Calculating Orbital Radius from Albedo and Temperature?

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SUMMARY

The discussion focuses on calculating the orbital radius of a hypothetical planet with the same mass and radius as Mercury, an albedo of 0.1, and a carbon dioxide atmosphere. The escape velocity is derived using the formula v_esc = sqrt(2GM/R), where M is the mass of Mercury (3.30 x 10^23 kg) and R is its radius (2.439 x 10^6 m). The theoretical maximum temperature calculated is 889.87K, and the relationship between albedo and equilibrium temperature is emphasized, indicating that the orbital radius can be determined from the incoming solar radiation absorbed by the planet.

PREREQUISITES
  • Understanding of escape velocity calculations using v_esc = sqrt(2GM/R)
  • Knowledge of root-mean-square molecular velocity and its relation to temperature
  • Familiarity with the concept of albedo and its impact on thermal equilibrium
  • Basic principles of planetary atmospheres and blackbody radiation
NEXT STEPS
  • Research the relationship between albedo and equilibrium temperature in planetary science
  • Learn about the Stefan-Boltzmann law and its application to blackbody radiation
  • Explore methods for calculating orbital radius based on temperature and solar radiation
  • Study the properties of carbon dioxide as a planetary atmosphere and its implications for escape velocity
USEFUL FOR

Astronomy students, astrophysicists, and anyone interested in planetary science, particularly those studying atmospheric dynamics and orbital mechanics.

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Homework Statement



Assume that a planet can have an atmosphere if the escape speed of the planet is 6 times larger than the thermal speed of the molecules in the atmosphere (also known as the root-mean-square molecular velocity). Suppose a hypothetical object having the same mass and radius as Mercury, and an albedo of 0.1, orbits the Sun at just the right location for this condition to be met. Assume that its atmosphere is made of up of carbon dioxide. What is the radius of the this object's orbit around the Sun?

Homework Equations



v_esc = sqrt(2GM/R)
M = M_Merc = 3.30 x 10^23 kg
R = R_Merc = 2.439 x 10^6 m
albedo = 0.1

v_esc = 6 v_rms = 6 sqrt (3kT/M_CO2); M_CO2 = 44(1.67e-27) = 7.348e-26

The Attempt at a Solution



I equated v_esc and 6 v_rms:

sqrt(2GM/R) = 6 sqrt(3kT/M_CO2)

and solved for T, getting me a theoretical maximum temperature of 889.87K.

After this I'm completely stuck. I don't know where albedo kicks in, and I don't know how to get the radius of an orbit around the Sun from the rms velocity or the escape velocity.

Any help would be appreciated. Thanks!
 
Physics news on Phys.org
Once you have the surface temperature you don't need velocities any more. This the astronomy part: if a planet absorbs .1 of the incoming light and acts as a perfect blackbody emitter for infrared, how does its equilibrium temperature depend on the incoming radiation (which then depends on the orbital radius)?
 

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