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7'1 Application of the Schrdinger Equation to the Hydrogen Atom

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Title: 7'1 Application of the Schrdinger Equation to the Hydrogen Atom


1
CHAPTER 7The Hydrogen Atom
  • 7.1 Application of the Schrödinger Equation to
    the Hydrogen Atom
  • 7.2 Solution of the Schrödinger Equation for
    Hydrogen
  • 7.3 Quantum Numbers
  • 7.4 Magnetic Effects on Atomic SpectraThe
    Zeeman Effect
  • 7.5 Intrinsic Spin
  • 7.6 Energy Levels and Electron Probabilities

Werner Heisenberg (1901-1976)
The atom of modern physics can be symbolized only
through a partial differential equation in an
abstract space of many dimensions. All its
qualities are inferential no material properties
can be directly attributed to it. An
understanding of the atomic world in that primary
sensuous fashionis impossible. - Werner
Heisenberg
2
7.1 Application of the Schrödinger Equation to
the Hydrogen Atom
  • The potential energy of the electron-proton
    system is electrostatic
  • Use the three-dimensional time-independent
    Schrödinger Equation.
  • For Hydrogen-like atoms (He or Li), replace e2
    with Ze2 (Z is the atomic number).
  • In all cases, for better accuracy, replace m with
    the reduced mass, m.

3
Spherical Coordinates
  • The potential (central force) V(r) depends on the
    distance r between the proton and electron.

Transform to spherical polar coordinates because
of the radial symmetry.
4
The Schrödinger Equation in Spherical Coordinates
Transformed into spherical coordinates, the
Schrödinger equation becomes
5
Separable Solution
This would make life much simpler, and it turns
out to work.
6
7.2 Solution of the Schrödinger Equation for
Hydrogen
Substitute
Multiply both sides by -r2 sin2q / R f g
7
Solution of the Schrödinger Equation for H
  • r and q appear only on the left side and f
    appears only on the right side.
  • The left side of the equation cannot change as f
    changes.
  • The right side cannot change with either r or q.
  • Each side needs to be equal to a constant for the
    equation to be true.
  • Set the constant to be -ml2
  • It is convenient to choose the solution to be
    .

azimuthal equation
8
Solution of the Schrödinger Equation for H
  • satisfies the azimuthal equation for any
    value of ml.
  • The solution must be single valued to be a valid
    solution for any f

Specifically
So
ml must be an integer (positive or negative) for
this to be true.
9
Solution of the Schrödinger Equation for H
  • Now set the left side equal to -ml2

Rearrange it and divide by sin2(q)
Now, the left side depends only on r, and the
right side depends only on q. We can use the
same trick again!
10
Solution of the Schrödinger Equation for H
  • Set each side equal to the constant l(l 1).

Radial equation
Angular equation
Weve separated the Schrödinger equation into
three ordinary second-order differential
equations, each containing only one variable.
11
Solution of the Radial Equation for H
  • The radial equation is called the associated
    Laguerre equation and the solutions R are called
    associated Laguerre functions. There are
    infinitely many of them, for values of n 1, 2,
    3,
  • Assume that the ground state has n 1 and l 0.
    Lets find this solution.
  • The radial equation becomes
  • The derivative of yields two terms

12
Solution of the Radial Equation for H
Set the second expression equal to zero and
solve for a0 Set the first expression equalto
zero and solve for E Both are equal to the Bohr
results!
13
Principal Quantum Number n
  • There are many solutions to the radial wave
    equation, one for each positive integer, n.
  • The result for the quantized energy is

A negative energy means that the electron and
proton are bound together.
14
7.3 Quantum Numbers
  • The three quantum numbers
  • n Principal quantum number
  • l Orbital angular momentum quantum number
  • ml Magnetic (azimuthal) quantum number
  • The restrictions for the quantum numbers
  • n 1, 2, 3, 4, . . .
  • l 0, 1, 2, 3, . . . , n - 1
  • ml -l, -l 1, . . . , 0, 1, . . . , l - 1, l
  • Equivalently
  • n gt 0
  • l lt n
  • ml l

The energy levels are
15
Hydrogen Atom Radial Wave Functions
  • First few radial wave functions Rnl

Sub-scripts on R specify the values of n and l.
16
Solution of the Angular and Azimuthal Equations
  • The solutions to the azimuthal equation are
  • Solutions to the angular and azimuthal equations
    are linked because both have ml.
  • Physicists usually group these solutions together
    into functions called Spherical Harmonics

spherical harmonics
17
Normalized Spherical Harmonics
18
Solution of the Angular and Azimuthal Equations
  • The radial wave function R and the spherical
    harmonics Y determine the probability density for
    the various quantum states. The total wave
    function depends on n, l, and ml. The
    wave function becomes

19
Probability Distribution Functions
  • We use the wave functions to calculate the
    probability distributions of the electrons.
  • The position of the electron is spread over
    space and is not well defined.
  • We may use the radial wave function R(r) to
    calculate radial probability distributions of the
    electron.
  • The probability of finding the electron in a
    differential volume element dt is

20
Probability Distribution Functions
  • The differential volume element in spherical
    polar coordinates is
  • Therefore,
  • At the moment, were only interested in the
    radial dependence.
  • The radial probability density is P(r)
    r2R(r)2 and it depends only on n and l.

21
Probability Distribution Functions
R(r) and P(r) for the lowest-lying states of the
hydrogen atom.
22
Probability Distribution Functions
  • The probability density for the hydrogen atom for
    three different electron states.

23
Orbital Angular Momentum Quantum Number l
  • Energy levels are degenerate with respect to l
    (the energy is independent of l).
  • Physicists use letter names for the various l
    values
  • l 0 1 2 3 4 5 . . .
  • Letter s p d f g h . . .
  • Atomic states are usualy referred to by their
    values of n and l.
  • A state with n 2 and l 1 is called a 2p state.

24
Orbital Angular Momentum Quantum Number l
  • Its associated with the R(r) and f(?) parts of
    the wave function.
  • Classically, the orbital angular momentum
    with L mvorbitalr.
  • L is related to l by
  • In an l 0 state,
  • This disagrees with Bohrs semi-classical
    planetary model of electrons orbiting a
    nucleus L nh.

Classical orbitswhich do not exist in quantum
mechanics
25
Magnetic Quantum Number ml
  • The solution for g(f) specifies that ml is an
    integer and is related to the z component of L

Example l 2 Only certain
orientations of are possible. This is called
space quantization.And (except when l 0) we
just dont know Lx and Ly!
26
Rough derivation of L2 l(l1)h2
  • We expect the average of the angular momentum
    components squared to be the same due to
    spherical symmetry

But
Averaging over all ml values (assuming each is
equally likely)
because
27
7.4 Magnetic Effects on Atomic SpectraThe
Zeeman Effect
28
The Zeeman Effect
The potential energy due to the magnetic field is
29
The Zeeman Effect
  • A magnetic field splits the ml levels. The
    potential energy is quantized and now also
    depends on the magnetic quantum number ml.
  • When a magnetic field is applied, the 2p level of
    atomic hydrogen is split into three different
    energy states with energy difference of ?E mBB
    ?ml.

30
The Zeeman Effect
  • The transition from 2p to 1s, split by a magnetic
    field.

31
The Zeeman Effect
  • An atomic beam of particles in the l 1 state
    pass through a magnetic field along the z
    direction.

The ml 1 state will be deflected down, the ml
-1 state up, and the ml 0 state will be
undeflected.
32
7.6 Energy Levels and Electron Probabilities
  • For hydrogen, the energy level depends on the
    prin-cipal quantum number n.

In the ground state, an atom cannot emit
radiation. It can absorb electromagnetic
radiation, or gain energy through inelastic
bombardment by particles.
33
Selection Rules
  • We can use the wave functionsto calculate
    transition probabilities for the electron to
    change from one state to another.
  • The probability is proportional to the mag
    square of the dipole moment
  • Allowed transitions
  • Electrons absorbing or emitting photons can
    change states when ?l 1 and ?ml 0, 1.
  • Forbidden transitions
  • Other transitions are possible but occur with
    much smaller probabilities.

where Yi and Yf are the initial and final states
of the transition.
34
7.5 Intrinsic Spin
  • In 1925, grad students, Samuel Goudsmit and
    George Uhlenbeck, in Holland proposed that the
    electron must have an intrinsic angular
    momentum and therefore a magnetic moment.
  • Paul Ehrenfest showed that, if so, the surface of
    the spinning electron should be moving faster
    than the speed of light!
  • In order to explain experimental data, Goudsmit
    and Uhlenbeck proposed that the electron must
    have an intrinsic spin quantum number s ½.

35
Intrinsic Spin
  • The spinning electron reacts similarly to the
    orbiting electron in a magnetic field.
  • The magnetic spin quantum number ms has only two
    values, ms ½.

The electrons spin will be either up or down
and can never be spinning with its magnetic
moment µs exactly along the z axis.
36
Intrinsic Spin
Recall
  • The magnetic moment is .
  • The coefficient of is -2µB and is a
    consequence of relativistic quantum mechanics.
  • Writing in terms of the gyromagnetic ratio, g
    gl 1 and gs 2
  • The z component of
    .
  • In an l 0 state
  • Apply ms and the potential energy becomes

and
no splitting due to .
37
Generalized Uncertainty Principle
Define the Commutator of two operators, A and B
Then the uncertainty relation between the two
corresponding observables will be
So if A and B commute, the two observables can be
measured simultaneously. If not, they
cant. Example
So
and
38
Two Types of Uncertainty in Quantum Mechanics
Weve seen that some quantities (e.g., energy
levels) can be computed precisely, and some not
(Lx). Whatever the case, the accuracy of their
measured values is limited by the Uncertainty
Principle. For example, energies can only be
measured to an accuracy of h /Dt, where Dt is how
long we spent doing the measurement. And there is
another type of uncertainty we often simply
dont know which state an atom is in. For
example, suppose we have a batch of, say, 100
atoms, which we excite with just one photon.
Only one atom is excited, but which one? We
might say that each atom has a 1 chance of being
in an excited state and a 99 chance of being in
the ground state. This is called a superposition
state.
39
Superpositions of states
Stationary states are stationary. But an atom
can be in a superposition of two stationary
states, and this state moves.
where ai2 is the probability that the atom is
in state i. Interestingly, this lack of knowledge
means that the atom is vibrating
40
Superpositions of states
Vibrations occur at the frequency difference
between the two levels.
Excited level, E2
DE hn
Energy
Ground level, E1
The atom is at least partially in an excited
state.
The atom is vibrating at frequency, n.
41
Calculations in Physics Semi-classical physics
The most precise computations are performed fully
quantum-mechanically by calculating the potential
precisely and solving Schrodingers Equation. But
they can be very difficult. The least precise
calculations are performed classically,
neglecting quantization and using Newtons
Laws. An intermediate case is semi-classical
computations, in which an atoms energy levels
are computed quantum-mechanically, but additional
effects, such as light waves, are treated
classically.
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