Difference between revisions of "Maxwellian velocity distribution"

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* [http://hyperphysics.phy-astr.gsu.edu/hbase/kinetic/kintem.html Hyperphysics (Georgia State)]
 
* [http://hyperphysics.phy-astr.gsu.edu/hbase/kinetic/kintem.html Hyperphysics (Georgia State)]
  
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* [[Local Thermodynamic Equilibrium]]
 
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Latest revision as of 15:57, 5 December 2017

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Thermal Velocities

Typical Speed: Back of the Envelope

We can estimate the typical speed of a particle of mass in thermal equilibrium with its surroundings. In thermal equilibrium, a particle is excited thermally. We can write its kinetic energy as:

Thus, a typical particle has speeds of

Velocity Distribution

Now we will derive , the distribution of velocities of a particle in thermal equilibrium. Since we are in thermal equilibrium, we can use Maxwell-Boltzmann statistics. Recall that for Maxwell-Boltzmann statistics, the probability of an energy state at temperature is given by:

The denominator is the normalization factor which is calculated by summing over all possible energy states. Now, consider a velocity . to calculate the probability of a particle of having that particular velocity.

To get , the normalizing factor, we need to sum over all possible velocities.

Because velocities are continuous, the sum then becomes an integral. And since velocity is in three dimensions, we need to integrate over .

We note that we can break this up into three Gaussian integrals:

We will define and integrate a Gaussian.

Plugging it all in, the velocity distribution is simply a Gaussian centered around zero with a typical fluctuation in the velocity of :

where . Note that has units of since to obtain a probability you need to integrate over all three velocity directions.

Maxwellian Speed Distributions

The Maxwellian Speed Distribution is a bit more interesting than the velocity distribution (and used more often). What we want to find is which is different than . This is because there are more ways to combine , , to make larger ’s so there are more available states at higher speeds. For a given speed , any combination of velocity components that satisfy will work. This is analogous to the surface area of a sphere and likewise we find that there are states at any given v. Thus, we can modify the Maxwell velocity distribution with the number of states at a given speed:

This is the Maxwell speed distribution and note that it has units of .

Typical Speeds Revisited

There are actually three ways to quantify typical speeds of a distribution of particles in thermal equilibrium and our back of the envelope calculation only gives us one of them. The first typical speed is the easiest to calculate: the most probable speed. The most probable speed occurs when is maximum. To calculate this we set the derivative to zero:

As the tilde suggests, is what we got earlier while solving for the Maxwell velocity distribution. is both the most probable speed and the typical spread in velocities. The next speed we will find is the mean speed, . To find this, we find the expectation value of :

Using the result that:

we get:

It turns out this is slightly greater than the most probably speed (). The last speed we will find is the root mean square velocity (). We define . To find :

Using the result that:

we get:

Thus, we find that:

We see that the rms speed is the speed we derive from the back of the envelope calculations. We also see that this typical speed is greater than both of the other two speeds. Here is a plot showing the Maxwell speed distribution and the three typical velocities. We can see from this plot that the Maxwell speed distribution is skewed to the right.

Plot of the Maxwell Speed Distribution and typical speeds

Applications to Planetary Atmospheres

One application of the Maxwell-Boltzmann distribution is to describe the loss of planetary atmospheres. Particles at the top of an atmosphere are moving randomly in all directions with speeds corresponding to the Maxwell-Boltzmann distribution. If the particles moving upwards have a velocity lower than the planet’s escape velocity, then the particles will curve back downwards in an elliptical pattern, and the planet will retain its atmosphere. However, if the particles moving upwards are at a higher velocity than the planet’s escape velocity, then the particles will move upwards in a hyperbolic pattern and will be ejected into space. The escape velocity is given by

where G is the gravitational constant, M is the mass of the body to escape from, and r is the distance from the particle to the center of mass of the body that it is escaping from.

Typically, only a small number of particles from the high-velocity tail of the Maxwell-Boltzmann distribution will be able to escape. However, the trajectories and speeds of the remaining atmospheric particles are continuously shuffled, leading to the gradual ejection of particles and a slow atmospheric loss. As a result of this effect, very small planets (which therefore also have very small escape velocities) are unable to retain atmospheres.