lecture 21 the hydrogen and hydrogenic atoms physics 420 spring 2006 dennis papadopoulos

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LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

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Page 1: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

LECTURE 21

THE HYDROGEN AND HYDROGENIC ATOMS

PHYSICS 420SPRING 2006Dennis Papadopoulos

Page 2: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

• 1 Application of the Schrödinger Equation to the Hydrogen Atom

• 2 Solution of the Schrödinger Equation for Hydrogen• 3 Quantum Numbers• 4. Energy Levels and Electron Probabilities• 5 Magnetic Effects on Atomic Spectra – The Normal

Zeeman Effect• 6 Intrinsic Spin

The Hydrogen AtomThe Hydrogen Atom

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 fashion…is impossible.

- Werner Heisenberg

Page 3: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

1: Application of the Schrödinger Equation to the Hydrogen Atom

• The approximation of the potential energy of the electron-proton system is electrostatic:

• Rewrite the three-dimensional time-independent Schrödinger Equation.

For Hydrogen-like atoms (He+ or Li++)• Replace e2 with Ze2 (Z is the atomic number).

Page 4: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Application of the Schrödinger Equation

• 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.

Insert the Coulomb potential into the transformed Schrödinger equation.

1/ (1/ ) (1/ )e ireduced mass m m

Page 5: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Fig. 8-5, p.266

Page 6: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Application of the Schrödinger Equation

• The wave function ψ is a function of r, θ, .• Equation is separable.• Solution may be a product of three functions.

• We can separate the SE into three separate differential equations, each depending on one coordinate: r, θ, or .

Page 7: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Solution of the Schrödinger Equation

• Eqs (8.11) to eqs (8.15) yield

• SE has been separated into three ordinary second-order differential equations each containing only one variable.

----Radial equation

----Angular equation

l

22

2

im

( )( ) --------Azimuthal equation

g e

l

d gm g

d

:

Page 8: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Solution of the Radial Equation

• The radial equation is called the associated Laguerre equation and the solutions R that satisfy the appropriate boundary conditions are called associated Laguerre functions.

• Assume the ground state has ℓ = 0 and this requires mℓ = 0. The radial equation becomes

or

Page 9: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Solution of the Radial Equation• Try a solution Take derivatives of R and insert them into the SE equation.

• To satisfy it for any r each of the two expressions in parentheses to be zero.Set the second parentheses equal to zero and solve for a0.

Set the first parentheses equal to zero and solve for E.

Both equal to the Bohr result.

Page 10: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Quantum Numbers• The appropriate boundary conditions to the radial and

angular equations leads to the following restrictions on the quantum numbers ℓ and mℓ:

– ℓ = 0, 1, 2, 3, . . .

– mℓ = −ℓ, −ℓ + 1, . . . , −2, −1, 0, 1, 2, . ℓ . , ℓ − 1, ℓ

– |mℓ| ≤ ℓ and ℓ < 0.

• The predicted energy level is

Page 11: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Hydrogen Atom Radial Wave Functions

• First few radial wave functions Rnℓ

• Subscripts on R specify the values of n and ℓ.

Page 12: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Solution of the Angular and Azimuthal Equations

• The solutions for azimuthal equation are .

• Solutions to the angular and azimuthal equations are linked because both have mℓ.

• Group these solutions together into functions.

---- spherical harmonics

Page 13: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

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

Page 14: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Normalized Spherical Harmonics

Page 15: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Table 8-2, p.269

Page 16: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Table 8-3, p.269

Page 17: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Probability Distribution Functions• We must use 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 dτis .

Page 18: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Probability Distribution Functions• The differential volume element in spherical polar coordinates

is

Therefore,

• We are only interested in the radial dependence.

• The radial probability density is P(r) = r2|R(r)|2 and it depends only on n and l.

Page 19: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos
Page 20: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Fig. 8-9, p.282

2 2( ) 4P r dr r dr

Isotropic States only

l=0

Page 21: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Fig. 8-10a, p.283

2 2

0

0

0

( ) 4

1 ( )

( ) ( )

( ) (3 / 2) o

P r r

P r dr

f f r P r dr

r rP r dr a

Average vs. most probable distance

Page 22: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Fig. 8-10, p.283

Page 23: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos
Page 24: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

R(r) and P(r) for the lowest-lying states of the hydrogen atom.

Probability Distribution Functions

Page 25: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Table 8-5, p.280

Page 26: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Fig. 8-11b, p.285

Page 27: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Fig. 8-11c, p.285

l=2

Page 28: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Fig. 8-12, p.286

Probability Densities

Symmetric about z-axis

Page 29: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos
Page 30: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

3: Quantum NumbersThe three quantum numbers:

– n Principal quantum number– ℓ Orbital angular momentum quantum number

– mℓ Magnetic quantum number

The boundary conditions:– n = 1, 2, 3, 4, . . . Integer– ℓ = 0, 1, 2, 3, . . . , n − 1 Integer

– mℓ = −ℓ, −ℓ + 1, . . . , 0, 1, . . . , ℓ − 1, ℓ Integer

The restrictions for quantum numbers:– n > 0– ℓ < n

– |mℓ| ≤ ℓ

Page 31: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Principal Quantum Number n• It results from the solution of R(r) in because R(r) includes

the potential energy V(r).

The result for this quantized energy is

• The negative means the energy E indicates that the electron and proton are bound together.

Page 32: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Orbital Angular Momentum Quantum Number ℓ

• It is associated with the R(r) and f(θ) parts of the wave function.

• Classically, the orbital angular momentum with L = mvorbitalr.

• ℓ is related to L by .

• In an ℓ = 0 state, .

It disagrees with Bohr’s semiclassical “planetary” model of electrons orbiting a nucleus L = nħ.

Page 33: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

0,1,2, 1n l K0,1,2, 1n l K

,3,2,1n ,3,2,1n The allowed energy levels are quantized much like or particle in a box. Since the energy level decreases a the square of n, these levels get closer together as n gets larger.

Page 34: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos
Page 35: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos
Page 36: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Chemical properties of an atom are determined by the least tightly bound electrons.

Factors:

•Occupancy of subshell

•Energy separation between the subshell and the next higher subshell.

Page 37: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Pauli principle and Minimum Energy Principle

Page 38: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

• He Z=2, n=1, l=0, m=0.

• Two electron with opposite spin

• Zero angular momentum

• High ionization energy 54.4 eV

• Inert2

213.6 4 13.6 54.4

ZE x eV

n

Page 39: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

• Li Z=3, n=1 full, go to n=2, L-shell

• Bigger atom, 4 times ao (~n2)

• Nuclear charge partially screened by n=1 electrons

• Low ionization potential

• Energy of outer electrons21

21.1 1.2

kZ eE

rZ

Page 40: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Fig. 9-15, p.321

Hund’s RuleUnpairedspins

Page 41: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Table 9-2a, p.322

Page 42: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Table 9-2b, p.323

Page 43: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos
Page 44: LECTURE 21 THE HYDROGEN AND HYDROGENIC ATOMS PHYSICS 420 SPRING 2006 Dennis Papadopoulos

Fig. 9-16, p.324