How Is Charge Density Calculated Between Two Altitudes?

In summary, to calculate the average volume charge density in the layer of air between 500 and 600 m, Gauss' theorem can be used on the thin slab of air between these two altitudes. By assuming the slab to be flat, the electric field can be solved for by using the formula E = kQ / r^2. The resulting charge density can then be divided by the thickness of the slab (100 m) to get the average volume charge density in C/m^3. By integrating the normal component of the electric field over the surface of the volume, the charge contained can also be determined.
  • #1
brunie
62
0
In the air over a particular region, at an altitude of 500 m above the ground, the electric field is 150 N/C directed downward. At 600 m above the ground, the electric field is 100 N/C downward. What is the average volume charge density in the layer of air between these two elevations?

charge denisty should be in C / m^3
so given field strength at different altitudes
use
E = kQ / r^2 to solve for Q for each altitude
then
charge density = Q / (4/3π r^3)

radius of Earth is 6378100 m
so respecitive heights are 6378600m and 6378700m

then average these or subtract or sumthing

is this process somewhat correct?
 
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  • #2
Use Gauss' theorem on the slab of air between 500 and 600 m. The slab is thin enough that you really don't need to worry about the curvature of the earth. Just pretend it's a flat slab.
 
  • #3
Dick said:
Use Gauss' theorem on the slab of air between 500 and 600 m. The slab is thin enough that you really don't need to worry about the curvature of the earth. Just pretend it's a flat slab.

i don't understnd why we can assume it is flat because the question indicates volume, not area

but treating it as a flat slab, then

E = ∂ / 2Eo
where solving for ∂ will give units C/m^2
then it would seem to be logical to divide by 100m (the difference) to acquire C/m^3

but if this is correct to say, which value is used for E?
 
  • #4
....
 
  • #5
Sorry. Guess I dozed off. By slab I mean some area by 100 m thick. If you integrate the normal component of the E field over the surface of that volume how is that related to the charge contained?
 
  • #6
sry, I am not too sure what u mean by integrating over the surface
 
  • #7
Did you do Gauss' theorem?
 

FAQ: How Is Charge Density Calculated Between Two Altitudes?

What is charge density at altitude?

Charge density at altitude is a measure of the electric charge present in a unit volume of air at a particular height above sea level. It is typically expressed in units of coulombs per cubic meter (C/m3).

How does charge density change with altitude?

The charge density at altitude generally decreases with increasing height. This is due to the decrease in air density, which means there are fewer air molecules to carry electric charges. Additionally, as altitude increases, the Earth's magnetic field becomes weaker, reducing the amount of charged particles that can be trapped in the atmosphere.

What factors affect charge density at altitude?

Several factors can affect charge density at altitude, including solar activity, thunderstorms, and geomagnetic disturbances. Solar activity, such as solar flares, can increase the amount of charged particles in the upper atmosphere, leading to higher charge density. Thunderstorms can also significantly increase charge density due to the separation of charges within the clouds. Geomagnetic disturbances, such as solar storms, can also influence charge density by altering the Earth's magnetic field.

Why is charge density at altitude important to study?

Charge density at altitude is crucial to understanding the dynamics of Earth's upper atmosphere. It can also impact a variety of technologies, such as satellite communications and GPS systems. Additionally, studying charge density can help us better understand and predict space weather events, which can have significant impacts on our daily lives.

How is charge density at altitude measured?

There are several methods used to measure charge density at altitude, including satellite instruments, ground-based instruments, and balloon experiments. These instruments typically measure the number and energy of charged particles in the atmosphere to calculate charge density. However, measuring charge density accurately can be challenging due to the constantly changing and complex nature of the upper atmosphere.

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