🌡️ Thermodynamics · Heat Transfer
📅 Березень 2026 ⏱ ≈ 7 хв читання 🟢 Beginner

How a Thermos Works

Heat can only travel in three ways: conduction through solid materials, convection through fluids, and radiation as electromagnetic waves. A vacuum flask systematically defeats all three — which is why a thermos can keep coffee hot for 12 hours.

The Three Modes of Heat Transfer

In thermodynamics, heat always flows from a hotter region to a cooler one — never the reverse (Second Law). But the route it takes depends on the medium:

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Conduction
Vibrating atoms pass kinetic energy along a solid. Fast in metals, slow in glass, essentially zero in vacuum.
Almost blocked by vacuum
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Convection
Hot fluid rises and carries energy with it. Requires a fluid (liquid or gas) to be present — impossible in a vacuum.
100% blocked by vacuum
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Radiation
Every object emits infrared electromagnetic waves. Passes freely through vacuum — must be stopped by reflection.
Reduced by silver coating

Mode 1 — Conduction

When you hold a metal spoon in hot soup, the heat travels along the spoon to your fingers. This is conduction: lattice vibrations and (in metals) free electrons carry thermal energy through solid matter.

Fourier's Law of heat conduction gives the rate of heat flow:

Q/t = k · A · ΔT / d k = thermal conductivity (W/m·K) A = cross-sectional area (m²) ΔT = temperature difference (K) d = thickness of material (m)

Thermal conductivity k varies enormously across materials:

Material k (W/m·K) Relative conductivity
Silver 429 Extremely high
Copper 401 Very high
Glass 1.0 Low
Air (still) 0.025 Very low
Vacuum ≈ 0 Essentially zero
Aerogel 0.015 Lowest solid known

A vacuum has essentially zero thermal conductivity because there are no atoms to vibrate and carry energy. A thermos flask has a vacuum gap between two glass (or steel) walls — typically about 1 mm wide at pressures below 0.001 Pa (≈10⁻⁵ atmospheres).

Why not just use foam? Foam insulation (like a coffee cup) traps still air in tiny pockets. Still air has k ≈ 0.025 W/m·K. A vacuum has k ≈ 0. This makes a vacuum roughly 30× more effective than foam of the same thickness at blocking conduction.

Mode 2 — Convection

Convection moves heat by bulk movement of fluid. When hot air or water rises (because it's less dense), cooler fluid replaces it, creating a convective current that efficiently redistributes thermal energy.

The rate of convective heat transfer is described by Newton's Law of Cooling:

Q/t = h · A · ΔT h = convection coefficient (W/m²·K) — depends on fluid, geometry, and flow speed

The convection coefficient h for a hot mug in still air is about 5–25 W/m²·K — enough to cool coffee noticeably in minutes. By removing the air from the gap between the flask walls, a thermos eliminates convective heat loss entirely. No fluid, no convection.

Mode 3 — Radiation

Unlike conduction and convection, radiation does not require any medium. Every object with a temperature above absolute zero emits electromagnetic radiation — predominantly infrared at everyday temperatures. This energy travels at the speed of light through vacuum.

The total power radiated per unit area is given by the Stefan–Boltzmann Law:

P = ε · σ · T⁴ ε = emissivity (0–1; 1 = perfect black body) σ = 5.67 × 10⁻⁸ W/m²·K⁴ (Stefan–Boltzmann constant) T = absolute temperature in Kelvin

Because radiation scales with T⁴, small temperature differences create large radiative fluxes. A mug at 80°C (353 K) radiates significantly more than its surroundings at 20°C (293 K).

Crucially, a vacuum cannot stop radiation — this is how the Sun's energy reaches Earth. To block radiation, the thermos uses a different trick.

How a Vacuum Flask Beats All Three

Sir James Dewar invented the vacuum flask in 1892 for storing liquid nitrogen and hydrogen. The design is elegantly simple:

  1. Double-walled construction: Two concentric glass (or stainless steel) cylinders.
  2. Vacuum gap: The air is evacuated from the space between the walls — blocks conduction and convection.
  3. Silvered walls: Both inner surfaces are coated with a thin layer of silver — reflects radiation back.
  4. Thin support: The two walls are connected only at the narrow neck — minimising the conduction pathway.
  5. Insulating stopper: The cork or plastic lid prevents convection at the opening.
Heat transfer mode Thermos countermeasure Effectiveness
Conduction (walls) Vacuum gap between walls ~99% blocked
Convection Vacuum gap (no gas to convect) 100% blocked
Radiation Silvered walls reflect IR ~95–99% reduced
Conduction (neck) Narrow glass/steel neck only Partially reduced
Convection (top) Insulating lid/stopper Significantly reduced

Stefan–Boltzmann Law: Why Silver Matters

The emissivity ε determines how efficiently a surface radiates (and absorbs) infrared. A perfect black body has ε = 1. Polished silver has ε ≈ 0.02 — it radiates (and absorbs) only 2% as much as a black body at the same temperature.

This means a silvered wall reflects about 98% of incoming infrared radiation. The net radiative heat transfer between the two silvered walls of a thermos is dramatically reduced:

P_net = σ · (T₁⁴ − T₂⁴) / (1/ε₁ + 1/ε₂ − 1) For silver: ε₁ = ε₂ = 0.02 Denominator = 1/0.02 + 1/0.02 − 1 = 99 → radiation reduced to ~1% of what uncoated glass would radiate
Emergency (space) blankets use this same principle. The thin aluminised Mylar foil has very low emissivity and reflects your body's infrared radiation back to you — providing lightweight thermal insulation without any bulk insulating material.

Real-World Performance Numbers

A typical quality vacuum flask loses heat at roughly 0.5–2°C per hour for a hot liquid, compared to 5–15°C per hour for a ceramic mug in still air. The remaining heat loss is almost entirely through:

Cold works the same way: A thermos keeps ice cream cold equally well — it's not "keeping cold in", it's "keeping heat out". The direction of heat flow reverses (heat flows inward from the warm surroundings), but the same three mechanisms are at work and the vacuum blocks them just as effectively.

Beyond the Thermos

Vacuum insulation principles appear in many engineering contexts:

Try It Yourself

Explore heat conduction and molecular dynamics — the microscopic origin of thermal conductivity — in the simulation:

⚛️ Molecular Dynamics Simulation →

See how the atmosphere traps radiated heat from the Earth's surface — the same Stefan–Boltzmann radiation at work on a planetary scale:

🌍 Read: The Greenhouse Effect →