Specific heat capacity (c) is the energy needed to raise the temperature of 1 kg of a substance by 1 °C (or 1 K). The formula Q=mcΔT appears in nearly every thermal physics paper.
Typical exam question: “A 2 kg aluminium block is heated from 20 °C to 50 °C. If c of aluminium is 900 J/(kg·°C), calculate the energy transferred.”
Steps: 1) Identify mass, c, and temperature change. 2) Multiply: Q=2×900×(50−20)=2×900×30=54,000J.
Key concept: Water has a high specific heat capacity, which is why it is used in cooling systems and why coastal climates are milder.
ΔT can be in °C or K because the size of one degree is the same.
Always include units for c – J/(kg·°C).
If a question asks ‘Explain why …’, link the high/low specific heat capacity to the time taken to heat/cool.
MYP frequently asks you to compare these three heat transfer methods (Criteria A: Knowing and understanding).
Conduction: transfer through solids (and to a small extent in fluids) by particle vibrations and free electrons. No overall movement of material.
Convection: transfer in fluids by bulk movement of the fluid itself (density changes).
Radiation: transfer by infrared electromagnetic waves; no medium needed.
Common application questions: vacuum flasks, solar water heaters, insulation in houses. For a vacuum flask, explain how each feature minimises heat transfer (silvered walls reduce radiation, vacuum stops conduction/convection, stopper reduces conduction/convection).
Never say heat ‘rises’ – it is the hot fluid that rises.
Dark, matt surfaces are good absorbers and emitters of radiation; shiny, light surfaces are poor absorbers and poor emitters (good reflectors).
Draw labelled diagrams when asked to explain a convection current – arrows must show the cycle of hot rising and cold sinking.
Q1. Through which process does heat travel from the Sun to the Earth?
Q2. Which material is generally the best thermal conductor?
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