Particle in a Potential Well Vc[1]
Transcript of Particle in a Potential Well Vc[1]
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Particle in a Potential Well
Figure 1
Figure 1 represents an infinite square well potential of width a. The potential
of this one dimensional well is V(x) = 0 for 0 x a, and V(x) = for x a.
1
V(x)
x = 0 x = ax
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The infinite square well potential corresponds to the motion of a particle
constrained by impenetrable walls to move in a region of width a where the
potential energy is constant. The potential energy is taken to be zero as the
potential energy is infinite at x = 0 and x = a, the probability of finding the
particle outside the well is zero. The wave function (x) thus vanishes for
xa.
However, there is a wave function in the region 0 x a
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Recall that the one dimensional time independent Schrodinger equation is
2 2
2( )
2
dV x E
m dx
+ =
h
Since V(x) = zero in this region, the second term vanishes and we now have
2 2
20
2
dE
m dx
+ =
h
or2
2 2
20
d mE
dx
+ =
h.
The Schrodinger equation of the particle with mass m and energy E in the
region 0 x a can thus be expressed as2
2 2
20
d mE
dx
+ =
h.
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Remember that the wave function must be continuous; then (x) must
vanish at the walls. The general solution of the Schrodinger equation is
1 22 2
2 2( ) cos sin
mE mE x c x c x
= +
h h
But (0) = 0
(0) = 0
( ) ( ) ( )1 2
1
0 cos 0 sin 0 0
0
c c
c
= + =
=
Thus the wave function can be expressed as
( ) 2 22
sinmE
x c x
= h
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Since the second boundary condition is (a) = 0, we have
( ) 2 22
sin 0mE
a c a
= = h
But c2 0 for the wave function to be in existence.
2
2
2sin 0
2or where 1, 2,3...
mEa
mEa n n
=
= =
h
h
Note that we exclude the case n = 0, which would also produce a wave
function that vanishes everywhere. This is contrary to the initial conditions
where we know that a wave function exists in a certain region i.e. the region
where 0 x a Since a is also fixed, the only free parameter is the energy
E. This tells us that the Schrodinger equation has a solution only for
certain discrete values ofE.
2 2
2
2, where 1, 2, 3...
2 E n n
ma= =h
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Note also that the smallest possible energy (n = 1) for the particle is not zero but
2 2
1 22E
ma= h
This is the minimum energy and is called the zero point energy of the infinite
potential well with Edefined, we now go back to the wave function
( ) 2 22
sinmE
x c x
= h
( )
( )
2
2
sin
or sinn
n xx c
a
n xx c
a
=
=
The constant c2 can be obtained by normalizing the wave function
( ) ( )2 2
2
2
2
2
sin
2
1
2
a a
n no o
n x x x dx c dxa
ac
ca
=
=
=
=
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Aside
2 2
sin sin
a a
o o
n x a n x n
dx d xa n a a
=
Let
0, 0
,
n x
a
x
x a n
=
= == =
( )
2 2
sin sin
11 cos 2
2
1 cos 2
2 2
sin 2
2 4
sin2
2 4
2
a n
o o
n
o
n n
o o
n n
o o
n x a
dx da n
ad
n
ad d
n
a
n
a n n
n
a
=
=
=
=
=
=
( )
( )
2sin for 0
and 0 for
n
n
n x x x a
a a
x x x a
=
=
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The first 3 stationary states are shown below
The wave functions n (x) are alternatively symmetric (for odd n) and antisymmetric (for even n) about x = 2
a .
Note that the solutions of the Schrodinger equation will be either symmetric or
anti symmetric.
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1 (x)
n = 1
o a
x
2 (x)
n = 2
o ax
3
(x)
o ax
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The function n (x) are mutually orthogonal, in the sense that
( ) ( ) 0m n x x dx =
whenever m n
( ) ( )2
sin sin
1cos cos
a
m no
a
o
m x n x x x dx dx
a a a
m n m n x x dx
a a a
=
+ =
Aside : ( ) ( )1
sin sin cos cos2
A B A B A B= +
( ) ( )( ) ( )
( ) ( )
( )
1 1sin sin
sin sin
0
0
a
m n
o
m n m n x x dx x x
m n a m n a
m n m n
m n m n
+ = +
+ = +
=
=
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THE UNCERTAINTY PRINCIPLE
The Uncertainty Principle states that the more precisely determined a particles
position, the less precisely the momentum is. The Heisenberg position
momentum uncertainty principle can thus be expressed as
xx p h
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Consider a particle of mass m in a one dimensional square well of width L. Thus
x L and p L
hif v= 0 at the bottom of the well, the energy of the
particle
2 2 2
2 2 22 2 8p hE
m mL mL= =h
If we apply the result to an electron trapped within L 1 , we have
10 E eV
This is about right for the K.E of an electron in the ground state of a hydrogen atom.
Thus the uncertainty principle gives a direct and simple approach to the estimation
of ground state energies.
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