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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

Give another example of a transverse wave.

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Answer

One example of a transverse wave is a light wave. Other examples include radio waves, microwaves, or X-rays.

Step 2

Calculate the wavelength of the wave.

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Answer

The wavelength can be calculated using the formula:

Wavelength=Distance between L and MNumber of wavelengths\text{Wavelength} = \frac{\text{Distance between L and M}}{\text{Number of wavelengths}}

Given that the distance is 32 m, and assuming there is one wavelength per distance:

Wavelength = 32 m / 10 = 3.2 m

Step 3

Calculate the frequency of the wave.

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To find frequency, use the formula:

Frequency=Number of peaksTime\text{Frequency} = \frac{\text{Number of peaks}}{\text{Time}}

Substituting the values:

Frequency = 12 / 15 = 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

Arrows should be drawn to indicate that the rock at R moves in the direction of the seismic wave, which is a longitudinal wave. This means the arrows will show back-and-forth motion along the path of the wave.

Step 5

Calculate the wavelength of the seismic wave, in metres.

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Answer

Using the formula:

Wavelength=Wave SpeedFrequency\text{Wavelength} = \frac{\text{Wave Speed}}{\text{Frequency}}

Substituting the values:

Wave Speed = 7 km/s = 7000 m/s,

Frequency = 12 Hz,

Wavelength = 7000 m/s / 12 Hz = 583.33 m (or approximately 580 m if rounding).

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

This method is not suitable because seismic waves cannot be easily counted like water waves. Seismic waves arrive as a series of peaks that may be difficult to distinguish, and relying on counting during a short time frame may not provide an accurate measurement. Additionally, because seismic waves travel through solid materials, their detection may require specialized equipment beyond simple counting.

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