F. Heat transfer coefficientsHeat transfer coefficient for convection fromthe cover to the environment, caused by air flow(wind) hc , c / ais given by the following relation je(Duffie i Beckman [12]):A ch c , c / a5.7 3.8 (11)A rHeat transfer coefficient for the radiation ofheat between the transparent cover and the sky hr , c / sis calculated by :2 2hr , c/s c Tc Ts Tc Ts (12)Convective heat transfer coefficient betweenthe surrounding pipe layer and the transparent cover,hc , e / cmay be calculated by [14]:Te Tc Aeh, / 3.25 0 .0085(13)c e c 4re ArHeat transfer coefficient originating from theradiation form the surrounding pipe layer to thetransparent cover hr , e / cis given by [14]:A cA r2 2 Te Tc Te Tc Aeh r , e / c1 / c Ae / Ac 1 / c 1 Ar(14)Heat transfer by convection through theevacuated area between the collector pipes and thesurroundin collector layer may be neglected, so theheat transfer ceofficient by convection is hc , r / e 0 .Heat transfer coefficient for radiation from thecollector pipe to the collector surrounding layerh r r e, is given as:, /2 2Te Tr Te Tr h r , r / e1 / r Ar / Ae 1 / e 1(15)Total heat transfer coefficient U r/f between the outsidesurface of the collector pipe and the working fluid is[14] :1U r / f (16)rr , o ln r, o /r, i Ar , orhfAr , iWhere r r,o i r r,i are outside and inside radiusof the pipe of the collector , λ r heat conductioncoefficient of the collector pipe h f coefficient of heattransfer by convection from the internal surface of thepipe of the collector to the working fluid. Coefficientof heat transfer by convection, from the internal pipeside to the fluid h f , is given as:N uf fh f(17)dWhere N uf is the Nusselt number calculatedaccording to Sieder and Tate relation [16, 17]:For laminar fluid flow through the pipe Re
Discretization energy balance equations for theworking fluidIn order create a discretized equation for the workingfluid, a control volume around a node I, is taken, asshown on Fig 3. Node i is marked by P, and theneighbouring nodes. Node i-1 i i+1 are marked by Wand E, respectively. Since the time is a one waycoordinate the solution is obtained by “marshcing”through time beginning with initial temperature field.Temperature T is set for the nodes in the t time step,and T values in the time step t+Δt should be found."Old" (set) values for T in the nodes will be marked0T fP ,0T fE ,0T fW and "new" (unknown) values in t+Δttimestep are marked as1T fP ,1T fE ,1T fW .Discretization of the diferential equations of energybalance for the working fluid is possible to conductby its integration for the control volume as on Fig.3.In the time interval t to t+Δt:W (i-1)wP (i)Figure 3. Grid for the working fluid of the CPC collectorT* *e t t ffcpfAfdtdzw t tz*t t e T* fcpfAffwzdzdtt w zt t eUr / fTrTf2 rr , odzdtt w(20)The order of the integration was chosen according theTto nature of the term. For the representation of ,tprevailing value for T in a node for "stepwise"scheme in the control volume. Which leaves:* *e t t Tf * * 1 0fcpfAfdtdz fcpfAfz TfPTfPw t t (21)For the integration of the convective term upwindscheme is used, thus the values of temperature at themid surface is equal to the value of temperature in thenode of the upwind side of the node:ezE (i+1)zAccording to the assumption of the model* *that this is an uncompressible fe we i and* *AfeAfwmore simple writing, new operator is introducedwe have that wze w zw. Further, due toA,B standing for the greater value from A and B.New sign F is introduced which stands for the*convection intensity (flow): Fe fewzei*Fwfwwzw.By sorting the equation (20) an equation for a node i)1for the fluid in the time step (1) is, T f , i :TtDiscretization of the energy balance equationfor collector pipe(23)By integragine differential equation of the energybalance for the collector pipe for the control volumein the dime interval from t to t+Δt, and then sorting,the equation for the node (i) temperature of the pipe inthe time step (1) is T 1 r , i :0 0 01 t b1 T , 1 b2T , b3 TTr i r i r, i 1r , i * * 0 0 r c r A r z b4T f , ib5Te , i b6(24)Equation (29) is a general equation set for any internalcontrol volume of the collector pipe. Boundary nodesi=1 and i=M are on adiabatic boundary. For theadiabatic boundaryTz0 .a T a T a T a T100 00f , i * * 1 f , i12 f , i 3 f , i14 r,ifcpfAfzDiscretization of the energy balanceequation for the transparent cover of thecollectorIn the same fashion, by integrating differentialequation for the energy balance equation fortransparent cover collector for the control volume inthe time interval t to t+Δt, an equation for temperatureof the node (i) is gained for the cover of the collectorin the time step (1)1 t0 0 0Te, i * *c1T e, i c2Tr , i c3Tc , i c4 e c e A e z(25)c*t t e T* fpfAffwzdzdtt w z0 0T , 0 , 0*fPFeTfEFecpfAft0 0TfWFw, 0 TfPFw, 0(22)Discretization of the energy balance equationfor transparent coverBy integrating the energy balance differentialequation for the tranparent cover for the controlvolume in the time interval t to t+Δt, an equation for105
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4 4 th IEEE International Symposium
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EXPRES 20124 th International Sympo
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Application of Thermopile Technolog
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Design of a Solar Hybrid System....
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environmental protection and global
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But can we use the human body sweat
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IX. REFERENCES[1] Todorovic B. Cvje
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Analysis of the Energy-Optimum of H
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V. OBJECTIVE FUNCTIONThe objective
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The Set-Up Geometry of Sun Collecto
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continuous east-west sun collector
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continuously measure the thermal ch
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CEvaluation of measurement resultsA
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Application of Thermopile Technolog
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Temperature of the components [C]90
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nighttime, to weather or to the cha
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To find the reasons for this disagr
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Toward Future: Positive Net-Energy
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EnergyPlus environment, we used mod
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