- Thermal conductivity k
- 0.04W/(m·K)
- Cross-sectional area A
- 10m²
- Temperature difference ΔT
- 20K
- Thickness d
- 0.1m
80.00W
Open with these values80.00W
Result: 80.00 WFourier's law in one line: Q = k × A × ΔT ÷ d. A 10 m² wall of mineral wool 100 mm thick with 20 K across it passes 80 watts. Double the thickness and the loss halves; the temperature difference may be negative, and then heat flows the other way.
80.00W
Open with these values12,000.00W
Open with these values4,000,000.00W
Open with these valuesQ = k × A × ΔT ÷ d
| k, A, ΔT, d | What that could be | Heat flow in W |
|---|---|---|
| 0.04, 10, -20, 0.1 | same wall, heat flowing inward | -80.00 |
| 1, 1, 1, 1 | unit check of the formula | 1.00 |
| 0.025, 5, 30, 0.05 | a 50 mm still-air gap | 75.00 |
| 0.04, 10, 20, 0.1 | 100 mm of mineral wool | 80.00 |
| 1, 4, 15, 0.005 | 5 mm of window glass | 12000.00 |
| 400, 2, 50, 0.01 | 10 mm of copper | 4000000.00 |
Use Fourier's law: multiply the conductivity by the area and the temperature difference, then divide by the thickness. A 10 m² panel with k = 0.04, ΔT = 20 K and d = 0.1 m passes 0.04 × 10 × 20 ÷ 0.1 = 80 W.
It is how readily a material passes heat, in W/(m·K). Insulators are low — air about 0.026, mineral wool about 0.04 — while glass sits near 1 and copper near 400.
The thickness is in the denominator, so the heat flow is inversely proportional to it. Doubling an insulation layer halves the loss at the same temperature difference.
Thermal resistance is R = d ÷ (k × A) in K/W, and the heat flow is simply Q = ΔT ÷ R. The two calculators use the same three inputs and answer opposite questions: how much heat gets through, and how hard the layer makes it.
It means both faces sit at constant temperatures and the flow no longer changes with time. While the wall is still warming up, the flow varies and this simple form does not apply.
Information, not professional advice.
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