Skip to content
Get started

2. Steady conduction

Take a slab occupying 0xL0\le x\le L, with cross-sectional area AA and constant conductivity kk. Assume temperature depends only on xx: side faces are insulated, end temperatures are uniform, and lateral variations are negligible. The steady equation from the previous chapter becomes

kT(x)=s.-kT''(x)=s.

We will integrate this equation twice and use two boundary conditions. Before doing so, predict the curvature: a positive source makes TT'' negative. An internally heated slab should bulge upward above the line joining its end temperatures.

With s=0s=0, T=0T''=0, so T=a+bxT=a+bx. Impose T(0)=TLT(0)=T_L and T(L)=TRT(L)=T_R:

T(x)=TL+TRTLLx,qx=kTLTRL.T(x)=T_L+\frac{T_R-T_L}{L}x, \qquad q_x=k\frac{T_L-T_R}{L}.

The heat rate is P=AqxP=Aq_x. Rearranging gives a useful circuit-like relation:

TLTR=PR,R=LkA.T_L-T_R=PR,\qquad R=\frac{L}{kA}.

Thermal resistance has units K/W. The area-normalized resistance L/kL/k has units m² K/W; specify which quantity you use. The physical slab and circuit analogy are developed in Glicksman, §2.

For an original arithmetic example, choose L=0.2L=0.2 m, A=0.5A=0.5 m², k=2k=2 W/(m K), TL=320T_L=320 K, and TR=300T_R=300 K. Then R=0.2R=0.2 K/W and P=100P=100 W. Doubling thickness halves this rate; doubling area doubles it. These are consequences of the assumed one-dimensional geometry.

Now take ss constant and both ends at TbT_b. Integrating gives

T=s2kx2+ax+b.T=-\frac{s}{2k}x^2+ax+b.

The left condition gives b=Tbb=T_b, and the right gives a=sL/(2k)a=sL/(2k):

T(x)=Tb+s2kx(Lx).T(x)=T_b+\frac{s}{2k}x(L-x).

Differentiate to find the maximum at x=L/2x=L/2:

TmaxTb=sL28k,qx(x)=s(xL2).T_{\max}-T_b=\frac{sL^2}{8k},\qquad q_x(x)=s\left(x-\frac L2\right).
text
x = 0 x = L/2 x = L
T = Tb maximum T = Tb
│ • │
│ . . │
│ . . │
• •
outward ← qx = 0 → outward
sL/2 sL/2

Conceptual profile, not numerical output. With equal end temperatures and uniform generation, heat leaves through both ends. The arrows label outward flux in W/m², while the curve indicates temperature in K.

At the left boundary qx=sL/2q_x=-sL/2, but its outward normal is 1-1: qn=sL/2>0q_n=sL/2>0. The right outward flux is also sL/2sL/2. Thus total outward power is A(sL/2+sL/2)=sALA(sL/2+sL/2)=sAL, exactly the generated power.

For s=1000s=1000 W/m³, L=0.2L=0.2 m, and k=2k=2 W/(m K), the maximum rise is 2.5 K. Each end carries 100 W/m² outward. With A=0.5A=0.5 m², each end removes 50 W and the whole slab generates 100 W. These numbers come from the equations, before any computer calculation.

The profile shows three useful sensitivities:

  • Double ss: double the temperature rise and the outward power.
  • Double kk: halve the temperature rise; outward power is unchanged because steady conservation still requires removal of the same generated power.
  • Double LL at fixed s,k,As,k,A: quadruple the temperature rise and double the total generated power.

A larger conductivity reduces the gradient needed to carry the same power. This distinction between temperature response and energy throughput will be valuable when interpreting the two-dimensional example.

Define ξ=x/L\xi=x/L and Θ=k(TTb)/(sL2)\Theta=k(T-T_b)/(sL^2). Then Θ=ξ(1ξ)/2\Theta=\xi(1-\xi)/2. All these slabs share one dimensionless curve. Such a collapse is a useful model prediction: a change in a constant parameter should rescale the curve, not change its shape.

A square is a different boundary-value problem

Section titled “A square is a different boundary-value problem”

Our Eqiora investigation cools all four sides of a square. A slab profile is constant in the transverse direction, so its warm interior would also touch the transverse boundary. It cannot satisfy a cool temperature on all four sides. Do not use the slab’s center value as an exact answer for that square.

The square has additional routes for heat loss. We will retain the slab’s qualitative predictions—positive interior rise, linear scaling with ss, inverse scaling with kk—and derive the square’s small finite element system separately.

  1. Derive the profile when uniform generation is present but TLTRT_L\ne T_R.
  2. Find its stationary point. Under what condition does it lie inside the slab?
  3. An engineer doubles kk and reports double the generated steady outward power with fixed s,L,As,L,A. What has gone wrong in the interpretation?
  4. Show that the mean temperature rise with equal ends is sL2/(12k)sL^2/(12k).
Solution hints
  1. Add the source-free linear solution to sx(Lx)/(2k)sx(L-x)/(2k).
  2. x=L/2+k(TRTL)/(sL)x_*=L/2+k(T_R-T_L)/(sL) for s>0s>0; check 0<x<L0<x_*<L.
  3. Conductivity changes the required gradient. Integrating the source still gives sALsAL, so the report must involve changed inputs, a flux convention, or an erroneous result.
  4. Integrate the parabola over 0xL0\le x\le L and divide by LL.

Previous: Conservation and Fourier’s law · Next: Boundaries and interfaces