Statistical Mechanics: particle density of an atmosphere

In summary, the problem is to find the particle density in Earth's atmosphere using statistical mechanics, with given parameters of particle mass, temperature, and the planet's mass. The suggested approach is to use the grand canonical ensemble, specifically the Boltzmann distribution. However, it is also possible to solve the problem using the ideal gas equation if the pressure and temperature are known.
  • #1
bjb406
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Homework Statement


I am supposed use stat mech to find the particle density in Earth's atmosphere given only the particle mass, and temperature, and the planet's mass I guess. And I don't really know where to begin. Obviously I need to use the grand canonical ensemble but I don't know where to start without knowing the number of particles in the system.

Homework Equations


Boltzmann distribution I guess? n(r) = A*e^(-(βρ^2)/(2m))*e^(-βmgr)


The Attempt at a Solution


I don't know what to do without knowing N
 
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  • #2
Well if you're given the pressure (1 atmosphere?) and the temperature, you can just go ahead and use the ideal gas equation. No fancy grand canonical stuff required! :smile:
 

Related to Statistical Mechanics: particle density of an atmosphere

1. What is Statistical Mechanics?

Statistical Mechanics is a branch of physics that uses statistical methods to explain the behavior of a large number of particles, such as atoms and molecules, in a system. It is used to understand the macroscopic properties of matter by studying the microscopic behavior of its constituent particles.

2. How is particle density of an atmosphere calculated using Statistical Mechanics?

The particle density of an atmosphere can be calculated using the ideal gas law, which is based on Statistical Mechanics principles. This law states that the product of the pressure and volume of an ideal gas is proportional to the number of particles and the temperature of the gas.

3. What factors affect the particle density of an atmosphere?

The particle density of an atmosphere is affected by several factors, including temperature, pressure, and the types of particles present. For example, increasing the temperature of a gas will cause the particles to move faster and spread out, leading to a lower particle density.

4. How does the particle density of an atmosphere relate to its pressure and temperature?

According to the ideal gas law, the particle density of an atmosphere is directly proportional to its pressure and inversely proportional to its temperature. This means that as pressure increases, particle density also increases, while as temperature increases, particle density decreases.

5. Can Statistical Mechanics also be used to explain the behavior of liquids and solids?

Yes, Statistical Mechanics can also be applied to study the behavior of liquids and solids. In these states, the particles are closer together and have stronger interactions, but the same principles of statistical methods and thermodynamics can be used to understand their properties and behavior.

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