Heat Transfer · Chapter 1 of 10 · Beginner

Introduction: The Three Modes of Heat Transfer

Thermodynamics tells you how much energy moves; heat transfer tells you how fast. Three modes carry it: conduction, convection, and radiation, each with its own rate law.

01

Readiness check

From Thermodynamics and Thermal Physics. Tick only what you can do closed-notes.

  • Write an energy balance: in minus out plus generated equals stored.
  • Use Q = mcΔT for stored thermal energy.
  • Keep watts (a rate) distinct from joules (an amount).
  • Convert °C to kelvin, and know radiation demands kelvin.
  • Judge when steady state is a fair assumption.
0 or 1 weak itemsContinue with this chapter.
2 weak itemsReview the energy balance in Thermodynamics first.
3 or more weak itemsStep back to Thermal Physics; heat transfer is that material made into rates.
02

The core idea

Heat always flows from hot to cold, by three modes, each with a rate law in watts.

q = kA ΔT/Lq = hA ΔTq = εσA(Ts⁴ − Tsurr⁴)

Conduction carries heat through matter, convection carries it to a moving fluid, and radiation carries it as electromagnetic waves across any gap, even a vacuum. Real surfaces usually lose heat by two or three modes at once, and an energy balance keeps the books.

The skill works when: you name the dominant mode first, then apply only the rate laws that matter at this temperature and geometry.
The skill breaks down when: radiation is ignored at moderate temperatures, or temperatures are left in Celsius inside the T⁴ of radiation.
The concept. Heat arrives at a surface by conduction, then leaves to the surroundings by convection and radiation at the same time. A real cooling problem is deciding which of the three controls.
03

The skills, taught in order

Six ideas turn "it gets hot" into a number in watts. Learn the three rate laws, the energy balance that links them, and the habit of finding the mode that dominates.

1.1 What heat transfer adds to thermodynamics

Thermodynamics counts totals: how much energy a process moves, and the equilibrium it ends at. Heat transfer asks the next two questions: how fast does the energy move (a rate, in watts), and what temperature distribution does that produce. Those rates set the size of every heat sink, radiator, and layer of insulation.

1.2 Conduction

Conduction is heat diffusing through matter, down the temperature gradient. Fourier's law for steady one-dimensional flow is q = kA ΔT/L, where k is the thermal conductivity (W/m·K), A the area, and L the thickness. Metals conduct hundreds of times better than insulators, which is the whole reason both exist.

Materialk (W/m·K, near room temperature)
Copper≈ 400
Aluminium≈ 237
Carbon steel≈ 50
Stainless steel≈ 15
Glass≈ 1.0
Water≈ 0.6
Foam or fibre insulation≈ 0.04
Still air≈ 0.026

Micro-example. A 3 mm glass pane (k ≈ 0.8) with 20 K across it passes q/A = kΔT/L = 0.8 × 20 / 0.003 ≈ 5300 W/m², which is why a window's heat loss is set by the air films, not the glass.

1.3 Convection

Convection is heat carried away by a moving fluid. Newton's law of cooling lumps the messy fluid mechanics into one coefficient: q = hA(Ts − T), where h is the convection coefficient (W/m²·K). Finding h for a given flow is most of the rest of this course.

SituationTypical h (W/m²·K)
Free convection, gases2 to 25
Free convection, liquids50 to 1000
Forced convection, gases25 to 250
Forced convection, liquids100 to 20 000
Boiling or condensation2500 to 100 000

Micro-example. A chip surface 35 K above the air sheds hA ΔT per unit area: 35 × 10 ≈ 350 W/m² in still air, but 35 × 80 ≈ 2800 W/m² under a fan. The fan, not the chip, changed h.

1.4 Radiation

Every surface radiates, with no medium required. The net exchange with large surroundings is q = εσA(Ts⁴ − Tsurr⁴), where σ = 5.67 × 10⁻⁸ W/m²·K⁴ is the Stefan-Boltzmann constant and ε is the emissivity (0 to 1). The fourth-power law means radiation is negligible when cool but dominant when hot, and the temperatures must be absolute (kelvin).

1.5 The energy balance

Every heat-transfer problem is an accounting statement: energy in minus energy out plus energy generated equals the change in stored energy. At steady state the stored term is zero, so in equals out. On a surface (which stores nothing) the modes crossing it must sum to zero.

1.6 Finding the dominant mode

Before computing anything, ask which mode carries most of the heat. Compare the would-be rates or, better, the thermal resistances of Chapter 2. A surface in still air loses comparable heat by free convection and radiation; the same surface in a strong wind is convection-dominated. Naming the controlling mode first keeps the analysis honest and short.

Engineering connection: the foundation of cooling, insulation, and thermal management in every later chapter and in Energy Systems. Builds directly on Thermodynamics.

04

Worked example 1: how a hot surface loses heat

The outer face of an electronics enclosure is at 70 °C, has area 0.05 m², and sits in a room at 25 °C with still air (free-convection coefficient h = 10 W/m²·K). Its painted surface has emissivity ε = 0.9. Find the heat lost by convection and by radiation, and say which matters.

Figure 1. A warm surface in still air loses heat by free convection and by radiation at once. Here they are 22.5 W and 15.2 W, so radiation carries 40% of the total.
convectionradiation
  1. ProblemFind the convective and radiative heat loss from the 70 °C surface of Figure 1, and compare them.
  2. Given / findTs = 70 °C, T = Tsurr = 25 °C, A = 0.05 m², h = 10 W/m²·K, ε = 0.9. Find qconv, qrad, and the total.
  3. AssumptionsSteady state, uniform surface temperature, large surroundings at the air temperature, σ = 5.67 × 10⁻⁸ W/m²·K⁴.
  4. ModelTwo parallel paths off the surface: Newton's law of cooling for convection and the Stefan-Boltzmann net exchange for radiation. Radiation needs kelvin: 343 K and 298 K.
  5. Equationsqconv = hA(Ts − T) qrad = εσA(Ts⁴ − Tsurr⁴)
  6. Solveqconv = 10 × 0.05 × (70 − 25) = 22.5 W. qrad = 0.9 × 5.67×10⁻⁸ × 0.05 × (343.15⁴ − 298.15⁴) = 15.2 W. Total = 37.7 W, of which radiation is 40%.
  7. CheckBoth terms are positive (the surface is hotter than its surroundings) and the same order of magnitude, which is exactly what free convection plus radiation gives at moderate temperatures. Units: (W/m²·K)(m²)(K) = W, and (W/m²·K⁴)(m²)(K⁴) = W.
  8. ConclusionIgnoring radiation here would underestimate the cooling by 40% and overpredict the chip temperature. At moderate temperatures with still air, radiation is not optional. A fan would raise h tenfold and make convection dominate instead.
Result. qconv = 22.5 W, qrad = 15.2 W, total 37.7 W. Radiation carries 40%, so it cannot be dropped.
05

Worked example 2: sizing insulation

A cold-room wall of area 12 m² must hold its heat gain to 60 W when the temperature difference across the foam insulation (k = 0.030 W/m·K) is 25 °C. How thick must the foam be?

Figure 2. Steady conduction through an insulating slab. Fixing the allowed heat gain and the temperature difference sets the thickness through Fourier's law.
  1. ProblemFind the foam thickness L that limits the heat gain to 60 W for the wall in Figure 2.
  2. Given / findq = 60 W, A = 12 m², ΔT = 25 °C, k = 0.030 W/m·K. Find L.
  3. AssumptionsSteady one-dimensional conduction through the foam, the foam the controlling resistance (surface films neglected), constant k.
  4. ModelFourier's law for a slab, solved for thickness.
  5. Equationsq = kA ΔT/L L = kA ΔT/q
  6. SolveL = (0.030 × 12 × 25) / 60 = 9 / 60 = 0.15 m = 15 cm.
  7. CheckUnits: (W/m·K)(m²)(K)/(W) = m. Scale: thick foam for a small heat leak is right, since foam's k is tiny. Halving the allowed heat gain to 30 W would double the thickness to 30 cm, the inverse relation Fourier predicts.
  8. ConclusionFifteen centimetres of foam meets the target. Conduction set the answer through one material constant and two geometry choices, which is the everyday arithmetic of insulation and the launching point for the resistance networks of Chapter 2.
Result. L = 0.15 m (15 cm) of foam. Thickness scales inversely with the allowed heat gain.
06

Misconceptions and diagnostics

MistakeSymptomDiagnostic questionCorrection
Heat and temperature confused"It is hot, so a lot of heat flows""Is this a temperature or a rate of energy?"Temperature (K) is a level; heat rate (W) depends on the temperature difference and the path. A warm, well-insulated wall passes little heat.
Radiation forgottenFree-convection problems solved with q = hA ΔT alone"Is the surface warm and the air still?"Then radiation rivals convection. Add q = εσA(T⁴) whenever h is small.
Celsius inside the T⁴Radiation answers wildly wrong"Are my radiation temperatures in kelvin?"The Stefan-Boltzmann law needs absolute temperature. Convert before raising to the fourth power.
Area or thickness droppedConduction reported in W/m² called the heat rate"Did I multiply by area and divide by thickness?"q = kA ΔT/L is a rate in watts; q/A = kΔT/L is a flux in W/m². Keep them separate.
07

Practice ladder

Level 1 · Direct skill

A 2 m² window of glass 4 mm thick (k = 1.0 W/m·K) has 18 °C across the pane itself. Find the conduction heat rate through the glass.

Show answer

q = kA ΔT/L = 1.0 × 2 × 18 / 0.004 = 9000 W. The glass barely resists heat; real windows rely on the air films and gas gaps, the resistances of Chapter 2.

Level 2 · Mixed concept

Repeat Worked Example 1 with a fan that raises h to 60 W/m²·K. Find the new convective loss and the new radiation share of the total.

Show answer

qconv = 60 × 0.05 × 45 = 135 W; radiation is still 15.2 W, so the total is 150.2 W and radiation is now only 10%. Forced convection swamps radiation, which is why radiation is most often dropped for cooled electronics but not for still-air ones.

Level 3 · Independent problem

A 1500 W electric heater element reaches steady state losing all its power from a 0.02 m² surface to a 20 °C room. If convection gives h = 30 W/m²·K, estimate the surface temperature, ignoring radiation. Then comment on whether ignoring radiation was safe.

Show answer

1500 = 30 × 0.02 × (Ts − 20) gives Ts − 20 = 2500 K, so Ts ≈ 2520 °C, absurdly hot. That signals the model is wrong: at such temperatures radiation (T⁴) carries most of the heat, so it cannot be ignored. Real heater elements glow precisely because radiation dominates.

Level 4 · Transfer to real engineering

Pick a real warm object (a laptop charger, a radiator, a mug of coffee). Estimate its surface temperature, area, and surroundings, then compute its convective and radiative losses and name the dominant mode.

What good work looks like

Stated temperatures in kelvin for radiation, both rate laws applied with reasonable h and ε, the two losses compared, and a one-sentence verdict on which mode controls and why.

08

Working with AI, and proving it yourself

Use AI as an examiner, not a solver

"Here is my mode breakdown for this surface. Check whether I was right to keep or drop radiation, and whether my temperatures are in kelvin."
"Give me five warm objects; I will name the dominant mode for each before you confirm."
"Compute the heat loss." Choosing which modes matter is the judgment this chapter trains.
"Which is bigger, convection or radiation?" Estimating both yourself is the skill.

Portfolio task

Write a one-page "Modes Card": the three rate laws with units, the k and h tables in your own words, and one worked surface where you compute all the active modes and declare the dominant one.

Must include: radiation worked in kelvin, the convection coefficient justified from the h table, and a stated dominant mode with its share of the total.
09

Retrieval and spaced review

Closed notes. Answer out loud, then reveal.

1. State the three rate laws with their units.

Conduction q = kA ΔT/L; convection q = hA ΔT; radiation q = εσA(Ts⁴ − Tsurr⁴). All give watts.

2. What does heat transfer add to thermodynamics?

Rates (how fast, in watts) and temperature distributions, where thermodynamics gave only totals and end states.

3. When can radiation not be ignored?

Whenever the convection coefficient is small (still air) or the surface is hot, because radiation grows as T⁴.

4. Write the general energy balance and its steady-state form.

In − out + generated = stored; at steady state stored = 0, so in = out.

5. Why must radiation temperatures be in kelvin?

The law uses absolute temperature raised to the fourth power; Celsius has an arbitrary zero and breaks T⁴.

TodayFinish this quiz and Levels 1 and 2 of the ladder.
+1 dayRe-derive the 70 °C surface losses from a blank page.
+3 daysOne dominant-mode estimate for a new object.
+7 daysMixed set: a conduction sizing plus a modes comparison.
+30 daysOpen Chapter 2 and turn these rate laws into resistance networks.
10

Textbook mapping

ItemMapping
Primary sourceLienhard and Lienhard, A Heat Transfer Textbook (6th ed), Chapter 1 (modes of heat transfer)
Cross-referenceIncropera, Fundamentals of Heat and Mass Transfer, Ch. 1 · Çengel and Ghajar, Ch. 1
Core topics1.1 Rates versus totals · 1.2 Conduction · 1.3 Convection · 1.4 Radiation · 1.5 Energy balance · 1.6 Dominant mode
Engineering connectionThe basis of all cooling, insulation, and thermal management; builds on Thermodynamics.
Read nextChapter 2: Steady Conduction and Thermal Resistance.