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SCIENCE · INVESTIGATE AND EXPLAIN

Combine thermal resistances in series

Explain how layers share a temperature difference without splitting the heat rate.

Learning outcome: Add series resistances, solve an interface temperature, and test how thickness and conductivity affect the whole assembly.

Starting recap

For a slab, thermal resistance L/(kA) has units K/W. A steady series path carries the same heat rate through every layer.

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Try

Doubling the thickness of one layer does not necessarily halve the heat rate through the whole wall.

Open the experiment

Predict

At conductivity 0.1 W/(m K), compare second-layer thicknesses 20 and 40 mm. Predict the heat-rate ratio and whether the interface becomes hotter or colder.

Experiment

Capture both thickness cases and add the resistances. Then set thickness 20 mm and conductivity 0.2: verify equal slopes and equal drops. Compare the minimum and maximum resistance cases without changing the outer surface temperatures.

Conduct heat through two layers

Worked teaching model · synthetic values · Steady one-dimensional conduction through two uniform layers in series, area 0.5 m². Layer 1 is 20 mm thick with conductivity 0.2 W/(m K). Maintained outer surface temperatures are 80 and 20 °C; they are not ambient air temperatures. Perfect thermal contact, no lateral losses, internal heat generation, temperature dependence, convection or radiation. The temperature profile is already established; no warm-up time, heat capacity or real insulation rating is inferred. Layer 2 properties are synthetic teaching choices.

Reset keeps your prediction, captures and practice history.

Temperature (°C) · fixed outer surface temperatures020406080100010203040506070Layer 1Layer 2Position through the layers (mm), not time

At the interface the temperature is continuous because perfect contact is assumed. A change in slope reflects a change in conductivity; it does not represent energy accumulation.

Equal heat rates, separate temperature drops
LayerThickness (mm)Conductivity (W/(m K))Resistance (K/W)Left temperature (°C)Right temperature (°C)Drop (K)Heat rate (W)
Layer 1200.2000.20080.00065.00015.00075.000
Layer 2300.1000.60065.00020.00045.00075.000

Heat travels from the maintained 80 °C surface to the maintained 20 °C surface. Energy entering equals energy leaving: there is no net energy storage in either layer at steady state. The hot source supplies 75.000 W and the cold sink removes the same rate.

Steady heat-transfer rate 75.000 W; interface temperature 65.000 °C.

The same 75.000 J/s crosses each layer. Total resistance 0.800 K/W; heat flux 150.000 W/m². In ten minutes at these maintained conditions, 45.000 kJ passes through the assembly, not twice that amount.

Captures preserve recipes and replay their calculated results. They are synthetic model evidence, not physical measurements.

Understand

Find the unknown interface temperature

Two layers share the 60 K difference between the 80 °C and 20 °C outer surfaces. The interface temperature is unknown. Treating both layers as if each spanned the full 60 K would describe incompatible boundaries. Instead use the fact that the same rate crosses both layers at steady state.

The control changes the thickness and conductivity of layer 2. Layer 1 remains 20 mm thick with k₁ = 0.2 W/(m K). Both layers share area A = 0.5 m², with perfect contact and no lateral leakage. Each selected setting describes a new steady condition.

Express each layer as a resistance

Rearrange the slab relation P = kAΔT/L to ΔT = PR, where R = L/(kA). R is thermal resistance in K/W: the temperature difference required per watt through the layer. A larger R means a smaller rate for the same face-temperature difference.

Do not confuse R with heat capacity C in J/K. Nor is this whole-assembly resistance the same quantity as an area-normalized insulation value in m² K/W. Here area is already included. The OpenStax conduction reference provides the slab relation; this lesson uses it to construct an original two-layer energy account.

For layer 1, R₁ = 0.020/(0.2 × 0.5) = 0.2 K/W. At the defaults, R₂ = 0.030/(0.1 × 0.5) = 0.6 K/W.

Add drops, not heat rates

The total temperature drop equals the sum across layers: Th − Tc = PR₁ + PR₂. Therefore P = (Th − Tc)/(R₁ + R₂). Series resistances add because the same energy-transfer rate passes through successive layers.

At the defaults, Rtotal = 0.8 K/W, so P = 60/0.8 = 75 W. Layer 1’s drop is PR₁ = 15 K and layer 2’s is PR₂ = 45 K. The interface temperature is 80 − 15 = 65 °C, also 20 + 45 = 65 °C. Both calculations must agree.

The larger resistance receives the larger share of the total temperature drop. The drop ratio is R₂/R₁ = 3. This does not mean layer 2 carries three times the heat rate or stores three times the energy; neither claim follows from a steady resistance account.

Test a tempting shortcut

Hold conductivity at 0.1 W/(m K). At 20 mm, layer 2 has R₂ = 0.4 K/W. Total R is 0.6 K/W and P is 100 W, with interface at 60 °C. Double that layer’s thickness to 40 mm: R₂ doubles to 0.8 K/W, but total R rises only to 1.0 K/W. The new rate is 60 W, with interface at 68 °C.

The whole-assembly rate falls to 60%, not 50%. Layer 1’s resistance did not double. The interface gets hotter because a smaller heat rate needs a smaller drop across the unchanged first layer. Capture both cases and explain each change from the resistance ledger.

Increasing layer 2 conductivity at fixed thickness reduces its resistance and increases the total rate. Equal conductivities produce equal temperature slopes because the same area and rate apply. If layer 2 is also 20 mm thick with k₂ = 0.2 W/(m K), both resistances are 0.2 K/W: the rate is 150 W, both drops are 30 K and the interface is 50 °C.

Keep the boundaries and path arrangement explicit

Adding a layer in series increases total resistance under these assumptions. A gap or a metal connection that creates another route for heat is a different geometry: parallel paths share boundary temperatures and their rates add. This widget does not calculate such a thermal bridge.

Real outer surface temperatures can differ from nearby air temperatures because convection and radiation also act at surfaces. Those effects require additional boundary relations. Imperfect contact can produce a temperature jump. Temperature-dependent conductivity can curve a profile. The current piecewise-linear graph does not estimate any of these effects.

Changing the order of these two constant-property layers would leave total resistance and rate unchanged, but it would change the interface temperature because a different resistance lies next to the hot surface. This conclusion depends on the ideal assumptions; it is not a rule for every composite material or boundary condition.

Transfer to three layers

Three series layers have resistances 0.1, 0.3 and 0.2 K/W. The outer surfaces are held at 70 °C and 10 °C. Calculate the common rate and temperatures after the first and second layers. Then add another 0.4 K/W layer and predict the new rate.

Check the resistance-network transfer

Total resistance is 0.6 K/W, so P = 60/0.6 = 100 W. Drops are 10, 30 and 20 K. The interfaces are 60 °C and 30 °C, ending at 10 °C. Adding 0.4 K/W in series gives total 1.0 K/W and P = 60 W. Do not retain the old interface temperatures: all drops must be recalculated with the new common rate.

Apply

Two layers in series have resistances 0.2 and 0.4 K/W. Their outer surfaces differ by 60 K. The steady heat rate is:

Public practice checks a specific claim. It does not establish independent mastery.

Explain why resistances add but heat rates do not. Distinguish this ideal series assembly from a wall with gaps, thermal bridges or ambient-air boundaries.

Continue

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