The thermal conductivity indicates how quickly energy is transmitted through a material by thermal conduction.
Lower thermal conductivity equates to a lower rate of heat loss, which can be achieved using thermal insulators.
The rate of energy transfer depends on the material’s thermal conductivity, temperature difference, and thickness.
Specific heat capacity is the energy needed to raise the temperature of 1 kg of a substance by 1 °C.
The change in thermal energy can be calculated using the formula: E=mc\theta
E is the change in thermal energy (J).
m is the mass (kg).
c is the specific heat capacity (J/kg°C)
\theta is the temperature change (°C).
All objects emit and absorb infrared radiation; hotter objects emit more.
Good absorbers of infrared radiation are also good emitters.
At a constant temperature, infrared radiation emitted equals infrared radiation absorbed.
An object's temperature increases if it absorbs infrared radiation at a higher rate than it emits it.
The Earth's temperature depends on reflection, absorption, and emission of light and infrared radiation.
Greenhouse gases trap infrared radiation, increasing Earth’s temperature.
Human activities increase greenhouse gases, causing climate change.
A black body absorbs 100% of radiation and is a perfect emitter.
Absorb: To take in energy or radiation.
Black Body: A theoretical object that absorbs all radiation.
Electromagnetic Spectrum: The range of all types of electromagnetic radiation.
Emit: To give out energy or radiation.
Greenhouse Gas: A gas that absorbs and re-emits infrared radiation.
Infrared Radiation: A type of electromagnetic radiation.
Specific Heat Capacity: The energy required to raise the temperature of 1 kg of a substance by 1 °C.
Thermal Conductivity: A measure of a material's ability to conduct heat.
Thermal Insulator: A material with low thermal conductivity.