1PH0 · CP5.9Core practical investigationsCore

CP5.9: Refraction in a Rectangular Glass Block

Use an approved ray source to produce a narrow visible ray. Outline the reflecting surface or transparent block on paper, mark several points along each visible ray and keep the apparatus in the same position. After removing the apparatus, join marked points with a ruler. A single broad mark gives poor direction evidence; two separated points define a path more clearly.

35 min Video by Science School Core practical investigations
Edexcel Core Practical 9-1 GCSE P5.9 Refraction in a rectangular glass blockCurated by Kepler, not produced by us. Watch it before the notes below.
Open on YouTube

Before you start

  • Use your teacher’s tier checklist: this overview can include Higher-only material, and is not a tier-specific revision list.
  • Pearson Edexcel separate GCSE Physics 1PH0. Use the original core-practical reference and retain every specified subpart; two guides can develop different parts of one core reference.
  • Draw a perpendicular normal and measure an angle with a protractor.
  • Use the centre’s approved supervised method and equipment limits. These notes prepare you to explain and evaluate practical work; they do not replace carrying it out and recording the evidence.

Watch, pause, try

Video by Science School. This demonstration develops Pearson CP5.9 rectangular glass-block refraction. Reflection and water-wave examples in the written guide are supporting comparisons rather than additional named CP5.9 procedures.

Viewing focus: Trace incident, reflected and refracted rays

After watching, attempt these questions before opening the answers. You can also use the written lesson below.

After watching 1: If a ray makes 30° with the surface, what is its incident angle and why?

Show answer and reasoning

The incident angle is 60°, measured from the normal perpendicular to the surface.

After watching 2: Explain why a rough surface can scatter reflected rays while each ray still obeys the reflection law.

Show answer and reasoning

The small surface regions have differently directed normals. Equal local incident/reflected angles therefore produce different outgoing directions.

What you'll be able to do

  • Trace incident, reflected and refracted rays
  • Measure angles from the local normal
  • Distinguish regular/diffuse reflection and material-dependent refraction
1

Trace paths that can be reconstructed accurately

Use an approved ray source to produce a narrow visible ray. Outline the reflecting surface or transparent block on paper, mark several points along each visible ray and keep the apparatus in the same position. After removing the apparatus, join marked points with a ruler. A single broad mark gives poor direction evidence; two separated points define a path more clearly.

At each boundary point, draw a normal perpendicular to the surface. The angle of incidence and the reflected or refracted angle are measured from that normal, not from the surface. Use different incident angles and retain the raw measurements. Avoid looking into the source or using an unapproved laser arrangement.

Pearson CP5.9 requires a light source with a grating to produce the beam and a rectangular glass block. Relate bending toward or away from the normal to entering or leaving the medium. Keep that required setup distinct from an optional prism or reflection comparison.

An incident light ray in air meets a horizontal glass surface obliquely. A dashed normal is perpendicular to the surface. Inside the glass the ray is closer to the normal. Both angles are measured from the normal.
Scroll the diagram to see the full view.
Original ray-direction schematic for oblique air-to-glass entry. Angles are measured from the local normal. The diagram is qualitative, not a measured refractive-index result.
2

Compare reflecting surfaces and materials

For a plane reflecting surface, the reflected and incident rays make equal angles with the local normal. A rough surface produces diffuse reflection because its small surface regions have different normals; the local law is not abolished. Compare a smooth surface with an appropriate rougher surface under similar illumination, distinguishing a spread of reflected directions from an absence of reflection.

For oblique incidence from air into common transparent glass or plastic, light slows and the ray bends toward the normal. On emerging into air it bends away from the local normal. A parallel-sided block in the same outside medium gives an emerging ray parallel to the incident ray but laterally displaced in the ideal geometry. At normal incidence there is no directional bending even though speed changes.

3

Identify the inference supported by the measurements

Compare repeated angle readings and the quality of the ray marks. A block moved after its outline was drawn gives a systematic path error. A thick ray, uncertain normal or protractor resolution affects angular precision. Improve a named limitation, such as using longer marked ray segments or securing the block, rather than saying only “use more accurate equipment”.

Comparing substances requires controlled geometry and the same incident-angle convention. Do not compare one refracted angle at 20° incidence with another at 60° and attribute the difference only to material. Wave reflection/refraction can also be observed at suitable water-depth boundaries; the medium conditions change wave speed and wavelength while the source frequency stays the same. The centre selects additional wave/matter contexts where required.

4

Worked applications

Attempt these problems on paper before opening the worked reasoning. Explain your steps as well as giving a final answer.

Example 1An incident ray is 35° from a plane mirror surface. Find its angle of incidence and angle of reflection.
1The normal is 90° from the surface.
2Incidence = 90 − 35 = 55°.
3The reflected angle is equal when measured from the normal.
Answer
55° incidence and 55° reflection.
Example 2A ray enters a parallel-sided glass block from air at 40° to the normal and travels inside at 25°. Describe the entry bend and ideal emerging direction.
1The internal angle is smaller, so the entry bend is toward the normal.
2At the second parallel face, the ray goes from glass to air and bends away from its normal.
3With the same external medium and parallel faces, it emerges parallel to the original ray.
Answer
Toward the normal on entry; emerging parallel but laterally displaced.
Example 3A water wave crosses into shallower water, where its speed falls from 0.40 to 0.30 m s⁻¹. The source remains at 10 Hz. Compare wavelengths.
1Initial λ = 0.40/10 = 0.040 m.
2Final λ = 0.30/10 = 0.030 m.
3The frequency remains fixed by the unchanged source.
Answer
Wavelength falls from 4.0 to 3.0 cm; frequency stays 10 Hz.

Common mistakes to avoid

Measuring ray angles from the block face.
Draw and use the normal.
Calling an emerging ray undisplaced because it is parallel.
Parallel direction and lateral position are different features.

Key takeaways

  • You can trace incident, reflected and refracted rays.
  • You can measure angles from the local normal.
  • You can distinguish regular/diffuse reflection and material-dependent refraction.

Apply it in an exam

Question 1: A water wave crosses into shallower water, where its speed falls from 0.40 to 0.30 m s⁻¹. The source remains at 10 Hz. Compare wavelengths.

Show answer and reasoning

Wavelength falls from 4.0 to 3.0 cm; frequency stays 10 Hz.

  • Initial λ = 0.40/10 = 0.040 m.
  • Final λ = 0.30/10 = 0.030 m.
  • The frequency remains fixed by the unchanged source.

Explore further

Return to this tomorrow

Close the notes and answer from memory. Revisit any explanation you cannot yet reconstruct.

  • Does diffuse reflection mean the local reflection law fails?
  • At normal incidence into glass, which statement is correct?

Test yourself

Answer a few questions, then review anything you missed.

Next step

Keep practising

Start with the quiz above to check the key ideas. You can also choose another topic from the practice library.

Browse practice topics

Related lessons

All 10 lessons