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Figure 11 shows a large tank of water - Edexcel - GCSE Physics - Question 6 - 2020 - Paper 1

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Figure 11 shows a large tank of water. (i) Water waves are transverse waves. Give another example of a transverse wave. (ii) Figure 12 shows a side view of part of... show full transcript

Worked Solution & Example Answer:Figure 11 shows a large tank of water - Edexcel - GCSE Physics - Question 6 - 2020 - Paper 1

Step 1

Water waves are transverse waves. Give another example of a transverse wave.

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Answer

One example of a transverse wave is an electromagnetic wave, such as light.

Step 2

Calculate the wavelength of the wave.

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Answer

The wavelength can be calculated using the formula:

Wavelength=Distance from L to MNumber of wavelengths\text{Wavelength} = \frac{\text{Distance from L to M}}{\text{Number of wavelengths}}

Given that the distance is 32 m:

Wavelength=32m10=3.2m\text{Wavelength} = \frac{32 m}{10} = 3.2 m

Step 3

Calculate the frequency of the wave.

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Answer

Frequency is calculated using the formula:

Frequency=Number of wavesTime\text{Frequency} = \frac{\text{Number of waves}}{\text{Time}}

Substituting the values:

Frequency=1215s=0.8(Hz)\text{Frequency} = \frac{12}{15 s} = 0.8 (Hz)

Step 4

Draw arrows on Figure 13 to show how the rock at R moves when the seismic wave passes through R.

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Answer

The arrows should show movement in the direction of the wave propagation, with one arrow moving to the right and one to the left, indicating that the rock at R oscillates back and forth.

Step 5

Calculate the wavelength of the seismic wave in metres.

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Answer

Using the equation:

Wavelength=Wave speedFrequency\text{Wavelength} = \frac{\text{Wave speed}}{\text{Frequency}}

Substituting in the values:

Wavelength=7000m/s12Hz=583.33m\text{Wavelength} = \frac{7000 m/s}{12 Hz} = 583.33 m

Rounding to a valid format, the wavelength is approximately 580 m.

Step 6

Explain why this would not be a suitable method for measuring the frequency of the seismic wave in part (b)(ii).

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Answer

Counting waves directly is not suitable for seismic waves because:

  1. Seismic waves are often not visible on the surface upon arrival, making counting difficult.
  2. A technician would require an accurate method, as they cannot rely on fast counting due to the rapid arrival of waves.
  3. The frequency of seismic waves might be too high to accurately count within the observed time frame.

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