Thermal Physics Summary
Kelvin scale: Absolute zero at -273°C (0 K); all gas pressure ceases to exist.
Thermal Capacity
Thermal capacity is the energy needed to raise the temperature of a body.
Specific heat capacity: energy required to raise 1 kg by 1°C (E = mcΔT).
Change of State
Matter changes state (e.g., boiling or melting) due to heating/cooling.
Boiling point: liquid becomes vapor; freezing point: liquid becomes solid.
Heat Transfer Methods
Conduction: Energy transfer through particle collisions.
Metals conduct heat better due to free electrons; non-metals transfer heat through vibrations.
Convection: Fluid circulation transfers heat efficiently; cooler fluid sinks while warmer fluid rises.
Real-world examples include heating systems and ocean currents.
Radiation: All objects emit infrared radiation; hotter objects emit more.
Dark, matte surfaces are better emitters/absorbers than shiny, light ones.
Greenhouse Effect
Greenhouse gases trap infrared radiation, warming the Earth and contributing to climate change.