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Angular Momentum

PropertyLinear MomentumAngular Momentum
Physical natureMotion along a straight lineRotation about an axis
Vector formp⃗=mv⃗\vec{p} = m\vec{v}L⃗=r⃗×p⃗\vec{L} = \vec{r} \times \vec{p}
Effective massmmI=mr2I = m r^2
Velocityvvω=vr\omega=\frac{v}{r}
Magnitude (scalar form)∣p⃗∣=mv\mid\vec{p}\mid = m v∣L⃗∣=Iω\mid\vec{L}\mid = I \omega
Kinetic energyEk=p22mE_k = \dfrac{p^2}{2m}Erot=L22IE_\text{rot} = \dfrac{L^2}{2I}
Quantum operatorp^x=−iℏ∂∂x\hat{p}_x = -i\hbar\dfrac{\partial}{\partial x}L^x=y^p^z−z^p^y\hat{L}_x = \hat{y}\hat{p}_z - \hat{z}\hat{p}_y
Conservation lawConserved if no net external force actsConserved if no net external torque acts
Conservation condition∑F⃗ext=0\sum \vec{F}_\text{ext} = 0∑τ⃗ext=0\sum \vec{\tau}_\text{ext} = 0

Conservation of momentum is due to symmetry

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Figure 1:Emmy Noether, a German mathematician whose first and second theorems are fundamental to mathematical physics. See more about her here.

Classical angular momentum

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Figure 2:Classical angular momentum, a vector given by the cross product of position and linear momentum. Its direction follows the right-hand rule.

L⃗=r⃗×p⃗=∣i⃗j⃗k⃗xyzpxpypz∣=(ypz−zpy)i⃗+(zpx−xpz)j⃗+(xpy−ypx)k⃗{\vec{L} = \vec{r}\times\vec{p} = \begin{vmatrix} \vec{i} & \vec{j} & \vec{k}\\ x & y & z\\ p_x & p_y & p_z\\ \end{vmatrix}= \left(yp_z - zp_y\right)\vec{i} + \left(zp_x - xp_z\right)\vec{j} + \left(xp_y - yp_x\right)\vec{k}}

Classical picture: Rotating dumbbell

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Figure 3:Conservation of angular momentum: with no external torque, total angular momentum stays constant, so lowering the moment of inertia speeds up rotation and raising it slows rotation down.

K=m1v122+m2v222=m1r12+m2r222ω2K=\frac{m_1 v_1^2}{2}+\frac{m_2 v_2^2}{2}=\frac{m_1 r_1^2+m_2 r^2_2}{2}\omega^2
K=Iω22=L22IK=\frac{I \omega^2}{2}=\frac{L^2}{2I}
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Figure 4:Angular momentum conservation

Spherical coordinates

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Figure 5:The spherical coordinate system, defined by radial coordinate rr, azimuthal angle ϕ\phi, and polar angle θ\theta.

Laplacian

Cartesian
Polar
∇2=∂2∂x2+∂2∂y2+∂2∂z2\nabla^2 = \frac{{\partial^2}}{{\partial x^2}} + \frac{{\partial^2}}{{\partial y^2}} + \frac{{\partial^2}}{{\partial z^2}}

Quantum angular momentum

Cartesian
Polar
L^x=−iℏ(y∂∂z−z∂∂y){\hat{L}_x = -i\hbar\left(y\frac{\partial}{\partial z} - z\frac{\partial}{\partial y}\right)}
L^y=−iℏ(z∂∂x−x∂∂z){\hat{L}_y = -i\hbar\left(z\frac{\partial}{\partial x} - x\frac{\partial}{\partial z}\right)}
L^z=−iℏ(x∂∂y−y∂∂x){\hat{L}_z = -i\hbar\left(x\frac{\partial}{\partial y} - y\frac{\partial}{\partial x}\right)}
L^2=Lx^2+Ly^2+Lz^2\hat{L}^2=\hat{L_x}^2+\hat{L_y}^2+\hat{L_z}^2

Components of angular momentum do not commute!

Eigenfunctions and eigenvalues of LL and LzL_z

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Figure 6:Angular momentum is quantized. Its magnitude can take specific values dictated by ll. Projections of angular momentum are also quantized and can take specific discrete values dictated by mm which can take 2l+12l+1 values never exceeding ll.

Spherical harmonics

Ylm(θ,ϕ) Y_{lm}(\theta, \phi) ExpressionColatitudinal NodesAzimuthal Nodes
Y00 Y_{00} 14π \frac{1}{\sqrt{4\pi}} 00
Y10 Y_{10} 34πcos⁡(θ) \sqrt{\frac{3}{4\pi}} \cos(\theta) 1 (equatorial)0
Y1−1 Y_{1-1} 34πsin⁡(θ)e−iϕ \sqrt{\frac{3}{4\pi}} \sin(\theta) e^{-i\phi} 01
Y20 Y_{20} 516π(3cos⁡2(θ)−1) \sqrt{\frac{5}{16\pi}} (3\cos^2(\theta) - 1) 2 (colatitudinal rings)0
Y2−1 Y_{2-1} 154πsin⁡(θ)cos⁡(θ)e−iϕ \sqrt{\frac{15}{4\pi}} \sin(\theta) \cos(\theta) e^{-i\phi} 1 (equatorial)1
Y2−2 Y_{2-2} 154πsin⁡2(θ)e−2iϕ \sqrt{\frac{15}{4\pi}} \sin^2(\theta) e^{-2i\phi} 02

Nodes of Spherical Harmonics

The nodal structure of spherical harmonics is influenced by both the degree l l and the order mm, defining the number and type of nodes as follows:

  1. Colatitudinal Nodes (Polar Nodes): The variable θ \theta defines “polar” nodes, which appear as circular bands around the sphere. The expression in cos⁡(θ) \cos(\theta) or sin⁡(θ) \sin(\theta) creates colatitudinal nodes:

    • For example, Y10 Y_{10} with cos⁡(θ) \cos(\theta) has a single node at θ=π/2 \theta = \pi/2 , creating an equatorial node.

    • Y20 Y_{20} , with (3cos⁡2(θ)−1) (3\cos^2(\theta) - 1) , introduces two polar nodes, dividing the sphere into three regions along the colatitude.

  2. Azimuthal Nodes (Longitudinal Nodes): The variable ϕ \phi defines “azimuthal” nodes due to the terms eimϕe^{im\phi}, which create lines of longitude where the function changes phase. The number of azimuthal nodes is determined by ∣m∣ |m| :

    • If m=0 m = 0 , there are no azimuthal nodes, as seen in Y00 Y_{00} and Y10 Y_{10} .

    • For m=±1 m = \pm 1 , a single azimuthal node occurs (e.g., Y1−1 Y_{1-1} , Y2−1 Y_{2-1} ), and for m=±2 m = \pm 2 , two azimuthal nodes appear (e.g., Y2−2 Y_{2-2} ).

  3. Total Nodes: equal to the sum of the polar and longitudinal nodes, and exactly equal to ll. For instance, l=0l=0 has no nodes and l=4l=4 has four nodes.

Orthogonality of Spherical Harmonics

The orthogonality of spherical harmonics is expressed as:

⟨l′,m′∣l,m⟩=δl,l′δm,m′\langle l', m'| l, m \rangle = \delta_{l,l'}\delta_{m,m'}

This orthogonality condition can be explicitly written as:

∫0π∫02πYl′m′∗(θ,ϕ)Ylm(θ,ϕ)sin⁡(θ) dθ dϕ=δl,l′δm,m′\int_0^{\pi} \int_0^{2\pi} Y_{l'}^{m'*}(\theta, \phi) Y_l^m(\theta, \phi) \sin(\theta) \, d\theta \, d\phi = \delta_{l,l'}\delta_{m,m'}
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Orthogonality Tests:
∫ Y(1,0) * Y(1,0)* = 1.00000 (should be close to 1)
∫ Y(1,0) * Y(1,1)* = 0.00000 (should be close to 0)
∫ Y(1,1) * Y(2,1)* = 0.00000 (should be close to 0)
∫ Y(2,1) * Y(2,1)* = 1.00000 (should be close to 1)
∫ Y(2,0) * Y(2,-1)* = -0.00000 (should be close to 0)

Plotting Spherical Harmonics

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l=1l=1 harmonics

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l=2l=2 harmonics

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Total number of nodes = ll

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Alternative visualizations of Spherical Harmonics

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Learn More about Spherical Harmonics