Question 6.16: During the period when hot water is not flowing through the ...

During the period when hot water is not flowing through the faucet, it cools in the pipes by surface convection and surface-radiation heat transfer from the pipe surface. This is shown in Figure (a). Assume that the vertical portion of the pipe shown in the figure and its water content have a uniform temperature T_{1}(t). Initially, we have T_{1}(t = 0) = 45^{\circ }C. The surface-convection heat transfer is due to a thermobuoyant motion. Use the correlation for vertical flat plate for the \left\langle Nu\right\rangle _{L} for pipe surface.
(a) Draw the thermal circuit diagram.
(b) Plot the temperature history T_{1}(t) for the set of parameters given below. Since the energy equation is an ordinary differential equation, and since for combined surface-convection and radiation heat transfer it cannot be analytically integrated, use the software.
(c) For the case of no radiation, compare the results for T (t) to that predicted by T_{1}(t)=T_{f,\infty }+[T_{1}(t=0)-T_{f,\infty }]e^{-t/\tau _{1}}+a_{1}\tau _{1}(1-e^{-t/\tau _{1}}).

T_{f,∞} = 20^{\circ }C    ,T_{s,∞} = 20^{\circ }C    , D = 8 cm    , l = 3 mm    ,  and    L = 30 cm

The pipe material is oxidized brass (Tables C.16 and C.18). Determine the air and water properties at T = 300 K.

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(a) The thermal circuit diagram is shown in Figure (b).

(b) The energy equation for the uniform temperature pipe-water segment is Q\mid_{A,1}=\int_{A_{1}}{(q_{ku}.s_{n})dA} =-(\rho c_{p}V)_{1}\frac{dT_{1}}{dt} +\dot{S}_{1}     for       Bi_{L}\lt 0.1, with Q_{1} =\dot{ S}_{ 1} = 0. Then we have

Q\mid_{A,1}=Q_{ku,1-\infty }+Q_{r,1-\infty }=-(\rho c_{p}V)_{1}\frac{dT_{1}}{dt}

The volume V is occupied by water (w) and brass (b), i.e.,

(\rho c_{p}V)_{1}=(\rho c_{p})_{w}\pi \frac{(D-2l)^{2}}{4}L +(\rho c_{p})_{b}\pi \frac{[D^{2}-(D-2l)^{2}]}{4}L

For surface radiation, for a two-surface enclosure, with A_{r,∞} \ll A_{r,1} and F_{1-∞} = 1, we have Q_{r,1-2}=A_{r,1}\epsilon _{r,1}[E_{b,1}(T_{1})-E_{b,2}(T_{2})]   for   F_{1-2}=1   with   \frac{A_{r,1}}{A_{r,2}}\simeq 0   or   \epsilon _{r,2} =1, i.e.,

Q_{r,1-∞} = A_{r,1}\epsilon_{r,1}σ_{SB}(T^{ 4}_{ 1} − T^{ 4}_{ s,∞}),       A_{r,1} = πDL = A_{ku}.

The surface convection is given by \left\langle Q_{ku}\right\rangle _{L( or D)}=\frac{T_{s}-T_{f,\infty }}{\left\langle R_{ku}\right\rangle_{L(or D)} } =A_{ku}\frac{k_{f}}{L(or D)}\left\langle Nu\right\rangle _{L(or D)}(T_{s}-T_{f,\infty }),       Re_{L(or D)}=\frac{u_{f,\infty }L(or D)}{v_{f}} , i.e.,

Q_{ku,1-\infty }=A_{ku}\left\langle Nu\right\rangle _{L}\frac{k_{f}}{L}(T_{1}-T_{f,\infty })

The Nusselt number is found from Table, where it is suggested that we use the correlation for the vertical plates, i.e.,

\left\langle Nu\right\rangle _{L}=[(\left\langle Nu_{L,l}\right\rangle) ^{6}+(\left\langle Nu_{L,t}\right\rangle )^{6}]^{1/6}

 

\left\langle Nu_{L,l}\right\rangle =\frac{2.8}{ln[(1 + 2.8/(a_{1}Ra^{1/4} )]}

 

\left\langle Nu_{L,t}\right\rangle =\frac{0.13Pr^{0.22}}{(1 + 0.61Pr^{0.81})^{ 0.42}} Ra_{L}^{1/3}

 

a_{1}=\frac{4}{3}\frac{0.503}{[1 + (0.492/Pr)^{9/16}] ^{4/9}}

 

Ra_{L}=\frac{g\beta _{f}(T_{f}-T_{f,\infty })L^{3}}{v_{f}\alpha _{f}}

The thermophysical properties are, at T = 300 K,

water : \rho _{w} = 997 kg/m^{3}               Table
c_{p,w} = 4,179 J/kg-K             Table
brass : \rho _{b} = 8,933 kg/m^{3}              Table
c_{p,b} = 355 J/kg-K               Table
\epsilon_{r,1} = 0.60                         Table
air : k_{f} = 0.0267 W/m-K                Table
β_{f} =\frac{1}{300}    1/K                         ideal gas \beta _{f}=\frac{1}{T_{f}}, p=\rho _{f}\frac{R_{g}}{M}T_{f}

ν_{f} = 1.566 × 10^{−5} m^{2}/s                 Table
α_{f} = 2.257 × 10^{−5} m^{2}/s                                     Table
Pr = 0.69                                     Table
other parameters : T_{f,∞} = T_{s,∞} = 293.15 K
D = 0.06 m   , l = 10^{−3} m    , L = 0.3 m.

The results for T_{1}(t) are plotted in Figure (c). The results with and without the surface radiation are shown. The surface radiation accelerates the cooldown. Note that within about one hour, the water temperature drops to near 30^{\circ }C. This is the average surface temperature for the human skin. Any further drop in the temperature results in a cold sensation when this water flows over the human hands.
(c) From the case of no surface radiation, Q_{r,1-∞} = 0, and T_{1}(t)=T_{f,\infty }+[T_{1}(t=0)-T_{f,\infty }]e^{-t/\tau _{1}}+a_{1}\tau _{1}(1-e^{-t/\tau _{1}}), for \dot{S}_{ 1} − Q_{1} = 0 (a_{1} = 0), we have

T_{1}(t) = T_{f,∞} + [T_{1}(t = 0) − T_{f,∞}]e^{−t/\tau_{1}} 

 

\tau_{1}= (ρc_{p}V)_{1}\left\langle R_{ku}\right\rangle _{L}

The solution is valid for a constant \left\langle R_{ku}\right\rangle _{L}. Here we use \left\langle R_{ku}\right\rangle _{L}(t = 0) = 4.353^{\circ }C/W.

\tau_{1} = 2307.2 × 3.997 = 9, 222 s

Now, after t = 2 hr = 7,200 s, we have

T^{1}(t = 2 hr) = 293.15(K) + (318.15 − 293.15)(K) e^{−[7,200 (s)]/[9,222 (s)]}

 

= 304.6 K = 31.45^{\circ}C.

This is what is found from the use of a solver (e.g., MATLAB) by setting \epsilon _{r,1} = 0, and using a constant \left\langle R_{ku}\right\rangle _{L}(t = 0), as shown in Figure (c). The effect of variable \left\langle R_{ku}\right\rangle _{L} is less profound compared to that of surface emissivity.

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