Change in atmopheric pressure with height (Thermodynamics)

In summary, the equation for pressure is pV = nRT where n is the number of mole, rho is the gas constant, and T is the temperature. The equation for force is F = mg, and p is given by pV = nRT.
  • #1
Slepton
21
0

Homework Statement



Think of Earth's atmosphere as an ideal gas of molecular weight [tex]\mu[/tex] in a uniform gravitational field. Let g denote the acceleration due to gravity.

If z denotes the height above the sea level, show that the change of atmospheric pressure p with height is given by

dp/dz = p([tex]\left([/tex]-[tex]\mu[/tex]g/RT)

where,
dp = change in pressure
dz = change in height
[tex]\mu[/tex] = molecular weight
R = Universal gas constant
T = temperature

Homework Equations



1) F = mg
2) P = F/A
3) PV = nRT

The Attempt at a Solution



With the relation between force and pressure, I derived an expression of p in terms of m and g. Using the ideal gas law, i obtained another equation for p. I am lost in my attempt to derive dp/dz. Please help.

Thank in advance,
Priam
 
Last edited:
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  • #2
Gas equation is given by pV = nRT, where is the number of mole.
n is given by [mass of the air column (ma) on unit area]/mu.
Hence pV = [(ma)/(mu)]RT ...(1)
Now p = rho*g*z...(2)
and dp/dz = rho*g...(3)
From equation (1) find the expression for rho and substitute in eq. (3)
 
  • #3
thank rl.bhat!

but the notations are confusing.
n = (ma)/(mu)
so ma is the mass of air column ? Can you explain a bit further please ?
 
  • #4
ma is the mas of the air column on unit area, mu is the molecular weight of air.
So number of mole = n = ma/mu.
 
  • #5
figured i have to derive yet another expression. This time I have to assume an adiabatic expansion and show

dp/p = {[tex]\gamma[/tex]/([tex]\gamma[/tex]-1)}{dT/T}

i.e.

dp/dT = {[tex]\gamma[/tex]/([tex]\gamma[/tex]-1)} {p/T}


My idea:

since it is an adiabatic expansion, i have
pz([tex]\gamma[/tex]-1) / T(Z)[tex]\gamma[/tex] = constant

I used it and tried to cook the needed expression, but i got lost.
 
  • #6
For adiabatic expression pV^gamma = K
You replace V by nR(T/p)
So p(nRT/p)^gamma = k or
p(T/p)^gamma = K'
i.e. T^gamma*p^(1-gamma) = K.
Take the differentiation and simplify.
 
  • #7
How would you derive the hydrostatic equation in spherical polars?

Thanks
 

Related to Change in atmopheric pressure with height (Thermodynamics)

1. How does atmospheric pressure change with height?

As you increase in altitude, the atmospheric pressure decreases. This is because the weight of the air above you decreases with increasing height, leading to a decrease in the number of air molecules pushing down on a given area.

2. Why does atmospheric pressure decrease with height?

This is due to the effect of gravity on the Earth's atmosphere. The closer you are to the Earth's surface, the stronger the gravitational pull, resulting in a greater number of air molecules and a higher atmospheric pressure. As you move away from the surface, the gravitational pull weakens and the atmospheric pressure decreases.

3. How is atmospheric pressure measured?

Atmospheric pressure is typically measured using a barometer, which measures the weight of the air above a given area. The most commonly used unit for atmospheric pressure is the kilopascal (kPa), although other units such as millibars (mb) and inches of mercury (inHg) are also used.

4. How does temperature affect atmospheric pressure?

In general, as temperature increases, atmospheric pressure decreases. This is because warmer air is less dense than cooler air, and therefore exerts less pressure on the Earth's surface. This relationship between temperature and pressure is described by the ideal gas law.

5. What is the relationship between atmospheric pressure and weather?

Changes in atmospheric pressure can indicate changes in weather patterns. High atmospheric pressure typically indicates fair weather, while low atmospheric pressure is associated with stormy weather. However, other factors such as wind patterns and temperature also play a role in determining weather conditions.

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