B.1.12—Conduction rate
- Syllabus
- First assessment 2025
- Objective
- —
- Level
- SL
Conduction rate
The rate of thermal energy transfer through a uniform slab is
ΔtΔQ=ΔxkAΔT
where k is the material’s thermal conductivity, A is cross-sectional area, ΔT is the temperature difference and Δx is the transfer distance.
Read the proportionalities
The rate increases with larger k, larger area and larger temperature difference. It decreases when the material is thicker, because Δx is in the denominator.
Calculation checks
Use consistent SI units: area in m², distance in m, temperature difference in K or °C, and k in W m⁻¹ K⁻¹. The rate is measured in watts, because 1 W = 1 J s⁻¹.
Worked example from local Question Bank row 127628
Ice has k=2.3Wm−1K−1, thickness 0.019m and temperature difference 6K. Per unit area,
A1ΔtΔQ=ΔxkΔT=0.019(2.3)(6)=7.3×102Wm−2
The result is a heat flux; multiply by area to obtain total power.
Common trap
Use the temperature difference across the slab, not an absolute temperature. A temperature gradient is a change per distance, so do not omit Δx.
The evidence tests a qualitative thickness trend and a graph-selection question for diameter, which changes cross-sectional area.
Explain / Determine
Use $\Delta Q/\Delta t=kA\Delta T/\Delta x$. Explain trends from the equation: increasing cross-sectional area increases rate, while increasing thickness decreases rate. For an ice layer that grows, state that the transfer rate falls because the conduction distance increases.
Reversing the thickness trend or treating diameter as proportional to area rather than area proportional to d².
Representative question
Explain how the rate calculated in (e)(i) changes as the layer of ice grows thicker.
«the thicker the layer the» lower the rate of transfer