Statistical Physics Problems: Gaussian Distribution and Harmonic Oscillator, Assignments of Physics

Three physics problems aimed at helping readers understand statistical physics concepts, with a focus on gaussian distribution and harmonic oscillator. The problems involve calculating normalization constants, average values, and root-mean-square spreads for gaussian distributions, as well as finding probabilities and average energies for harmonic oscillators in thermal equilibrium. These problems are essential for students studying statistical physics, particularly those related to probability density functions and energy distributions.

Typology: Assignments

Pre 2010

Uploaded on 09/17/2009

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These problems will serve the purpose of letting you carry out some statistical
physics calculations for yourself. Hopefully you will realize how powerful
these methods can be once you get over your natural fear of all those
integrals!
Problem 1.
One very commonly encountered probability density is the Gaussian or
normal distribution given by
w(x)=C e
!x2
2
"
2
.
Suppose we are measuring the x-position of a particle and the results scatter
around according to a Gaussian distribution, with any value of x between
negative infinity and positive infinity being possible, but those near where the
distribution is maximum (i.e near zero) being the most likely. Remember
what
w(x)
actually means. The probability of finding the particle to lie
between position x and position
x+dx
is just given by
P(x,x+dx)=w(x)dx
.
(a.) To become familiar with this function, calculate the value of the
normalization constant
C
. If you look up the integral you will find that
e!a2x2
dx =
"
a
!#
#
$
.
(b.) Show that the average value of
x
is 0, i.e
, as you would expect.
(c.) Show that
x2=
!
2
. The fact that
x2
!"
"
#e
!x2
2
$
2dx =
%
2a3
should be
useful. You can get this from the first integral by taking the derivative of
both sides with respect to a, which brings down a factor of
x2
, inside the
integral, which is a nifty trick!
(d.) Show that the root-mean-square spread in the measured values of x will
just equal
!
. Root-mean-square spread means the square root of the average
of the quantity
(x!x)2
, so in this case you already know the answer!
Problem 2.
Probably the most fundamental and useful result from all of statistical physics
is that the probability of finding a system in a particular state (called it state #
pf3

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These problems will serve the purpose of letting you carry out some statistical

physics calculations for yourself. Hopefully you will realize how powerful

these methods can be once you get over your natural fear of all those

integrals!

Problem 1.

One very commonly encountered probability density is the Gaussian or

normal distribution given by

w ( x ) = C e

!

x

2

2 "

2

.

Suppose we are measuring the x-position of a particle and the results scatter

around according to a Gaussian distribution, with any value of x between

negative infinity and positive infinity being possible, but those near where the

distribution is maximum (i.e near zero) being the most likely. Remember

what w ( x ) actually means. The probability of finding the particle to lie

between position x and position x + dx is just given by P ( x , x + dx ) = w ( x ) dx.

(a.) To become familiar with this function, calculate the value of the

normalization constant C^. If you look up the integral you will find that

e

! a

2 x

2

dx =

"

a

!#

(b.) Show that the average value of x is 0, i.e x = 0 , as you would expect.

(c.) Show that x

2 =!

2

. The fact that x

2

!"

"

e

!

x

2

2 $

2

dx =

2 a

3

should be

useful. You can get this from the first integral by taking the derivative of

both sides with respect to a , which brings down a factor of x

2 , inside the

integral, which is a nifty trick!

(d.) Show that the root-mean-square spread in the measured values of x will

just equal!. Root-mean-square spread means the square root of the average

of the quantity ( x! x )

2 , so in this case you already know the answer!

Problem 2.

Probably the most fundamental and useful result from all of statistical physics

is that the probability of finding a system in a particular state (called it state #

i ) is proportional to e

!

Ei

kBT , where E i

is the energy of the system when it is in

state i. This theorem applies to any system that is in thermal equilibrium at

temperature T.

Of course, to find the actual probability we must impose the requirement that

the sum of the probabilities for all possible states must be exactly 1.000,

because the system must be in one of its states.

For quantum systems the idea of a state is naturally well-defined. For

example, a one-dimensional harmonic oscillator has states that are defined by

a single integer, n. When the oscillator is in state # n , it has energy

E

n

= ( n + 1 / 2 )!! , where! is the natural angular frequency of the oscillator,

and! is Planck’s constant divided by 2! , which is an exceedingly small

number (1.05! 10

" 34 Joule seconds). The fact that! is so small explains

why we never notice that we can’t give a harmonic oscillator whatever energy

we like, but that actually we can only change its energy by one unit at a time.

The lowest possible energy an oscillator can have is not zero as you might

have expected but is instead equal to half the energy difference between

levels.

(a.) Using the fact that the oscillator must be in one of its states, i.e. the sum

of all the probabilities must be exactly 1.000, show that the probability of

finding an oscillator (that is in thermal equilibrium at temperature T ) to be in

state # n is given by P ( n ) = 1! e

!

! w

kBT

e

!

n! (

kBT

. (Hint: You are trying to sum a

geometric series of the form 1 + x + x

2

  • ...., where x < 1 .)

(b.) Using the result of part (a.) find the average energy the oscillator has at

temperature T. (You should get

!! e

"

!!

kBT

1 " e

"

!!

kBT

, if you are sufficiently

careful!) You will find it useful to know that n e

! nx

n = 0

n ="

e

! x

1! e

! x $ %

2

. If you

are mathematically inclined, you can prove this by taking the derivative of