Heat Transfer Calculator.

Three modes, one equation. Every mode is a thermal resistance, so Q = ΔT/R holds in all three, and the convection coefficient h is computed from real correlations rather than typed in.

Mode
Units
Transfer mode

Conduction — Fourier’s Law

Conduction — carbon steel · k = 60.5 W/m·KhotcoldT(x)T₁ = 300 °CHOT FACET₂ = 50 °CCOLD FACEL = 0.1 mA = 2 m²L and A are drawn to a compressed scale — every printed value is exact
00.0250.050.0750.125100175250325position through the wall (m)temperature (°C)a straight line, because k is constant

Heat rate Q

302.5 kW

Thermal resistance R

0.0008264 K/W

Heat flux q

151,250 W/m²

Driving ΔT

250 K

Conductivity k

60.5 W/m·K

Temp. gradient

2,500 K/m

Mode

Conduction

Formula

Q = kAΔT / L

No warnings — every assumption behind these numbers holds for this set-up.

The arithmetic, with your numbers in it

R = L / (k·A) = 0.100 / (60.500 × 2.00) = 8.26e-4 K/W

Q = ΔT / R = 250.0 / 8.26e-4 = 302500.0 W

q = Q / A = 302500.0 / 2.00 = 151250.0 W/m²

Presets

Pick a preset to load a real case, or set your own with the controls below.

Material

How to calculate conduction, convection and radiation

  1. Pick the mode. Conduction is heat through a solid, convection is heat between a surface and a moving fluid, and radiation is heat crossing empty space. The controls change completely between them, because the three mechanisms genuinely need different information.
  2. Set the geometry and the two temperatures. Every mode needs an area and a driving difference; conduction also wants a thickness and a material, convection wants a fluid and a speed, and radiation wants an emissivity and two ABSOLUTE temperatures in kelvin.
  3. Read the resistance, not just the answer. All three modes are shown as a thermal resistance R, and in every one of them Q = ΔT/R. That is what lets you compare a wall against a breeze against a radiant panel on the same footing.
  4. In convection, watch where h comes from. The working shows the Reynolds number, the Prandtl number, the correlation used and the Nusselt number it produced — h is a result of those, not something you look up.
  5. Use the mode pages for depth. Each of the three has its own page with the law it obeys, where it dominates in practice, and the mistakes that cost marks.

Three modes, one equation

Conduction, convection and radiation are usually taught as three different subjects with three different formulas. They are better understood as three different thermal resistances. In every one of them the heat rate is the temperature difference divided by a resistance, Q = ΔT / R, exactly as current is voltage over resistance in a circuit. What changes between the modes is only how R is worked out.

Mode Resistance R at our defaults Q at our defaults
Conduction R = L / (k·A) 0.0008264 K/W 302.5 kW
Convection R = 1 / (h·A) 0.08142 K/W 1.535 kW
Radiation R = 1 / (h_r·A) 0.02745 K/W 18.21 kW

The defaults are a carbon steel wall 100 mm thick over 2 m² between 300 °C and 50 °C; a flat plate at 150 °C in 5 m/s of 25 °C air; and two facing surfaces at 800 K and 300 K with an emissivity of 0.8. The figures come from the same solver the instrument runs, so they move if the model does.

Which mode wins, and when

All three modes are nearly always at work together, and one of them usually dominates. Inside a solid only conduction is possible. Across a vacuum only radiation is. Between a surface and the air around it, convection and radiation run side by side, and which one leads depends almost entirely on temperature.

Take a 1 m² vertical surface in still 20 °C air. Free convection carries heat away roughly in proportion to the temperature difference. Radiation carries it in proportion to the difference of the fourth powers of the absolute temperatures, and that difference grows much faster:

  • At 350 K (77 °C), free convection removes about 287.8 W and radiation 359.9 W.
  • At 600 K (327 °C), free convection removes about 2.233 kW and radiation 5.558 kW.
  • At 900 K (627 °C), free convection removes about 4.655 kW and radiation 29.44 kW.

That is why a radiator is named after the smaller of its two effects, why furnace engineers design around radiation, and why a vacuum flask has to silver its walls: once conduction and convection are removed, radiation is the only path left.

Putting the modes together

Because each mode is a resistance, a real problem is a small circuit. Resistances that the heat must cross one after another add in series. Resistances that offer the heat a choice of paths, such as convection and radiation from the same outer surface, combine in parallel as 1/R = 1/R₁ + 1/R₂.

Put a still-air film on the cold face of the default steel wall and it becomes two resistances in series. The wall contributes 0.0008264 K/W and the air film 0.1128 K/W, with h ≈ 4.431 W/m²·K from the free-convection correlation. The film is about 137 times the wall. With the room at 20 °C the loss falls from 302.5 kW to 2.464 kW, which shows how an insulating layer of still air can matter more than the steel itself.

Heat exchanger designers do the same sum and call the result the overall coefficient U, through 1/(UA) = ΣR. The heat exchanger simulator picks up from there.

Heat transfer — common questions

What are the three modes of heat transfer?

Conduction, convection and radiation. Conduction moves heat through a solid or between solids in contact, and obeys Q = kAΔT/L. Convection moves it between a surface and a moving fluid, and obeys Q = hAΔT. Radiation moves it as electromagnetic waves and needs no medium at all, obeying Q = εσFA(T₁⁴ − T₂⁴). All three are usually present at once; one usually dominates.

Are conduction, convection and radiation really the same equation?

Structurally, yes, and that is the idea this tool is built around. Each mode is a thermal resistance, and in every one of them Q = ΔT/R. Conduction gives R = L/(kA), convection gives R = 1/(hA), and radiation gives R = 1/(hrA) where hr = εσF(T₁+T₂)(T₁²+T₂²). The radiation form is an exact identity rather than a linearisation, because T₁⁴ − T₂⁴ factorises precisely that way.

Which mode dominates in a given situation?

Inside a solid, conduction is the only mode available. Between a surface and a fluid, convection usually leads — free convection weakly, forced convection strongly. Across a vacuum, radiation is the only mode that can cross at all. Above roughly 600 °C radiation tends to take over even in air, because it scales as the fourth power of absolute temperature while convection is close to linear.

How do you combine the three modes?

Add their resistances. A hot pipe losing heat to a room conducts through its wall, then loses heat from its outer surface by convection and radiation acting in parallel. Series resistances add directly; parallel ones combine as 1/R = 1/R₁ + 1/R₂. That total is exactly what a heat exchanger calls the overall coefficient U, through 1/U = ΣR referred to unit area.

Where does the convection coefficient h come from?

It is computed, not looked up. h depends on the fluid, the geometry, the flow speed and the temperature difference, and it is obtained through the Reynolds, Prandtl and Nusselt numbers using an empirical correlation for the shape in question. Most calculators ask you to type it in; this one derives it and shows every step, which is what the convection mode is really for.

Is this heat transfer calculator free to use?

Yes — it runs entirely in your browser, needs no signup, and the results update as you change the inputs. You can share a particular setup by copying the link, which carries the parameters in readable form so the person you send it to sees exactly the case you did.

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