The internsity of a particular earthquake wave

In summary, the intensity of a particular earthquake wave is measured to be 2.2 * 10^6 W/m^2 at a distance of 100km from the source. Using the equation "I2/I1 = r1^2/r2^2", we can find that the intensity at a distance of 4km from the source is 1.76 * 10^10 W/m^2. To find the total power passing through an area of 5.0 m^2 at this distance, we can simply multiply the intensity by the area, giving us a total power of 8.8 * 10^10 W.
  • #1
klmdad
9
0
:confused: The internsity of a particular earthquake wave is measured to be 2.2 * 10^6 W/m^2 at a distance of 100km from the source. Now here is the part that I'm lost. What was the intensity when it passed a point only 4.0km from the source? And what was the total power passing through an area of 5.0m^2 at a distance of 4.0km?
 
Physics news on Phys.org
  • #2
You can make two different assumptions. that the earthquake's power spreads out from a point on the earth. The power density gets lower and lower the farther you go from the source. This is more then likely what the question is asking for.

If you have a class that likes to pull very hard problems out of nowhere if could be that you have assume that source is a certain distance underground. Then the power dissipation would that follow an easy r^2 or r^3 route. Easiest way to do this would be using spherical coordinates. If you have not used spherical coordinates yet I highly doubt this is the question they are asking.

If I were you I would solve it assuming the source of the earthquake was on the surface. All the power in a 100km radius from the source would then also be present at 4 km away from the source but the perimeter of the circle is smaller so the power density will be higher.
 
  • #3
I'm still trying to understand your reply to my Question. If this will helps you to help me it has to do with energy transported by waves. As the wave moves outward, the energy it carries is spread over a larger and larger area since the surface area of asphere of radius r is 4pir^2. Thus the intensity of a wave is I = P/A = P/4pir^2 if we consider two points at distances r1 and r2 from the source then I1 = P/4pir1^2 and I2 = P/4pir2^2, so I2/I1 = r1^2/r2^2
 
  • #4
In your original question it was unclear weather you would be dealing with a 2 dimensional problem or a three dimensional problem.

Your second post indicates it is a three dimensional problem deal with a sphere rather then a circle.

What is still unclear is if 100 km is through the ground or over the surface of the ground. This makes a difference since you do not say the depth of the source.

Is the source considered on the surface of the Earth or some distance inside the earth?

From you second post it seems like you know how to correlate a power density from one radius to another, if this is so what difficulty are you having with the problem:?
 
  • #5
where I am having problems with is what was the total power passing through an area of 5.0 m^2 at a distance of 4.0 km. I don't see how to work the problem.
 
  • #6
You came up with the equation "I2/I1 = r1^2/r2^2", and you know r1 and r2 100km and 4 km and you know I1. So you can solve for I2. Now I2 would be in units of [W/m^2]. You know how many watts per square meter there are, so know all you need to do is figuare out how many watts there are in 5 metters squared.
 

Related to The internsity of a particular earthquake wave

1. What is the intensity scale used to measure earthquake waves?

The intensity scale used to measure earthquake waves is called the Modified Mercalli Intensity Scale. It ranges from I (not felt) to XII (total destruction) and is based on observed effects on people, buildings, and the environment.

2. How is the intensity of an earthquake wave determined?

The intensity of an earthquake wave is determined by analyzing the effects of the earthquake on people, buildings, and the environment. This information is then used to assign a value on the Modified Mercalli Intensity Scale.

3. Can the intensity of an earthquake wave change over time?

Yes, the intensity of an earthquake wave can change over time. This is because different areas experience different effects from the earthquake and these effects can change as the earthquake propagates through the Earth's crust.

4. What factors can affect the intensity of an earthquake wave?

The intensity of an earthquake wave can be affected by several factors, including the magnitude of the earthquake, the distance from the epicenter, the type of soil and rock in the area, and the design and construction of buildings and structures.

5. Why is it important to measure the intensity of an earthquake wave?

Measuring the intensity of an earthquake wave allows us to better understand the effects of earthquakes on people and the environment. This information can be used to improve building codes and emergency preparedness, as well as to assess the potential damage and danger of future earthquakes in a specific area.

Similar threads

  • Earth Sciences
Replies
1
Views
781
Replies
2
Views
791
  • Earth Sciences
Replies
5
Views
985
  • Introductory Physics Homework Help
Replies
11
Views
1K
  • Introductory Physics Homework Help
Replies
1
Views
83
  • Introductory Physics Homework Help
Replies
10
Views
2K
  • Introductory Physics Homework Help
Replies
2
Views
6K
  • Programming and Computer Science
Replies
1
Views
720
  • Introductory Physics Homework Help
Replies
4
Views
1K
  • Introductory Physics Homework Help
Replies
2
Views
773
Back
Top