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18. Waves & Sound
Wave Intensity
5:58 minutes
Problem 15.17b
Textbook Question
Textbook Question(II) What is the ratio of
(b) the amplitudes, of an earthquake P wave passing through the Earth and detected at two points 15 km and 55 km from the source?
Verified step by step guidance
1
Identify the type of wave mentioned in the problem. In this case, it's a P wave, which is a type of seismic wave that compresses and expands the material through which it passes.
Understand that the amplitude of seismic waves decreases with distance from the source. This is due to the energy of the wave spreading out and being absorbed by the material it passes through.
Set up the ratio of the amplitudes at the two specified distances. Let A1 be the amplitude at 15 km from the source and A2 be the amplitude at 55 km from the source. The ratio of the amplitudes can be expressed as A1/A2.
Consider any given attenuation model or empirical data that describes how the amplitude of a P wave decreases with distance. This could involve an exponential decay model or other relevant models based on the properties of the Earth's material.
Calculate the ratio using the chosen model or data. This involves substituting the distances into the model's formula and simplifying to find the ratio A1/A2.
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Key Concepts
Here are the essential concepts you must grasp in order to answer the question correctly.
P Waves
P waves, or primary waves, are a type of seismic wave that compress and expand the material they travel through. They are the fastest seismic waves and can move through solids, liquids, and gases. Understanding their behavior is crucial for analyzing how they propagate through different geological layers and how they are detected at various distances from the earthquake source.
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Amplitude of Seismic Waves
The amplitude of a seismic wave refers to the maximum displacement of particles from their rest position as the wave passes. In the context of earthquakes, amplitude is directly related to the energy released by the seismic event. The amplitude detected at different distances can vary due to factors such as attenuation, which describes how the wave's energy diminishes as it travels through the Earth.
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Attenuation of Seismic Waves
Attenuation is the reduction in amplitude and intensity of seismic waves as they propagate through the Earth. This phenomenon occurs due to scattering, absorption, and geometric spreading of the waves. Understanding attenuation is essential for calculating the ratio of amplitudes detected at different distances from the earthquake source, as it influences how the waves are perceived at various locations.
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