Atmospheric Temperature and Air Molecule Density Calculation

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SUMMARY

The discussion focuses on calculating the average number of air molecules per cm³ at an altitude of 50 km, where the average atmospheric temperature is 0°C. The formula used is derived from the barometric formula, specifically P(sub h) = P(sub 0) x e^(-Mgh/RT), with constants defined as M = 28.97 g/mol, g = 9.81 m/s², R = 8.314 J/K•mol, and T = 273.15 K. The final calculation yields approximately 5.16 x 1016 molecules per cm³. Key errors identified include unit inconsistencies and the need for proper conversion factors.

PREREQUISITES
  • Understanding of the Ideal Gas Law and its applications.
  • Familiarity with the barometric formula for atmospheric pressure calculations.
  • Knowledge of unit conversions, particularly between metric and imperial systems.
  • Basic proficiency in logarithmic functions and their applications in scientific calculations.
NEXT STEPS
  • Study the Ideal Gas Law and its implications for atmospheric science.
  • Learn about the derivation and applications of the barometric formula.
  • Explore unit conversion techniques, especially for pressure and volume in gas calculations.
  • Investigate the significance of scale height in atmospheric physics.
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Students in atmospheric science, physics enthusiasts, and professionals involved in meteorology or environmental science will benefit from this discussion, particularly those interested in gas behavior at high altitudes.

Jilly
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Homework Statement


At an altitude of 50 km, the average atmospheric temperature is 0C. what is the average number of air molecules per cm^3 of air at this atmosphere?

Given formula:
P(sub h) =
P(sub 0) x e^(-Mgh/RT) =
-(Mgh x 10^5)/2.303RT
Assuming P = 1 atm at sea level and h in km

M=28.97g/mol=28.97cm^3/mol
g = 9.81 m/s^2 = .0981 km/s^2
h = 50 km
R = 8.314 J/K•mol =
82.06cm^3•atm/K•mol
T = 0 C = 273.15 K

I'm having trouble because using the scale height form of the equation (second form) I get lost in the units, and I'm receiving an error on my TI using the first.

The Attempt at a Solution



Using second equation:[/B]

Log P(sub h) =
(-Mgh x 10^5)/2.303RT =
-(28.97)(.0981)(50)(10^5)/
(2.303)(82.057)(273.15) =
-275.28
10^(-275.28) = 5.23... But the units after the conversion don't add up ... Suggestions?
 
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*5.23x10^-276
 
Jilly said:

Homework Statement


At an altitude of 50 km, the average atmospheric temperature is 0C. what is the average number of air molecules per cm^3 of air at this atmosphere?

Given formula:
P(sub h) =
P(sub 0) x e^(-Mgh/RT) =
-(Mgh x 10^5)/2.303RT
Assuming P = 1 atm at sea level and h in km

M=28.97g/mol=28.97cm^3/mol
g = 9.81 m/s^2 = .0981 km/s^2
h = 50 km
R = 8.314 J/K•mol =
82.06cm^3•atm/K•mol
T = 0 C = 273.15 K

I'm having trouble because using the scale height form of the equation (second form) I get lost in the units, and I'm receiving an error on my TI using the first.

The Attempt at a Solution



Using second equation:[/B]

Log P(sub h) =
(-Mgh x 10^5)/2.303RT =
-(28.97)(.0981)(50)(10^5)/
(2.303)(82.057)(273.15) =
-275.28
10^(-275.28) = 5.23... But the units after the conversion don't add up ... Suggestions?

Whew! What a dog's breakfast of units! Let's see if we can clean this mess up a bit.

R can be expressed in a variety of different units:

http://en.wikipedia.org/wiki/Gas_constant

-Mgh/RT should be dimensionless. Unfortunately, you picked km as your distance unit, which really doesn't fit in with your units for R. Meters would be the better choice.

The molar mass M for air should be expressed in proper units, which is kg/mol. It's not clear how you obtained M = 28.97 cm3/mol.

You use the formula:

P(sub h) =
P(sub 0) x e^(-Mgh/RT) =
-(Mgh x 10^5)/2.303RT

where did the last part -(Mgh x 10^5)/2.303RT) come from? That's not equivalent to raising the number e to the power of (-Mgh/RT).

See what you can do to fix this and we can talk again.
 
SteamKing said:
Whew! What a dog's breakfast of units! Let's see if we can clean this mess up a bit.

R can be expressed in a variety of different units:

http://en.wikipedia.org/wiki/Gas_constant

-Mgh/RT should be dimensionless. Unfortunately, you picked km as your distance unit, which really doesn't fit in with your units for R. Meters would be the better choice.

The molar mass M for air should be expressed in proper units, which is kg/mol. It's not clear how you obtained M = 28.97 cm3/mol.

You use the formula:

P(sub h) =
P(sub 0) x e^(-Mgh/RT) =
-(Mgh x 10^5)/2.303RT

where did the last part -(Mgh x 10^5)/2.303RT) come from? That's not equivalent to raising the number e to the power of (-Mgh/RT).

See what you can do to fix this and we can talk again.

Okay so, this second equation was derived from the first using an 8 km scale height and is true under the conditions of atm pressure units, according to my textbook, that's whereni acquired all of my information, I've attached a photo of the page, maybe you can see what I'm not understanding... Or rather misunderstanding.
image.jpg
 
The site autorotated the photo, here's an adjustment.
 

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The textbook image answers a lot of questions.

log (Ph) = (-Mgh x 105) / 2.303 RT, where log here is the base-10 log, not the natural log. ln (10) ≈ 2.303

The factor 105 converts altitude in kilometers into altitude in centimeters.

The molecular weight of air M = 28.97 grams / mol, as specified in the text.
g = 981 cm / s2, as specified in the text
R = 8.314 * 107 erg / K-mol, as specified in the text.

If we use h = 8 km as the scale height, then the pressure at this altitude is

log (Ph) = (-28.97 * 981 * 8 x 105) / (2.303 * 8.314 * 107 * 288)

log (Ph) = -0.4124

Ph = 10-0.4124

which means Ph = 0.3869, or about 39% of the pressure at sea level, which is as described in the text.

Now, you should be able to work the original HW problem for an altitude of 50 km.
 
SteamKing said:
The textbook image answers a lot of questions.

log (Ph) = (-Mgh x 105) / 2.303 RT, where log here is the base-10 log, not the natural log. ln (10) ≈ 2.303

The factor 105 converts altitude in kilometers into altitude in centimeters.

The molecular weight of air M = 28.97 grams / mol, as specified in the text.
g = 981 cm / s2, as specified in the text
R = 8.314 * 107 erg / K-mol, as specified in the text.

If we use h = 8 km as the scale height, then the pressure at this altitude is

log (Ph) = (-28.97 * 981 * 8 x 105) / (2.303 * 8.314 * 107 * 288)

log (Ph) = -0.4124

Ph = 10-0.4124

which means Ph = 0.3869, or about 39% of the pressure at sea level, which is as described in the text.

Now, you should be able to work the original HW problem for an altitude of 50 km.

Thank you!
 
SteamKing said:
The textbook image answers a lot of questions.

log (Ph) = (-Mgh x 105) / 2.303 RT, where log here is the base-10 log, not the natural log. ln (10) ≈ 2.303

The factor 105 converts altitude in kilometers into altitude in centimeters.

The molecular weight of air M = 28.97 grams / mol, as specified in the text.
g = 981 cm / s2, as specified in the text
R = 8.314 * 107 erg / K-mol, as specified in the text.

If we use h = 8 km as the scale height, then the pressure at this altitude is

log (Ph) = (-28.97 * 981 * 8 x 105) / (2.303 * 8.314 * 107 * 288)

log (Ph) = -0.4124

Ph = 10-0.4124

which means Ph = 0.3869, or about 39% of the pressure at sea level, which is as described in the text.

Now, you should be able to work the original HW problem for an altitude of 50 km.

Log P(sub h) =
(-28.97*981*50*10^5)/
(2.303*[8.314x10^7]*273.15)
LogP(sub h) = -2.72
p(sub h) = 0.00192 atm

n=PV/RT=(.00192atm*1cm^3)/ (273.15K*82.057cm^3atm•K*-1•mol^-1)

n = 8.566 x 10^-8 mol
= 5.16 x 10^16 molecules,

Yes?
 
Your calculation seems to be OK.
 

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