Calculate the volume charge density of the atmosphere

In summary, the conversation discusses using Gauss's Law to calculate the volume charge density of the atmosphere between altitudes of 250 m and 400 m. The suggested Gaussian surface is a sphere with a radius of the Earth plus 250 m. The electric flux through this surface can be calculated using the electric fields measured at altitudes of 250 m and 400 m. The resulting equation can then be solved for the volume charge density of the atmosphere.
  • #1
sonutulsiani
138
0

Homework Statement



In the atmosphere and at an altitude of 250 m, you measure the electric field to be 150 N/C directed downward, and you measure the electric field to be 170N/C directed downward at an altitude of 400 m. Calculate the volume charge density of the atmosphere in the region between altitudes of 250 m and 400m, assuming it to be uniform.

Homework Equations





The Attempt at a Solution



I just want to know. When I substitute the values in E = (sigma/epsilon 0) and then sigma = Q/Area.. So I get Q = 150 (epsilon 0) A. Now this I will substitute in the formula rho = Q / V.

Now my question is what will be Area? What value of r should I write in 4 pi r^2 ?
Will it be radius of Earth or the altitude of 250 m? If it's radius of earth, where will I write 250m then?
 
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  • #2
This is a Gauss's Law application. If you can picture the Gaussian surface that you should use, you will know what to do with r and what its value(s) ought to be. So what kind of Gaussian surface should you use to "calculate the volume charge density of the atmosphere in the region between altitudes of 250 m and 400m, assuming it to be uniform"?
 
  • #3
Hmm may be cylinder? But how in the world do I get the idea of gaussian surface?!
 
  • #4
sonutulsiani said:
Hmm may be cylinder? But how in the world do I get the idea of gaussian surface?!

Choose a Gaussian surface that reflects the symmetry of the problem. The Earth is more closely approximated to a sphere than a cylinder. Also, the expression E = σ/ε0 applies only in cases where there is a surface charge. There is no surface charge in the atmosphere at heights of 250 m or 400 m or any height. There is only volume charge density in the atmosphere.
 
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  • #5
So what it should be E = rho / epsilon 0?
And I got what you are saying. I got the charge in the sphere, Q inside as = 4 E pi epsilon 0 r^(2)

Is that right? If that is right, then r=radius of the Earth only
 
  • #6
Ok I tried it once again.

This time I took rho = Q / V

And then substituted Q inside = 4 E pi epsilon 0 r^(2)
with rho V = 4 E pi epsilon 0 r^(2)

=> rho 4/3 pi r^3 = 4 E pi epsilon 0 r^(2)

Is it correct?? In that way I can find rho, but then I am still confused about the 'r' s
 
  • #7
Wait the r will be radius of Earth plus 250m ?
 
  • #8
You know that the E field at RE+400 m is 170 N/C and that the E field at RE+250 m is 150 N/C. Both fields are radially in.

Can you calculate the electric flux through the area of a sphere of radius RE+400 m and then through a sphere of radius RE+250 m?

The sum of the two would be the total flux through a shell of inner radius RE+250 m and outer radius RE+400 m. What should this total flux be equal to according to Gauss's law?
 

FAQ: Calculate the volume charge density of the atmosphere

What is volume charge density?

Volume charge density is a measure of the amount of electric charge per unit volume in a given region of space.

Why is it important to calculate the volume charge density of the atmosphere?

Calculating the volume charge density of the atmosphere helps us understand the distribution of electric charge in the atmosphere, which is important for studying atmospheric phenomena such as lightning and electric fields.

How is the volume charge density of the atmosphere measured?

The volume charge density of the atmosphere can be measured using instruments such as lightning mapping arrays, which use radio waves to detect the electric fields generated by lightning strikes.

What factors can affect the volume charge density of the atmosphere?

The volume charge density of the atmosphere can be affected by various factors such as temperature, humidity, and atmospheric pressure, which can influence the distribution and movement of charged particles in the atmosphere.

Is the volume charge density of the atmosphere constant?

No, the volume charge density of the atmosphere can vary depending on the location, time of day, and weather conditions. It can also be affected by human activities such as air pollution and industrial emissions.

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