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Heat transfer and thermal systems

Symmetric slab with uniform heat generation

Temperature in a slab of half-thickness L, with both faces held at Ts and uniform volumetric heating q‴, measured from the centreline.

Ref
HTS-06
Rev
v1
Field
Heat transfer and thermal systems
Result
T [K]

In a slab of half-thickness L with both faces at Ts and uniform heating q‴, the temperature is a parabola, T(x) = Ts + q‴(L² − x²)/(2k), with its maximum at the centre. The heat generated in each half leaves through its face, so the face flux is q‴L. Use the half-thickness, not the full thickness.

Temperature in a slab of half-thickness L, with both faces held at Ts and uniform volumetric heating q‴, measured from the centreline. Steady one-dimensional conduction with constant conductivity.

Calculator

Solve for
K
K
2501,000
W/m³
1,0001e9
m
0.010.2
m
00.01
W/(m K)
0.1500
  • Centreline temperature, Ts + q‴L²/(2k)340 K
  • Centreline rise above the faces40 K
  • Heat flux leaving each face, q‴L20,000 W/m²

What drives the result

Each variable is moved across its typical range while the others stay at the values above. The longest bar is the key driver.

Temperature at x (K) current value 330 K
q‴Volumetric heat generationKey driver
30030,300
LHalf-thickness
3004,290
kThermal conductivity
3001,800
TsFace temperature
2801,030
xDistance from the centre
340
  • At x = 0.01 m the slab is at 330 K, and the centre reaches 340 K, a rise of 40 K above the faces.
  • Each face removes 20,000 W/m²; doubling the thickness would quadruple the centre rise but only double the face flux.
Chart data as tables

Ranked variables

VariableTypical rangeLowest resultHighest resultSwing (K)Local stepChange in result
q‴ Volumetric heat generation1,000 to 1e9 W/m³30030,30030,000+10%+0.909 %
L Half-thickness0.01 to 0.2 m3004,2903,990+10%+2.55 %
k Thermal conductivity0.1 to 500 W/(m K)300.31,8001,500+10%−0.826 %
Ts Face temperature250 to 1,000 K2801,030750+10%+9.09 %
x Distance from the centre0 to 0.01 m33034010+10%−0.636 %

Sweep of Half-thickness

Half-thickness (m)Temperature at x (K)
0.01300
0.03375403.9
0.0575620.6
0.08125950.2
0.1051,392
0.12881,948
0.15252,616
0.17633,396
0.24,290

Sweep one variable

Temperature at x (K)Hover, touch, or use the arrow keys on the chart
01000200030004000 0.050.10.150.2 Half-thickness (m) now 330

Variables and how each one contributes

T

Temperature at x

Result · K

What the equation gives you. Everything else feeds it.

Ts

Face temperature

K · typical 250 to 1,000

The temperature of both faces, in K. Raises the temperature everywhere by the same amount. Raising it by 10 % (to 330) moves the result by +9.09 %, from 330 to 360 K.

q‴

Volumetric heat generation

W/m³ · typical 1,000 to 1e9

The uniform volumetric heat generation, in W/m³. Raises the temperature rise above the faces in direct proportion. Raising it by 10 % (to 1,100,000) moves the result by +0.909 %, from 330 to 333 K.

L

Half-thickness

m · typical 0.01 to 0.2

The half-thickness of the slab, in m. A thicker slab raises the temperature rise with the square of L. Raising it by 10 % (to 0.022) moves the result by +2.55 %, from 330 to 338.4 K.

x

Distance from the centre

m · typical 0 to 0.01

The distance from the centre plane, in m. Moving towards the face lowers the temperature, to Ts at x = L. Raising it by 10 % (to 0.011) moves the result by −0.636 %, from 330 to 327.9 K.

k

Thermal conductivity

W/(m K) · typical 0.1 to 500

The thermal conductivity, in W/(m K). A higher conductivity lowers the temperature rise in inverse proportion. Raising it by 10 % (to 5.5) moves the result by −0.826 %, from 330 to 327.3 K.

Worked example with the values above

  1. Geometry term: L² − x² = 0.02² − 0.01² = 3×10−4 m².
  2. Rise above the face: q‴(L² − x²)/(2k) = 1,000,000 × 3×10−4 / (2 × 5) = 30 K.
  3. T = 300 + 30 = 330 K.

Assumptions and limits

  • Uniform volumetric generation and constant conductivity in a steady state.
  • The stated boundary condition holds exactly, for example a fixed surface temperature or an insulated inner surface.

Common mistakes

  • Mixing the factor 2, 4 or 6 between the slab, cylinder and sphere.
  • Using the half-thickness or the full thickness in the wrong place.
  • Forgetting that generation is per unit volume, not per unit area.

Statistics and uncertainty

Volumetric heating is often known only to 10 % to 20 %, and the peak temperature scales directly with it. Use a margin on predicted centreline or hot-spot temperatures.

Where it is used

  • Hot-spot checks in busbars, fuel rods, heated plates and spherical particles.
  • Finding the surface temperature a coolant must hold for a given peak.

Maths you need

  • Volumetric generation: q‴ in W/m³
  • Steady conduction equation: k∇²T + q‴ = 0
  • Symmetry: zero gradient at the centre

Related formulas

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