7
Infinite square well We now turn to the most straightforward (and therefore educational) non-zero potentials. We just discussed a free particle; we now turn to a bound particle, and will shortly discuss potentials that can lead to both. The infinite square well potential is given by: ( ) > < = a x x a x x V , , , 0 0 0 A particle under the influence of such a potential is free (no forces) between x = 0 and x = a, and is completely excluded (infinite potential) outside that region. Now, the first lesson to take from this problem is that one does not have to solve the TISE everywhere at once – one can solve for the wave function piecemeal in the different regions where the potential is given by one function. However, the wave function must behave as a whole in certain ways as we discussed earlier. We first look for the wavefunction in the region outside of 0 to a. Here, where the particle is excluded, the wave function must be zero. Great, half of the problem solved. Inside the region from zero to a, the wavefunction must be a solution of ( ) ( ) x E dx x d m ψ ψ = 2 2 2 2 h since V(x) = 0. The solution to this simple differential equation is simply the free particle solutions: ( ) h mE k Be Ae x ikx ikx 2 = + = , ψ But now we have to apply whatever boundary conditions we have. We know that continuity of the wave function insists that ψ(0) = ψ(a) = 0, so,

t is e Infinite Square

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Page 1: t is e Infinite Square

Infinite square well We now turn to the most straightforward (and therefore educational) non-zero potentials. We just discussed a free particle; we now turn to a bound particle, and will shortly discuss potentials that can lead to both. The infinite square well potential is given by:

( )⎩⎨⎧

><∞≤≤

= axxax

xV ,,,

000

A particle under the influence of such a potential is free (no forces) between x = 0 and x = a, and is completely excluded (infinite potential) outside that region. Now, the first lesson to take from this problem is that one does not have to solve the TISE everywhere at once – one can solve for the wave function piecemeal in the different regions where the potential is given by one function. However, the wave function must behave as a whole in certain ways as we discussed earlier. We first look for the wavefunction in the region outside of 0 to a. Here, where the particle is excluded, the wave function must be zero. Great, half of the problem solved. Inside the region from zero to a, the wavefunction must be a solution of

( )( )xE

dxxd

mψψ

=− 2

22

2h

since V(x) = 0. The solution to this simple differential equation is simply the free particle solutions:

( )h

mEkBeAex ikxikx 2=+= − ,ψ

But now we have to apply whatever boundary conditions we have. We know that continuity of the wave function insists that ψ(0) = ψ(a) = 0, so,

Page 2: t is e Infinite Square

( )

( ) ( )( ) ( )

( ) ...,,,sin

...,,,sin

sin

210

210

0

0 00

=⎟⎠⎞

⎜⎝⎛=

⇒=

⇒==

⇒==

=−=

⇒−=

⇒+=

+=

nxa

nAx

ank

nnka

kaAa

kxAAeAex

AB

BA

BeAe

nn

ikxikx

ikik

πψ

ππ

ψ

ψ

ψ

But, n=0 is a trivial solution, so we have:

( ) ...,,,sin 321=⎟⎠⎞

⎜⎝⎛= nx

anAx nnπψ

These are our stationary state solutions to the infinite square well potential. We choose to normalize these state solution for reasons that will become evident later:

( )

β

πψ

in

n

a

nn

ea

AA

aA

dxxa

nAdxx

2

12

1

2

0

222

==

⇒=

⇒=⎟⎠⎞

⎜⎝⎛= ∫∫

∞−

sin

where beta is an arbitrary phase, and since it has no consequence on measurement, we take it to be zero:

aA 2

=

So that the normalized stationary states are:

( ) ...,,,sin 3212=⎟

⎠⎞

⎜⎝⎛= nx

an

axn

πψ

Let’s take a moment to study some of the properties of these solutions, as they are in general applicable to solutions to most potentials that you will encounter:

Page 3: t is e Infinite Square

1) These functions are alternatively even and odd about the center of the potential well. This will be true for any symmetric potential. 2) With increasing n, each successive state has one more node in the wavefunction. This is true regardless of the shape of the potential. 3) The states are orthogonal. This means that:

( ) ( ) nmdxxx nm ≠=∫∞

∞−

∗ ,0ψψ

We show a proof:

( ) ( )

( ) ( )

( )[ ]( )

( )[ ]( )

01

11

1

2

0

0

0

=⎭⎬⎫

⎩⎨⎧

++

−−−

=

⎭⎬⎫

⎩⎨⎧

⎟⎠⎞

⎜⎝⎛ +

+−⎟

⎠⎞

⎜⎝⎛ −

−=

⎟⎠⎞

⎜⎝⎛ +

−⎟⎠⎞

⎜⎝⎛ −

=

⎟⎠⎞

⎜⎝⎛

⎟⎠⎞

⎜⎝⎛=

∫∫∞

∞−

nmnm

nmnm

xa

nmnm

xa

nmnm

dxxa

nmxa

nma

dxxa

nxa

ma

dxxx

a

a

a

nm

πππ

ππ

ππ

ππ

ππψψ

sinsin

sinsin

coscos

sinsin

This, together with the fact that when m = n, the same integral gives one (this is why we normalized the state functions) gives:

( ) ( )

⎩⎨⎧

=≠

=

=∫∞

∞−

nmnm

dxxx

mn

mnnm

,

,

1,0

δ

δψψ

where δmn is called the Kronecker delta. These statements are combined to say that the states are orthonormal (both orthogonal and normalized). This is also a general result of state functions regardless of the potential (assuming you normalize them). 4) The state functions form a complete set. This is perhaps the most interesting and useful of the properties. Although not universal, it will usually be the case for potentials you will encounter. This means that any other function f(x) can be written in terms of these functions:

( ) ( ) ∑∑∞

=

=⎟⎠⎞

⎜⎝⎛==

11

2n

nn

nn xa

nca

xcxf πψ sin

Page 4: t is e Infinite Square

Then, finding the values of the constants cn is straightforward using Fourier’s trick (just using the orthonormal nature of the state functions):

( ) ( ) ( ) ( )

( ) ( )∫

∑∑ ∫∫∗

=

=

∗∗

=

⇒===

dxxfxc

ccdxxxcdxxfx

nn

mn

mnnn

nmnm

ψ

δψψψ11

OK, we will get back to these properties of the state functions in a minute, but let’s put the whole picture together first. The general state solutions are given by:

( ) ...,,,sin, 3212=⎟

⎠⎞

⎜⎝⎛=Ψ − nex

an

atx tiE

nn hπ

where we can determine the energies En from above:

2

222

2

2

manE

anmEk

nh

h

π

π

=

⇒==

so that the boundary conditions impose specific, allowed values of the energy.

Page 5: t is e Infinite Square

Now, if someone asks you: “What is the wavefunction for a particle in an infinite square-well potential?” what would you answer? No, let’s say you don’t know its energy. The answer is a superposition of all the Ψn’s:

( ) ( ) 2

222

1 22

manEex

anc

atxctx n

n

tiEn

nnn

nhh ππ

=⎟⎠⎞

⎜⎝⎛=Ψ=Ψ ∑∑

=

− ,sin,,

But how do you find the cn’s? To determine these, you have to have an additional boundary condition, namely at some time, call it t = 0, you have to know something else about the particle. Example: A particle in an infinite square well has as an initial wave function

( )( )

⎪⎩

⎪⎨⎧

><≤≤−

=Ψ axaxxaAx

x 000

0,

, for some constant A. Find Ψ(x,t).

First, we must determine A using the normalization condition (since if Ψ(x,0) is normalized, Ψ(x,t) will stay normalized, as we showed earlier):

( ) ( ) ( )

5

52

5552

0

54322

0

43222

0

222

0

2

30

13054

2354

23

20

aA

aAaaaAxxaxaA

dxxaxxaAdxxaxAdxx

a

aaa

=

⇒==⎟⎟⎠

⎞⎜⎜⎝

⎛+−=⎟⎟

⎞⎜⎜⎝

⎛+−=

+−=−=Ψ ∫∫∫ ,

Now we turn to our method for determining the coefficients cn:

( ) ( ) ( ) ( )∫∑ ∗∞

=

== dxxfxcxcxf nnn

nn ψψ ,1

so,

Page 6: t is e Infinite Square

( ) ( )

( ) ( )

( )

( )( )

( )( )

( )( )

( )( )

( )( ) ( )[ ]

( )⎪⎩

⎪⎨

⎧=

−=

⎥⎦

⎤⎢⎣

⎡+

−+−=

⎪⎭

⎪⎬⎫

⎥⎥⎦

⎢⎢⎣

⎡⎟⎠⎞

⎜⎝⎛−

−⎟⎠⎞

⎜⎝⎛

⎟⎠⎞

⎜⎝⎛

⎪⎩

⎪⎨⎧

−⎥⎦

⎤⎢⎣

⎡⎟⎠⎞

⎜⎝⎛−⎟

⎠⎞

⎜⎝⎛

⎟⎠⎞

⎜⎝⎛=

⎭⎬⎫

⎩⎨⎧

⎟⎠⎞

⎜⎝⎛−⎟

⎠⎞

⎜⎝⎛=

−⎟⎠⎞

⎜⎝⎛=

Ψ=

∫∫

∑∗

=

oddn if158evenn if0

0154

022152

22

152

152

302

0

0

3

3

33

3

23

3

3

0

3

22

0

2

3

0

2

03

05

1

,

,

coscos

coscoscos

cossin

cossin

sinsin

sin

,

,

π

ππ

ππ

πππ

π

ππ

πππ

ππ

ππ

ππ

π

ψ

ψ

n

nn

nan

nnan

na

a

xa

nan

axnx

anx

na

xa

nnaxx

an

naa

a

dxxa

nxdxxa

nxaa

dxxaxa

xa

na

dxxxc

xcx

a

a

aa

a

nn

nnn

So that now we can form our time dependent wavefunction by putting this all together:

( ) ∑=

−⎟⎠⎞

⎜⎝⎛

⎟⎠⎞

⎜⎝⎛=Ψ

...,,sin,

531

23

32221230

n

matinexa

nna

tx hπππ

Now, let’s study this wavefunction, and its implications on measurable quantities. We first ask what the expectation value of the energy is.

Page 7: t is e Infinite Square

( ) ( ) ( ) ( ) ( ) ( )

( ) ( ) ( ) ( )

( ) ( ) ( ) ( )

( ) ( )

( ) ( )

∑∑ ∑

∑∑ ∫

∑ ∑ ∫

∫ ∑∑

∫ ∑∑

∫ ∑∑∫

==

=

=

⎟⎠

⎞⎜⎝

⎛=

⎟⎠

⎞⎜⎝

⎛=

⎟⎠

⎞⎜⎝

⎛=ΨΨ=

∗∗

∗∗

∗∗∗

∗∗∗

∗∗∗∗

nnn

m nmnnmn

m nnmnmn

m nnnmmn

nnnnn

mmmm

nnnn

mmmm

nnnn

mmmm

EcccE

dxxxccE

dxxcxcE

dxtxEctxc

dxtxHctxc

dxtxcHtxcdxtxHtxE

ψψ

ψψ

φψφψ

φψφψ

φψφψ

)

)),,

So, we can think of the |cn|2 as the probability that one will measure En, remembering again that you will only measure one of these values, and then the total probability to measure one of the En’s must be one or:

12 =∑m

nc

We can show this since the wave function is normalized, each stationary state is normalized and the initial condition is also normalized, then:

( ) ( ) ( ) ( )

( ) ( )

( ) ( )

1

00

2 ===

=

=

⎟⎠

⎞⎜⎝

⎛=ΨΨ

∑∑ ∑

∑∑ ∫

∑ ∑ ∫

∫ ∑∑∫

∗∗

∗∗

∗∗∗

mn

m nmnnm

m nnmnm

m nnnmm

nnn

mmm

ccc

dxxxcc

dxxcxc

dxxcxcdxxx

δ

ψψ

ψψ

ψψ,,

The cn’s can also be thought to tell you the amount of Ψn that is in the total wavefunction. In the example above, you can see that the initial wavefunction closely resembles ψ1, and if we look at c1:

....99855501582

3

2

1=⎟⎟

⎞⎜⎜⎝

⎛=

πc

very close to one indicating that the 1st state dominates.