Thermal conduction calculator

Heat flow, thermal resistance and U-value of a single layer.

Inputs

Thermal conduction calculator

4 fields

One-dimensional steady conduction through one layer with constant k. Surface films, radiation, thermal bridges, contact resistances and heat storage are excluded. Negative ΔT reverses flow; zero ΔT gives zero flow.

Fill in the fields and the result will appear here automatically.

Calculate steady heat flow through one flat uniform layer. Enter the temperature difference between its faces; conductivity is constant. The shown coefficient k/d belongs to this layer, not a complete wall or window with surface heat transfer. Daily energy assumes the same conditions for all 24 hours.

FAQ
4 questions
Freshness
formula-based

How it works

Formula and logic

Flow = conductivity × area × temperature difference ÷ thickness. Thermal resistance = thickness ÷ conductivity, and the U-value is its reciprocal.

Example

A 10 m² wall with 200 mm of mineral wool at a 25 K difference passes 50 W.

Fields and units

  • Area — m²
  • Layer thickness — m
  • Thermal conductivity λ — W/(m·K)
  • Temperature difference — K

How to use

  • — Enter the area of the construction.
  • — Set the layer thickness in metres: 200 mm is 0.2.
  • — Give the conductivity: mineral wool 0.04, brick 0.7, glass 1.0, timber 0.15 W/(m·K).
  • — Set the temperature difference across the layer.

Method and limitations

Calculation method
Formula and logic
Data or methodology source
OpenStax: steady conduction through a layer
Limitation
One-dimensional steady conduction through one layer with constant k. Surface films, radiation, thermal bridges, contact resistances and heat storage are excluded. Negative ΔT reverses flow; zero ΔT gives zero flow.

FAQ

Why does glass give such an enormous flow?

Because only the conduction of the glass itself is counted, and its resistance is negligible. A real window holds heat through the air films at its surfaces and the cavity between panes.

How do I combine several layers?

For plane layers in series with equal area, Rlayers=Σdᵢ/kᵢ. A complete assembly coefficient also needs the relevant surface and contact resistances. They depend on conditions and are not automatically inserted here.

How is this different from a heating power calculator?

That works out how much heat a room needs from its volume. This works out how much escapes through one specific construction from its conductivity.

Why can the difference be negative?

Because the flow can run inward: in summer the outside is warmer than the room. The sign shows direction; the magnitude is unchanged.