Heat Transfer

Thermal energy moves from a region of higher temperature to one of lower temperature by three mechanisms: conduction, convection, and radiation.

Conduction

Conduction transfers heat through a material without bulk movement of the material itself. In metals, free (conduction) electrons gain kinetic energy from the hot end and diffuse rapidly through the metal, transferring energy to cooler regions. In non-metals, energy is transferred by vibrations passing between adjacent atoms, this is slower, making non-metals poor conductors.

Conductors and insulators:

• Good conductors: metals (copper, aluminium, iron). Copper is used in heat exchangers, car radiators, and solar heater pipes because it conducts heat rapidly.
• Poor conductors (insulators): wood, glass, plastic, air, fibreglass. Insulators are used in building walls, clothing, and handles of cooking utensils.

Liquids and gases are generally poor conductors because their particles are more widely spaced. Air is a particularly good insulator when trapped (in double-glazed windows, foam, or expanded polystyrene).

Convection

Convection transfers heat through a fluid (liquid or gas) by the bulk movement of the fluid itself. When a fluid is heated, it expands, becomes less dense, and rises. Cooler, denser fluid sinks to take its place, creating a convection current.

Land and Sea Breezes

Convection currents at the coast produce daily wind patterns relevant to the Caribbean:

Sea breeze (daytime): The land heats up faster than the sea. Air above the land becomes warmer, expands, and rises. Cooler air from over the sea flows in to replace it, this is the sea breeze, experienced as a cooling breeze on Caribbean coasts during the day.

Land breeze (night-time): The land cools faster than the sea. Air above the sea is now warmer, rises, and air from the land flows out to replace it, a gentle breeze blowing from land toward the sea.

Radiation

Radiation transfers heat as electromagnetic waves (infrared radiation). Unlike conduction and convection, radiation does not require a medium, it travels through a vacuum. This is how the Sun's energy reaches Earth.

Factors Affecting Absorption and Emission of Radiation

The rate at which a surface absorbs or emits radiation depends on:

A dull black surface is the best absorber and the best emitter of radiation. A shiny white surface is the poorest absorber (it reflects most radiation) and the poorest emitter.

Applications:

• Car radiator: should be dull black and have a large surface area so it emits heat quickly.
• Roof of a Caribbean home: should be white or light-coloured (to reflect solar radiation) and smooth (to reduce absorption), keeping the interior cool.
• Vacuum flask (thermos): reduces all three modes of heat loss, silvered walls reflect radiation, vacuum prevents conduction and convection, cork stopper reduces conduction through the neck.

The Solar Water Heater and the Greenhouse Effect

A solar water heater uses the greenhouse effect in miniature:

1. The glass cover transmits short-wavelength solar radiation to the absorbing surface.
2. The black absorbing surface heats up and emits longer-wavelength infrared radiation.
3. Glass is opaque to this longer-wavelength radiation, so the energy is trapped inside the collector.
4. Water circulating through copper pipes in the collector absorbs this heat.

The greenhouse effect in Earth's atmosphere works similarly. Gases such as carbon dioxide, methane, and water vapour absorb and re-emit infrared radiation from Earth's surface, warming the atmosphere. This natural greenhouse effect makes Earth habitable. The enhanced greenhouse effect from burning fossil fuels increases CO₂ concentration, absorbing more infrared radiation and contributing to global warming.

FLASHCARD SET • 6 CARDSHeat Transfer: Quick Recall