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Heat transfer modes and steady conduction

Given conditionsModel and checks
Plane layers, fixed end temperatures or surface filmsSeries resistance, Eq. 1; include each exposed film.
Heat can cross separate side-by-side pathsCombine each series path before putting paths in parallel, Eq. 4.
Hollow cylinder or sphereUse the radial resistance, Eq. 5 or Eq. 7; area varies with radius.
Internal heat generationUse the source term in the energy balance and solve for the temperature profile, Eq. 11.
Section through a ceramic cup of hot tea. Arrows show circulation in the tea, rising warm air outside, conduction through the wall and into the bench, radiation to the room, and evaporation from the free surface.
Figure 1: Section through a ceramic cup of hot tea. Arrows show circulation in the tea, rising warm air outside, conduction through the wall and into the bench, radiation to the room, and evaporation from the free surface.

A cup of hot tea cools because it loses heat to its surroundings. Let’s assume the air, bench and room surfaces are cooler than the tea.

There are several modes of heat transfer at work here. Heat passes through the ceramic wall by conduction. The tea near the wall cools, becomes denser and sinks. Warmer tea rises through the middle to replace it, forming the circulation shown in Figure 1. Outside the cup, air in contact with the wall warms and rises. In both cases, temperature differences cause density differences that drive the fluid motion. This phenomenon is called natural convection.

The cup also loses heat by radiation to the cooler room surfaces. So, at the outer wall, convection and radiation occur at the same time. There are other ways for heat to leave the tea as well. Heat passes through the base into the bench by conduction. At the exposed tea surface, water evaporates into the air and takes energy with it. Evaporation therefore involves both heat and mass transfer.

Let’s follow the heat leaving through the side wall. It first passes from the tea to the inner wall by convection, then through the ceramic by conduction. From the outer wall, it leaves by convection to the air and radiation to the room surfaces. These steps help explain why we use thermal resistances in series and in parallel. Heat must pass through the inner convection resistance and the wall resistance in sequence, so these are in series. At the outer wall, convection and radiation provide parallel routes for heat loss. Heat leaving through the tea surface or the base follows separate routes.

How do we calculate the heat transferred? For one-dimensional conduction, we use Fourier’s law, q=−k dT/dxq=-k\,dT/dx. Here qq is the heat transferred per unit area per unit time, or heat flux, measured in W m−2\mathrm{W\,m^{-2}}. The thermal conductivity kk has units of W m−1 K−1\mathrm{W\,m^{-1}\,K^{-1}}. The minus sign tells us that heat flows towards lower temperature.

For convection, we use q=h(Ts−T∞)q=h(T_s-T_\infty). Here TsT_s is the surface temperature and T∞T_\infty is the fluid temperature away from the surface. The heat transfer coefficient hh has units of W m−2 K−1\mathrm{W\,m^{-2}\,K^{-1}}. It depends on the fluid, the geometry and how the fluid flows. For example, blowing air over the cup changes hh and can increase the rate of heat loss.

Consider these three cases:

  1. Heat passes across a layer of stationary air, with radiation neglected.
  2. Water flows over a hot plate and removes heat from it.
  3. Heat passes between two surfaces separated by a vacuum.

Which sequence gives the heat transfer mode in each case, in the order listed?

  • Convection, conduction, radiation.
  • Conduction, convection, radiation. ✓
  • Conduction, radiation, convection.
  • Radiation, convection, conduction.
Explanation

The air is stationary, so there is no heat transport by bulk fluid motion. With radiation neglected, heat crosses the air layer by conduction. Heat transfer from the plate to the flowing water is convection. It combines conduction near the plate with heat transport by the moving water. Across a vacuum, heat transfers by radiation, which requires no material medium.

A fan blows air over a metal plate. Suppose we turn up the fan so the air flows faster, while keeping the plate and air temperatures the same. What happens to the plate’s thermal conductivity kk and the heat transfer coefficient hh?

  • Both kk and hh stay the same because the temperatures have not changed.
  • kk increases, while hh stays the same.
  • kk stays the same, while hh generally increases. ✓
  • Both kk and hh increase as the air flows faster.
Explanation

Turning up the fan changes the air flow over the plate. It does not change the metal or its temperature, so kk stays the same. The coefficient hh depends on the flow conditions and generally increases with air speed. More heat can therefore leave the plate for the same temperature difference between the plate and the air.

4 Case 1: 1D steady conduction without heat generation

Section titled “4 Case 1: 1D steady conduction without heat generation”

Let’s consider the three-layer wall in Figure 2, with hot fluid on one side and cold fluid on the other. The fluid temperatures are ThT_h and TcT_c, with Th>TcT_h>T_c. Each layer has the same area AA, but its thickness LiL_i and thermal conductivity kik_i may differ.

Assume steady, one-dimensional conduction through the wall, with no heat generation. The conductivity of each layer is constant, and the layers are in perfect thermal contact.

Heat first passes from the hot fluid to the wall by convection. It then conducts through each layer before leaving the wall by convection to the cold fluid. At steady state, heat enters and leaves each layer at the same rate. If heat entered a layer faster than it left, the layer would store energy and warm up.

Schematic temperature profile from hot fluid to cold fluid through three solid layers, with surface and interface temperatures, conductivities and thicknesses labelled.
Figure 2: Schematic temperature profile from hot fluid to cold fluid through three solid layers, with surface and interface temperatures, conductivities and thicknesses labelled.

The wall surfaces are at T1T_1 and T4T_4, and the two interfaces are at T2T_2 and T3T_3. The heat transfer coefficients on the hot and cold sides are hhh_h and hch_c, respectively. We can write the heat rate through each part as

Heat-transfer stepHeat rate
Hot fluid to wallQ˙x=hhA(Th−T1)\dot Q_x=h_hA(T_h-T_1)
Through solid layer iiQ˙x=kiALi(Ti−Ti+1)\dot Q_x=\frac{k_iA}{L_i}(T_i-T_{i+1})
Wall to cold fluidQ˙x=hcA(T4−Tc)\dot Q_x=h_cA(T_4-T_c)

The middle equation applies to all three solid layers, with i=1,2,3i=1,2,3. Heat passes through each layer and fluid film at the same rate Q˙x\dot Q_x. The temperature drop across each layer depends on its thermal resistance.

Rearranging the three heat-rate equations above to express their temperature differences gives

Th−T1=Q˙xhhA,T_h-T_1=\frac{\dot Q_x}{h_hA}, Ti−Ti+1=Q˙xLikiAT_i-T_{i+1}=\frac{\dot Q_xL_i}{k_iA}

and

T4−Tc=Q˙xhcA.T_4-T_c=\frac{\dot Q_x}{h_cA}.

Each has the form ΔT=Q˙xR\Delta T=\dot Q_xR, so the factor multiplying Q˙x\dot Q_x is the thermal resistance:

Rh=1hhA,Ri=LikiA,Rc=1hcAR_h=\frac{1}{h_hA},\qquad R_i=\frac{L_i}{k_iA},\qquad R_c=\frac{1}{h_cA}(1)

The convection resistances RhR_h and RcR_c are often called film resistances. They represent heat transfer between each fluid and the adjacent wall surface.

Now add the temperature drops from the hot fluid to the cold fluid:

(Th−T1)+(T1−T2)+(T2−T3)+(T3−T4)+(T4−Tc)=Q˙x(Rh+R1+R2+R3+Rc)(T_h-T_1)+ (T_1-T_2)+ (T_2-T_3)+ (T_3-T_4)+ (T_4-T_c) =\dot Q_x (R_h+R_1+R_2+R_3+R_c)

Each intermediate temperature appears once with a positive sign and once with a negative sign. These terms cancel, leaving the overall temperature difference Th−TcT_h-T_c. Therefore,

Q˙x=Th−Tc∑R=UA(Th−Tc)\dot Q_x=\frac{T_h-T_c}{\sum R}=UA(T_h-T_c)(2)

The overall heat transfer coefficient is

U=1A∑RU=\frac{1}{A\sum R}

Here

∑R=Rh+R1+R2+R3+Rc.\sum R=R_h+R_1+R_2+R_3+R_c.

The overall heat transfer coefficient UU, in W m−2 K−1\mathrm{W\,m^{-2}\,K^{-1}}, combines the effects of both convection processes and all three solid layers.

We can compare this wall to an electrical circuit with resistors in series. A temperature difference drives heat transfer, just as a voltage difference drives electric current. The same heat rate passes through both fluid films and all three layers, so their thermal resistances add to give the total resistance.

Once we know the heat rate, we can calculate the surface and interface temperatures. Starting at the hot fluid, subtract the temperature drop across each resistance in turn. This gives T1=Th−Q˙xRhT_1=T_h-\dot Q_xR_h at the hot wall surface, followed by T2=T1−Q˙xR1T_2=T_1-\dot Q_xR_1 at the first interface. Since each drop is Q˙xR\dot Q_xR and the heat rate is the same throughout, the largest temperature drop occurs across the largest resistance.

At fixed fluid temperatures, reducing the total resistance increases the heat rate. At fixed area, the film resistance is inversely proportional to the heat transfer coefficient hh. Increasing the fluid speed generally increases hh and therefore reduces the film resistance. A thinner solid layer or a material with higher conductivity reduces the conduction resistance. The effect depends on how much that resistance contributes to the total. Halving a small resistance changes the total much less than halving the largest one. For insulation, the aim is to increase the total resistance and reduce heat loss.

Let’s consider the wall in Figure 3. Layers E and H extend across the full area AA. Between them, materials F and G each occupy half the area and have the same thickness, LF=LGL_F=L_G. The outer faces are held at uniform temperatures T1T_1 and T2T_2, with T1>T2T_1>T_2.

Assume steady conduction, constant thermal conductivities, no heat generation and perfect contact between materials. The top and bottom edges are insulated.

Composite wall with thicknesses, conductivities and areas labelled. Network (a) assumes uniform temperatures on the internal interfaces; network (b) prevents heat flow across the horizontal midline.
Figure 3: Composite wall with thicknesses, conductivities and areas labelled. Network (a) assumes uniform temperatures on the internal interfaces; network (b) prevents heat flow across the horizontal midline.

Heat passes through E, then through F or G, and finally through H. To represent this wall by a resistance network, we need an assumption about how temperature varies across the internal interfaces. The figure shows two possible models.

In model (a), we assume that each internal interface has a uniform temperature. F and G therefore have the same temperature difference ΔT\Delta T across them. Their heat rates depend on their individual resistances and add to give the total heat rate:

Q˙=Q˙F+Q˙G=ΔTRF+ΔTRG=ΔT(1RF+1RG)\dot Q=\dot Q_F+\dot Q_G =\frac{\Delta T}{R_F}+\frac{\Delta T}{R_G} =\Delta T\left(\frac{1}{R_F}+\frac{1}{R_G}\right)

F and G are in parallel. We can replace them with an equivalent resistance RFGR_{FG} such that Q˙=ΔT/RFG\dot Q=\Delta T/R_{FG}. Comparing this expression with the equation above gives

1RFG=1RF+1RG,RFG=RFRGRF+RG\frac{1}{R_{FG}}=\frac{1}{R_F}+\frac{1}{R_G},\qquad R_{FG}=\frac{R_FR_G}{R_F+R_G}(3)

Each resistance must use the area through which heat passes. E and H occupy the full area, whereas F and G each occupy A/2A/2:

RE=LEkEA,RH=LHkHAR_E=\frac{L_E}{k_EA},\qquad R_H=\frac{L_H}{k_HA} RF=LFkF(A2),RG=LGkG(A2)R_F=\frac{L_F}{k_F\left(\frac{A}{2}\right)},\qquad R_G=\frac{L_G}{k_G\left(\frac{A}{2}\right)}

The total heat rate passes through E and H, so these two resistances are in series with the parallel combination of F and G. The equivalent resistance for model (a) is therefore

Ra=RE+RFG+RHR_a=R_E+R_{FG}+R_H

In model (b), we instead assume that no heat crosses the horizontal midline. Heat then follows two separate paths through the wall. The upper path passes through E, F and H; the lower path passes through E, G and H. Each path has three resistances in series, and the two complete paths are in parallel between T1T_1 and T2T_2.

Each path uses half the area of E and H. Since conduction resistance is inversely proportional to area, their resistances in each path are 2RE2R_E and 2RH2R_H. The definitions of RFR_F and RGR_G already use A/2A/2. The equivalent resistance for model (b) is therefore

1Rb=12RE+RF+2RH+12RE+RG+2RH\frac{1}{R_b}= \frac{1}{2R_E+R_F+2R_H}+ \frac{1}{2R_E+R_G+2R_H}(4)

The actual wall generally has two-dimensional heat flow. Heat can pass between its upper and lower parts, and the internal interface temperatures need not be uniform. Under the stated assumptions, the two models give lower and upper bounds on its thermal resistance:

Ra≤R≤RbR_a\le R\le R_b

If F and G have the same conductivity, the two models give the same result because the temperature varies only through the wall thickness. If the estimates differ substantially, a two-dimensional conduction calculation is needed to determine the resistance more precisely.

For either model, use its equivalent resistance to calculate the total heat rate from

Q˙=T1−T2R.\dot Q=\frac{T_1-T_2}{R}.

Dividing this heat rate by the full area AA gives the average heat flux through the wall.

So far, we have assumed that adjacent layers are in perfect thermal contact, with no temperature difference at their interface. Real surfaces have small irregularities. When two solids are pressed together, contact occurs at a limited number of points, leaving gaps elsewhere, as shown in Figure 4. Heat must pass through these contact regions and any material in the gaps, adding a thermal resistance at the interface.

Two rough solid surfaces touch at small contact areas, with air gaps between them. Heat flows from the left solid to the right solid.
Figure 4: Two rough solid surfaces touch at small contact areas, with air gaps between them. Heat flows from the left solid to the right solid.

We describe heat transfer across the interface using the thermal contact conductance hcontacth_{\mathrm{contact}}. Let T−T_- and T+T_+ be the temperatures of the two contacting surfaces. The heat rate and contact resistance are

Q˙=hcontactA(T−−T+)\dot Q=h_{\mathrm{contact}}A(T_--T_+)

The corresponding contact resistance is

Rcontact=T−−T+Q˙=1hcontactAR_{\mathrm{contact}}=\frac{T_--T_+}{\dot Q} =\frac{1}{h_{\mathrm{contact}}A}

Here AA is the nominal contact area, rather than the sum of the small areas where the solids actually touch. The contact conductance has units of W m−2 K−1\mathrm{W\,m^{-2}\,K^{-1}}, and the contact resistance has units of K W−1\mathrm{K\,W^{-1}}. We add this resistance to the other resistances in series. The resulting temperature drop at the interface is T−−T+=Q˙RcontactT_--T_+=\dot Q R_{\mathrm{contact}}.

A cold-room panel has two continuous linings with insulation between them. A solid metal support passes through part of the insulation, connecting the two linings. Treat each surface between a lining and the core as having a uniform temperature.

Heat passes through an outer lining, splits between insulation and a metal support, then passes through the inner lining. The two core paths connect the same interface temperatures.
Figure 5: Heat passes through an outer lining, splits between insulation and a metal support, then passes through the inner lining. The two core paths connect the same interface temperatures.

Heat flows steadily from the warmer surroundings into the cold room, with no heat generation in the panel. Which statement must be true?

  • The two linings have equal temperature drops, and the insulation and support have equal heat rates.
  • The same heat rate passes through each lining, the insulation and the support.
  • Both linings, the insulation and the support all have the same temperature drop.
  • The same total heat rate passes through each lining. The insulation and metal support have the same temperature drop. ✓
Explanation

Heat passes through the outer lining, divides between the insulation and metal support, then passes through the inner lining. The heat rate through each lining is therefore the sum of the rates through the two middle paths. The insulation and support connect the same two uniform-temperature surfaces, so they have the same temperature drop. Their heat rates depend on their resistances and need not be equal.

An engineer is checking the temperature profile through a furnace wall. For a 1 m21\ \mathrm{m^2} section, the thermal resistances from the hot gas to the room air are listed below. Assume steady heat transfer with no heat generation. All five resistances are in series.

PartThermal resistance RR in K W−1\mathrm{K\,W^{-1}}
Hot-side gas film0.0400.040
Firebrick0.1000.100
Insulation1.2001.200
Steel casing0.0001250.000125
Cold-side air film0.1000.100

Across which part should the engineer expect the largest temperature drop?

  • The insulation layer. ✓
  • The steel casing, because steel has a high thermal conductivity.
  • The hot-side gas film, because it is closest to the furnace.
  • All five parts should have the same temperature drop.
Explanation

The same heat rate passes through all five parts. Across each part,

∣ΔTi∣=∣Q˙∣Ri|\Delta T_i|=|\dot Q|R_i

The insulation has the largest resistance, so it has the largest temperature drop. The steel has a very small resistance and therefore a small temperature drop.

Let’s apply the resistance method to the wall of a long pipe. The wall has length LL, inner radius r1r_1, outer radius r2r_2 and thermal conductivity kk. Unlike a plane wall, its area normal to heat flow changes through the thickness.

Assume steady conduction, constant conductivity, no heat generation and negligible heat loss through the ends. The surface conditions are uniform along the pipe and around its circumference. Temperature therefore varies only with radius, T=T(r)T=T(r).

At steady state, heat enters and leaves each part of the wall at the same rate. The heat rate Q˙r\dot Q_r is therefore independent of radius. At radius rr, heat passes through the cylindrical area 2πrL2\pi rL, so Fourier’s law gives

Q˙r=−2πrkLdTdr\dot Q_r=-2\pi rkL\frac{dT}{dr}

Let the inner and outer surface temperatures be T1=T(r1)T_1=T(r_1) and T2=T(r2)T_2=T(r_2). Separating the temperature and radius terms, then integrating between these surfaces, gives

Q˙r∫r1r2drr=−2πkL∫T1T2dT\dot Q_r\int_{r_1}^{r_2}\frac{dr}{r} =-2\pi kL\int_{T_1}^{T_2}dT

Evaluating the integrals gives

Q˙rln⁡(r2r1)=2πkL(T1−T2)\dot Q_r\ln\left(\frac{r_2}{r_1}\right)=2\pi kL(T_1-T_2)

We can now write the result as

Q˙r=T1−T2R.\dot Q_r=\frac{T_1-T_2}{R}.

Comparing this form with the integrated equation gives the cylindrical resistance:

Rcyl=ln⁡(r2r1)2πkLR_{\mathrm{cyl}}=\frac{\ln\left(\frac{r_2}{r_1}\right)}{2\pi kL}(5)

The heat rate is then

Q˙r=T1−T2Rcyl\dot Q_r=\frac{T_1-T_2}{R_{\mathrm{cyl}}}

Integrating between r1r_1 and any radius rr within the wall gives

T(r)=T1−(T1−T2)ln⁡(rr1)ln⁡(r2r1)T(r)=T_1-(T_1-T_2)\frac{\ln\left(\frac{r}{r_1}\right)}{\ln\left(\frac{r_2}{r_1}\right)}

Temperature varies logarithmically with radius because the area changes through the wall. It therefore does not have the straight-line profile obtained for a plane wall with constant conductivity.

The local heat flux is

qr=Q˙r2πrL.q_r=\frac{\dot Q_r}{2\pi rL}.

For outward heat flow, the same heat rate passes through progressively larger areas. The heat flux therefore decreases as 1/r1/r, even though the heat rate remains constant.

Now consider three concentric layers, A, B and C, with successive radii r1,r2,r3,r4r_1,r_2,r_3,r_4. Heat passes from the inner fluid through its film, through all three layers, and then through the outer film to the outer fluid. These five resistances are in series, as shown in Figure 6.

Layered cylindrical wall: cross-section, pipe geometry and series resistance network. The same heat rate passes through both films and all three layers.
Figure 6: Layered cylindrical wall: cross-section, pipe geometry and series resistance network. The same heat rate passes through both films and all three layers.

The total resistance is

Rtotal=1h12πr1L+ln⁡(r2r1)2πkAL+ln⁡(r3r2)2πkBL+ln⁡(r4r3)2πkCL+1h42πr4LR_{\mathrm{total}}=\frac{1}{h_1 2\pi r_1L} +\frac{\ln\left(\frac{r_2}{r_1}\right)}{2\pi k_AL} +\frac{\ln\left(\frac{r_3}{r_2}\right)}{2\pi k_BL} +\frac{\ln\left(\frac{r_4}{r_3}\right)}{2\pi k_CL} +\frac{1}{h_4 2\pi r_4L}(6)

The overall temperature difference is between the two fluids. With inner and outer fluid temperatures T∞,1T_{\infty,1} and T∞,4T_{\infty,4}, the heat rate is

Q˙r=T∞,1−T∞,4Rtotal.\dot Q_r=\frac{T_{\infty,1}-T_{\infty,4}}{R_{\mathrm{total}}}.

The film resistances use different areas: Ai=2πr1LA_i=2\pi r_1L on the inside and Ao=2πr4LA_o=2\pi r_4L on the outside. We must therefore state which area is used when defining an overall heat transfer coefficient. Either choice gives the same heat rate, provided that

UiAi=UoAo=1Rtotal.U_iA_i=U_oA_o=\frac{1}{R_{\mathrm{total}}}.

The values of UiU_i and UoU_o themselves are generally different.

For a thin wall, r2−r1≪r1r_2-r_1\ll r_1, the change in area is small. Using

ln⁡(r2r1)≃r2−r1r1\ln\left(\frac{r_2}{r_1}\right)\simeq\frac{r_2-r_1}{r_1}

in Eq. 5 gives the plane-wall expression with thickness r2−r1r_2-r_1 and area 2πr1L2\pi r_1L.

Rcyl≃r2−r12πr1kL=ΔxkAR_{\mathrm{cyl}}\simeq\frac{r_2-r_1}{2\pi r_1kL} =\frac{\Delta x}{kA}

Here Δx=r2−r1\Delta x=r_2-r_1 and A=2πr1LA=2\pi r_1L.

The same resistance method applies to a hollow spherical wall, such as insulation around a spherical process vessel. Let its inner and outer radii be r1r_1 and r2r_2, and its thermal conductivity be kk.

Assume steady conduction, constant conductivity and no heat generation. The surface conditions are uniform over each spherical surface, so temperature varies only with radius, T=T(r)T=T(r).

At steady state, the same heat rate passes through every spherical surface. At radius rr, the area normal to heat flow is 4πr24\pi r^2. Fourier’s law therefore gives

Q˙r=−4πr2kdTdr\dot Q_r=-4\pi r^2k\frac{dT}{dr}

Let the inner and outer surface temperatures be T1=T(r1)T_1=T(r_1) and T2=T(r2)T_2=T(r_2). Separating the temperature and radius terms, then integrating between the surfaces, gives

Q˙r∫r1r2drr2=−4πk∫T1T2dT\dot Q_r\int_{r_1}^{r_2}\frac{dr}{r^2} =-4\pi k\int_{T_1}^{T_2}dT

Evaluating the integrals gives

Q˙r(1r1−1r2)=4πk(T1−T2)\dot Q_r\left(\frac{1}{r_1}-\frac{1}{r_2}\right) =4\pi k(T_1-T_2)

We can now write the result as

Q˙r=T1−T2R.\dot Q_r=\frac{T_1-T_2}{R}.

Comparing this form with the integrated equation gives the spherical resistance:

Rsph=1r1−1r24πkR_{\mathrm{sph}}=\frac{\frac{1}{r_1}-\frac{1}{r_2}}{4\pi k}(7)

The heat rate is then

Q˙r=T1−T2Rsph\dot Q_r=\frac{T_1-T_2}{R_{\mathrm{sph}}}

Integrating between r1r_1 and any radius rr within the wall gives

T(r)=T1−(T1−T2)1r1−1r1r1−1r2T(r)=T_1-(T_1-T_2)\frac{\frac{1}{r_1}-\frac{1}{r}}{\frac{1}{r_1}-\frac{1}{r_2}}

Temperature varies linearly with 1/r1/r, rather than with rr. The local heat flux is

qr=Q˙r4πr2.q_r=\frac{\dot Q_r}{4\pi r^2}.

For outward heat flow, it decreases as 1/r21/r^2 because the same heat rate passes through progressively larger areas.

Now consider three concentric spherical layers, A, B and C, with radii r1,r2,r3,r4r_1,r_2,r_3,r_4. Heat passes through the inner fluid film, all three solid layers and the outer fluid film. Their resistances add in series, as shown in Figure 7.

Layered spherical wall: central section, spherical geometry and series resistance network. Each layer has a different area as the heat flows outwards.
Figure 7: Layered spherical wall: central section, spherical geometry and series resistance network. Each layer has a different area as the heat flows outwards.

The total resistance is

Rtotal=1h14πr12+1r1−1r24πkA+1r2−1r34πkB+1r3−1r44πkC+1h44πr42R_{\mathrm{total}}=\frac{1}{h_1 4\pi r_1^2} +\frac{\frac{1}{r_1}-\frac{1}{r_2}}{4\pi k_A} +\frac{\frac{1}{r_2}-\frac{1}{r_3}}{4\pi k_B} +\frac{\frac{1}{r_3}-\frac{1}{r_4}}{4\pi k_C} +\frac{1}{h_4 4\pi r_4^2}(8)

With inner and outer fluid temperatures T∞,1T_{\infty,1} and T∞,4T_{\infty,4}, the heat rate is

Q˙r=T∞,1−T∞,4Rtotal\dot Q_r=\frac{T_{\infty,1}-T_{\infty,4}}{R_{\mathrm{total}}}

Each film uses the area of its own surface, Ai=4πr12A_i=4\pi r_1^2 or Ao=4πr42A_o=4\pi r_4^2. Either area can define an overall heat transfer coefficient, provided that

UiAi=UoAo=1Rtotal.U_iA_i=U_oA_o=\frac{1}{R_{\mathrm{total}}}.

For a thin spherical wall, r2−r1≪r1r_2-r_1\ll r_1, the two surface areas are nearly equal. Writing

1r1−1r2=r2−r1r1r2\frac{1}{r_1}-\frac{1}{r_2}=\frac{r_2-r_1}{r_1r_2}

in Eq. 7 and taking r2≃r1r_2\simeq r_1 gives the plane-wall limit:

Rsph≃r2−r14πkr12=ΔxkAR_{\mathrm{sph}}\simeq\frac{r_2-r_1}{4\pi kr_1^2} =\frac{\Delta x}{kA}

Here Δx=r2−r1\Delta x=r_2-r_1 and A=4πr12A=4\pi r_1^2.

A spherical vessel has insulation extending from r1=0.50 mr_1=0.50\ \mathrm{m} to r2=0.55 mr_2=0.55\ \mathrm{m}. Take the insulation conductivity as k=0.040 W m−1 K−1k=0.040\ \mathrm{W\,m^{-1}\,K^{-1}}. Its inner and outer insulation surface temperatures are 80 °C80\,\degree\mathrm{C} and 20 °C20\,\degree\mathrm{C}. Assume steady radial conduction and neglect heat flow through supports and pipe connections. What is the heat loss through the insulation?

Worked solution

The given temperatures are at the insulation surfaces, so the required resistance is the insulation resistance alone. From Eq. 7,

Rsph=10.50−10.554π(0.040)≃0.362 K W−1R_{\mathrm{sph}}=\frac{\frac{1}{0.50}-\frac{1}{0.55}}{4\pi(0.040)} \simeq0.362\ \mathrm{K\,W^{-1}}

The outward heat loss is

Q˙r=80−20Rsph≃166 W\dot Q_r=\frac{80-20}{R_{\mathrm{sph}}} \simeq166\ \mathrm{W}

If the given temperatures were fluid temperatures, the fluid-film resistances would also be needed. For a vessel containing a cold fluid, the same resistance method gives the inward heat gain.

4.5.1 Conduction into an infinite surrounding fluid

Section titled “4.5.1 Conduction into an infinite surrounding fluid”

Consider a sphere surrounded by an infinite, stationary fluid, with heat transfer through the fluid by conduction alone. Taking r2→∞r_2\to\infty in Eq. 7 gives

R=14πkr1,R=\frac{1}{4\pi kr_1},

where kk is the fluid’s thermal conductivity. Equating this to

1h(4πr12)\frac{1}{h\left(4\pi r_1^2\right)}

gives h=k/r1h=k/r_1.

A long steam pipe is insulated. Heat leaks outwards through the insulation at steady state. Temperature varies only with radius, and there is no heat generation in the insulation or heat loss through the ends.

Moving from the pipe surface to the outside of the insulation, what happens to the total heat rate Q˙r\dot Q_r and local heat flux qrq_r?

  • Both the heat rate and heat flux increase.
  • The heat rate decreases, while the heat flux stays the same.
  • The heat rate stays the same, while the heat flux decreases. ✓
  • Both the heat rate and heat flux stay the same.
Explanation

At steady state, the heat entering the insulation must leave it. The same heat rate passes through every cylindrical surface:

Q˙r=2πrLqr=constant\dot Q_r=2\pi rLq_r=\text{constant}

Thus,

qr=Q˙r2πrLq_r=\frac{\dot Q_r}{2\pi rL}

As radius increases, the heat crosses a larger area. The heat flux therefore decreases even though the total heat rate stays the same.

Glass window: heat loss and inside surface temperature

Section titled “Glass window: heat loss and inside surface temperature”

Consider a 0.8-m-high and 1.5-m-wide glass window with a thickness of 8 mm and a thermal conductivity of k=0.78 W/(m⋅°C)k=0.78\ \mathrm{W/(m\cdot\degree C)}. Determine the steady rate of heat transfer through this glass window and the temperature of its inner surface for a day during which the room is maintained at 20 °C20\ \degree\mathrm{C} while the temperature of the outdoors is −10 °C-10\ \degree\mathrm{C}. Take the heat transfer coefficients on the inner and outer surfaces of the window to be h1=10 W/(m2⋅°C)h_1=10\ \mathrm{W/(m^2\cdot\degree C)} and h2=40 W/(m2⋅°C)h_2=40\ \mathrm{W/(m^2\cdot\degree C)}, which includes the effects of radiation.

Worked solution

Heat passes from the room air to the inner glass surface, through the glass, and then from the outer glass surface to the surroundings. These three steps form a series resistance network.

Heat flows from room air at 20 degrees Celsius through the inside film, glass and outside film to air at minus 10 degrees Celsius. The two glass surface temperatures are the unknown intermediate temperatures.
Figure 8: Heat flows from room air at 20 degrees Celsius through the inside film, glass and outside film to air at minus 10 degrees Celsius. The two glass surface temperatures are the unknown intermediate temperatures.

Data

QuantitySymbolValue
Window heightHH0.8 m0.8\ \mathrm{m}
Window widthWW1.5 m1.5\ \mathrm{m}
Glass thicknessLL8 mm=0.008 m8\ \mathrm{mm}=0.008\ \mathrm{m}
Glass thermal conductivitykk0.78 W m−1 K−10.78\ \mathrm{W\,m^{-1}\,K^{-1}}
Room air temperatureT∞,1T_{\infty,1}20 °C20\,\degree\mathrm{C}
Outside air temperatureT∞,2T_{\infty,2}−10 °C-10\,\degree\mathrm{C}
Inside heat transfer coefficienth1h_110 W m−2 K−110\ \mathrm{W\,m^{-2}\,K^{-1}}
Outside heat transfer coefficient, including radiationh2h_240 W m−2 K−140\ \mathrm{W\,m^{-2}\,K^{-1}}

A temperature difference of 1 °C1\,\degree\mathrm{C} equals 1 K1\ \mathrm{K}. We can therefore express the supplied conductivity and heat transfer coefficients using kelvin-based units in the calculation.

We need the heat loss Q˙\dot Q and the inside glass surface temperature Ts,inT_{s,\mathrm{in}}.

Assumptions

  • Steady state.
  • Unidirectional heat flow, normal to the glass.
  • Heat transfer through the edges and frame is neglected.
  • No heat generation within the glass.
  • Constant thermal conductivity and heat transfer coefficients.
  • Uniform temperature on each glass surface.

The supplied outside heat transfer coefficient includes radiation, so no separate radiation resistance is added.

Calculations

First calculate the area normal to heat flow:

A=HWA=HW

Substituting the window dimensions gives

A=0.8×1.5=1.2 m2A=0.8\times1.5=1.2\ \mathrm{m^2}

The inside film resistance is

Rin=1h1AR_{\mathrm{in}}=\frac{1}{h_1A}

Using the inside coefficient and window area gives

Rin=110×1.2=0.083333 K W−1R_{\mathrm{in}}=\frac{1}{10\times1.2} =0.083333\ \mathrm{K\,W^{-1}}

For conduction through the glass,

Rg=LkAR_g=\frac{L}{kA}

Substituting the thickness, conductivity and area gives

Rg=0.0080.78×1.2=0.008547 K W−1R_g=\frac{0.008}{0.78\times1.2} =0.008547\ \mathrm{K\,W^{-1}}

The outside film resistance is

Rout=1h2AR_{\mathrm{out}}=\frac{1}{h_2A}

Substituting the outside coefficient gives

Rout=140×1.2=0.020833 K W−1R_{\mathrm{out}}=\frac{1}{40\times1.2} =0.020833\ \mathrm{K\,W^{-1}}

The same heat rate passes through all three resistances, so they add in series:

Rtotal=Rin+Rg+RoutR_{\mathrm{total}}=R_{\mathrm{in}}+R_g+R_{\mathrm{out}}

Substituting the three resistances gives

Rtotal≃0.112714 K W−1R_{\mathrm{total}}\simeq0.112714\ \mathrm{K\,W^{-1}}

The temperature difference between the air on either side is

ΔT=T∞,1−T∞,2\Delta T=T_{\infty,1}-T_{\infty,2}

Substituting the air temperatures gives

ΔT=20−(−10)=30 K\Delta T=20-(-10)=30\ \mathrm{K}

The heat loss can now be calculated using Eq. 2. Writing that relation for this window gives

Q˙=T∞,1−T∞,2Rtotal\dot Q=\frac{T_{\infty,1}-T_{\infty,2}}{R_{\mathrm{total}}}

Substituting the temperature difference and total resistance gives

Q˙=300.112714≃266.16 W\dot Q=\frac{30}{0.112714}\simeq266.16\ \mathrm{W}

Heat flows from the warmer room to the colder outdoors. To find the inside glass temperature, consider the temperature drop across the inside film:

T∞,1−Ts,in=Q˙RinT_{\infty,1}-T_{s,\mathrm{in}}=\dot QR_{\mathrm{in}}

The calculated heat rate gives an inside-film temperature drop of

ΔTin=266.16×0.083333≃22.180 K\Delta T_{\mathrm{in}}=266.16\times0.083333 \simeq22.180\ \mathrm{K}

Rearranging the inside-film relation gives

Ts,in=T∞,1−Q˙RinT_{s,\mathrm{in}}=T_{\infty,1}-\dot QR_{\mathrm{in}}

Subtracting the temperature drop from the room temperature gives

Ts,in=20−22.180=−2.180 °CT_{s,\mathrm{in}}=20-22.180=-2.180\,\degree\mathrm{C}

We can check this result by working from the outside air towards the room. The outer glass surface must be warmer than the outside air by Q˙Rout\dot QR_{\mathrm{out}}:

Ts,out=T∞,2+Q˙RoutT_{s,\mathrm{out}}=T_{\infty,2}+\dot QR_{\mathrm{out}}

Substitution gives

Ts,out=−10+266.16×0.020833≃−4.455 °CT_{s,\mathrm{out}}=-10+266.16\times0.020833 \simeq-4.455\,\degree\mathrm{C}

The temperature drop through the glass is therefore approximately

−2.180−(−4.455)=2.275 K.-2.180-(-4.455)=2.275\ \mathrm{K}.

Dividing this drop by RgR_g recovers the heat rate of approximately 266 W266\ \mathrm{W}. The surface temperatures also have the expected order: temperature falls from the room air to the inner glass surface, then to the outer surface and finally to the outside air.

Answer

The heat loss from the room through the window is

Q˙≃266 W\dot Q\simeq266\ \mathrm{W}

The inside glass surface temperature is

Ts,in≃−2.18 °CT_{s,\mathrm{in}}\simeq-2.18\,\degree\mathrm{C}

Most of the resistance is in the two fluid films, with the largest drop across the inside film. This explains why the glass surface is much colder than the room air. Adding a trapped air layer, as in double glazing, increases the resistance and reduces heat loss at the same air temperatures. The calculated inside surface is below freezing, so frost may form if sufficient moisture reaches it.

5 Case 2: 1D steady conduction with heat generation

Section titled “5 Case 2: 1D steady conduction with heat generation”

In the previous examples, no heat was generated within the wall. We now consider a solid with internal heat generation. At steady state, each region must lose both the heat entering it and the heat generated within it. We will use this balance to find the temperature distribution in an electrically heated wire.

5.1 Electric wire and shell energy balance

Section titled “5.1 Electric wire and shell energy balance”

Consider a long wire of radius RR and length LL. A uniform electrical current density II passes through it. Here II is current per unit area, in A m−2\mathrm{A\,m^{-2}}. Let kek_e be the electrical conductivity, in S m−1\mathrm{S\,m^{-1}}, and kk the thermal conductivity. Electrical resistance produces heat throughout the wire at the volumetric rate Se=I2/keS_e=I^2/k_e, in W m−3\mathrm{W\,m^{-3}}.

Assume steady state, constant thermal and electrical conductivities, uniform heat generation and negligible heat loss through the ends. The wire is stationary, and its surface is held at a uniform temperature T0T_0. Conditions do not vary around the circumference.

Temperature then depends only on radius, T=T(r)T=T(r). This makes the conduction problem one-dimensional, although the wire itself has three dimensions. Variation along the wire or around its circumference would require a model with additional spatial coordinates.

Longitudinal cutaway of a solid wire of radius R and length L. The narrow hatched strips are cuts through the annular control volume, with inner radius r and thickness delta r. Arrows show the radial heat flux at its inner and outer faces.
Figure 9: Longitudinal cutaway of a solid wire of radius R and length L. The narrow hatched strips are cuts through the annular control volume, with inner radius r and thickness delta r. Arrows show the radial heat flux at its inner and outer faces.

The shell balance follows Shah (n.d.), slides 22 and 23, and Bird et al. (2006), section 10.2.

Choose the thin cylindrical shell between rr and r+Δrr+\Delta r in Figure 9. Heat enters its inner face at the rate 2πrLqr(r)2\pi rLq_r(r) and leaves its outer face at the rate

2π(r+Δr)Lqr(r+Δr).2\pi(r+\Delta r)Lq_r(r+\Delta r).

The areas differ because the two faces are at different radii.

The shell volume is π[(r+Δr)2−r2]L\pi[(r+\Delta r)^2-r^2]L. Multiplying it by SeS_e gives the heat generated within the shell. With no accumulation, the balance is heat in minus heat out plus heat generated equals zero:

0=2πrLqr(r)−2π(r+Δr)Lqr(r+Δr)+Seπ[(r+Δr)2−r2]L0=2\pi rLq_r(r)-2\pi(r+\Delta r)Lq_r(r+\Delta r) +S_e\pi[(r+\Delta r)^2-r^2]L(9)

Dividing this balance by 2πLΔr2\pi L\Delta r and moving the heat-flow terms to the left gives

(r+Δr)qr(r+Δr)−rqr(r)Δr=Se(r+Δr2)\frac{(r+\Delta r)q_r(r+\Delta r)-rq_r(r)}{\Delta r} =S_e\left(r+\frac{\Delta r}{2}\right)

The left side is the change in rqrrq_r divided by the shell thickness. Taking the limit as Δr→0\Delta r\to0 gives

d(rqr)dr=rSe\frac{d(rq_r)}{dr}=rS_e(10)

The radius remains inside the derivative because the heat-flow area changes with rr. Treating the two shell faces as having the same area would give an incorrect radial balance. In a finite-volume calculation, we can instead apply Eq. 9 to each cell, retaining its actual inner and outer face areas.

5.2 Integrate and apply the boundary conditions

Section titled “5.2 Integrate and apply the boundary conditions”

To find the heat flux, integrate Eq. 10 with respect to radius:

rqr=Ser22+C1qr=Ser2+C1rrq_r=\frac{S_er^2}{2}+C_1 \qquad q_r=\frac{S_er}{2}+\frac{C_1}{r}

At the axis, the flux must be finite. A nonzero C1C_1 would make C1/rC_1/r unbounded as r→0r\to0, so C1=0C_1=0. The resulting flux, qr=Ser/2q_r=S_er/2, is zero at the axis, consistent with symmetry.

Substituting qr=−k dT/drq_r=-k\,dT/dr gives the temperature gradient. A second integration gives the temperature:

dTdr=−Ser2kT=−Ser24k+C2\frac{dT}{dr}=-\frac{S_er}{2k} \qquad T=-\frac{S_er^2}{4k}+C_2

We determine C2C_2 from the prescribed surface temperature T(R)=T0T(R)=T_0. Substitution gives

C2=T0+SeR24k,C_2=T_0+\frac{S_eR^2}{4k},

and hence

T(r)−T0=Se4k(R2−r2)T(r)-T_0=\frac{S_e}{4k}(R^2-r^2)(11)

The radial heat flux is

qr=Ser2q_r=\frac{S_er}{2}

Temperature decreases parabolically from its maximum at the axis to T0T_0 at the surface. The radial heat flux behaves differently: it is zero at the axis and increases linearly with radius. Each cylindrical surface must release all the heat generated inside it. At the axis, the temperature gradient is zero, so Fourier’s law gives zero flux even though the temperature is highest there.

The centre-to-surface temperature difference is SeR2/(4k)S_eR^2/(4k). Doubling RR therefore increases this difference by a factor of four when SeS_e and kk are fixed. The condition of fixed SeS_e matters. If the total electrical current were held fixed instead, changing the radius would also change the current density and the heat generation per unit volume.

A long solid wire generates heat uniformly, and its surface is held at T0T_0. At steady state, temperature varies only with radius. What must be true at the axis, r=0r=0?

  • The temperature equals the surface temperature T0T_0.
  • The temperature gradient dT/drdT/dr and radial heat flux are both zero. ✓
  • The radial heat flux is infinite because the cylindrical area is zero.
  • The temperature gradient has its largest magnitude.
Explanation

There is no preferred radial direction at the axis. Symmetry requires

[dTdr]r=0=0\left[\frac{dT}{dr}\right]_{r=0}=0

Fourier’s law then gives

qr(0)=−k[dTdr]r=0=0q_r(0)=-k\left[\frac{dT}{dr}\right]_{r=0}=0

The centre can still be hotter than the surface. Its temperature is a maximum, where the gradient is zero.

A long wire generates heat uniformly at a rate SeS_e per unit volume. At steady state, its centre is 12 K12\ \mathrm{K} hotter than its surface. Suppose we increase the radius from 2 mm2\ \mathrm{mm} to 4 mm4\ \mathrm{mm}, keeping SeS_e, thermal conductivity kk and surface temperature T0T_0 unchanged. Neglect heat loss through the ends. What is the new centre-to-surface temperature difference?

  • 6 K6\ \mathrm{K}.
  • 12 K12\ \mathrm{K}.
  • 24 K24\ \mathrm{K}.
  • 48 K48\ \mathrm{K}. ✓
Explanation

At the axis, Eq. 11 gives

Tmax⁡−T0=SeR24kT_{\max}-T_0=\frac{S_eR^2}{4k}

With heat generation and conductivity unchanged, doubling the radius makes this temperature difference four times as large:

(Tmax⁡−T0)new=22(12)=48 K(T_{\max}-T_0)_{\mathrm{new}}=2^2(12)=48\ \mathrm K

To find the mean temperature, we must weight each temperature by the volume of material at that radius. A ring of thickness drdr has area 2πr dr2\pi r\,dr, so equal radial intervals contain more material near the surface than near the axis.

Temperature is uniform along the wire, so the length cancels from the volume average. We can therefore average over the cross-section. Using Eq. 11 gives

T‾−T0=∫0R[Se(R2−r2)4k] 2πr drπR2=SeR28k\overline T-T_0= \frac{\int_0^R \left[\frac{S_e(R^2-r^2)}{4k}\right]\,2\pi r\,dr} {\pi R^2}=\frac{S_eR^2}{8k}(12)

Evaluating the integrals uses

∫0Rr dr=R22\int_0^R r\,dr=\frac{R^2}{2}

and

∫0R(R2r−r3) dr=R44.\int_0^R(R^2r-r^3)\,dr=\frac{R^4}{4}.

The mean temperature rise is half the centre-to-surface rise. Averaging temperatures at equally spaced radii without the factor rr would overestimate the mean by giving too much weight to the hotter material near the axis.

We can check conservation of energy using the flux at r=Rr=R. Multiplying by the curved surface area gives the total heat loss:

Q˙R=qr(R) 2πRL=SeR2 2πRL=SeπR2L\dot Q_R=q_r(R)\,2\pi RL =\frac{S_eR}{2}\,2\pi RL =S_e\pi R^2L

The result is exactly the heat generation per unit volume multiplied by the wire volume. All the heat generated leaves through the curved surface, as required by the assumptions. A numerical solution should satisfy this overall balance as well as the local energy equation.

Temperature and conservation in a heated wire

Section titled “Temperature and conservation in a heated wire”

A wire has radius R=0.002 mR=0.002\ \mathrm{m}, length L=0.50 mL=0.50\ \mathrm{m}, thermal conductivity k=15 W m−1 K−1k=15\ \mathrm{W\,m^{-1}\,K^{-1}} and electrical conductivity ke=106 S m−1k_e=10^6\ \mathrm{S\,m^{-1}}. Its current density is I=106 A m−2I=10^6\ \mathrm{A\,m^{-2}}, and its surface is held at T0=25 °CT_0=25\ \degree\mathrm{C}. Use the wire model above to calculate the centre temperature, mean temperature and heat loss through the curved surface. Verify that the heat loss equals the total heat generation.

Calculation and answer

The electrical current produces heat at the volumetric rate Se=I2/ke=106 W m−3S_e=I^2/k_e=10^6\ \mathrm{W\,m^{-3}}.

From Eq. 11, the centre-to-surface temperature difference is

106(0.002)24×15=0.066667 K.\frac{10^6(0.002)^2}{4\times15}=0.066667\ \mathrm{K}.

The mean rise from Eq. 12 is half this value, 0.033333 K0.033333\ \mathrm{K}. Adding these rises to T0T_0 gives Tmax⁡=25.0667 °CT_{\max}=25.0667\ \degree\mathrm{C} and T‾=25.0333 °C\overline T=25.0333\ \degree\mathrm{C}.

The surface flux is

qr(R)=106×0.0022=1000 W m−2.q_r(R)=\frac{10^6\times0.002}{2}=1000\ \mathrm{W\,m^{-2}}.

Multiplying by the curved area

2πRL=0.00628319 m22\pi RL=0.00628319\ \mathrm{m^2}

gives Q˙R=6.28319 W\dot Q_R=6.28319\ \mathrm{W}.

Independently, the total heat generation is SeπR2L=6.28319 WS_e\pi R^2L=6.28319\ \mathrm{W}. This equals the surface heat loss, confirming the energy balance. The wire loses approximately 6.28 W6.28\ \mathrm{W} at steady state.

The shell balance gave the energy equation for a particular geometry. We can also obtain it by simplifying the general energy equation. For an incompressible Newtonian fluid with constant properties and negligible compression work, this equation can be written as

ρC^p(∂T∂t+u⋅∇T)=k∇2T+S\rho\widehat C_p\left(\frac{\partial T}{\partial t} +\boldsymbol u\cdot\nabla T\right)=k\nabla^2T+S(13)

Here ρ\rho is density, C^p\widehat C_p is specific heat capacity per unit mass and u\boldsymbol u is fluid velocity. The source SS represents heat generation per unit volume, in W m−3\mathrm{W\,m^{-3}}. Viscous dissipation must either be negligible or be included in SS.

The left side accounts for the local temperature change and heat transport by fluid motion. The terms on the right account for conduction and internal heat generation. In the stationary wire, u=0\boldsymbol u=0 and S=SeS=S_e.

The material derivative DT/DtDT/Dt describes the rate of temperature change of a fluid element as it moves. It combines the local time derivative with the change due to motion through a temperature field. In Cartesian coordinates, the material derivative is

DTDt=∂T∂t+ux∂T∂x+uy∂T∂y+uz∂T∂z\frac{DT}{Dt}=\frac{\partial T}{\partial t} +u_x\frac{\partial T}{\partial x} +u_y\frac{\partial T}{\partial y} +u_z\frac{\partial T}{\partial z}

The Laplacian is

∇2T=∂2T∂x2+∂2T∂y2+∂2T∂z2\nabla^2T=\frac{\partial^2T}{\partial x^2} +\frac{\partial^2T}{\partial y^2} +\frac{\partial^2T}{\partial z^2}

For cylindrical coordinates, we use radius rr, angle θ\theta and axial position zz. The distances are measured in metres and the angle in radians. The material derivative is

DTDt=∂T∂t+ur∂T∂r+uθr∂T∂θ+uz∂T∂z\frac{DT}{Dt}=\frac{\partial T}{\partial t} +u_r\frac{\partial T}{\partial r} +\frac{u_\theta}{r}\frac{\partial T}{\partial\theta} +u_z\frac{\partial T}{\partial z}(14)

The Laplacian is

∇2T=1r∂∂r(r∂T∂r)+1r2∂2T∂θ2+∂2T∂z2\nabla^2T=\frac{1}{r}\frac{\partial}{\partial r} \left(r\frac{\partial T}{\partial r}\right) +\frac{1}{r^2}\frac{\partial^2T}{\partial\theta^2} +\frac{\partial^2T}{\partial z^2}(15)

Substituting these expressions into Eq. 13 gives its cylindrical form. The radial conduction term contains the same factor rr as the shell balance because the area normal to radial heat flow increases with radius.

The volumetric heat capacity ρC^p\rho\widehat C_p is the energy required per unit volume for a unit temperature rise. Dividing Eq. 13 by this quantity gives

DTDt=α∇2T+SρC^p\frac{DT}{Dt}=\alpha\nabla^2T+\frac{S}{\rho\widehat C_p}

Here the thermal diffusivity is

α=kρC^p\alpha=\frac{k}{\rho\widehat C_p}(16)

Each term in the temperature equation has units of K s−1\mathrm{K\,s^{-1}}. Thermal diffusivity combines two effects. A higher conductivity allows heat to redistribute more readily, while a higher volumetric heat capacity requires more energy for the same temperature change. Their ratio determines the rate at which temperature differences diminish by conduction.

We can use thermal diffusivity to estimate the time required for conduction over a distance LL. With no fluid motion or heat generation, the energy equation is

∂T∂t=α∇2T.\frac{\partial T}{\partial t}=\alpha\nabla^2T.

For a temperature change of order ΔT\Delta T over distance LL and time tt, the two terms have the approximate magnitudes

∂T∂t∼ΔTtα∂2T∂y2∼αΔTL2\frac{\partial T}{\partial t}\sim\frac{\Delta T}{t} \qquad \alpha\frac{\partial^2T}{\partial y^2}\sim\alpha\frac{\Delta T}{L^2}

Balancing these magnitudes and cancelling ΔT\Delta T gives

tdiff∼L2αt_{\mathrm{diff}}\sim\frac{L^2}{\alpha}(17)

The diffusion time scale therefore increases with the square of the distance. For the same material, doubling LL increases the estimated time by a factor of four.

For example, consider a piece of beef 2 cm2\ \mathrm{cm} thick, heated from both sides. Conduction must act over L=0.01 mL=0.01\ \mathrm{m} to reach the centre. Taking α=1.4×10−7 m2 s−1\alpha=1.4\times10^{-7}\ \mathrm{m^2\,s^{-1}} gives tdiff∼714 st_{\mathrm{diff}}\sim714\ \mathrm{s}, or about twelve minutes.

This is a characteristic time for temperature changes to extend through the thickness. Finding the time for the centre to reach a specified temperature requires the initial and boundary conditions. The estimate also does not predict surface browning, which involves chemical reactions.

A mould is repeatedly heated and cooled. A designer proposes using an alloy with a higher thermal conductivity so that temperature changes spread through the mould faster. Is conductivity alone enough to tell whether the proposed alloy has a higher thermal diffusivity?

  • Yes. Thermal diffusivity depends only on thermal conductivity.
  • Yes. Density and heat capacity affect steady conduction only.
  • No. We also need the density and specific heat capacity of each alloy. ✓
  • No. A higher conductivity always gives a lower diffusivity.
Explanation

Thermal diffusivity depends on conductivity, density and specific heat capacity:

α=kρC^p\alpha=\frac{k}{\rho\widehat C_p}

A higher conductivity increases this ratio, while a higher volumetric heat capacity reduces it. We need all three properties to compare the two alloys.

In a moulding process, a polymer sheet is heated from both sides. For a 10 mm10\ \mathrm{mm} thick sheet, the estimated diffusion time from either surface to the centre is 50 s50\ \mathrm{s}.

What is the estimated diffusion time for a 30 mm30\ \mathrm{mm} thick sheet of the same polymer? Assume the thermal diffusivity is unchanged and use tdiff∼L2/αt_{\mathrm{diff}}\sim L^2/\alpha, where LL is the distance from a heated surface to the centre.

  • 150 s150\ \mathrm{s}.
  • 450 s450\ \mathrm{s}. ✓
  • 50 s50\ \mathrm{s}.
  • 50/9 s50/9\ \mathrm{s}.
Explanation

The conduction distance is half the sheet thickness. It increases from 5 mm to 15 mm. For the same diffusivity,

tnewtold=(155)2=9\frac{t_{\mathrm{new}}}{t_{\mathrm{old}}}=\left(\frac{15}{5}\right)^2=9

Thus,

tnew=9(50)=450 st_{\mathrm{new}}=9(50)=450\ \mathrm s

This is a diffusion time estimate. Finding the time to reach a particular temperature also requires the initial and surface conditions.

6.4 Apply the general equation to the wire

Section titled “6.4 Apply the general equation to the wire”

Let’s recover the wire equation from the general energy equation. Substitute the material derivative in Eq. 14 and the Laplacian in Eq. 15 into Eq. 13, then apply the wire assumptions:

  1. At steady state, ∂T/∂t=0\partial T/\partial t=0.
  2. The wire is stationary, so ur=uθ=uz=0u_r=u_\theta=u_z=0 and there is no heat transport by bulk motion.
  3. Conditions are uniform around the circumference, so derivatives with respect to θ\theta are zero.
  4. End effects are negligible, so derivatives with respect to zz are zero in the region considered.

Only radial conduction and heat generation remain. Taking S=SeS=S_e and constant kk gives

0=krddr(rdTdr)+Se0=\frac{k}{r}\frac{d}{dr}\left(r\frac{dT}{dr}\right)+S_e(18)

Rearranging after multiplication by r/kr/k, then integrating, gives

ddr(rdTdr)=−SerkdTdr=−Ser2k+Cr\frac{d}{dr}\left(r\frac{dT}{dr}\right)=-\frac{S_er}{k} \qquad \frac{dT}{dr}=-\frac{S_er}{2k}+\frac{C}{r}

A nonzero CC would produce a logarithmic temperature term that diverges at r=0r=0. The temperature must remain finite, so C=0C=0. A second integration, followed by the boundary condition T(R)=T0T(R)=T_0, recovers Eq. 11.

We can also compare the differential equations. Substituting Fourier’s law, qr=−k dT/drq_r=-k\,dT/dr, into Eq. 18 gives

d(rqr)dr=rSe,\frac{d(rq_r)}{dr}=rS_e,

exactly as in Eq. 10. The shell balance and the general energy equation therefore give the same model. The first derives it from heat entering, leaving and being generated in a control volume; the second obtains it by simplifying an existing energy equation.

We want the steady temperature distribution in a long, stationary wire that generates heat uniformly. Temperature does not vary along the wire or around its circumference, and heat loss through the ends is negligible. Which terms remain in the energy equation after applying these assumptions?

  • Accumulation and radial conduction.
  • Advection and internal heat generation.
  • Radial and axial conduction.
  • Radial conduction and internal heat generation. ✓
Explanation

Steady state removes accumulation. The wire is stationary, so there is no advection. Temperature is uniform around the circumference, so there is no angular conduction. Negligible end effects allow us to neglect axial conduction. Only radial conduction and internal heat generation remain, and they balance at steady state.

A furnace wall separates hot gas at 600 °C600\ \degree\mathrm{C} from air at 25 °C25\ \degree\mathrm{C}. From the hot side, the layers are 0.12 m0.12\ \mathrm{m} of firebrick, 0.060 m0.060\ \mathrm{m} of insulation and 0.0020 m0.0020\ \mathrm{m} of steel. Their thermal conductivities are 1.21.2, 0.0500.050 and 16 W m−1 K−116\ \mathrm{W\,m^{-1}\,K^{-1}}, respectively. The hot-side and cold-side heat transfer coefficients are 2525 and 10 W m−2 K−110\ \mathrm{W\,m^{-2}\,K^{-1}}, respectively.

Assume steady, one-dimensional heat transfer, constant properties, perfect contact and negligible radiation. Calculate the heat flux and all surface and interface temperatures. Determine which solid layer has the largest temperature drop. Then calculate the heat flux if the insulation thickness is doubled, with all other conditions unchanged.

Worked solution

Heat passes through the hot-side film, firebrick, insulation, steel and cold-side film in series. We need the heat flux and the temperature at every solid interface.

The furnace wall has three solid layers between hot gas and outside air. A common heat flux passes through all five resistance elements.
Figure 10: The furnace wall has three solid layers between hot gas and outside air. A common heat flux passes through all five resistance elements.

Data

QuantitySymbolValue
Hot-gas and cold-air temperaturesTh,TcT_h,T_c600,25 °C600,25\,\degree\mathrm C
Firebrick thickness and conductivityLf,kfL_f,k_f0.12 m,1.2 W m−1 K−10.12\ \mathrm m,1.2\ \mathrm{W\,m^{-1}\,K^{-1}}
Insulation thickness and conductivityLi,kiL_i,k_i0.060 m,0.050 W m−1 K−10.060\ \mathrm m,0.050\ \mathrm{W\,m^{-1}\,K^{-1}}
Steel thickness and conductivityLs,ksL_s,k_s0.0020 m,16 W m−1 K−10.0020\ \mathrm m,16\ \mathrm{W\,m^{-1}\,K^{-1}}
Hot-side and cold-side coefficientshh,hch_h,h_c25,10 W m−2 K−125,10\ \mathrm{W\,m^{-2}\,K^{-1}}

Assumptions

  • Steady one-dimensional heat flow with constant properties.
  • Perfect contact between the layers.
  • No generation, edge loss or separate radiative transfer.

Calculations

We can calculate the heat flux directly by using R′′=ARR''=AR, with units of m2 K W−1\mathrm{m^2\,K\,W^{-1}}. The temperature drop is then ΔT=q′′R′′\Delta T=q''R''. For each solid layer, Ri′′=Li/kiR_i''=L_i/k_i; for each film, Rh′′=1/hR_h''=1/h. In order from hot gas to cold air, these values are

ElementResistance per unit area, m2 K W−1\mathrm{m^2\,K\,W^{-1}}
Hot gas film, 1/hh1/h_h0.0400.040
Firebrick, Lf/kfL_f/k_f0.1000.100
Insulation, Li/kiL_i/k_i1.2001.200
Steel, Ls/ksL_s/k_s0.0001250.000125
Cold air film, 1/hc1/h_c0.1000.100

The total is Rtotal′′=1.440125 m2 K W−1R_{\mathrm{total}}''=1.440125\ \mathrm{m^2\,K\,W^{-1}}. Dividing the gas-to-air temperature difference by this resistance gives

q′′=600−251.440125=399.3 W m−2q''=\frac{600-25}{1.440125}=399.3\ \mathrm{W\,m^{-2}}

The temperature drop across each element is q′′Ri′′q''R_i''. Subtracting these drops successively from the hot-gas temperature gives

  • Hot gas: 600 °C600\ \degree\mathrm{C}.
  • Hot firebrick surface: 584.0 °C584.0\ \degree\mathrm{C}.
  • Firebrick-insulation interface: 544.1 °C544.1\ \degree\mathrm{C}.
  • Insulation-steel interface: 64.98 °C64.98\ \degree\mathrm{C}.
  • Outer steel surface: 64.93 °C64.93\ \degree\mathrm{C}.
  • Cold air: 25 °C25\ \degree\mathrm{C}.

The insulation has the largest temperature drop, 479.1 K479.1\ \mathrm{K}. The drops through the firebrick and steel are 39.93 K39.93\ \mathrm{K} and 0.0499 K0.0499\ \mathrm{K}, respectively. Since the heat flux is the same through all three layers, these differences are determined by Li/kiL_i/k_i. The insulation has the largest resistance because of its combination of thickness and low conductivity.

Doubling the insulation thickness adds another 1.200 m2 K W−11.200\ \mathrm{m^2\,K\,W^{-1}} to the total resistance. The new heat flux is

qnew′′=5751.440125+1.200=217.8 W m−2q''_{new}=\frac{575}{1.440125+1.200} =217.8\ \mathrm{W\,m^{-2}}

The heat loss decreases by 45.5%45.5\%. It does not halve because the films, firebrick and steel still contribute the same resistances. For the original wall, adding all five temperature drops recovers the full 575 K575\ \mathrm{K} difference between the gas and air.

Answer

The outward heat flux is 399 W m−2399\ \mathrm{W\,m^{-2}}. The solid temperatures from the hot side are 584.0584.0, 544.1544.1, 64.9864.98 and 64.93 °C64.93\,\degree\mathrm C. Doubling the insulation thickness reduces the flux to 218 W m−2218\ \mathrm{W\,m^{-2}}, a reduction of 45.5 percent.

The two cold-side interface temperatures retain guard digits to show the small contact-temperature drop.

Insulation and boil-off from a spherical vessel

Section titled “Insulation and boil-off from a spherical vessel”

A thin spherical vessel of radius 0.50 m0.50\ \mathrm{m} holds boiling liquid nitrogen at 77 K77\ \mathrm{K}. Its shell is at the liquid temperature, and the surrounding air is at 293 K293\ \mathrm{K}. Insulation with conductivity 0.040 W m−1 K−10.040\ \mathrm{W\,m^{-1}\,K^{-1}} extends from the vessel surface to an outer radius of 0.54 m0.54\ \mathrm{m}.

Take the outside heat transfer coefficient as 10 W m−2 K−110\ \mathrm{W\,m^{-2}\,K^{-1}} for both insulated and bare vessels. Neglect shell resistance, radiation and heat transfer through supports. The liquid remains at its boiling temperature.

Calculate the heat leak into the insulated vessel, the nitrogen boil-off rate and the outer insulation temperature. Compare the heat leak and boil-off rate with those of the bare vessel. The latent heat is 198 kJ kg−1198\ \mathrm{kJ\,kg^{-1}}. Use the supplied outside coefficient; no convection correlation is required.

Worked solution

Warm air supplies heat through the outside film and spherical insulation. That heat evaporates nitrogen at its maintained boiling temperature.

The cold spherical vessel has inner insulation radius ri and outer radius ro. Heat flows inward from ambient air through the outside film and insulation.
Figure 11: The cold spherical vessel has inner insulation radius ri and outer radius ro. Heat flows inward from ambient air through the outside film and insulation.

Data

QuantitySymbolValue
Vessel and outer insulation radiiri,ror_i,r_o0.50,0.54 m0.50,0.54\ \mathrm m
Liquid and air temperaturesTN,T∞T_N,T_\infty77,293 K77,293\ \mathrm K
Insulation conductivitykk0.040 W m−1 K−10.040\ \mathrm{W\,m^{-1}\,K^{-1}}
Outside coefficienthh10 W m−2 K−110\ \mathrm{W\,m^{-2}\,K^{-1}}
Nitrogen latent heathfgh_{fg}198000 J kg−1198000\ \mathrm{J\,kg^{-1}}

Assumptions

  • Steady heat transfer with constant properties.
  • Negligible shell resistance, support losses and radiation.
  • The liquid remains at its boiling temperature.
  • The same supplied outside coefficient is used for the insulated and bare comparisons.

Calculations

Heat flows from the warmer air through the outside film and then through the insulation to the nitrogen. The film and spherical conduction resistances are in series. Using Eq. 7 gives

Rins=10.50−10.544π(0.040)=0.2947 K W−1R_{ins}=\frac{\frac{1}{0.50}-\frac{1}{0.54}}{4\pi(0.040)} =0.2947\ \mathrm{K\,W^{-1}}Rfilm=110(4π)(0.54)2=0.02729 K W−1R_{film}=\frac{1}{10(4\pi)(0.54)^2} =0.02729\ \mathrm{K\,W^{-1}}

Adding these resistances gives the heat leak:

Q˙in=293−77Rins+Rfilm=670.8 W\dot Q_{in}=\frac{293-77}{R_{ins}+R_{film}} =670.8\ \mathrm W

The outside film uses the area at r=0.54 mr=0.54\ \mathrm{m}. The insulation resistance uses both radii to account for the changing area through the layer. A plane-wall expression with a single area would only approximate the spherical conduction resistance.

The heat entering the vessel evaporates nitrogen while its temperature remains constant. Dividing the heat rate by the latent heat gives

m˙boil=Q˙inhfg=670.8198000=0.003388 kg s−1=12.20 kg h−1\dot m_{boil}=\frac{\dot Q_{in}}{h_{fg}}=\frac{670.8}{198000} =0.003388\ \mathrm{kg\,s^{-1}} =12.20\ \mathrm{kg\,h^{-1}}

The drop from the air to the outer insulation surface is Q˙inRfilm\dot Q_{in}R_{film}. The surface temperature is therefore

To=293−Q˙inRfilm=274.7 K,T_o=293-\dot Q_{in}R_{film}=274.7\ \mathrm{K},

between the air and liquid temperatures as expected for inward heat flow.

For the bare vessel, there is no insulation resistance. The outside film now acts over the spherical area at r=0.50 mr=0.50\ \mathrm{m}, giving

Q˙bare=10(4π)(0.50)2(293−77)=6786 W\dot Q_{bare}=10(4\pi)(0.50)^2(293-77) =6786\ \mathrm W

The resulting boil-off rate is

m˙bare=123.4 kg h−1\dot m_{bare}=123.4\ \mathrm{kg\,h^{-1}}

The insulation reduces both heat leak and boil-off by 90.1%90.1\% for the specified conditions. This comparison uses the same hh in both cases. If hh were calculated from a convection correlation, changes in diameter and surface temperature could also affect its value.

Answer

With insulation, the heat leak is 671 W671\ \mathrm W, nitrogen boil-off is 12.2 kg h−112.2\ \mathrm{kg\,h^{-1}} and the outside insulation surface is at 274.7 K274.7\ \mathrm K. The bare vessel receives 6.79×103 W6.79\times10^3\ \mathrm W and boils off 123 kg h−1123\ \mathrm{kg\,h^{-1}}.

A heat-generating cylinder with an unknown surface temperature

Section titled “A heat-generating cylinder with an unknown surface temperature”

A long solid cylinder has radius 0.010 m0.010\ \mathrm{m}, length 1.0 m1.0\ \mathrm{m} and thermal conductivity 5.0 W m−1 K−15.0\ \mathrm{W\,m^{-1}\,K^{-1}}. Uniform heat generation occurs at Se=2.0×106 W m−3S_e=2.0\times10^6\ \mathrm{W\,m^{-3}}. Its curved surface is cooled by fluid at 300 K300\ \mathrm{K}, with a heat transfer coefficient h=200 W m−2 K−1h=200\ \mathrm{W\,m^{-2}\,K^{-1}}.

Assume steady radial conduction, constant properties and negligible heat loss through the ends. Derive the temperature profile and calculate the surface and centre temperatures. Check the overall heat balance.

Compare two modifications: doubling hh, and replacing the cylinder by four cylinders of half the radius. Each smaller cylinder has the same length, conductivity, heat generation per unit volume and original heat transfer coefficient. The coolant temperature is unchanged.

Worked solution

The radial geometry is the same as the wire model in Figure 9. Here the surface temperature must be found from convection before the centre temperature can be evaluated.

Data

QuantitySymbolValue
Cylinder radius and lengthR,LR,L0.010,1.0 m0.010,1.0\ \mathrm m
Thermal conductivitykk5.0 W m−1 K−15.0\ \mathrm{W\,m^{-1}\,K^{-1}}
Volumetric heat generationSeS_e2.0×106 W m−32.0\times10^6\ \mathrm{W\,m^{-3}}
Coolant temperatureT∞T_\infty300 K300\ \mathrm K
Surface coefficienthh200 W m−2 K−1200\ \mathrm{W\,m^{-2}\,K^{-1}}

Assumptions

  • Steady radial conduction with uniform heat generation.
  • Constant conductivity and convection coefficient.
  • Negligible heat flow through the ends.
  • Each comparison cylinder sees the same specified coolant temperature.

Calculations

The governing equation is the same as for the heated wire. At the axis, symmetry requires a zero radial temperature gradient:

1rddr(rdTdr)+Sek=0[dTdr]r=0=0\begin{gathered} \frac1r\frac{d}{dr}\left(r\frac{dT}{dr}\right) +\frac{S_e}{k}=0\\ \left[\frac{dT}{dr}\right]_{r=0}=0 \end{gathered}

Integration with the symmetry condition gives

dTdr=−Ser2k.\frac{dT}{dr}=-\frac{S_er}{2k}.

The surface temperature is now unknown, so we need a convection boundary condition at r=Rr=R. At steady state, the conductive flux reaching the surface equals the convective flux leaving it:

−k[dTdr]r=R=SeR2=h(Ts−T∞)-k\left[\frac{dT}{dr}\right]_{r=R} =\frac{S_eR}{2}=h(T_s-T_\infty)

Rearranging gives

Ts−T∞=SeR2h.T_s-T_\infty=\frac{S_eR}{2h}.

Integrating the temperature gradient and using this surface temperature gives

T(r)=T∞+SeR2h+Se4k(R2−r2)T(r)=T_\infty+\frac{S_eR}{2h} +\frac{S_e}{4k}(R^2-r^2)

The two temperature rises come from different parts of the model. The surface rise follows from the overall generation-to-convection balance:

Ts−T∞=SeR2h=2.0×106(0.010)2(200)=50.0 KT_s-T_\infty=\frac{S_eR}{2h} =\frac{2.0\times10^6(0.010)}{2(200)}=50.0\ \mathrm K

The conduction profile then gives the additional centre rise:

Tmax−Ts=SeR24k=2.0×106(0.010)24(5.0)=10.0 KT_{max}-T_s=\frac{S_eR^2}{4k} =\frac{2.0\times10^6(0.010)^2}{4(5.0)}=10.0\ \mathrm K

The surface-to-coolant temperature difference is 50.0 K50.0\ \mathrm{K}. The centre-to-surface difference is a further 10.0 K10.0\ \mathrm{K}. The temperatures are therefore Ts=350.0 KT_s=350.0\ \mathrm{K} and Tmax⁡=T(0)=360.0 KT_{\max}=T(0)=360.0\ \mathrm{K}.

The total heat generated is SeπR2L=628.3 WS_e\pi R^2L=628.3\ \mathrm{W}. The surface heat loss is

h(2πRL)(Ts−T∞)=628.3 W,h(2\pi RL)(T_s-T_\infty)=628.3\ \mathrm{W},

so the overall energy balance is satisfied. This check also confirms the surface boundary condition used to obtain the temperature profile.

Doubling hh halves the surface-to-coolant difference to 25.0 K25.0\ \mathrm{K}. The centre-to-surface difference stays at 10.0 K10.0\ \mathrm{K} because SeS_e, RR and kk are unchanged. The new centre temperature is

300+25+10=335.0 K.300+25+10=335.0\ \mathrm{K}.

Four cylinders of half the radius have the same total volume and heat generation as the original cylinder, but twice its total curved surface area. In each smaller cylinder, the surface-to-coolant difference is 25.0 K25.0\ \mathrm{K} and the centre-to-surface difference is 2.50 K2.50\ \mathrm{K}. The centre temperature is therefore

300+25+2.50=327.5 K.300+25+2.50=327.5\ \mathrm{K}.

The smaller radius reduces both temperature differences. At fixed SeS_e, hh and kk, the surface-to-coolant difference varies as RR, whereas the centre-to-surface difference varies as R2R^2. These results assume that every smaller cylinder is exposed to the same coolant temperature and specified heat transfer coefficient.

Answer

The original cylinder has Ts=350.0 KT_s=350.0\ \mathrm K, Tmax=360.0 KT_{max}=360.0\ \mathrm K and total heat loss 628 W628\ \mathrm W. Doubling hh lowers the centre to 335.0 K335.0\ \mathrm K. Four cylinders of half the radius lower each centre to 327.5 K327.5\ \mathrm K while preserving the original total heat generation.

8 What you should now be able to calculate

Section titled “8 What you should now be able to calculate”

Calculate heat loss and interface temperatures in plane and radial networks, and find a maximum temperature when heat is generated inside the solid.

Practice: Workshop 5 for resistance networks, heat generation and variable conductivity.

To report an error, email Ranjeet Utikar. Include the title Heat transfer modes and steady conduction, the URL /heat-transport/steady-conduction/, and the equation or passage that needs correction.

Bird, R. Byron, Warren E. Stewart, and Edwin N. Lightfoot. 2006. Transport Phenomena. Revised 2nd. John Wiley & Sons. https://www.wiley-vch.de/en/areas-interest/engineering/transport-phenomena-978-0-470-11539-8.
Çengel, Yunus A., and Afshin J. Ghajar. 2015. Heat and Mass Transfer: Fundamentals and Applications. 5th ed. McGraw-Hill Education. https://glencoe.mheducation.com/sites/0073398187/information_center_view0/application_chapters.html.
Shah, Milinkumar. n.d. “CHEN3001-TP: Heat Transport 1.” Curtin University. Unpublished.