Heisenbergs Uncertainty Relation

Position-momentum uncertainty

As an example for a wave packet we chose plane waves whose amplituds obey a Gaussian distribution centered at k0,

C(k)=C0e(a2)2(kk0)2.

Then the one-dimensional wave packet results in

ψ(z,t)=C0+e(a2)2(kk0)2ei(kzωt)dk.

We examine the integration and determine for the case of t=0 the normalization constant C0=a(π)3/4. The wave packet and propability denisty then read as

ψ(z,0)=(2πa2)14e(za)2eik0z

and

|ψ(z,0)|2=2πa2e2(za)2,

respectively. The latter obye the normalization condition.

Our wave packet exhibits a maximum at z=0. At z1,2=±a/2 the propability density drops to |ψ(z,0)|2=1/e of teh maximum. Commonly, the width z1z2=Δz=a is defined as full width of the wave packet.

Concerning the wave number, the wave packet is comprised of plane waves which obey the amplitude distribution C(k). If we know wonder for the width Δk=k1k0 fulfilling the condition |C(k)|2=C02/e, it deriectly follows Δk=1/a.

Now we can conclude, the product of the spatial width of the wave packet Δz and the width of the wavenumber interval Δk equals 1,

ΔzΔk=1.

A first indication of this fact you got already when introducing wave packets. As depicted, the broader the wavenumber intervall, the narrower the width in z. The meaning of the condition between Δz and Δk becomes clear, if we use the momentum on the basis of the de Broglie wavelength pz=k. Then, the product reads as ΔzΔpz=. In the case of a Gaussian distribution, the product ΔzΔpz= is the smallest. In the case of any other distribution function, the product is larger ΔzΔpz>. On teh basis of these consideration, we can formulate Heisenberg’s uncertainty relation,

ΔzΔpz.

For the other two directions of the three-dimentional space one obtains analogously

ΔxΔpxΔyΔpy

Often the spatial width Δz is defined as the width where the wave packet drops to 1/e of the maximum amplitude. Then it follows for the spatial width Δz=2a and for the wavenumber interval Δk=2/a. As a consequence the product Δzpz=2.

If we assume a constant amplitude (as we did for introducing matter waves inteh previous chapter), we might also define the distance between the first root at either side as width of the wave packet. The root is located at uroot=2π/Δk. Making use of u=(dω/dk)k0z it follows Δz=4π/Δk and ΔzΔk4π. As a consequence, the uncertainty relation reads as ΔzΔpz2h with h=2π.

Thus, the exact value of the limit of ΔzΔpz does depent on the definition of the spatial uncertainty Δz and in accord Δpz.

One illustrative example is provided on the basis on electron diffraction at a single slit. Let us assume a single slit parallel to the x axis with a width of Δx=b and an electron beam with the momentum p=(0,py,0)T. Before the electrons pass the slit their momentum along x is px=0, while we cannot provide any details about their x coordinate. At the slit only those electrons can pass whose x coordinate is in the interval between x=0b/2 and x=0+b/2. Thus, for the transmitted electron we can constrain the space of possible x values down to Δx=b and in accord to the uncertainty relation the momentum along the x direction becomes px/b. As a consequence, after passing the slit the electrons are distributed about an angle θφ+θ with the condition

sin(θ)=Δpxp=hbp.

If we describe the electrons by means of the de Broglie wavelength λ=p/h, then the wave is diffracted at the slit and we get a central maximum of the diffraction pattern with the width Δφ=2θ. Analogously to the diffraction of light we get

sin(θ)=λb.

On the basis of this exmaple we see that the uncertainty arise from the description of a particle as wave and the spatial constraints of this wave.

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Fig.: Scheme of an electron with a momentum uncertainty along :math:`x` of :math:`Delta p_x = 0` and thus :math:`Delta x = infty` before it enters the slit. Due to the localization through the slit (:math:`Delta x` becomes a finite number), the electron experiences an uncertainty of the momentum :math:`Delta p_x > 0`.

Another example might be constructed, if we assume to observe a microscopic particle at rest via a miocroscope.Therefore, we have to shine light on that particle in order to detect the scattered light of wavelength λ within the opening angle of the objective 2α (sin(α)tan(α)=d/(2y), with d and y being the diameter of the objective and the particle-objective distance, respectively). The momentum of the scattered photon then has an uncertainty along x

Δpx=pphsin(α)hλd2y

Due to the conservation of overall momentum, the particle that scattered the photon (and got a momentum because of this event) has the same uncertainty Δpx. In addition, if parallel light is focused by means of an objective, diffraction at teh objective’s edge will lead to a diffraction pattern in teh focal plane. The central intensity maximum (0-th order diffraction peak) has a diameter of

1.22=dλsin(θ)dλtan(θ)=dλD2y.

Remember the lecture about diffraction and the Airy disk. As a consequence, we cannot determine the position of the particle more precise than Δx=D (the diameter of the Airy disk). If we now combine both equations, we get

=1.22h.

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Fig.: (left) A photon is scattered by a particle and propagtes within the opening angle of the objective. (right) In order to localize the particle, it has to be bigger than the Airy disc.

As we have learned on the basis of diffraction at a pinhole, one might use light with a shorter wavelength in order to reduce Δx. However, at the very same moment one will increase Δpx about the same amount one has decreased Δx resulting in a constant product ΔxΔpx.

Energy-time uncertainty

As we have seen, the spatial distribution of the wave packet Δx depends on the wavenumber interval Δk, used to construct the wave packet. Now we want to discuss how precise we can measure the energy ω0 of a wave packet with the central frequency ω0 if we measure during a time interval Δt.

As we did previously, we comprise the wave packet as superpostion of partial waves, but do not integrate over the wavenumber interval Δk but rather over the frequency interval Δω,

ψ(z,t)=+C(ω)ei(ωtkz)dω.

Completely analogous as in the previous case of matter waves we make us of a Taylor series

k=k0+(dkdω)ω0(ωω0)+

and substitute u=t(dk/dω)ω0z, which allows us to calculate

ψ(z,t)=2C(ω)sin(Δωu)uei(ω0tk0z).

At the fixed position z0 the maximum appears at t0=(dk/dω)ω0z0 and the two roots left and right of the central maximum are at poistion z0 at times

t1,2=(dkdω)ω0z0±πΔω,

respectively. Thus, the central maximum needs the time Δt=2π/Δω to completely pass the position x0. Conversely, if we record a wave packet onlöy within the time interval Δt, then we can estimate its central frequency only with an uncertainty Δω.

For example we measure a monochromatic wave C0ei(kzω0t) at position z=0 during the interval Δt. The Fourier transform of the amplitude distribution of this wave train then reads as

C(ω)=t=Δ/2+Δ/2C0ei(ωω0)tdt=C0sin(ωω02Δt)ωω02Δt.

The central maximum has a width of Δω=2π/Δt. Since the energy is connected with the frquency in accord to E=ω, we finally obtain

ΔEΔωh.

If we use a Gaussian distribution of the amplitude instead of a constant, we will result in ΔEΔω. However, if we observe a particle only during a limitted period of time Δt, we can estimate its energy only with the certainty of ΔEh/Δt.

Spreading of wave packets

As we have seen previously the center of a matter wave propagates with the group velocity vg which is tantamount to the velocity of a particle vp=p/m. Since the initial momentum of the particle p allready bears a particular uncertainty Δp, we cannot determine the momentum of the particle more precise than p±Δp. As a consequence vg also bears a particular uncertainty $ \Delta `v_{:nbsphinx-math:mathrm{g}`}$ with

Δvg=1mΔp=1mΔz0,

with Δz0 being the uncertainty of the particle’s position at time t=0. Due to the uncertainty of the particle propagation, the uncertainty to determine Δz at a later time than t=0 grows with increasing time, namely

Δz(t)=Δvgt=mΔz0t.

Here, Δz(t) denotes the width of the wave packet at time t>0. The area under the curve of the wave packet, however, remains constant. This is an immediate consequence of the normalization condiziont,

+|ψ(z,t)|2dz=1.

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Fig.: The spreading of a wave packet with Gaussian amplitude during time. Note the actual amplitude of the wave packet is decrasing while its width is increasing. The area under the curve, however, is constant.

Furthermore, it is evident that the better the particle is located at time t=0 (Δx0 small), the greater the spread over time. This arises from an increased momentum uncertainty as a consequence of the reduced position uncertainty, and hence an increased uncertainty of the particle velocity.