999精品在线视频,手机成人午夜在线视频,久久不卡国产精品无码,中日无码在线观看,成人av手机在线观看,日韩精品亚洲一区中文字幕,亚洲av无码人妻,四虎国产在线观看 ?

The Influence of Gravitational Field on Generalized Thermoelasticity with Two-Temperature under Three-Phase-Lag Model

2015-12-12 11:58:15MohamedOthmanHasonaandNehalMansour
Computers Materials&Continua 2015年3期

Mohamed I.A.Othman,W.M.Hasonaand Nehal T.Mansour

The Influence of Gravitational Field on Generalized Thermoelasticity with Two-Temperature under Three-Phase-Lag Model

Mohamed I.A.Othman1,2,3,W.M.Hasona2,4and Nehal T.Mansour2,5

The problem of the generalized thermoelastic medium for three different theories under the effect of a gravitational field is investigated.The Lord-Shulman,Green-Naghdi III,three-phase-lag theories are discussed with two temperature.The normal mode analysis is used to obtain the analytical expressions of the displacement components,force stress,thermodynamic temperature and conductive temperature.The numerical results are given and presented graphically,when the thermal force is applied.Comparisons are made with the results predicted by three-phase-lag model,Green-Naghdi III and Lord-Shulman theories in the presence and absence of gravity as well as two temperature.

gravity,three-phase-lag,thermoelastic,thermodynamic temperature,conductive temperature,normal-mode.

Nomenclature

λ,μ Lame’s parameter counterparts

u,wdisplacement components

ggravity

athe volume coefficient of thermal expansion

δijKronecker delta

ρ mass density

cespecific heat at constant strain

K(≥0) thermal conductivity

K?material characteristic of the theory

Tthermodynamic temperature

T0reference temperature

φ conductive temperature

τvphase lag of thermal displacement gradient

τtphase lag of temperature gradient

τqphase lag of heat flux

b constant material"two temperature parameter"

ωijskew symmetric tensor called the rotation tensor

1 Introduction

The effect of mechanical and thermal disturbances on an elastic body is studied by the theory of thermoelasticity.This theory has two defects,it has been studied by Biot(1956).He deals with a defect of the uncoupled theory that mechanical causes have no effect on temperature.This theory predicts an in finite speed of propagation of heat waves which is a defect that it shares with the uncoupled theory.The first theory was studied by Lord and Shulman(1967),who formulated the generalized thermoelasticity theory involving one thermal relaxation time.The second theory was discussed by Green-Lindsay(1972).They introduced two different relaxation times in the entropy expression and stress-strain relations.The third generalization of the coupled theory of thermoelasticity introduced by Green and Naghdi(1993)whose developed different theories labeled type I,type II,and type III.The Green-Naghdi(G-N)theory of type I in the linearized theory is equivalent to the classical coupled thermoelasticity theory,the(G-N)theory of type II does not admit energy dissipation,and the third(G-N)theory of type III admits dissipation of energy and the heat flux is a combination of type I and type II.The fourth generalization of the coupled theory of thermoelasticity is developed by Tzau(1995)and Chandrasekhariah(1998)and is referred to the dual-phase-lag thermoelasticity.Abbas and Othman(2012)have studied the generalized thermoelsticity of thermal shock problem in an isotropic hollow cylinder and temperature dependent elastic moduli.Raychoudhuri(2007)has recently introduced the three-phase-lag,heat conduction equation in which the Fourier law of heat conduction is replaced by an approximation to a modi fication of the Fourier law with the introduction of three different phase-lag for the heat flux vector,the temperature gradient and the thermal displacement gradient.The stability of the three-phase-lag,the heat conduction equation is discussed by Quintanilla and Racke(2008).Reflection and transmission of waves from the imperfect boundary between two heat conducting micropolar thermoelastic solids by Marin(2014a).Weak solutions in elasticity of dipolar bodies with stretch were studied by Marin(2013).On temporal behav-ior of solutions in thermoelasticity of porous micropolar bodies by Marin(2014b).The effect of initial stress on generalized thermoelastic medium with three-phaselag model under temperature dependent properties has studied by Othman et al.(2014a).Subsequently Kar and Kanoria(2009)have employed this theory of thermoelasticity with three-phase-lag to discuss a problem of thermoelastic interactions on functional graded orthotropic hollow sphere under thermal shock.

In the classical theory of elasticity,the gravity effect is generally neglected.Generalized thermoelastic medium with temperature-dependent properties for different theories under the effect of gravity field has studied by Othman et al.(2013a).The effect of gravity in the problem of propagation of waves in solids,in particular on an elastic globe,was first studied by Bromwich(1898).The influence of the gravitational field and rotation on a generalized thermoelastic medium using a dual-phase-lag model has studied by Othman et al.(2013b).Subsequently,an investigation of the influence of the gravitational field and rotation on thermoelastic solid with voids under Green-Naghdi theory was considered by Othman et al.(2013c).The effect of gravity on the surface waves,on the propagation of waves in an elastic layer has been studied by De and Sengupta(1974 and 1978).The effect of rotation on micropolar generalized thermoelasticity with two temperature using a dual-phase-lag model has studied by Othman et al.(2014b).Generalized thermoelsticity of thermal shock problem in a non-homo-geneous isotropic hollow cylinder with energy dissipation studied by Othman and Abbas(2012).

The two temperature theory of thermoelasticity was introduced by Gurtin and Williams(1967),Chen and Gurtin(1968),and Chen et al.(1968),in which the classical Clausius-Duhem inequality was replaced by another one depending on two temperature;the conductive temperature and the thermodynamic temperature,the first is due to the thermal processes,and the second is due to the mechanical processes inherent between the particles and the layers of elastic material,this theory was also investigated by Iesan(1970).The two-temperature model was underrated and unnoticed for many years thereafter.Only in the last decade has the theory been noticed,developed in many works,and find its applications,mainly in the problems in which the discontinuities of stresses have no physical interpretations.Among the authors who contribute to develop this theory,Quintanilla(2004)studied existence,structural stability,convergence and spatial behavior of this theory.Youssef (2006) introduced the generalized Fourier’s law to the field equations of the two-temperature theory of thermoelasticity and proved the uniqueness of the solution for homogeneous isotropic material,Puri and Jordan(2006)studied the propagation of harmonic plane waves.Recently,Maga?a and Quintanilla(2009)have studied the uniqueness and growth solutions for the model proposed by Youssef(2006).

The present paper is concerned with the investigations related to the effect of gravity with two temperature on a generalized thermoelastic medium based on threephase-lag model by applying the normal mode analysis.Also,the effect of gravity and two-temperature on the physical quantities are discussed numerically and illustrated graphically.

2 Formulation of the problem and basic equations

We consider a homogeneous thermoelastic half-space with two-temperature under the influence of gravity.All the considered quantities are functions of the time variabletand of the coordinatesxandzWe consider the normal source acting on the plane surface of generalized thermoelastic half-space under the influence of gravity.The system of governing equations of a linear thermoelasticity with gravity and without body forces consists of:

The stress-strain relation written as:

The equation of motion in the absence of body force

The equation of heat conduction under three phase lag model

For a two dimensional problem inxz-plane,Eqs.(2)-(4)can be written as:

For the purpose of numerical evaluation,we introduce dimensions variables

Using the above dimensions quantities,Eqs.(8)-(10)become

We define displacement potentialsqand ψ which relate to displacement componentsuandwas,

Using Eq.(14)in Eqs.(11)-(13),we obtain:

3 Normal mode analysis

The solution of the considered physical variable can be decomposed in terms of normal modes as the following form

Where,ω is the complex time constant andais the wave number inx-direction.Using(18)in Eqs.(15)-(17),we obtain

The solution of Eq.(22)has the form

Where,Mn(n=1,2,3)are some constants,are the roots of the characteristic equation of Eq.(22).

Dimensionless variables of the stress components yields the following,

Using Eq.(14)and Eqs.(23)-(26)in(27)-(29)

Where,

4 Boundary conditions

The boundary conditions on the plane surfacez=0 are:

Using Eqs.(32),(34)and(35)in boundary conditions(36),we get three equations in three constantsMn(n=1,2,3)as:

Solving Eqs.(37)-(39)the constantsMn(n=1,2,3)are defined as follows:

Where,

5 Numerical results

To study the effect of gravity and two-temperature,we now present some numerical results.For this purpose,copper is taken as the thermoelastic material for which we take the following values of the different physical constants.

The numerical technique,outlined above,was used for the distribution of the real part of the temperatureT,the displacement componentsu,wand the stress components σxx,σzz,σxzfor the problem.There are three lines expressing theories are,the"solid line"expresses the 3PHL theory,the"cross line"expresses the L-S theory,and the"dashed line"expresses the G-N III theory.Figs.1(a,b)-6(a,b)show the distribution of the physical quantities based on L-S,G-N III and 3PHL in the case ofg=0,9.8 respectively.Fig.1(a,b)depict that the displacement componentuincreases with the increase of gravity in the three theories.In the absence and presence of gravity(i.e.g=0,9.8),ubegins to increase then smooth decreases and takes the form of wave and try to return to zero.Fig.2(a,b)exhibit that the displacement componentwincreases with the decrease of gravity,and takes the form of a wave until it develops to zero,that’s mean that the displacementwis inversely proportional with gravity.Fig.3(a,b)demonstrate that the behavior of temperatureTdecreases forg=0,9.8 and takes the form of a wave until it develop to zero.Fig.4(a,b)show that the stress component σxzincreases with the increase of gravitygin L-S,and decreases with the decrease of the gravity in G-N III and 3PHL and takes the form of the wave until it develop to zero.Fig.5(a,b)depict that the stress component σxxbegins from the value zero and satis fies the boundary condition atz=0 in the three theories.The stress component σxxdecreases with the increase of gravity in L-S and 3PHL,and decreases during the period 0≤z≤1,then increasing and takes the form of the wave until it develop to zero atg=9.8 in G-N III,while increases in the period 0≤z≤1,then decreasing and takes the form of the wave until it develop to zero atg=0 in G-N III.Fig.6(a,b)explain that the stress component σzzdecreases in the case ofg=0,9.8 and decays to zero.

Figs.7(a,b)-12(a,b)exhibit the distribution of the physical quantities based on L-S,G-N III and 3PHL in the case ofb=0,0.1.Fig.7(a,b)show that the displacement componentuincreases with the increase ofbin G-N III and L-S theories,while,it decreases with the increase ofbin 3PHL theory,and try to return to zero at infinity in three theories.Fig.8(a,b)demonstrate that the displacement componentwincreases atb=0.1,in three theories,in the range 0≤z≤1,while decreases atb=0,in 3PHL theory,then,increases atb=0,in the range 0≤z≤0.5,in G-N III and L-S theories,and takes the form of the wave until it develop to zero in three theories.Fig.9(a,b)explain that the temperature satis fies the boundary conditions atz=0 and decreases,in the three theories to a minimum value in the range 0≤z≤1,atb=0.1,while,increases forz≥0.75,atb=0,then,it decays to zero in the two cases.Fig.10(a,b)explain that the stress component σxzdecreases atb=0.1,in the range 0≤z≤0.5 of the three theories,while decreases in the range 0≤z≤0.5 forb=0 in the two theories L-S and 3PHL,but it increases forb=0 in G-N III,and takes the form of the wave until it develop to zero in L-S and G-N III and 3PHL theories.Fig.11(a,b)show that the stress component σxxsatis fies the boundary condition and decreases to a minimum value in the range 0≤z≤1,and increases in the range 1≤z≤2,but,decays to zero in the three theories,forb=0.1,while,increases in the range 0≤z≤0.5 forb=0 in 3PHL and G-N III theories and decays to zero,then,decreases in the range 0≤z≤0.5 forb=0,and increases in the range 0.5≤z≤1 forb=0 until it develop to zero in L-S theory.Fig.12(a,b)show that the stress component σzzdecreases forb=0.1,in the three theories,and it decreases forb=0,in L-S and G-N III,but increases forb=0,in 3PHL then,decays to zero.

Figure 1:Distribution of displacement component u in the presence and absence of g.

Figure 2:Distribution of displacement component w in the presence and absence of g.

Figure 3:Distribution of the temperature T in the presence and absence of g.

Figure 5:Distribution of the stress component σxxin the presence and absence of g.

Figure 6:Distribution of the stress component σzzin the presence and absence of g.

Figure 7:Distribution of displacement component u in the presence and absence of b.

Figure 8:Distribution of displacement component w in the presence and absence of b.

Figure 9:Distribution of the temperature T in the presence and absence of b.

Figure 10:Distribution of the stress component σxzin the presence and absence of b.

Figure 11:Distribution of the stress component σxxin the presence and absence of b.

Figure 12:Distribution of the stress component σzzin the presence and absence of b.

6 Conclusion

By comparing the figures obtained under the three theories,important phenomena are observed:

1.Analytical solutions based upon normal mode analysis of the thermoelastic problem in solids have been developed.

2.The method that is used in the present article is applicable to a wide range of problems in hydrodynamics and thermoelasticity.

3.There are significant differences in the field quantities under GN-III,3PHL and L-S theories.

4.The presence of the gravitational field and two-temperature plays a significant role on all physical quantities.

5.The comparison of the three theories of thermoelasticity,Lord-Shulman theory,three-phase-lag model and Green-Naghdi III is carried out.

6.The value of all the physical quantities converges to zero,and all the functions are continuous.

Abbas,I.A.,Othman,M.I.A.(2012):Generalized thermoelsticity of thermal shock problem in an isotropic hollow cylinder and temperature dependent elastic moduli.Chinese Physics B,vol.21,no.1,pp.14601-14606.

Biot,M.A.(1956):Thermoelasticity and irreversible thermodynamics.Journal of Applied Physics,vol.7,pp.240-253.

Bromwich,T.J.(1898):On the influence of gravity on elastic waves and in particular on the vibrations of an elastic globe.The Proceedings of the London Mathematical Society,vol.30,pp.98-120.

Chandrasekharaiah,D.S.(1998):Hyperbolic thermoelasticity:A review of recent literature.Applied Mechanics Reviews,vol.51,pp.705-729.

Chen,P.J.;Gurtin,M.E.(1968):On a theory of heat conduction involving two temperatures.Journal of Applied Mathematics and Physics,vol.19,pp.614-627.

Chen,P.J.;Gurtin,M.E.;Williams,W.O.(1968):A note on non-simple heat conduction.Journal of Applied Mathematics and Physics,vol.19,pp.969-970.

De,S.N.;Sengurta,P.R.(1974):In fluence of gravity on wave propagation in an elastic layer.The Journal of the Acoustical Society of America,vol.55,pp.919-921.

De,S.N.;Sengurta,P.R.(1976):Surface waves under the influence of gravity.Gerlands Beitr Geophys(Leipzig),vol.85,pp.311-318.

Green,A.E.;Lindsay,K.A.(1972):Thermoelasticity.Journal of Elasticity,vol.2,pp.1-7.

Green,A.E.;Naghdi,P.M.(1993):Thermoelasticity without energy dissipation.Journal of Elasticity,vol.31,pp.189-209.

Gurtin,M.E.;Williams,W.O.(1967):An axiom foundation for continuum thermo-dynamics.Archive for Rational Mechanics and Analysis,vol.26,pp.83-117.

Ie?san,D.(1970):On the linear coupled thermoelasticity with two-temperatures.Journal of Applied Mathematics and Physics,vol.21,pp.583-591.

Kar,A.;Kanoria,M.(2009):Generalized thermoelastic functionally graded orthotropic hollow sphere under thermal shock with three-phase-lag effect.EuropeanJournal of Mechanics-A/Solids,vol.28,pp.757-767.

Lord,H.W.;Shulman,Y.A.(1967):Generalized dynamical theory of thermoelasticity.Journal of the Mechanics and Physics of Solids,vol.15,pp.299-309.

Maga?a,A.;Quintanilla,R.(2009):Uniqueness and growth of solutions in two temperature generalized thermoelastic theories.Mathematics and Mechanics of Solids,vol.14,pp.622-634.

Marin,M.(2013):Weak solutions in elasticity of dipolar bodies with stretch.Carpathian Journal of Math,vol.29,no.1,pp.33-40.

Marin,M.(2014a):Reflection and transmission of waves from imperfect boundary between two heat conducting micropolar thermoelastic solids.Annales Universitatis Scientiarum Ovidius,Mathematics Series,vol.22,no.2,pp.151-175.

Marin,M.(2014b):On temporal behaviour of solutions in thermoelasticity of porous micropolar bodies.Annales Universitatis Scientiarum Ovidius,Mathematics Series,vol.22,no.1,pp.169-188.

Othman,M.I.A.;Abbas,I.A.(2012):Generalized thermoelsticity of thermal shock problem in a non-homogeneous isotropic hollow cylinder with energy dissipation.International Journal of Thermophysics,vol.33,no.5,pp.913-923.

Othman,M.I.A.;Elmaklizi,Y.D.;Said,S.M.(2013a):Generalized thermoelastic medium with temperature-dependent properties for different theories under the effect of gravity field.International Journal of Thermophysics,vol.34,pp.521-537.

Othman,M.I.A.;Hasona,W.M.;Eraki,E.M.(2013b):In fluence of gravity field and rotation on a generalized thermoelastic medium using a dual-phase-lag model.Journal of Thermoelasticity,vol.1,pp.2328-2401.

Othman,M.I.A.;Zidan,M.E.M.;Hilal,M.I.M.(2013c):The influence of gravitational field and rotation on thermoelastic solid with voids under Green-Naghdi theory.Journal of Physics,vol.2,pp.22-34.

Othman,M.I.A.;Hasona,W.M.;Abd-Elaziz,E.M.(2014a):The effect of initial stress on generalized thermoelastic medium with three-phase-lag model under temperature dependent properties.Canadian Journal of Physics,vol.92,pp.448-457.

Othman,M.I.A.;Hasona,W.M.;Abd-Elaziz,E.M.(2014b):Effect of rotation on micropolar generalized thermoelasticity with two temperature using a dualphase-lag model.Canadian Journal of Physics,vol.92,pp.149-158.

Puri,P.;Jordan,P.M.(2006):On the propagation of harmonic plane waves under the two-temperature theory.International Journal of Engineering Science,vol.44,pp.1113-1126.

Quintanilla,R.(2004):On existence,structural stability,convergence and spatial behavior in thermoelasticity with two-temperatures.Acta Mechanica,vol.168,pp.61-73.

Quintanilla,R.;Racke,R.(2008):A note on stability in three-phase-lag heat conduction.International Journal of Heat and Mass Transfer,vol.51,pp.24-29.

Roy Choudhuri,S.K.(2007):On thermoelastic three phase lag model.Journal of Thermal Stresses,vol.30,pp.231-238.

Tzou,D.Y.(1995):A uni fied field approach for heat conduction from macro to microscales.The ASME Journal of Heat Transfer,vol.117,pp.8-16

Youssef,H.M.(2006):Theory of two-temperature generalized thermoelasticity.IMA,Journal of Applied Mathematics,vol.71,pp.383-390.

1Department of Mathematics,Faculty of Science,Taif University 888,Saudi Arabia.

2Department of Mathematics,Faculty of Science,Zagazig University,P.O.Box 44519,Zagazig,Egypt.

3E-mail:m_i_a_othman@yahoo.com

4E-mail:wahedhasona@yahoo.com

5E-mail:nehal.tarek23@yahoo.com

主站蜘蛛池模板: 8090成人午夜精品| 午夜精品国产自在| 国产视频入口| 国模沟沟一区二区三区| 亚洲一区二区精品无码久久久| 人人91人人澡人人妻人人爽| 无码中字出轨中文人妻中文中| 免费无码在线观看| 久久先锋资源| 欧美激情伊人| 免费国产在线精品一区| 国产成人喷潮在线观看| AV无码无在线观看免费| 小说区 亚洲 自拍 另类| 欧美自慰一级看片免费| 素人激情视频福利| 国产欧美又粗又猛又爽老| 好吊妞欧美视频免费| 色婷婷亚洲综合五月| 国产成人久视频免费| 漂亮人妻被中出中文字幕久久| 青青操国产视频| 国产一区亚洲一区| 国产大片黄在线观看| 欧美激情首页| 先锋资源久久| 欧美日韩国产成人在线观看| 在线观看国产精品第一区免费| 久久a毛片| 亚洲美女一级毛片| 午夜人性色福利无码视频在线观看| 亚洲男人天堂2020| 粗大猛烈进出高潮视频无码| 国产精品成人免费视频99| 国产成人免费手机在线观看视频| 91欧美在线| 亚洲免费福利视频| 久草性视频| 亚洲天堂首页| 中国国产A一级毛片| 黄色网址手机国内免费在线观看| 欧美国产日韩在线观看| 色综合中文| 国产成人成人一区二区| 老汉色老汉首页a亚洲| 5555国产在线观看| 欧美国产在线看| 国产亚洲精品在天天在线麻豆| 日日拍夜夜嗷嗷叫国产| 国产xx在线观看| 国产va视频| 国产香蕉在线视频| 欧美国产日韩一区二区三区精品影视| 久久婷婷六月| 精品1区2区3区| 精品少妇人妻无码久久| 国产在线拍偷自揄观看视频网站| 国产精品福利在线观看无码卡| 无遮挡国产高潮视频免费观看 | 国产日韩久久久久无码精品| 国产区人妖精品人妖精品视频| 久久国产精品夜色| 91亚洲影院| 中文无码精品a∨在线观看| 天天做天天爱夜夜爽毛片毛片| 国产精品女人呻吟在线观看| 国产丝袜第一页| 四虎亚洲国产成人久久精品| 国产福利在线免费| 亚洲无码精品在线播放| 国产精品一区不卡| 国产理论最新国产精品视频| 天天干伊人| 婷婷丁香在线观看| 波多野结衣一区二区三区四区视频| 日本精品中文字幕在线不卡| 激情六月丁香婷婷| 天堂中文在线资源| 国产一区二区三区免费观看| 无遮挡一级毛片呦女视频| 国产亚洲欧美日本一二三本道| 黄色一级视频欧美|