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\title{A Unified Field Approach on Fractional-Ordered Micropolar Thermoelasticity with Diffusion}
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             \author[1]{Dr. Soumen  Shaw}

             \affil[1]{  Bengal Engineering and Science university, Shibpur.}

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\date{\small \em Received: 2 November 2011 Accepted: 2 December 2011 Published: 16 December 2011}

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\begin{abstract}
        


The present paper is completely devoted on derivation of some basic fundamental  relations in generalized thermodiffusive micropolar elasticity with fractional-ordered derivatives.  The generalized heat conduction and mass diffusion equations have been modified by using  fractional calculus. A variational principle is obtained and hence the uniqueness theorem for  those equations has been   proved.      

\end{abstract}


\keywords{Fractional calculus, Micropolar elasticity, Thermodiffusion, Variational principle, Uniqueness theorem.}

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\let\tabcellsep& 	 	 		 
\section[{INTRODUCTION}]{INTRODUCTION}\par
t is well established that the thermoelasticity theory is a fusion of the theory of heat conduction and the theory of elasticity. In classical theory of thermoelasticity there was a diffusive phenomenon on the heat propagation and thermal signals propagate with infinite speed. This physically unacceptable drawback of infinite speed of heat propagation was inherent in that theory. Modifying the Fourier's law of heat conduction, Lord-Shulman \hyperref[b0]{[1]} introduced one nonclassical theory of heat propagation with one relaxation time which can avoid that paradox. Green-Lindsay \hyperref[b1]{[2]}, in the year 1972, Proposed another one with two relaxation times. These non-classical theories are referred as generalized theory of thermoelasticity. Dhaliwal and Sherief \hyperref[b2]{[3]} extended that generalized theory for anisotropic media. Later on, during the year 1991-1993 Green and Naghdi \hyperref[b3]{[4,}\hyperref[b4]{5,}\hyperref[b5]{6]} introduced a new theory of thermoelasticity and divide their theory into three parts, referred as types I, II and III. In an extensive review work on the development of generalized/ hyperbolic thermoelasticity till 1998 is available in the review article of Chandrasekharaiah \hyperref[b6]{[7]}.\par
Diffusion can be defined as the random movement of the particles from the higher concentrated regions to the lower concentrated regions because of the non-zero concentration gradient which can be expressed in terms of changes of the concentration at that position. In recent past it has been observed that there are so many researchers are interested to study on this aspects due to a great application in geophysics and in industry e.g. so many oil companies are interested in the thermodiffusion process for more efficient extraction of oil from the oil deposits.Diffusion is used to form base and emitter in bipolar transistors, form integrated resistors and used to introduce 'dopants' in controlled amounts into the semiconductor substrate. The thermodiffusion in elastic solids is due to the coupling among the temperature, elastic strain and mass diffusion in addition with the exchange between heat and mass in the nature.\par
In 1974, Nowacki \hyperref[b7]{[8]}\hyperref[b8]{[9]}\hyperref[b9]{[10]}\hyperref[b10]{[11]} developed the theory of coupled thermoelastic diffusion. The generalized theory in thermoelastic diffusion was introduced by Sherief et al. \hyperref[b11]{[12]} in 2004. Again, in the year 2005, Sherief et al. \hyperref[b12]{[13]} studied a half space problem in the theory of generalized thermoelastic diffusion. The influence of diffusion on generalized thermoelastic problems of infinite body with a cylindrical cavity studied by Ronghou et al. \hyperref[b13]{[14]}. Singh \hyperref[b14]{[15,}\hyperref[b15]{16]} in his couple of papers discussed the reflection of waves from the free surface in generalized thermoelastic diffusion. In recent times Kumar and Kansal \hyperref[b16]{[17,}\hyperref[b17]{18]} studied about the Rayleigh and Lamb wave propagation on free surface in transversely isotropic thermoelastic diffusion. Sharma et al. \hyperref[b18]{[19]}\hyperref[b19]{[20]} studied on thermodiffusive surface wave propagation in heat conducting materials and Kumar et al. \hyperref[b20]{[21]} discussed on the plane strain deformation in generalized thermoelastic diffusion in 2007-2008.\par
The linear theory of micropolar thermoelasticity has been developed by extending the theory of micropolar elasticity including thermal effect by Eringen \hyperref[b21]{[22,}\hyperref[b22]{23]} and Nowacki \hyperref[b23]{[24,}\hyperref[b24]{25]}. Minagawa et al. \hyperref[b25]{[26]} discussed the propagation of plane harmonic waves in a cubic micropolar medium. Kumar and Rani \hyperref[b26]{[27]} studied time harmonic sources in a thermally conducting cubic crystal and Mechanical/ thermal sources in a micropolar thermoelastic medium with cubic symmetry by Kumar and Aliawalia \hyperref[b27]{[28]}. In the year 2006, Kumar and Aliawalia \hyperref[b28]{[29]} studied on deformation due to time harmonic sources in micropolar thermoelastic medium with two relaxation times.\par
Fractional calculus has been used successfully to modify many existing model of physical process. In the formulation of tautochrone problem, Abel applied fractional calculus to solve integral equation and that was first application of fractional derivatives. Using fractional derivatives, for the description of viscoelastic materials, Caputo \hyperref[b30]{[30]}, Caputo and Mainardi \hyperref[b32]{[31]} found an agreement between the experimental results with theoretical one. Recently, Sherief et al. \hyperref[b33]{[32]} introduced the fractional ordered thermoelasticity by using Caputo's \hyperref[b30]{[30]} Phenomenon.\par
In the present investigation we are concerned about the interaction between thermoelastic diffusion with micropolar-elasticity by using fractional derivatives. ?  
\section[{FUNDAMENTAL EQUATIONS}]{FUNDAMENTAL EQUATIONS}\par
The Riemann-Liouville fractional integral is introduced as a natural generalization of the convolution type integral \hyperref[b34]{[33,}\hyperref[b35]{34,}\hyperref[b36]{35,}\hyperref[b37]{36,}\hyperref[b38]{37]},( ) ( ) ( ) ( ) ? ? ? Î?" = t d f t t f I 0 1 1 ? ? ? ? ? ? , (\textbf{)}0 > ? (2.1)\par
The Laplace transform for this fractional integral is defined by,( ) [ ] ( ) [ ] t f L s t f I L ? ? 1 = .\par
(2.\par
2)\par
The Riemann-Liouville derivative of fractional of fractional order ? is defined as the left-inverse of the fractional integral? I as ( ) ( ) ( ) ( ) ( ) ? ? ? ? ? ? Î?" = = t n n n n n RL d f t dt d n t f I D t f D 0 1 1 ? ? ? ? ? ? ? , n n < < ? ? 1 (2.3)\par
and for Laplace transform, the initial values of the fractional integral ( )t f I n ? ? and its derivatives of order 1 , ... , 3 , 2 , 1 ? = n k are required, where ( ) [ ] ( ) [ ] ( ) ? ? = ? ? ? ? = 1 0 1 0 n k n k k n RL f I D s t f L s t f D L ? ? ? , n n < < ? ? 1 . (2.4)\par
An alternative definition of fractional derivative was proposed by Caputo \hyperref[b30]{[30]} as,( ) ( ) ( ) ( ) ? ? ? ? ? Î?" = t n n n C d f dt d t n t f D 0 1 1 ? ? ? ? ? ? , n n < < ? ? 1 (2.5)\par
and for the Laplace transform, this definition has an advantage, the initial values of ( )t f and its integer derivatives of order 1 , ... , 3 , 2 , 1 ? = n k\par
are required unlike the fractional ordered derivatives given by the equation (2.3), so that Here we shall use the fractional derivatives of order ( ] 1 , 0 ? ? , according to Caputo \hyperref[b30]{[30]}. Let V be any arbitrary volume element of a material body bounded by the closed surface A. Now the first law of thermoelasticity, the law of conservation of energy for the volume element V can be written in the following form:( ) [ ] ( ) [ ] ( ) ( ) ? ? = ? ? ? = 1 0 1 0 n k k k C f s t f L s t f D L ? ? ? , n n < < ? ? 1 (2.? V dt d ? ( U +K ) = L + dt dQ (2.7) Here, L ( ) ( ) ? ? + + + = A j i ji i ji V i i i i dA n m u t dV l u F ? ? ? ? ? (2.8) ? ? + ? = V A i WdV dA n i q Q ? (2.9)\par
Now the equations of the motion are as follows:i i j ji u F t ? ? ? ? = + , (2.10) l l mn lmn k kl l t m ?? ? ? = + + , (2.11)\par
wheren l mn klm l kl k j j ? ? ? ? ? + = ?\par
After using divergence theorem and the equations of motion (2.10), (2.11) we obtain from the equation (2.7),? V dt d ? ( U +K ) = ( ? ? ? ? V dt d ? K ( ) dV q j m u t j j l j i kl ijk j i ji k ijk j i ji ? ? ? ? + + + + , , , ) ? ? ? ?? ? ? ? (2.12)\par
Now for micropolar thermoelastic solids, the deformations, micro-rotations and the changes of temperature are very small in natural state of the body, so a linear approximation is possible. For linear approximation we introduce, as was done by Eringen \hyperref[b22]{[23]}, the norm function of the array ( )i i i u W , , , , , , , ? ? ? ? ? ? ? = by ( ) 2 1 W W W ? = = ?\par
and for some neighborhood of 0 = ? , there exist positive constants k and n such that( ) . 0 , 0 , > > ? ? n k k n n ? ?\par
Now, for linear (1 st order) approximation equation (2.12) can be written in the following form:W q m i i ij ji ji + ? + = , ji t U ? ? ? ? ? ? (2.13) Where, k ijk j i ji u ? ? ? + = , (2.14)\par
Now we consider the entropy balance law,W P q S T i i i i + + ? = , , ? ? ? (2.15)\par
The equation of conservation of mass: C i i ? ? = , ? (2.+ + + = ? ? ? ? ji t U (2.17)\par
For further proceedings, we introduce the helmholtz free energy function ? given by, TS -U = ?\par
(2.18) Now using the equation (2.17), the total differential of the function ? can be written as,SdT PdC d m d t d ij ji ji ji ? ? ? ? ? + + = ? (2.19)\par
Here the function ? and all other functions under consideration can be expressed in terms of the independent variablesT C kl kl , , ,? ? . Now by chain rule we get, dC C dT T d d d ij ij ji ji ? ? ? + ? ? ? + ? ? ? + ? ? ? = ? ? ? ? ? ? ? ? ? ? (2.20)\par
Comparing the equations (2. \hyperref[b18]{19}) and (2.20) we obtain,ji ji t ? ? ? ? ? = (2.21) ij ji m ? ? ? ? ? = (2.22) C P ? ? ? = ? (2.23) ? ? ? ? ? = ? ? ? ? = T S (2.24)\par
Now expanding the function ? into the Taylor series in terms of independent variables about its natural state, we obtain, + + + + + ? + + + + ? + + + + ? = ? kl ji jikl ij ij ij ij kl ij ijkl ji ji ji ji lk ji jilk E ij ij ji ji C C d c B C a C b a A bC T C B C b A a ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? where 0 0 , T T T ? = ?\par
is the temperature of the medium in natural state such that1 0 << T ? .\par
In the natural state of the material body, we consider,. 0 , 0 , 0 , 0 , 0 , 0 = = = = = = ? ij ij ij C t ? ? ? and we obtain, . 0 , 0 , 0 , 0 , 0 0 0 0 = = = = = ? ij ji B b A a\par
Now equation (2.25) can be recast in following form keeping only second order terms, ? ? ? ? ? ? ? ? ? ? ? ? ? ij ij kl ij ijkl ji ji ji ji lk ji jilk E c B C a C b a A bC T C + + ? + + + + ? = ? 2 1 2 1 2 1 2lk ijlk ij ij kl ijkl ij C C b a A t ? ? ? + + + = (2.27) lk jikl ij ij kl ijkl ji C C d c B m ? ? ? + + + = (2.28) ij ij ji ji d a b bC P ? ? ? + ? + = (2.29) ij ij ji ji E c aC a T C S ? ? ? ? ? ? + ? = 0 (2.30)\par
Now, in isotropic solids, from the equation (2.26) it has been seen that, since free energy is a scalar quantity, each terms of right hand side of equation (2.26) are scalars and hence, ( )jk il jl ik kl ij ijkl A ? µ? ? ? ? µ ? ?? + + + = , jl ik jk il kl ij ijkl B ? ?? ? ?? ? ?? + + = , 0 = ijkl C , ij ij a ? ? 1 ? = , ij ij b ? ? 2 ? = , 0 = ij c .\par
Diffusion is a random walk of the particles of the material body from higher concentrated regions to lower concentrated regions. Here ij d represents the coupling coefficients between ij ? and the concentration C of the body, in an isotropic solid the gradient of microrotation and the concentration are independent. So we take 0 = ij d in isotropic body. In addition, the material is called spin-isotropic if?? ?? ? j j = .\par
Hence, in isotropic solids constitutive equations are, ( )ij ij ji ij ij kk ij C t ? ? ?? ? µ? ? ? µ ? ?? 2 1 ? ? + + + = (2.31) ji ij ij kk ij m ?? ?? ? ?? + + = (2.32) ? ? ? a bC P kk ? ? = 2 (2.33) C aT T C S T kk E 0 0 1 0 + + = ? ? ? ? ? (2.34)\par
Now, the linear equations of balance law are given by,? ? ? ?? ? ? u F t ? ? = + , (2.35) ? ? ? ? ?? ? ? ? ? ? ? j l t m mn mn = + + , (2.36)\par
The linearized form of heat conduction is,W q S T i i + ? = , ? ? (2.37)\par
and without contradiction with the second law of thermodynamics, we assume a generalized form of Fourier's law of heat conduction equation as,i i K q t , 0 1 ? ? ? ? ? = ? ? ? ? ? ? ? ? ? ? + (2.38)\par
where ? is a constant such that  We may consider the equation (2.39) is an extended version of fractional ordered heat conduction equation in isotropic, micropolar, thermodiffusive elastic solids. Now we consider the equation of mass flux vector,   ) ( )? ? ? ? ? ? ? ? ? ? ? ? + + ? ? ? ? ? ? ? ? ? ? ? ? + + ? ? ? ? ? ? ? ? ? ? ? ? + = ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? 0 0 0 0 1 0 , 1 1 1 W t ? ? ? ? ? ? ? ? ? ? + ? ? ? ? 0 1 (2.i i DP t , 1 1 ? = ? ? ? ? ? ? ? ? ? ? + ? ? ? ? (2.? ? ? ? ? ? ? ? ? ? ? ? + + + ? = ? ? ? ? ? ? 1 ,W t C C aT t t T C K kk E ii ? ? ? ? ? ? ? ? + ? + + ? ? ? ? ? ? ? ? ? ? + ? ? + + = ? ? ? ? ? ? ? ? ? ? 1 0 2 2 0 1 , ? ? ? ? ? ? (2.42) C t t Da D DbC ii kk ii ? ? ? ? ? ? ? ? ? ? + ? ? + + ? = 2 2 , 2 2 , ? ? ? ? (2.43)\par
These are the generalized heat conduction and mass diffusion equations in isotropic, micropolar elastic solids. Again, when0 , 1 ? ? ? ? equations (2.39), (2.41) transform to ( ) W t t C t aT u t T t t C K E ii ? ? ? ? ? ? ? ? + ? ? ? ? ? ? ? ? ? ? ? + + ? ? ? ? ? ? ? ? ? ? + + ? ? ? ? ? ? ? ? ? ? + = ? ? ? ? ? ? ? ? 1 1 1 1 0 0 1 , ? ? ? (2.44) ( ) t C t Da u D DbC ii ii ? ? ? ? ? ? ? ? ? ? + + + ? ? ? = ? ? ? 1 , 2 2 , 
\section[{? ?}]{? ?}\par
(2.45) Equations (2.44) and (2.45) represent the heat conduction and mass diffusion equations for isotropic elastic solids, as was done by Sherief et al. \hyperref[b11]{[12]}. 
\section[{III.}]{III.} 
\section[{A VARIATIONAL PRINCIPLE}]{A VARIATIONAL PRINCIPLE}\par
The variational theorem in classical thermoelasticity first derived by Biot \hyperref[b39]{[38]} and explained their applications by means of several examples. The variational theorem on classical thermoelastic diffusion was done by Sherief et al. \hyperref[b11]{[12]}. In micropolar thermoelasticity the variational principle and uniqueness theorem was done by Eringen \hyperref[b21]{[22,}\hyperref[b22]{23]}. Recently, a variational principle of fractional order generalized thermoelasticity was done by Youssef and Al-Lehaibi \hyperref[b40]{[39]}. Now we shall present a compact derivation of a variational principle on fractional-ordered micropolar thermoelastic diffusion. We consider,W [ ] ? + = V mn kl klmn mn kl klmn dV B A ? ? ? ? 2 1 , (3.1)\par
where the integrand is homogeneous quadratic form of strain tensor and microrotation tensors. Now we consider a virtual displacement i.e. for a neighboring state in which the displacement, strain tensor, microrotation tensors are changed by the quantities ( )i u ? , ij ?? , ij ?? respectively, we\textbf{obtain, ? W ( ) ( ) ( ) ( ) [ ] ?}ij ij ji ij ij kk ij C t ? ? ?? ? µ? ? ? µ ? ?? 2 1 ? ? + + + = (3.3) ji ij ij kk ij m ?? ?? ? ?? + + = (3.4)\par
Taking into account the equations of motion;? ? ? ?? ? ? u F t ? ? = + , (3.5) ? ? ? ? ?? ? ? ? ? ? ? j l t m mn mn = + + ,\textbf{(3.6)}\par
Corresponding boundary conditions;j ji i n t p = (3.7) j ji i n m m = (3.8)\par
and using divergence theorem, we obtain,? ? ? ? ? ? ? ? + + + V i i V i i A i i V i i A i i V i i dV j dV u u dA m dV l dA u p dV u F ? ? ? ? ? ? ?? ?? ? ? ? ? ? ? ? ? ? = W ? ? ? ? V kk V kk dV C dV ?? ? ? ? ? ? 2 1 (3.9)\par
This is the first variational equation and it would be complete for uncoupled thermoelasticity if the temperature? and the concentration C in last two integrations of the right hand side of the equation (3.9) were known. Taking into account the coupling between the strain field, temperature and concentration it is observed that ? and C are unknown. Hence it is necessary to introduce other relations considering the phenomena of heat conduction as well as mass diffusion. Now we introduce one vector H ? as was done by Biot \hyperref[b41]{[40]}, related with entropy by,i i H H div S , ? = ? = ? ? (3.10)\par
Again we know the relations, C aT T C S T kk E 0 0 1 0 + + = ? ? ? ? ? (3.11) S T q i i ? 0 , ? ? = (3.12) i i K q t , 0 1 ? ? ? ? ? = ? ? ? ? ? ? ? ? ? ? + (3.? = ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? + ? ? + + + V i i i dV H H t t K T 0 1 1 0 0 , ? ? ? ? ? (3.17) Now, ? ? ? ? ? + + + = V V kk V E A i i V i i dV C a dV dV T C dA H n ? ? ? 1 0 , (3.18)\par
Using the equation  {\ref (3.18)}, from the equation (3.17) we obtain,? ? ? ? + + + V V kk V E A i i dV C a dV dV T C dA H n ? ? ?? ? ? ? ? ? ? ? ? 1 0 0 1 1 0 0 = ? ? ? ? ? ? ? ? ? ? + ? ? + ? + + dV H H t t K T i V i ? ? ? ? (3.19)\par
Here we introduce heat potential function,    {\ref (} )? = V E dV T C IP? ? ? ? ? ? ? ? ? ? ? + ? ? = + + V i i dV H H t t K T ID ? ? ? ? ?0 1 = + + + + ? ? ? V V kk A i i dV C a dV ID IP dA H n ? ? ?? ? ? ? ? ? (3.23)\par
This is the second variational equation connected with heat conduction. In order to obtain the variational equation connected with the process of thermodiffusion we introduce another vector as was done by Sherief et al \hyperref[b11]{[12]} related with mass concentration by, C i i ? ? = , ? (3.26) i i DP t , 1 1 ? = ? ? ? ? ? ? ? ? ? ? + ? ? ? ? (3.27)\par
and using the equation (3.24) we obtain,i i G ? = ? (3.28) i i DP G t t , 1 1 1 ? = ? ? ? ? ? ? ? ? ? ? + ? ? + + ? ? ? (3.29)\par
Now multiplying both sides of equation (3.29) by i G ? and then integrating over the region V we obtain,  ? = ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? + ? ? + + + V i i i dV G G t t D P 0 1 1 1 1 , ? ? ? ? (3.30) Now, ? ? ? ? ? ? ? + = V V kk V A i i V i i dV C a dV C dV C C b dA G n P dV G P ? ? ? ? ? ? ? ? 2 ,? ? ? ? ? = ? ? ? ? ? ? ? ? ? ? + ? ? + ? + ? + + V i i V V V kk A i i dV G G t t D dV C a dV C C b dV C dA G n P 0 1 1 1 1 2 ? ? ? ? ? ? ? ? ? ? ? (3.? ? ? ? ? ? ? ? ? ? ? + ? ? = ? + + V i i dV G G t t D D I ? ? ? ? ? 1 1 1 1 (3.35)\par
Therefore, from the equation (3.32) we obtain, 
\section[{(}]{(}\par
)     0 2 = ? + ? + ? ? ? ? ? D I P I dV C a dV C dA G n P V V kk A i i ? ? ? ? ? ? ? (3.? W ] ? ? ? ? ? = ? ? + + ? + + A i i A i i V kk dA G n P dA H n dV C D I ID P I IP ? ? ? ? ? 2 ? ? ? ? ? ? ? ? + + + + V i i V i i A i i V i i A i i V i i dV j dV u u dA m dV l dA u p dV u F ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? (3.37) Now, dt u u i i ? = ? , dt ? ? ? ? = , dt H H i i ? = ? , dt G G i i ? = ? etc. Therefore, equation (3.37) reduces to, [ dt d W +K ] ? ? ? + = + ? + + ? + + V i i V i i V dV l dV u F dV P b a D I ID P I IP ? ? ? ? ? ? ? ? ? ? ? ? + ? ? + + + A i A A i i A i i\begin{figure}[htbp]
\noindent\textbf{}\includegraphics[]{image-2.png}
\caption{\label{fig_0}}\end{figure}
                  \begin{figure}[htbp]
\noindent\textbf{} \par 
\begin{longtable}{P{0.5144736842105263\textwidth}P{0.022368421052631576\textwidth}P{0.04473684210526315\textwidth}P{0.022368421052631576\textwidth}P{0.04473684210526315\textwidth}P{0.022368421052631576\textwidth}P{0.04473684210526315\textwidth}P{0.06710526315789474\textwidth}P{0.06710526315789474\textwidth}}
d\tabcellsep d\tabcellsep ji\tabcellsep m\tabcellsep ji\tabcellsep d\tabcellsep ij\tabcellsep TdS\tabcellsep PdC\\
2011\tabcellsep \tabcellsep \tabcellsep \tabcellsep \tabcellsep \tabcellsep \tabcellsep \tabcellsep \\
December\tabcellsep \tabcellsep \tabcellsep \tabcellsep \tabcellsep \tabcellsep \tabcellsep \tabcellsep \\
I )\tabcellsep \tabcellsep \tabcellsep \tabcellsep \tabcellsep \tabcellsep \tabcellsep \tabcellsep \\
(\tabcellsep \tabcellsep \tabcellsep \tabcellsep \tabcellsep \tabcellsep \tabcellsep \tabcellsep \\
Global\tabcellsep \tabcellsep \tabcellsep \tabcellsep \tabcellsep \tabcellsep \tabcellsep \tabcellsep \end{longtable} \par
 
\caption{\label{tab_1}}\end{figure}
 \begin{figure}[htbp]
\noindent\textbf{40} \par 
\begin{longtable}{P{0.159375\textwidth}P{0.10625\textwidth}P{0.053125\textwidth}P{0.10625\textwidth}P{0.10625\textwidth}P{0.10625\textwidth}P{0.053125\textwidth}P{0.159375\textwidth}}
DbC\tabcellsep ii\tabcellsep D\tabcellsep kk\tabcellsep Da\tabcellsep ii\tabcellsep t\tabcellsep t C\end{longtable} \par
 
\caption{\label{tab_3}40 )}\end{figure}
 			\footnote{© 2011 Global Journals Inc. (US)} 			\footnote{December} 			\footnote{Global I ) 2011 December ( A Unified Field Approach on Fractional-Ordered Micropolar Thermoelasticity with Diffusion} 		 		\backmatter  			 
\subsection[{UNIQUENESS THEOREM}]{UNIQUENESS THEOREM}\par
Uniqueness theorem states that there is only one solution of the equations  {\ref (2.25)} ( ) ( )\par
, where the body occupying the region V bounded by the surface .\par
Proof : We consider, if possible, there exist two sets of solutions ( )  {\ref , ?  ?   and (} ) 			 			  				\begin{bibitemlist}{1}
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