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Quantisation of Angular Momentum - Explained (Visually)

19:05EnglishBy For the Love of PhysicsTranscribed May 26, 2026
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0:00

The old model of the atom, an electron

0:02

revolving around a nucleus, had one

0:04

obvious thing, angular momentum. And

0:07

this is a very important physical

0:09

quantity because for rotating systems,

0:12

angular momentum is conserved in nature.

0:15

But now, in modern physics, this

0:17

electron revolving around a nucleus has

0:19

been replaced by a stationary electron

0:23

cloud model of the atom.

0:25

This is because quantum mechanics can

0:27

predict the probability density of where

0:29

the electron is most likely to be found

0:31

in the atom. Now, in this model, the

0:34

angular momentum quantity may not be

0:35

very obvious, but it is still

0:37

ever-present. And more importantly, in

0:39

atomic physics, it is quantized.

0:42

So, the question is what is quantization

0:45

of angular momentum?

0:46

You see, in the classical model of a

0:48

particle revolving around a nucleus,

0:50

there is no restriction on the magnitude

0:53

or the direction of the angular

0:55

momentum. Depending upon the speed,

0:57

radial distance, or the plane of

0:59

revolution, the angular momentum vector

1:01

can take any direction or magnitude in

1:04

classical physics.

1:06

But that is not true in quantum physics

1:09

because when we talk about quantum

1:11

systems, angular momentum can only take

1:14

those values which is allowed by the

1:16

theory of quantum mechanics.

1:18

In fact, the magnitude and the direction

1:20

of angular momentum can only take very

1:23

specific [music] values,

1:25

which is known as the quantization of

1:27

angular momentum.

1:33

You see, in the quantum mechanical

1:35

framework, this quantity is associated

1:37

with four distinct operators that can

1:39

give us some meaningful information

1:40

about the system. So, Lx, for example,

1:43

is the operator associated with the x

1:46

component of angular momentum vector. Ly

1:49

and Lz are the operators corresponding

1:51

to the y and z component of this angular

1:53

momentum vector. When we combine these

1:55

operators to create the magnitude, we

1:58

end up getting the L squared operator.

2:00

Now, in theory, together these operators

2:02

can give us all the information about

2:04

angular momentum vector, but the problem

2:07

is in quantum mechanics, we have

2:08

something called the uncertainty

2:10

principle.

2:12

You must have all heard of the position

2:14

and the linear momentum uncertainty

2:15

principle that for a moving particle,

2:18

you cannot measure the position and the

2:20

linear velocity at any given point in

2:22

time simultaneously with absolute

2:25

accuracy. Similar uncertainty

2:26

relationships also exist for the angular

2:29

momentum, which says that you cannot

2:30

measure the components of angular

2:32

momentum LX, LY, and LZ simultaneously

2:37

with absolute accuracy for a given

2:39

system. In fact, there is a limit given

2:42

by these uncertainty relations, beyond

2:44

which you cannot accurately measure them

2:47

in a given system. Now, these kinds of

2:49

uncertainty relations goes back to

2:52

commutator algebra of the quantum

2:54

mechanical framework. You see, whenever

2:55

two operators do not commute, they have

2:58

a corresponding uncertainty relationship

3:00

for them. And this is true for LX, LY,

3:03

and LZ. However, what is interesting is

3:07

that this is not necessarily true for L

3:09

squared operator. So, if we find the L

3:12

squared commutator with either LX or LY

3:16

or LZ separately, then we find that they

3:19

do commute, which means we can measure L

3:23

squared and LX together or L squared and

3:27

LY together or L squared and LZ

3:31

together. So, that means we have to make

3:33

a choice. And by convention in the

3:35

physics community, we choose L squared

3:39

and LZ representation. And therefore,

3:42

the theory of quantum mechanics can give

3:44

us precise information about L squared,

3:47

the magnitude of angular momentum, and

3:50

LZ, the Z component of angular momentum

3:53

for a given system. But, this is an

3:55

information that we can obtain only from

3:57

the wave function solution of the

3:59

system. So, coming to the wave function

4:01

solution, it is a solution of the

4:03

Schrödinger equation when we try to

4:05

solve for central potentials like the

4:07

Coulombic interaction of an atom. And

4:09

because of spherical symmetry, we write

4:11

this wave function in terms of spherical

4:13

coordinates r theta phi. And when we do

4:16

that, the wave function can be written

4:17

in three distinct parts. The radial

4:20

solution, as the name suggests, gives us

4:22

that part of the wave function solution

4:24

which varies with respect to the radial

4:26

distance from the nucleus. While the

4:28

angular solution gives us that part of

4:31

the wave function solution which varies

4:32

as we go from north to south. And the

4:35

azimuthal solution gives us that part of

4:38

the wave function solution as you go

4:39

from west to east along the equator or

4:43

along a latitude. And the various

4:45

boundary conditions associated with

4:47

these solutions lead to three distinct

4:50

quantum numbers n, l, and m. Now, n is

4:54

related to energy of the system, so we

4:56

are not concerned with that in today's

4:57

video. L and m, however, are very much

5:01

responsible for the angular momentum of

5:03

the system. In fact, if we combine the

5:06

angular solution and the azimuthal

5:08

solution, we get what is called

5:10

spherical harmonics which are

5:12

effectively the eigen states of angular

5:15

momentum vector. So, if we apply these

5:17

operators L squared and LZ onto the

5:20

spherical harmonics, we get two very

5:23

beautiful solutions. In fact, these

5:25

equations are known as the eigenvalue

5:28

equations for angular momentum operator.

5:30

And these solutions, or the eigenvalues

5:33

corresponding to L squared and LZ, they

5:36

depend on the quantum numbers L and M.

5:39

I'll try to show you an intuitive way of

5:41

how these quantum numbers are decided.

5:43

So, first the azimuthal solutions, which

5:45

are nothing but oscillatory solutions

5:47

given by e to the power i m phi. Phi

5:51

being the angle from west to east if you

5:54

go along a latitude. Now, we can look at

5:56

the behavior of cos m phi which is

5:58

similar to that of sin m phi although

6:00

separated by a phase difference of pi by

6:02

2. So, for m is equal to 2, you end up

6:05

getting this kind of an oscillatory

6:07

solution. Now, these kinds of solutions

6:09

are easy to understand because we are

6:11

very much used to oscillatory solutions

6:13

along the x-axis. But, what if I try to

6:16

represent the same oscillation in a

6:18

polar plot because that is a much better

6:21

representation of the azimuthal nature

6:23

of the solutions. So, in this plot, the

6:26

radial distance represents the

6:27

functional value of the oscillation and

6:30

wherever the function goes to zero, the

6:32

radius becomes zero and the plot looks

6:35

something like this. I can do the same

6:37

for other values of m, m equals 0, 1, 2,

6:42

3 and we end up getting more and more

6:44

number of oscillations and as a result,

6:47

more and more lobes in the polar plot.

6:50

So, this gives you a very beautiful

6:52

visual idea of what m really represents.

6:57

It represents the oscillations of the

6:59

wave function around the azimuthal

7:01

direction and with greater and greater

7:03

value of m, you end up getting more

7:06

oscillations which by the way

7:07

corresponds to a greater value of

7:10

angular momentum because with more

7:12

oscillations, the effective wavelength

7:14

decreases and we know that wavelength

7:16

and angular momentum or momentum in

7:18

general have an inverse proportionality.

7:20

But, you may ask why integral values of

7:23

m? This is because when we undergo one

7:26

complete revolution, I want to come back

7:28

to the same point with the same value of

7:31

the function. And if I try to do that

7:33

for let's suppose m is equal to 2.5,

7:36

then that doesn't happen.

7:38

If you notice the polar plot, the wave

7:41

does not close in on itself. And these

7:44

kinds of values are therefore not

7:46

allowed. The wave function must, at the

7:48

end of the day, have the same value at

7:50

the same location, even though you took

7:53

one complete revolution and came back to

7:55

the same point. So, this boundary

7:57

condition effectively restricts the

7:59

value of the quantum number m to only

8:02

integral values. You can have 0 1 2 3 4

8:06

like that, or the negative values,

8:08

because even the negative values are

8:09

allowed. The positive and the negative

8:11

of m simply changes the direction of the

8:14

angular momentum vector.

8:17

Now, if we come to the angular

8:18

solutions, that part of the Schrödinger

8:21

equation which is responsible for theta,

8:24

then we effectively get something called

8:26

associated Legendre functions. The

8:29

associated Legendre functions gives us

8:32

how the wave function varies as we go

8:36

from north to south pole.

8:39

I know the mathematical expressions are

8:40

quite complicated here, but notice a few

8:43

essential details. The Legendre

8:45

functions are mth order derivatives of

8:48

what is known as a Legendre polynomial.

8:51

The Legendre polynomial is given by the

8:53

Rodrigues formula. Students who are

8:55

familiar with mathematical physics may

8:57

have seen these expressions before. Now,

8:59

the way to solve this kind of a

9:01

differential equation corresponding to

9:02

theta is to essentially employ what is

9:05

known as the power series method. But

9:08

the power series method does not really

9:10

give us finite solutions for all cases.

9:12

It only gives us finite solutions when

9:15

the power series terminates after a

9:18

particular series number. So, the short

9:20

answer is to get a finite wave function

9:23

solution, we must terminate the power

9:26

series solution that leads to

9:29

very specific integral values of l. l

9:33

essentially represents the number of

9:35

terms present in the power series

9:37

solution. So, L therefore is now

9:39

restricted to values like 0 1 2 3 like

9:42

that. But, if you also look at the

9:43

connection between associated Legendre

9:46

function and the Rodrigues formula, the

9:47

Legendre polynomial is a polynomial of

9:50

the order of L. And if you take a

9:52

derivative of a polynomial of the order

9:54

of L, you cannot do the derivative more

9:57

than L number of times because if you do

9:59

that, you'll end up getting zero. Which

10:01

means that M is now therefore restricted

10:04

to all the values less than L. So, for

10:07

example, if L equals 0, then M can only

10:09

have a zero value. But, if L is equal to

10:12

1, M can have values of -1 0 or +1. And

10:16

then you can take it forward for L is

10:17

equal to 2 3 and further. So, given

10:20

these quantum numbers, I can write down

10:22

the mathematical expressions for each of

10:24

them.

10:25

And I can in fact represent them in a

10:27

normal 2D plane graph. You can clearly

10:30

see the oscillatory nature of these

10:32

solutions. What's even interesting is if

10:35

I try to plot them in a polar plot with

10:38

respect to theta, then suddenly we have

10:40

these beautiful diagrams, these lobe and

10:43

petal-like shapes. In fact, if we

10:45

combine the azimuthal solutions that you

10:48

saw earlier and these associated

10:50

Legendre polynomial plots, we

10:53

effectively get an idea about the shape

10:56

of the orbitals and why orbitals have

10:58

those unique shapes of lobes and petals

11:01

etc. But, a detailed discussion on that

11:03

is probably a topic for the next video.

11:05

Today, I want to focus on angular

11:07

momentum.

11:11

So, coming back to those equations, we

11:13

can now see how the various values of L

11:15

and M quantum number influences what is

11:19

going to be the angular momentum

11:20

magnitude and the angular momentum

11:22

direction.

11:24

So, for example, if we take L is equal

11:26

to 0, the S orbital, it's clear that the

11:29

magnitude of angular momentum is zero

11:32

and the Z component of angular momentum

11:33

is zero.

11:35

That means the S orbital has no angular

11:39

momentum at all.

11:43

And this is kind of the easiest example

11:45

to understand. But if we go to L is

11:47

equal to 1, what happens then? Here, the

11:51

magnitude of angular momentum is root 2

11:54

H cut. But the Z component can have

11:56

three distinct values of minus H cut,

11:59

zero, and plus H cut. How do we

12:01

represent them in a diagram, for

12:03

example?

12:05

It can only have a fixed length, so it

12:08

can only be found on the surface of a

12:10

sphere. Any value above that or any

12:14

value below that is not allowed. So for

12:17

a P orbital, the angular momentum vector

12:20

will lie only on the surface of the

12:22

sphere. Now, what if we include the Z

12:24

component? The Z component is

12:26

effectively the component of this L

12:29

vector onto the Z axis. Now, all the

12:32

angular momentum vectors that will have

12:34

a very specific Z component lies along

12:37

the conical surface, which intersects

12:39

with the sphere and creates the circular

12:42

shape. Now, this diagram visually

12:45

demonstrates beautifully

12:47

what are the magnitudes and the

12:49

directions of the angular momentum

12:51

vector for the P orbital. As far as

12:53

magnitude is concerned, only one value

12:56

is possible, root 2 H cut. No other

12:58

value is allowed. But as far as the

13:00

direction is concerned, the angular

13:02

momentum vector can lie on any one of

13:04

these conical or circular surfaces. Now,

13:07

at this point in time, there are a few

13:09

questions that may have come up in your

13:11

mind. First of all, when we earlier

13:13

talked about the convention of L squared

13:16

and L Z, I specifically mentioned that

13:18

these are the only two quantities that

13:20

we can precisely know. But from the

13:23

diagram, you may say that wait, the

13:25

choice of coordinate axis is ours,

13:28

right? So, why don't we choose the Z

13:30

axis to be along the direction of the

13:33

angular momentum vector? Now, if you

13:34

notice, if I do make that choice, if I

13:37

choose the Z axis to be the in the

13:40

direction of the angular momentum

13:41

vector, then Ly and Lz will become

13:45

precisely equal to zero. Now, that is

13:48

not allowed in quantum mechanics. It

13:50

goes back to the uncertainty principle.

13:52

So, therefore, this is the only

13:53

reasonable explanation. And even by the

13:56

way here, as the angular momentum vector

13:58

can take any orientation on the conical

14:01

shape, if you look at its rotation at

14:04

each point along the circle, it projects

14:07

different values on the XY plane, which

14:09

is perpendicular to the Z axis. And

14:11

because it projects different values on

14:13

the XY plane, the components of Lx and

14:16

Ly is constantly changing. In fact, the

14:19

average of Lx and average of Ly comes

14:22

out to be zero because they can take

14:24

positive and negative values here. So,

14:26

the theory can only tell us what Lz and

14:30

L magnitude is. It cannot tell us what

14:33

Lx and Ly are. And one more

14:35

misconception that may arise here in

14:38

this diagram is is the angular momentum

14:40

vector precessing around the Z axis?

14:43

Even though I've shown the animation in

14:45

this manner to create a visual

14:47

representation, there is no precession

14:50

involved. If I look at all these three

14:52

distinct cases separately, what these

14:56

shapes actually mean is that the angular

14:59

momentum vector can take any direction

15:01

lying on the inverted cone, the circle,

15:04

and the cone. So, even specifying the

15:06

angular momentum vector with an arrow is

15:08

kind of misleading because it can be

15:11

anywhere in this particular shape. It is

15:14

only the magnitude and the Z component

15:16

that we are pretty much sure of. The

15:19

exact direction is still kind of smeared

15:23

along the cone or along the circular

15:26

surface.

15:27

We can do the same thing for D orbital

15:29

for quantum number L equals to two.

15:33

If I do that, we will see that the

15:34

magnitude here comes out to be root six

15:37

H cut and the possible Z components

15:39

comes out to be plus two H cut, plus H

15:42

cut, zero, minus H cut and minus two H

15:44

cut.

15:45

In a very similar manner, we can

15:47

represent them in this beautiful

15:48

diagram. The angular vector has a

15:51

magnitude which is root six H cut, which

15:53

is fixed by the radius of a sphere. And

15:57

their Z components leads to these kinds

15:59

of conical and circular surfaces where

16:02

the angular momentum vector is

16:03

effectively smeared across those

16:05

surfaces.

16:15

Now, till this point in time, we have

16:17

only talked about the orbital angular

16:19

momentum of an electron in the presence

16:22

of a nucleus. However, the electron also

16:25

has its own distinct spin angular

16:28

momentum. This is an intrinsic property

16:31

of the angular momentum that an electron

16:33

has and as it turns out, the eigen value

16:36

equations for the spin operator is also

16:38

somewhat similar.

16:41

The only difference is that the quantum

16:42

number S can only take values of half.

16:46

So, if we represent that visually, we

16:48

get this kind of a shape.

16:53

The electron's intrinsic angular

16:55

momentum can only have plus H cross by

16:58

two in the positive Z axis or minus H

17:01

cross by two in the negative Z [music]

17:03

axis.

17:07

Now, this is something that is verified

17:09

by what is known as the Stern-Gerlach

17:11

experiment. So, in the Stern-Gerlach

17:13

experiment, we pass a beam of electrons

17:17

through a non-uniform magnetic field.

17:20

And when we do that, because the

17:21

non-uniform magnetic field interacts

17:24

slightly differently with the spin up

17:26

and the spin down, so the beam splits

17:28

into two parts. And this result is an

17:30

actual proof that the electron has an

17:33

intrinsic spin. Now, we can perform a

17:35

similar experiment for the orbital

17:36

angular momentum case. So, for example,

17:38

if we take S orbital, L is equal to

17:41

zero, you'll end up getting a scenario

17:42

in which the beam does not split because

17:44

the S orbital has no angular momentum in

17:46

the first place. But, for L is equal to

17:48

one, there are three distinct

17:49

orientations, so the beam will split

17:51

into three spots. While for L is equal

17:55

to two, there are five distinct

17:56

orientations, so the beam will split

17:58

into five distinct spots. Now, this is

18:00

something that I've only shown for a

18:02

visual understanding perspective because

18:05

the Stern-Gerlach experiment is a little

18:06

bit hard to perform for orbital angular

18:09

momentum because usually in atoms, the

18:11

orbital angular momentum and the spin

18:13

angular momentum couple together to

18:16

create a sort of an effective angular

18:18

momentum of the system.

18:20

Nonetheless, both the spin angular

18:22

momentum and the orbital angular

18:24

momentum in an atom are quantized. They

18:27

can only have very specific magnitudes

18:30

and specific directions, which is

18:32

allowed by the quantum mechanical

18:33

theory. And this is one of the ways in

18:35

which a quantum system is so vastly

18:38

different from our classical

18:40

understanding of angular momentum. I

18:42

have made a lot of effort in creating

18:45

these visualizations to give you a

18:47

better understanding of the topic. If

18:49

this is something that you are

18:50

interested in, then please make a

18:51

comment in the video and I'll try to

18:53

create more such animated and visual

18:56

perspective of understanding various

18:58

topics in physics. I'm Divyendu Das.

19:00

This is For the Love of Physics. Thank

19:01

you so much. Take care. Bye-bye.

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