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```THE HEISENBERG UNCERTAINTY PRINCIPLE
[Reading: Shankar Chpt. 9 and/or Griffiths 3.5]
Overview: Consider a quantum system in state
(with eigenvalues
and eigenvectors
A measurement of
yields
with probability
, and two observables A, B
).
. (Likewise for B.)
The uncertainty
measures the overall spread in possible outcomes of the
measurement (i.e., it measures the width of the probability distribution). It is
defined as
So a system in a general quantum state
lacks a well-defined -value. The
exception is if
happens to be an eigenstate
, in which case its
-value
is unambiguous and hence the uncertainty
associated with the measurement
is zero. In this case we can say that the system is “in” the state with the definite
observable value
.
Question: When is it possible to say that a quantum system is in a state with
definite observable values
and ? (i.e., zero uncertainty in either
measurement value)
Answer: Only if the two observables
commute!
The reason: Recall that if two operators commute, then they share a common
set of eigenvectors. So if a system starts, say, in an eigenstate of
, (so that
it’s -value is known with zero uncertainty), then it is also automatically in an
eigenstate of , and hence its
-value is also known precisely (with no
uncertainty).
Consider instead the case where the two observables don’t commute (and
hence have different eigenvectors). Suppose the system is in a state with a
definite -value (i.e., it’s in an eigenstate of
.) Can it also have a definite
-value at the same time? No! For this to happen the system would have to be
in a pure eigenstate of . But it’s not! It’s in eigenstate
, which we can
think of as being made up from some linear combination of the
eigenstates.
Thus, if
were measured, a range of possible -values could result (and
thus,
).
Said differently, if the initial state of a system is
(so that its -value is definite),
then a subsequent measurement of B can yield a range of possible values. Once
this measurement of
is actually made, the system will be thrown into some
eigenstate
. Hence, the measurement of
has actually altered the state of the
system from
to
. Hence, a subsequent re-measurement of
can yield a
range of possible
-values. Observables
and
are said to be
incompatible; a measurement of one “interferes with” measurement of the other.
The inability to attribute definite values of two non-commuting observables to a
given state of a system is not the result of a “flaw” or inadequate technological
advancement in our measuring devices. Even if we had better, more accurate
equipment, we couldn’t get around this issue – it’s deeper than that. In short, if
two observables
don’t commute, then there is no such thing as a state
with a well-defined
value and -value!
The uncertainty principle captures this idea! Loosely speaking, it says the
uncertainties in measurements of non-commuting observables can never both
be zero!
(In fact, there is a lower bound on the product of the uncertainties.)
Now let’s be more precise about all this ….
APPLICATIONS:
Apart from its deep philosophical import, the Heisenberg uncertainty
principle also provides a useful tool for making crude, heuristic estimations
of things, such as the ground-state energies of various quantum systems.
Example 1: Estimating ground-state energy of a SHO
Example 2: Estimating ground-state energy of a hydrogen atom
Example 3: Estimating ground-state energy of a particle in a box of size L
Some other uncertainty relations:
1) In 3-D,
(Note: there is no uncertainty relation between, say, observables x
and py, nor between, say, x and z, since these pairs commute.)
2) Angular momentum: (We’ll study this later)
The Energy—Time “Uncertainty” Principle
Here we encounter another uncertainty principle that resembles in form the
type we have been discussing:
However, it is altogether different in spirit. For one, time “t” is not a dynamical
variable represented by a hermitian operator in the same way that position or
momentum can be. Hence Δt above means a very different thing than the
type of uncertainty associated with an observable that we’ve studied before.
Let’s define and derive precisely what we mean. To start, consider an arbitrary
observable
, and let’s look at how its expectation value evolves in time:
For now, we’ll look at one of its implications (directly relating to our new
uncertainty principle) – we’ll have more to say about its other implications
later.
For simplicity, assume the operator
on time. In this case, we have
in question does not depend explicitly
Now let’s recall our generalized uncertainty relation:
Note that since the first term on the RHS is positive, we can drop it and
the inequality still holds:
Choosing
relation becomes
Finally, defining
and using Ehrenfest’s theorem, the uncertainty
yields
Interpretation and Implication:
Δt can be thought of as the amount of time needed for the expectation value of the
observable in question to change substantially, i.e., by one standard deviation.
Note that Δt depends on which observable of a system is being measured.
Note too the following implications of the energy-time uncertainty principle:
1) If the state of the system has a very narrow spread in energy (ΔE small), then Δt
is necessarily large, i.e., the expectation values of all observables will evolve
slowly. (Indeed, in the extreme case where the system is in an energy
eigenstate (ΔE=0), then we recover a result that we already knew, namely, that
the expectation value of any observable does not vary in time!)
2) If the expectation value of any observable of a system is changing very rapidly,
then the uncertainty principle demands that the system must be in a state with a
3) A number of alternate interpretations of the time-energy uncertainty relation also
exist, though they may not be quite so “kosher”:
e.g. if a system or state of a system has only been in existence for a short period of time
Δt, then that system will necessarily have a spread of energies ΔE whose size is dictated
by the uncertainty relation.
e.g., a system can temporarily “borrow” energy ΔE (in apparent violation of energy
conservation), provided it “pays it back” within a time
(although some physicists
vehemently disagree with this interpretation!)
Example (from Constantinescu and Magyari): In a Frank and Hertz
experiment, a beam of mono-energetic electrons collide with hydrogen atoms,
temporarily raising the atoms from their ground state to their first excited state.
(These excited states typically have extremely short “lifetimes” – i.e., the atoms
following the collisions, the electrons of the beam are no longer monoenergetic, but rather display a range of energies on the order of 10-6 eV.
Why does this happen? What is the mean lifetime of the excited atoms?
Answer: Let τ denote the mean life of an excited hydrogen atom. Since the
excited state is only localized in time within a precision τ≈Δt, its excitation
energy has an uncertainty ΔE ≥
. It is these fluctuations that in turn are
responsible for the corresponding energy fluctuations seen in the electron
beam. Using the measured value of ΔE given above, we estimate the lifetime
of the excited states to be about τ≈3x10-10s.
In light of this example, we mention that the spectral lines associated with
short-lived excited states of atoms are never infinitely narrow, but rather
display a natural width owing to the energy uncertainty associated with their
short lives!
Example (from Constantinescu and Magyari): The π-meson is associated with
the nuclear force, which has an approximate range of about 1.4 Fermi (1 Fermi
=10-13cm). Assuming that it cannot travel faster than c, estimate the mass of the
π-meson.
The minimum-uncertainty wave packet
The position-momentum uncertainty principle is
Question: What shape wavefunction
uncertainty limit?
A gaussian!
will hit the minimum-
Here’s the justification:
So a general gaussian wavepacket (centered at x0 with average momentum
p0) hits the uncertainty limit!
*Caution: if, at some instant in time, a wavefunction is gaussian, then we
know that, at that moment,
. However, as time passes the
wavefunction will evolve according to the Schroedinger equation, and in
general will not remain gaussian.
An interesting exception occurs in the case of the quantum harmonic
oscillator: Here, it is possible to find mimimum uncertainty states that
remain minimum-uncertainty states throughout time (i.e., at any instant they
look gaussian, though not necessarily the same gaussian as they were
before). These states are called “coherent states.”
Question: Can you show that coherent states are eigenstates of the
lowering operator? (Griffiths’ problem 3.35 walks you through this.)
Approaching the Classical Limit
Warm-up Question: In our earlier study of a particle encountering a step
potential, we found that, quantum mechanically, when E>V0, a portion of the
wave is reflected.
For example, if E=2V0, then quantum mechanics predicts R=0.17 – hence we
should see reflection a moderate fraction of the time.
But if we actually go to the lab and set up a potential that approximates the above
step potential and then send in a baseball with twice the energy of the step, we in
fact will NOT observe any reflection – we’ll just observe the classical result of
100% transmission! Moreover, even if we replace the baseball by an electron, we
still may not observe any reflection! So we must face the question “Under what
conditions will classical physics suffice as a good approximation to our quantum
world, and when must we use quantum mechanics?
Different approaches to understanding the classical-quantum correspondence:
1) Ehrenfest’s theorem:
Setting
(where we used the fact that
Similarly, letting
and letting
).
, Ehrenfest’s theorem yields
yields
Note the striking similarity to Hamilton’s equations (i.e., Newtons IInd law).
The only difference is the presence of the brackets (i.e., the expectation
values) in the quantum case.
In particular, if we were allowed to replace
then the expectation values <x> and <p> would precisely obey the
Newton’s laws of classical physics!
So when is the above approximation valid? -- Basically, when the potential
V(x) or force (as defined by the derivative of the potential) don’t vary much
over the “size” (i.e., spread in x) of the wavepacket. In this case, classical
physics is a good approximation (and we don’t need quantum).
2) A closely related way of thinking about the classical limit is as follows:
Look at the de Broglie wavelength of the particle in question:
If the potential V(x) of the problem doesn’t vary much over a distance
scale defined by the particle’s de Broglie wavelength, then we recover
classical physics. (If the potential does vary rapidly over length scale λ,
then we expect to observe quantum effects.)
So go back to our example of a particle going over a step potential.
First note that in practice we can never have a true (infinitely abrupt)
“step” in a potential – the transition region (where the potential rapidly
rises from 0 to V0) may be narrow but never infinitely so.
Now suppose the incident particle we send toward the step is a 100eV
electron. Since
we would thus expect that if the transition region of the potential is
comparable to (or narrower than) about 10-10m, then we should
observe quantum reflection about 17% of the time!
But if the transition region is much wider than 10-10m (which is about
an atomic radius), then we will not see any such quantum effects.
3) It is also sometimes said that
If one likes, this can be regarded as simply another way of interpreting
lim λ  0 (since λ=h/p). But it can also be thought of slightly
differently. In particular, as h  0, quantum uncertainty goes away!
(i.e., think of Δx Δp ≥
.)
This notion that the classical regime corresponds to the limit h  0 can
be formalized using the so-called WKB approximation, in which the
solution to the Schroedinger equation is found in powers of . This
method is described in your texts (Shankar or Griffiths), but we will not
be discussing it this semester.
4) The “Bohr Correspondence Principle”
This basically says that we “recover” (in a certain sense) classical mechanics
as we go to higher and higher quantum numbers. This is best seen via an
illustration (here we’ll use the eigenstate of the simple harmonic oscillator):
Comparison of Quantum Probability (n=20 state) and Classical Probability
```
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