Leave a mug of tea on the table and it goes cold. Warm your hands on it and they heat up. Stand in sunshine and your face glows. In every case energy is on the move — and it always travels the same way round: from the hotter thing to the cooler thing, never the other way, until everything reaches the same temperature.
But how does that thermal energy actually get from hot to cold? Nature has exactly three ways of doing it, and the whole of this page is about telling them apart:
They sound similar — all three "make things warmer" — but they work by completely different machinery, and knowing which is which is one of the most useful ideas in all of physics. Learn them by contrast: what each one needs, and what it can't do.
Hold a metal spoon in a hot cup of tea and, within a few seconds, the far end you're holding goes warm too — even though that end never touched the tea. That is conduction.
Picture the
Because the particles have to be close enough to knock into each other, conduction works best in solids, where particles are packed tight in a fixed lattice. It is feeble in liquids and gases, whose particles are spread far apart with little to bump into — which is exactly why gases like air are such good insulators.
Metals are the champion conductors, and there is a lovely reason. Inside a metal, the outer electrons of every atom are not tied to any one atom — they roam free through the whole lump as a "sea" of free electrons. These tiny, fast movers pick up energy at the hot end and shuttle it across to the cold end almost instantly, on top of the slower particle-to-particle jostling. Wood, plastic and glass have no free electrons, so their only trick is the slow bumping — which is why a wooden spoon stays cool in the same hot pan that makes a metal one too hot to hold. It's also why a metal railing feels colder than a wooden one on the same frosty morning: the metal conducts heat out of your hand far faster, even though both are at the very same temperature.
Conduction can't get very far in a liquid or a gas — so fluids use a different, cleverer trick. When you heat the bottom of a pan of water, the water down there warms up, and warm water expands. Spreading the same particles over more space makes it less dense — lighter for its size — so it floats upwards, exactly as a cork bobs up through water. Cooler, denser fluid sinks down to take its place, gets heated in turn, and rises too.
The result is a never-ending loop called a convection current: hot fluid rising, cooling at the top, sinking at the sides, and being reheated at the bottom. Notice the huge difference from conduction — here the warm particles themselves travel, physically carrying their energy along for the ride.
Convection is everywhere once you spot it:
And here is the catch that defines convection: it needs particles that are free to flow. That means it can only happen in a fluid — a liquid or a gas. It can never happen in a solid, because a solid's particles are locked in place and can't rise or sink.
Now the strangest of the three. Conduction and convection both need stuff — particles to bump, or fluid to flow. But the warmth of the Sun reaches us across 150 million kilometres of empty space, where there are almost no particles at all. It can't be conduction or convection. It is thermal radiation.
Radiation is energy carried by infrared — a kind of
A few key facts, all worth knowing:
That surface rule explains a hundred everyday things: a black car gets scorching in the sun while a white one stays cooler; houses in hot countries are painted white to reflect the Sun's heat; the shiny foil blanket wrapped round a marathon runner reflects their own infrared back onto them; and solar hot-water panels are painted matt black to soak up as much radiation as possible.
Use the top control to switch between conduction, convection and radiation, and drag the Run it slider to set each one going. Watch the contrast: in conduction the energy hops along a solid bar while the particles stay put; in convection a whole current of fluid loops round, physically carrying the heat; in radiation the energy leaps a completely empty gap as infrared waves.
These three mix-ups cost more marks than anything else in this topic:
A vacuum flask (a "Thermos") keeps a hot drink hot for hours — and a cold drink cold — by cleverly shutting down every one of the three heat-transfer routes at the same time. Look at how it does it:
Defeat conduction, convection and radiation together and heat has almost nowhere to go — which is the whole trick behind the flask, and behind the shiny, vacuum-panelled walls of a modern cool-box too.