Multilayer Wall Conduction
This lab applies **Fourier’s law** in **steady, one-dimensional** conduction through **three homogeneous layers in series**. In each slab, temperature varies **linearly** with thickness. Per unit area, layer resistance is **R″ = L/k** (L in metres, k in W/(m·K)). Total resistance adds: **R″_tot = Σ R″_i**, heat flux **q″ = (T_left − T_right) / R″_tot**, and **U = 1/R″_tot**. The drawing shows a color gradient by temperature, a **T(x)** polyline at interfaces, and an arrow for **q″** from hot to cold. A one-click preset loads **plaster / brick / mineral wool** thicknesses and conductivities as a teaching example, not a certified U-value for a real building.
Who it's for: Introductory heat transfer and building-science intuition; complements the 2D heat-transfer playground.
Key terms
- Fourier conduction
- thermal resistance R″
- U-value
- series layers
- heat flux q″
- thermal conductivity k
How it works
Steady one-dimensional conduction through three layers in series: temperature is linear in each slab, and the heat flux q″ = (T_left − T_right) / Σ(L/k) per unit area. Compare thermal resistance of plaster, masonry, and insulation.
Frequently asked questions
- Why is T a straight line inside each layer?
- With no internal sources and steady 1D conduction in a uniform material, the heat equation reduces to d²T/dx² = 0, so T is linear in x. Different slopes appear in different layers because k and thickness change the thermal resistance.
- Does this U-value match my wall certificate?
- No. Real envelopes include surface resistances, air gaps, moisture, and 2D/3D bridges. The simulator isolates bulk conduction in three slabs with ideal interfaces.
- What if T_right is hotter than T_left?
- Then q″ is negative: heat flows from right to left. The arrow and displayed flux magnitude reflect that sign convention.
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