THE UNIVERSITY OF BRITISH COLUMBIA
Physics 108
Assignment #
1:
THERMAL PHYSICS
Wed. 05 Jan. 2005 - finish by Wed. 12 Jan.
- "STAT - EC":
Consider the following simplified model of
a sort of stock market:
A given stock
has a total of shares on the market
for a fixed price .
At a given time, of these shares are
bought and the remaining are unwanted.
Thus the net investment in is
. [Here and
are measured in monetary units, say dollars;
I have used the same notation as for energy
for reasons that will soon become evident.]
To keep things simple, we shall assume that
the price of a given stock
does not change. Further, let's make the
outrageous assumption that the stock market as a whole
is a priori equally likely to be found in
any one of the fully specified states accessible to it
-- i.e. that a given amount of capital is equally likely
to be distributed amongst the various stocks in any of
the possible ways that give the same total.1
- Invent a general definition for an economic analogue of
temperature [measured in monetary units]
that has the desired predictive power:
that (given our starting assumptions)
capital will tend to flow spontaneously from stocks with
higher into others with lower
and will stop flowing between two stocks only when they
are in "economic equilibrium" - i.e. when they have the
same "economic temperature" .
- Now assume that the entire market is in "economic
equilibrium" and is so much larger than any of its parts
that we may treat it as a "capital reservoir"
at an "economic temperature" of = $100.
Consider one share of one stock,
valued at = $200:
What is the probability that it will be bought at any given time?
- Assuming that is also huge compared to
the entire offering of shares of stock
valued at = $200,
what is the expected total investment in
when = $100?
- If the economic temperature drops to = $50,
which stock will be likely to have the most capital invested in it,
with shares
at = $200 per share
or with shares
at = $100 per share?
- MARS-EQUIVALENT ATMOSPHERIC PRESSURE:
The composition of Mars' atmosphere is nominally
95.3% CO, 2.7% N, 1.6% Ar, 0.15% O
and 0.03% HO.
Mean atmospheric pressure at the surface of Mars
is 1-9 millibar, depending on altitude; the average is about 7 mb,
compared to 1000 mb at sea level on Earth.
At what altitude here on Earth would the atmospheric pressure
be the same as that at the surface of Mars?
(Assume an isothermal Earth atmosphere at 300 K.
Are any other assumptions needed?)
- ORTHO- vs. PARA-HYDROGEN:
Molecular hydrogen, H, consisting of two protons bound together
with two electrons, can form in either the "singlet" state
called parahydrogen, in which the total spin
(intrinsic angular momentum) of the molecule is zero,
or in any one of three "triplet" states of orthohydrogen,
in which the proton spins combine to make a total spin
of (the fundamental unit of angular momentum).
For this problem, all you need to know is that the three
triplet states are degenerate - i.e. they all
have the same energy relative to the singlet state,
namely
J.
(The energy of the singlet state
can be taken to be zero, for reference.)
Assume that the spin degrees of freedom of the H
molecules are unaffected by,
but are in thermal equilibrium with,
all their other degrees of freedom
(like translational, rotational or vibrational).
In this case, what fraction of H molecules
will be found (on average) in ortho states
- at room temperature (300 K)?
- at the boiling point of liquid nitrogen
at atmospheric pressure (77 K)?
- at the freezing point of molecular hydrogen
at atmospheric pressure (14 K)?
Jess H. Brewer
2005-01-03