oni, Combined effect of heat source, porosity and thermal radiation on mixed convection flow in a vertical annulus:
Trang 2permeable cylinder with heat generation or absorption and
chem-ical reaction He concluded that the role of Hartmann number is to
decrease fluid velocity Trujillo et al.[12]studied the heat and mass
transfer process during the evaporation of water from a circular
cylinder through CFD modeling In other related work, Mujtaba
and Chamkha[13] discussed the heat and mass transfer from a
permeable cylinder in a porous medium with magnetic field and
heat generation/absorption Ganesan and Loganathan [14,15]
investigated an unsteady natural convective flow past
semi-infinite vertical cylinder with heat and mass transfer under
differ-ent physical situations Hossain et al.[16]reported the radiation
conduction interaction on mixed convection from a horizontal
cir-cular cylinder using an implicit finite-difference scheme
Also, Ganesan and Loganathan[17]studied the radiation and
mass transfer effects on flow of an incompressible viscous fluid
past a moving vertical cylinder Gnaneswar and Reddy[18,19]
ana-lyzed the radiation and mass transfer effects on an unsteady MHD
free convection flow of an incompressible viscous fluid past a
mov-ing vertical cylinder Radiation effects on hydromagnetic free
con-vective and mass transfer flow of a gas past a circular cylinder with
uniform heat and mass flux was studied by Hakiem[20] He also
found that magnetic field parameter retards fluid velocity Yih
[21]analyzed the radiation effect on natural convection over a
ver-tical cylinder embedded in a porous media Suneetha and Bhaskar
[22]analyzed the radiation and mass transfer effects on MHD free
Convection flow past a moving vertical cylinder embedded in a
porous medium Other related articles on radiation effect on heat
transfer of mixed convection flow for different fluid can be seen
in[23–25]
The purpose of this paper is to examine theoretically the effects
of thermal radiation and porosity on viscous, incompressible and
heat generating fluid in a vertical annulus filled with porous
mate-rial Exact solution for temperature, velocity, skin-friction and
Nus-selt number are obtained and the effects of governing parameters
are discussed with the aid of line graphs
2 Mathematical analysis Consider the steady laminar mixed convection flow of a viscous incompressible heat generating fluid The axis of cylinder is taken along the z-axis, while r-axis is taken in the radial direction The inner surface of the outer cylinder is assumed to be heated to a temperature Tw greater than that of surrounding fluid and outer surface of the inner cylinder having temperature T0 The radius
of the inner and outer cylinder walls are a and b respectively as
Nomenclature
a radius of inner cylinder
b radius of outer cylinder
g gravitational acceleration
h convective heat transfer coefficient
H dimensionless heat generating (source) parameter
In modified Bessel’s function of first kind on order n
Where n¼ 0; 1; 2; 3;
Jn Bessel’s function of first kind on order n Where
n¼ 0; 1; 2; 3;
Kn modified Bessel’s function of second kind on order n
Where n¼ 0; 1; 2; 3;
Nu0 rate of heat transfer at the outer surface of the inner
cylinder
Nu1 rate of heat transfer at the inner surface of the outer
cylinder
p dimensional pressure difference
P dimensionless pressure difference
Q0 dimensional heat generating (source) parameter
R dimensionless coordinate
T dimensional temperature of the fluid
T0 initial temperature
Tw final temperature
u dimensional velocity of fluid
U dimensionless velocity of fluid
Yn Bessel’s function of second kind on order n Where
n¼ 0; 1; 2; 3;
Z dimensionless coordinate Greek alphabets
a thermal diffusivity
b coefficient of thermal expansion
j mean absorption coefficient
k aspect ratioðb=aÞ
h dimensionless temperature of fluid
Subscript
1 outer surface of inner cylinder
k inner surface of outer cylinder
Fig 1 Schematic diagram.
Please cite this article in press as: M.O Oni, Combined effect of heat source, porosity and thermal radiation on mixed convection flow in a vertical annulus:
Trang 3seen in Fig 1 The following assumptions are made in order to
obtain an exact solution:
i The fluid motion is fully developed both thermally and
hydrodynmaically
ii All physical quantities except pressure gradient are
indepen-dent on z-axis
iii Viscous dissipation and displacement currents terms are
neglected in the energy equation
iv The fluid is considered to be a gray, absorbing emitting
radi-ation but non-scattering medium
Under the above assumptions, the governing equations of the
flow are respectively the continuity, momentum and energy
equations:
dðv0Þ
meff r
d
dr r
du0 dr
þ bgðT T0Þ mu0
K 1
k
qCp
1 r
d
dr r
dT0 dr
q1Cp
1 r
d
drðrqrÞ þQ0ðT T0Þ
u0¼ 0 T ¼ T0 at r¼ a
By using the Rosseland approximation (Brewster [26]), the radiative heat flux is given by qr
qr¼ 4r
3k
@T4
Following[27], the function T4in Eq.(5)can be expressed as a linear function by expanding it in a Taylor series about Tw and neglecting higher powers of T as follows:
-0.2 0 0.2 0.4 0.6 0.8 1 1.2 1.4
R
H = 0.5
H = 2.5
N = 0.5, 1.5, 2.5, 3.5
Fig 2 Temperature profile versus R varying H and N at k = 2.0.
0 0.2 0.4 0.6 0.8 1
R
N = 0.5
N = 3.5
λ = 2.2, 2.0, 1.8
Fig 3 Temperature profile versus R varying k and N at H = 1.5.
Please cite this article in press as: M.O Oni, Combined effect of heat source, porosity and thermal radiation on mixed convection flow in a vertical annulus:
Trang 4T4¼ 4T2
wT 3T4
Introducing the following dimensionless parameters:
U¼u0
u0; Re ¼ul0a; k ¼ba; c¼meff
m ; P ¼upa0l; Da¼aK2;
h ¼ T T0
Tw T0; R ¼ra; Z ¼az; N ¼ jk
4rT3; H2
¼Q0b2
k ;
Gr¼gbðT2 T0Þa3
Eqs.(2)–(6)in dimensionless form become:
c
R
d
dR R
dU
dR
þGrReh DaU dPdZ¼ 0 ð8Þ
1 R
d
dR R
dh dR
þ 3H 2 N
U¼ 0 h ¼ 0 at R ¼ 1
The solution of Eqs.(8)–(10)is obtained as:
hðRÞ ¼ C1J0ðm1RÞ þ C2Y0ðm1RÞ ð11Þ UðRÞ ¼ C3I0
R ffiffiffiffiffiffiffiffiffi
Dac
p
!
þ C4K0
R ffiffiffiffiffiffiffiffiffi
Dac
p
!
þGr Re
Da
cm2Daþ 1
C½ 1J0ðm1RÞ
þC2Y0ðm1RÞ DadP
0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6
R
H = 0.5
H = 2.5
γ = 0.5, 1.0, 1.5
Fig 4 Velocity profile versus R varying H andcat N = 1.5, k = 2.0, Gr/Re = 50, Da = 0.1.
0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6
R
N = 0.5
N = 3.5
Da = 0.001, 0.01, 0.1
Fig 5 Velocity profile versus R varying Da and N at H = 2.5,c= 1.5, k = 2.0, Gr/Re = 50.
Please cite this article in press as: M.O Oni, Combined effect of heat source, porosity and thermal radiation on mixed convection flow in a vertical annulus:
Trang 5The rate of heat transfer between the surfaces of the cylinders
and the fluid is obtained by differentiating the temperature and
is given by:
Nu1¼dh
dR
R ¼1
¼ m1½C1J1ðm1Þ þ C2Y1ðm1Þ ð13Þ
Nuk¼ dh
dR
R ¼k
¼ m1½C1J0ðkm1Þ þ C2Y0ðkm1Þ ð14Þ
The skin friction at the outer surface of inner cylinder and inner
surface of outer cylinder is respectively given by:
s1¼dU
dR
R ¼1
¼ ffiffiffiffiffiffiffiffiffi1
Dac
p C3I1
1 ffiffiffiffiffiffiffiffiffi
Dac
p
!
C4K1
1 ffiffiffiffiffiffiffiffiffi
Dac
p
!
GrRe Dam1
ðcm2Daþ 1Þ½C1J1ðm1Þ þ C2Y1ðm1Þ ð15Þ
sk¼ dUdR
R¼k¼ ffiffiffiffiffiffiffiffiffi1
Dac
p C4K1 ffiffiffiffiffiffiffiffiffik
Dac
p
!
C3I1 ffiffiffiffiffiffiffiffiffik
Dac
p
!
þGr Re
Dam1
ðcm2Daþ 1Þ½C1J1ðkm1Þ þ C2Y1ðkm1Þ ð16Þ
The amount of fluid passing through the annulus is given by the volume flow rate and defined as:
V¼
Zk 1
where n1; n2; n3; n4are constants defined in theAppendix The pressure gradient is obtained using the conservation law as:
Z k 1 RUðRÞdR ¼
Z k 1
0 0.5 1 1.5 2
R Gr/Re = 200, 150, 100, 50, 0, -50, -100, -150, -200
Fig 6 Velocity profile versus R varying Gr/Re at H = 1.5, N = 1.5,c= 1.5, k = 2.0.
1
1
1.5
1.5
2
2
2.5
2.5
3
3
3
3
3.5
3.5
3.5
3.5
4
4
4
4
4.5
4.5
4.5
5
5
5
5 5
H
2 3 4 5 6 7 8
Fig 7 Nusselt number for different values of H and N at k = 2.0, R = 1.
Please cite this article in press as: M.O Oni, Combined effect of heat source, porosity and thermal radiation on mixed convection flow in a vertical annulus:
Trang 6dZ¼p1
p2
ð20Þ
where p1and p2are constants defined inAppendix
The critical Gr=Re is obtained by:
dU
dR
Using Eq.(21), the reverse flow occurrence at the outer surface
of inner cylinder and inner surface of outer cylinder is respectively
given by:
Gr
Re
R¼1¼t23
Gr Re
R¼1¼t25
there tifor i¼ 1; 2; 3; are constant defined inAppendix
3 Results and discussion The solution obtained from Eqs.(11)–(23)are seen to be govern
by heat source parameterðHÞ, radiation parameter ðNÞ, Darcy num-berðDaÞ, aspect ratio ðkÞ, viscosity ratio ðcÞ and mixed convection parameterðGr=ReÞ In order to see the effect of these parameters, lines graphs are plotted to capture the physical situation Through-out this work, the heat source parameter is taken over the range
0:5 6 H 6 3:0 with reference value of 2.5, thermal radiation over
1
1
1.5
1.5
2
2
2.5
2.5
2.5
2.5
3
3
3
3
3.5
3.5
3.5
3.5
4
4
4
4
4.5
4.5
4.5
4.5
5
5
5
5 5
H
0 1 2 3 4 5
Fig 8 Nusselt number for different values of H and N at k = 2.0, R = k.
0 5 10 15 20 25 30
H
τ1
N = 0.5
N = 3.5
Da = 0.1, 0.01, 0.001
Fig 9 Skin friction for different values of H, Da and N atc= 1.5, k = 2.0, Gr/Re = 50, (R = 1).
Please cite this article in press as: M.O Oni, Combined effect of heat source, porosity and thermal radiation on mixed convection flow in a vertical annulus:
Trang 70:5 6 N 6 3:5, 0:001 6 Da 6 0:1 and 0:5 6c6 1:5 to capture
different physical problems Mixed convection parameter
200 6 ðGr=ReÞ 6 200 has been chosen to capture cases when
the natural convection dominates, ðGr=ReÞ P 0 and otherwise
ðGr=ReÞ 6 0
Fig 2presents the effect of heat source parameterðHÞ and
ther-mal radiation parameterðNÞ on temperature distribution at different
points in the annulus, the effect of heat generation and radiation
parameter is to increase the fluid temperature It is observed that
for small heat generation parameter the effect of thermal radiation
is insignificant on fluid temperature in the annulus
Fig 3on the other hand depicts effect of aspect ratioðkÞ on
tem-perature distribution in the annulus It is found that ask increases,
fluid temperature decreases In addition, magnitude of
tempera-ture is seen increase with increase in thermal radiation parameter
Fig 4 shows combined effect of viscosity ratio ðcÞ and heat
sourceðHÞ on fluid velocity in the annulus It is observed that fluid
velocity is an increasing function of heat source parameterðHÞ and
viscosity ratio ðcÞ at the center of the annulus but the reverse is observed at the region close to the surfaces of the annulus Two points of inflexion are noticed in this figure, at these points, fluid velocity is independent on heat source parameter
In similar manner,Fig 5gives the combined effect of radiation ðNÞ and porosity of porous material ðDaÞ on fluid velocity As expected, as ðDaÞ increases, velocity also increases This can be attributed to the fact that Darcy numberðDaÞ is directly propor-tional to the permeability which widens the pores of the porous material and as such enhances fluid motion The reverse situation
is noticed at the region close to the surfaces of the cylinders In addition, the maximum velocity is reached at the center of the annulus
Fig 6presents the effect of mixed convection parameterðGr=ReÞ
on fluid velocity For positive values ofðGr=ReÞ i.e when natural convection dominates over forced convection, fluid velocity is seen
to be higher at the inner surface of the outer cylinder than outer surface of the inner cylinder On the other hand, when
0 5 10 15 20 25 30
H
τ λ
N = 0.5
N = 3.5
Da = 0.1, 0.01, 0.001
Fig 10 Skin friction for different values of H, Da and N atc= 2.0, k = 1.5, Gr/Re = 50 (R = k).
-30 -25 -20 -15 -10 -5 0 5 10
H
τ1
γ =0.5
γ = 1.0
γ = 1.5
Gr/Re = 150, 100, 50, 0
Fig 11 Skin friction for different values of H,cand Gr/Re at k = 1.5, N = 1.5, Da = 0.1.
Please cite this article in press as: M.O Oni, Combined effect of heat source, porosity and thermal radiation on mixed convection flow in a vertical annulus:
Trang 8ðGr=ReÞ < 0, the reverse result is obtained When ðGr=ReÞ ¼ 0, i.e.
no natural convection (purely forced convection), the velocity is
seen to be symmetric Also, a point of inflexion is noticed at the
center of the annulus At this point, fluid velocity is independent
whether forced or natural convection
Figs 7 and 8display the rate of heat transfer at the outer surface
of the inner cylinder and inner surface of outer cylinder
respec-tively for different values of radiation and heat source parameter
It is observed that radiationðNÞ and heat source ðHÞ enhance rate
of heat transfer at the outer surface of inner cylinder This can be
attributed to the fact that increase heat source and radiation
parameter, enhances fluid temperature which in turn increase
the rate at which heat is transfers between the fluid and the
sur-faces of the cylinders In addition, the rate of heat transfer is seen
to be higher at the outer surface of inner cylinder than inner
sur-face of outer cylinder
Figs 9 and 10illustrate combined effect of radiationðNÞ
poros-ityðDaÞ and heat source ðHÞ on the skin-friction at the outer
sur-face of inner cylinder and inner sursur-face of outer cylinder At both
surfaces of the cylinders, the skin-friction is seen to decrease with
increase in Darcy numberðDaÞ, radiation parameter ðNÞ and heat
source parameterðHÞ It is interesting to note that skin-friction is
independent on radiation or porosity for small value of heat source
parameter This can be explained form the solution obtained, that
for small heat source parameter, temperature profile is
indepen-dent of H and hence the velocity/skin friction Further, skin friction
is higher at the inner surface of outer cylinder than outer surface of
inner cylinder
Figs 11 and 12depict combined effect of viscosity ratio and
mixed convection parameter on the skin-friction at the surfaces
of the cylinders The skin-friction at the outer surface of inner
cylinder inFig 11is seen to decrease with increase in heat source
parameter and mixed convection parameter but increase with
increase in viscosity ratio The reversed result is noticed for
skin-friction at the inner surface of outer cylinder inFig 12 Also, the
maximum skin friction is observed at the inner surface of outer
cylinder
Table 1presents the critical values of mixed convection
param-eter varying radiation paramparam-eter, Darcy number and viscosity
ratio It is found that the critical Gr=Re increase with increase in
viscosity ratio but decreases with increase in radiation parameter
as well as Darcy number
4 Conclusions
In this work, an exact solution of combined effects of heat source and thermal radiation on mixed convection flow in a verti-cal annulus filled with porous material is obtained Closed-form expression for temperature distributions, velocity profiles, Nusselt number (representing the rate of heat transfer), skin-friction and mass flow rate are obtained in term of Bessel’s function and mod-ified Bessel’s function of first and second kinds respectively The effects of governing parameters such as heat source parameter ðHÞ, radiation parameter ðNÞ, mixed convection parameter ðGr=ReÞ, Darcy number ðDaÞ, aspect ratio ðkÞ and viscosity ratio
ðcÞ on temperature, velocity, Nusselt number and skin-friction are illustrated with the use of line graphs Based on the figures depicted, the following conclusions can be drawn:
6 8 10 12 14 16 18 20 22 24
H
τ λ
γ = 0.5
γ = 1.0
γ = 1.5
Gr/Re = 150, 100, 50, 0
Fig 12 Skin friction for different values of H,cand Gr/Re at k = 2.0, N = 1.5 (R = k).
Table 1 Numerical values for critical Gr
for different values of N; Da andcat H ¼ 1:5; k ¼ 2:0.
R¼k
Please cite this article in press as: M.O Oni, Combined effect of heat source, porosity and thermal radiation on mixed convection flow in a vertical annulus:
Trang 91 Thermal radiation as well as heat source parameter increase
fluid temperature
2 Fluid velocity decreases with increase in heat source, viscosity,
radiation and mixed convection parameter but increases with
increase in Darcy number at the outer surface of inner cylinder
while the reverse trend is occurs at the inner surface of outer
cylinder
3 The rate of heat transfer at the surfaces of the cylinders
increases with increase in radiation and heat source
4 The skin-friction at the surfaces of the cylinders is reduced by
porosity (Darcy number), heat source parameter and radiation
parameter
5 Reverse flow occurrence at the surfaces of the cylinder
decreases with increase in porosity and radiation parameter,
but increases with increase in viscosity ratio
6 Reverse flow in the annulus can be avoided by choosing
appro-priate values for heat source parameter, radiation parameter,
Darcy number and viscosity ratio
When Gr=Re ¼ 0, this work reduces to pressure driven flow and
the effect of N and H on velocity profile and skin friction is
suppressed
Acknowledgements
The author is thankful to his supervisors Prof B.K Jha and Prof
A.O Ajibade for their support throughout the compilation of this
article and their fatherly impartations
Appendix
m1¼
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
3NH2
3Nþ 4
s
; m2¼
ffiffiffiffiffiffiffiffiffi 1
cDa
s
; m3¼ 1
m2
C1¼ Y0ðm1Þ
½Y0ðkm1ÞJ0ðm1Þ J0ðkm1ÞY0ðm1Þ;
C2¼ J0ðm1Þ
½Y0ðkm1ÞJ0ðm1Þ J0ðkm1ÞY0ðm1Þ
C3¼ t4
dP
dZþ t5
Gr
Re; C4¼ t8
dP
dZþ t9
Gr
Re;
n1¼ C3m3½kI1ðkm2Þ I1ðm2Þ
n2¼ C4m3½K1ðm2Þ kK1ðkm2Þ;
n3¼ C1DaGr
Reðcm2Daþ 1Þm1½kJ1ðkm1Þ J1ðm1Þ
n4¼ C2DaGr
Reðcm2Daþ 1Þm1
½kY1ðkm1Þ Y1ðm1Þ;
n5¼ DadPdZðk
2 1Þ
2
t1¼ Da½K0ðkm2Þ K0ðm2Þ; t2¼ DaK0ðm2Þ
ðcm2Daþ 1Þ
t3¼ ½K0ðkm2ÞI0ðm2Þ I0ðkm2ÞK0ðm2Þ; t4¼t1
t3; t5¼t2
t3
t6¼ Da½I0ðkm2Þ I0ðm2Þ; t7¼ DaI0ðm2Þ
ðcm2Daþ 1Þ; t8¼t6
t3;
t9¼t7
t3
t10¼Daðk
2 1Þ
2 ; t11¼ðk
2 1Þ 2
t12¼ Da
ðcm2Daþ1Þ
C1
m1ðkJ1ðkm1Þ J1ðm1ÞÞ þC2
m1ðkY1ðkm1Þ Y1ðm1ÞÞ
t13¼ kI1ðkm2Þ I1ðm2Þ; t14¼ kK1ðkm2Þ K1ðm2Þ
t15¼ m3ðt9t14 t5t13Þ t12; p1¼ t11þGr
Re½t15;
p2¼ m3ðt4t13 t8t14Þ t10
t16¼ Dam1
ðcm2Daþ 1Þ; t17¼ t8m2K1ðm2Þ t4m2I1ðm2Þ;
t18¼ t5m2I1ðm2Þ t9m2K1ðm2Þ t16ðC1J1ðm1Þ þ C2Y1ðm1ÞÞ
t19¼ t8m2K1ðkm2Þ t4m2I1ðkm2Þ; t22¼p2
p1
t20¼ t5m2I1ðkm2Þ t9m2K1ðkm2Þ t16ðC1J1ðkm1Þ
þ C2Y1ðkm1ÞÞ; t21¼t11
p1
t23¼ t17t21; t24¼ t18 t17t22; t25¼ t19t21; t24¼ t20 t19t22:
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