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IB Physics SL B.1 Thermal Energy Transfers Question Bank

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

  • Explain solids, liquids and gases with molecular models and relate Kelvin temperature to average kinetic energy.
  • Use Q=mcΔT and Q=mL to analyse heating, cooling and phase changes.
  • Compare conduction, convection and radiation, then apply black-body, luminosity and Wien relationships.

B.1 Thermal energy transfers 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 B.1 Thermal energy transfers 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 100C-100^{\circ} \mathrm{C} and 100C100^{\circ} \mathrm{C}. Graph 2 shows the same graph enlarged for the range 0 to 10C10^{\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 6.0C-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 2.3Wm1 K12.3 \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 2.0C2.0^{\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 =4.2×103Jkg1 K1 Latent heat of fusion of water =3.3×105Jkg1ρwater =1000 kg m3\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 ]

B.1 Thermal energy transfers 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 B.1 Thermal energy transfers 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}.

B.1 Thermal energy transfers question 3

[Maximum number: 1]

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

A

-373 K

B

-173 K

C

173 K

D

373 K373 \mathrm{~K}

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