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Thermodynamics Problems: Heat Transfer and Temperature Profiles, Assignments of Heat and Mass Transfer

Solutions to five thermodynamics problems involving heat transfer and temperature profiles. The problems cover concepts such as heat conduction, energy balance, and boundary conditions. The solutions include calculations and formulas for temperature differences, heat flux, and energy accumulation.

Typology: Assignments

2011/2012

Uploaded on 04/27/2012

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koofers-user-tgr-1 🇺🇸

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Download Thermodynamics Problems: Heat Transfer and Temperature Profiles and more Assignments Heat and Mass Transfer in PDF only on Docsity! Problem 1 For a constant mass, pressure process p dT Q mC dt = so ( ) f f i i T Tt t t p p p 0 0 T T dT Q Qdt mC dt m C dT mR C / R dT dt = = = =∫ ∫ ∫ ∫ ( )f i T 2 t T Q mR A BT CT dT= + +∫ ( ) ( ) ( )2 2 3 3t f i f i f iB CQ mR A T T T T T T2 3  = − + − + −   The molecular weight of water is 18g / mol , so 1 mol m 500 g x 27.78 mol 18 g = = , or J 1 mol R 8.314 x 0.4619 J / g K mol K 18 g = = − − o i o 3 6 f T 25 C 298.15K T 100 C 373.15K A 8.712 B 1.25 x10 C 0.18x10− − = = = = = = = − so 5tQ 1.58 x10 J =  Problem 2 at thermal equilibrium, f f1 2 fT T T= = For block 1: ( )f i T 1 t,1 1 1 1 1 f 1T U Q m C dT m C T T∆ = = = −∫ (constant mass; no volume change) For block 2: ( )2 t,2 2 2 f 2U Q m C T T∆ = = − with t ,1 t ,2Q Q= − then ( ) ( )1 1 f 1 2 2 f 2m C T T m C T T− = − − ( ) ( ) ( ) 1 1 f 1 2 2 f 2 f 1 1 2 2 1 1 1 2 2 2 m C T T m C T T 0 T m C m C m C T m C T − + − = + = + 1 1 1 2 2 2f 1 1 2 2 m C T m C T T m C m C  += +  The final temperature is simply a weighted average of the initial temperatures, with the weights related to the product mC for each block. For ( )1 2 1 2 f 1 2 1 m m , C C T T T 2 = = = + ( ) ( )1 2 1 2 f 1 1 2 2 1 2m m , C C T m T m T / m m≠ = = + + Since t ,1 t ,2 t ,1Q Q , we choose to solve for Q= − , in which ( ) ( )1 1 2 2 11 1 1 2 2 2t,1 1 1 f 1 1 1 1 1 2 2 1 1 2 2 m C m C )Tm C T m C T Q m C T T m C m C m C m C m C + += − = − + +  so ( )1 1 2 2 2 1 1 t,1 1 1 2 2 m C m C T T U Q m C m C −  ∆ = = +  ( )1 1 2 2 1 2 2 t,2 1 1 2 2 m C m C T T U Q m C m C −  ∆ = = +  where 1 2U U∆ = −∆ m1 C1 m2 C2 T1 T2 T1 f T2 f time (seconds) T To T1 a 3a 0 time (seconds) 0 Q a 3a ( ) ( )11 oo T T m A B T T a − + −   ( )1 omA T T a − ( )1 2 omA T T a − − ( ) ( )11 2 o o T T m A B T T a − − + −   time (seconds) Qt 0 a 3a 0 ( ) ( ) 2 1 1 2 o o B T T m A T T  − − +     (A,B>0) Problem 4 For one dimensional steady-state conduction, with constant cross-sectional area ( )1 2T Tq k L − = The x-axis is defined such that the + x direction is to the right. Hence, if q > 0 then heat is flowing from left to right, or in the + x direction. If q < 0, then heat is flowing from right to left, or in the –x direction. Also, dT q k dx = − Fourier’s Law of heat conduction so dT q k 25 W / m K L 0.5 m dx k = − = − = Case 1: 1 2T 400K T 300K= = so ( )( ) 225W / m K 100Kq 5000W / m 0.5m − = = dT q 200 K / m dx k = − = − or ( ) ( )2 1T T 300 400 KdT 200 K / m dx L 0.5 m − − = = = − Case 2: o1 dT T 100 C 250K / m dx = = − 2 dT q k 6250W / m dx = − = Now 1 2 qL T T 125K k − = = this unit is really a temperature difference and not an absolute temperature Note that 1 degree Kelvin = 1 degree o C so o2T 25 C= − x T 0 L 180oC 80oC direction of heat flux dT/dx>0 T2 T1 Case 3: 2 dT W K q k 25 200 5000 W / m dx m K m   = − = − = −  −   1 2 o o 1 o 2 qL T T 100K k 100 C with T 80 C then T 180 C − = = − = − = = Case 4: ( ) ( )( ) ( ) 2 o 1 2 0.5mqL T T 4000W / m 80K 80 C temperature difference k 25W / m K − = = = = − with o2T 5 C= − then o1T 75 C= Finally, ( )1 2 2 1T T T TdT q 160K / m dx k L L − −−= = − = = − Case 5: ( ) ( )( ) 2 1 2 0.5mqL T T 3000W / m 60K k 25W / m K − = = − = − − with o o1 2T 30 C, then T 90 C= = 2 1 T TdT 120K / m dx L −= = Case 2 Case 3 x T 0 L T1 T2 100oC -25oC direction of heat flux dT/dx<0
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