IB Physics SL B 1 Thermal Energy Transfers Questions

Practise IB Physics SL B.1 by connecting molecular models to temperature, internal energy, phase changes, conduction, convection and radiation.

Syllabus
First assessment 2025
Course
Physics SL
Level
SL

Exam points

  • relate particle spacing, density, temperature and internal energy by comparing molecular motion and energy across solids, liquids and gases
  • determine thermal-energy transfer direction and equilibrium, then explain particle-energy changes during phase change at constant temperature
  • apply Q=mcΔT and Q=mL to heating, cooling and phase-change calculations using power, mass and temperature data
  • distinguish conduction, convection and radiation and interpret how material, density difference, thickness and surface emission affect transfer
  • use black-body spectra, Stefan–Boltzmann, apparent brightness and Wien’s law to compare stellar or cosmic temperatures, powers and distances

Question 1

[Maximum number: 10]

A cylindrical cork of height H and cross-sectional area A is floating stationary in water. Its depth below the water surface is D.

Figure for Question 1 — IB Physics SL

Question (a)

(a)

Explain why the density of most substances in a solid state is larger than its density in a liquid state.

Water shows an anomaly with respect to what is stated in (c)(i).
Graph 1 shows the variation with temperature of the density of water between −100∘C-100^{\circ} \mathrm{C} and 100∘C100^{\circ} \mathrm{C}. Graph 2 shows the same graph enlarged for the range 0 to 10∘C10^{\circ} \mathrm{C}.

[ 2 ]

Question (b)

(b)

On a winter day, the surface of a lake is frozen. The temperature of the air above the lake is −6.0∘C-6.0^{\circ} \mathrm{C}. The layer of ice frozen on the surface of the lake has a thickness of 1.9 cm .

[ 8 ]

Question (i)

(i)

The thermal conductivity of ice is 2.3Wm−1 K−12.3 \mathrm{Wm}^{-1} \mathrm{~K}^{-1}. Calculate the rate per unit area at which thermal energy leaves the lake by conduction through the ice layer.

[ 2 ]

Question (ii)

(ii)

The depth of water below the ice is 22 m and its average initial temperature is 2.0∘C2.0^{\circ} \mathrm{C}. Estimate the minimum thermal energy per unit area that must be removed to freeze all the water in the lake.

The following data are available:

 Specific heat capacity of water =4.2×103Jkg−1 K−1 Latent heat of fusion of water =3.3×105Jkg−1ρwater =1000 kg m−3\begin{aligned} \text { Specific heat capacity of water } & =4.2 \times 10^{3} \mathrm{Jkg}^{-1} \mathrm{~K}^{-1} \\ \text { Latent heat of fusion of water } & =3.3 \times 10^{5} \mathrm{Jkg}^{-1} \\ \rho_{\text {water }} & =1000 \mathrm{~kg} \mathrm{~m}^{-3} \end{aligned}

Layers of ice on lakes do not grow thicker than a small percentage of the lake's depth even when the exterior temperature remains constant below the freezing point for some time.

[ 3 ]

Question (iii)

(iii)

Explain how the rate calculated in (e)(i) changes as the layer of ice grows thicker.

[ 1 ]

Question (iv)

(iv)

Discuss why the anomaly in the value of the density of water supports life in water on Earth.

[ 2 ]

Question 2

[Maximum number: 2]

This question is about a tidal power station.

A tidal power station is built for a coastal town. Sea water is stored in a tidal basin behind a dam at high tide and released in a controlled manner between high tides, so that it passes through turbines to generate electricity.

The following data are available.

Table for Question 2 — IB Physics SL

Show that the mass of sea water released between successive high and low tides is about 2.8×108 kg2.8 \times 10^{8} \mathrm{~kg}.

Question 3

[Maximum number: 1]

Which of the following is equivalent to a temperature of −100∘C-100^{\circ} \mathrm{C} ?

A

-373 K

B

-173 K

C

173 K

D

373 K373 \mathrm{~K}

All question bank results loaded