This page is a drill . The parent note built the machinery; here we point it at every kind of case you can meet, so no exam or homework question is a stranger. We reuse only three tools, all defined in the parent:
Recall The three tools we lean on (from the parent)
Conjugate momentum p i ≡ ∂ q ˙ i ∂ L — the "L -slope in the direction of the velocity q ˙ i ".
Cyclic coordinate : if L has no q k in it, then ∂ q k ∂ L = 0 and p k is frozen.
Noether charge : for a symmetry q i → q i + ϵ δ q i with δ L = ϵ d t d F , the constant is
Q = ∑ i p i δ q i − F .
When F = 0 this is just ∑ i p i δ q i .
Recall Two more results we will quote (also from the parent)
Euler–Lagrange equation (the equation of motion for each coordinate):
d t d ( ∂ q ˙ i ∂ L ) − ∂ q i ∂ L = 0 ⟺ d t d p i = ∂ q i ∂ L .
Read the right-hand form as: "the rate of change of a momentum equals how strongly L leans on that coordinate." If L does not lean on q i (the coordinate is absent), the momentum cannot change.
Energy function (the time-translation charge) : the conserved quantity of t → t + ϵ is
h = ∑ i p i q ˙ i − L ,
and its rate obeys the identity d t d h = − ∂ t ∂ L . So h is frozen exactly when L has no explicit time .
Everything below feeds off the vault chain Lagrangian Mechanics → Euler-Lagrange Equation → the big three Conservation of Energy , Conservation of Momentum , Angular Momentum .
Think of Noether problems as a grid. Each column is a type of symmetry ; each row is a type of trap (a sign, a zero, a degenerate or limiting case). Our job is to hit every cell at least once.
Cell
What makes it tricky
Which example hits it
A. Pure cyclic coordinate
spot "L has no q " instantly
Ex 1
B. Symmetry present but L looks like it depends on the coord
need δ L = 0 check, not eyeballing
Ex 2
C. Rotation → angular momentum, sign of the cross product
getting δ r = n ^ × r right, sign of L z
Ex 3
D. Symmetry broken → NOT conserved (degenerate case)
explicit time / position dependence kills conservation
Ex 4
E. Boundary term F = 0 (Galilean boost)
must subtract F , else wrong charge
Ex 5
F. Canonical p = m v (velocity-dependent term)
charged particle in a field
Ex 6
G. Limiting / zero input
what happens as a parameter → 0
Ex 7
H. Real-world word problem
translate a physical story into a symmetry
Ex 8
I. Exam-style twist (partial symmetry)
only one component is conserved
Ex 9
J. Pathological / edge cases
non-invertible L , singular coordinate maps
Ex 10
Ten examples for ten cells. Read the Forecast and guess before you scroll.
Worked example Free particle in polar coordinates
A free particle in a plane, written in polar coordinates ( r , ϕ ) , has
L = 2 1 m ( r ˙ 2 + r 2 ϕ ˙ 2 ) .
Find a conserved quantity by inspection.
Forecast: Which coordinate is missing from L ? Guess the frozen quantity before reading.
Scan L for a missing coordinate. L contains r , r ˙ , ϕ ˙ — but no bare ϕ . So ϕ is cyclic.
Why this step? Apply the Euler–Lagrange equation to ϕ : d t d p ϕ = ∂ ϕ ∂ L . Since ϕ never appears in L , the right side is 0 , so d t d p ϕ = 0 . Spotting the missing coordinate is spotting the symmetry (rotational).
Compute the conjugate momentum p ϕ .
p ϕ = ∂ ϕ ˙ ∂ L = m r 2 ϕ ˙ .
Why this step? The Noether charge for the shift ϕ → ϕ + ϵ is p ϕ ⋅ δ ϕ with δ ϕ = 1 , i.e. just p ϕ .
State the conservation law. m r 2 ϕ ˙ = const — this is the angular momentum L z .
Verify: Units: kg ⋅ m 2 ⋅ s − 1 = J⋅s , correct for angular momentum. Sanity: even though r does appear in L , r is not cyclic (there is an r 2 ϕ ˙ 2 term), so p r is not conserved — only p ϕ . That asymmetry is the whole point.
Worked example Two particles joined by a spring
L = 2 1 m x ˙ 1 2 + 2 1 m x ˙ 2 2 − 2 1 k ( x 1 − x 2 ) 2 .
Both coordinates x 1 and x 2 appear in L . Is anything conserved?
Forecast: Neither coordinate is cyclic on its own. Does that mean nothing is conserved? Guess.
Try the translation symmetry δ x 1 = 1 , δ x 2 = 1 (shift both particles equally).
Why this step? The potential depends only on the difference x 1 − x 2 . Shifting both by the same amount leaves x 1 − x 2 untouched — that is the symmetry, even though each coordinate individually appears.
Check δ L = 0 .
δ L = ∂ x 1 ∂ L ( 1 ) + ∂ x 2 ∂ L ( 1 ) = − k ( x 1 − x 2 ) ( 1 ) − k ( x 2 − x 1 ) ( 1 ) = 0. ✓
Why this step? Noether needs δ L = 0 (here F = 0 ). Eyeballing "x 1 appears" would wrongly conclude no symmetry; the honest check catches it.
Build the charge Q = p 1 δ x 1 + p 2 δ x 2 = m x ˙ 1 + m x ˙ 2 = P total .
Verify: d t d P = m x ¨ 1 + m x ¨ 2 . Equations of motion: m x ¨ 1 = − k ( x 1 − x 2 ) , m x ¨ 2 = − k ( x 2 − x 1 ) = + k ( x 1 − x 2 ) . Sum = 0 . So total momentum is genuinely constant. ✓ (The internal spring cannot push the center of mass — Newton's third law reborn as a symmetry.)
Worked example Central-force particle in 2D
L = 2 1 m ( x ˙ 2 + y ˙ 2 ) − V ( x 2 + y 2 ) .
The potential depends only on distance r = x 2 + y 2 . Find the conserved charge from rotational symmetry, being careful with signs.
Forecast: Will the charge be + ( x y ˙ − y x ˙ ) or − ( x y ˙ − y x ˙ ) ? Guess the sign now.
What the figure shows: the dashed lavender circle is one orbit of radius r ; the mint dots are sample points on it; each coral arrow is that point's displacement δ r under a tiny rotation. Notice every arrow points along the circle, in the counter-clockwise sense, and is perpendicular to the slate radius line — that is the geometric meaning of δ r = z ^ × r = ( − y , x ) .
Write the infinitesimal rotation. A rotation by small angle ϵ about z ^ sends r → R r , giving δ r = z ^ × r . In components (each coral arrow in the figure):
δ x = − y , δ y = + x .
Why this step? We need the shape δ q i of the symmetry. The cross product z ^ × r = ( − y , x ) is the velocity of a point being spun counter-clockwise — that is what "rotate the whole picture" means locally.
Check δ L = 0 . Kinetic part: δ x ˙ = − y ˙ , δ y ˙ = x ˙ , so m ( x ˙ δ x ˙ + y ˙ δ y ˙ ) = m ( − x ˙ y ˙ + y ˙ x ˙ ) = 0 . Potential part: r is unchanged by rotation, so δ V = 0 . Total δ L = 0 . ✓
Why this step? Rotational invariance is only real if both pieces are invariant. Distance-only potentials pass automatically.
Build the charge.
Q = p x δ x + p y δ y = m x ˙ ( − y ) + m y ˙ ( x ) = m ( x y ˙ − y x ˙ ) = L z .
So the sign is positive m ( x y ˙ − y x ˙ ) .
Verify: Take a particle at r = ( 1 , 0 ) moving with v = ( 0 , 1 ) (counter-clockwise), m = 1 . Then L z = 1 ⋅ ( 1 ⋅ 1 − 0 ⋅ 0 ) = + 1 > 0 , correctly positive for counter-clockwise motion — matching the arrow direction in the figure. Units kg⋅m 2 / s . ✓
Worked example Driven oscillator — the classic "energy not conserved" trap
L = 2 1 m x ˙ 2 − 2 1 k x 2 + x F 0 cos ( ω t ) .
A spring plus an external push that varies with time . Is energy conserved?
Forecast: Intro physics says "energy is always conserved." Is it here? Guess before checking.
Test time-translation symmetry t → t + ϵ . This is a symmetry only if L has no explicit t .
Why this step? The energy function h = ∑ i p i q ˙ i − L (recalled in the box at the top) is the Noether charge of time-translation , and its rate is d t d h = − ∂ t ∂ L . No time-symmetry ⇒ no reason for h to be frozen.
Look for explicit t . The term x F 0 cos ( ω t ) contains t directly . So ∂ t ∂ L = − x F 0 ω sin ( ω t ) = 0 .
Why this step? This single non-zero partial derivative is the whole verdict.
Compute the actual rate of change of energy. Using the identity from the recall box,
d t d h = − ∂ t ∂ L = + x F 0 ω sin ( ω t ) = 0.
Energy is not conserved: the driver pumps energy in and out.
Verify: Turn the drive off, F 0 = 0 . Then ∂ L / ∂ t = 0 and d h / d t = 0 — energy conservation returns. This is the correct limiting behaviour : the broken symmetry heals exactly when the time-dependent term vanishes. ✓
Worked example Free particle under a velocity boost
L = 2 1 m x ˙ 2 .
Apply the boost x → x + ϵ t (give the whole system a small extra velocity ϵ ). Find the conserved charge — the naive Noether formula will lie unless you include F .
Forecast: Guess: will the naive charge p δ x be conserved by itself, or do we need a correction?
Read off δ x . x → x + ϵ t means δ x = t (and δ x ˙ = 1 , since d t d ( ϵ t ) = ϵ ).
Why this step? The "shape" of a boost grows with time — that is what distinguishes it from a plain shift.
Compute δ L — it is NOT zero.
δ L = ∂ x ˙ ∂ L δ x ˙ = m x ˙ ⋅ 1 = m x ˙ = d t d ( m x ) .
So δ L = d t d F with F = m x .
Why this step? The action changes only by a boundary term, so the symmetry is still valid — but the parent's formula demands we subtract F .
Build the corrected charge.
Q = p δ x − F = ( m x ˙ ) ( t ) − m x = m ( x ˙ t − x ) .
Verify: For a free particle x ˙ = const ⇒ x = x 0 + x ˙ t . Then Q = m ( x ˙ t − x 0 − x ˙ t ) = − m x 0 = const . ✓ It literally encodes the starting position x 0 — the boost symmetry conserves "where the center of mass was at t = 0 ". Had we forgotten F , the naive p δ x = m x ˙ t would grow linearly and be nonsense.
Worked example Charged particle in a uniform magnetic field
With vector potential A x = − 2 1 B y , A y = 2 1 B x (uniform field B z ^ ),
L = 2 1 m ( x ˙ 2 + y ˙ 2 ) + q ( x ˙ A x + y ˙ A y ) = 2 1 m ( x ˙ 2 + y ˙ 2 ) + 2 q B ( x y ˙ − y x ˙ ) .
Find the conserved charge from rotational symmetry — and beware what "p " means.
Forecast: Will the conserved quantity be plain m ( x y ˙ − y x ˙ ) , or something with an extra B -term? Guess.
Check rotation invariance. Under δ x = − y , δ y = x , the kinetic term is invariant (Ex 3) and the term x y ˙ − y x ˙ is itself the z -component of r × v , which is rotation-invariant. So δ L = 0 . ✓
Why this step? Uniform field along z ^ has full rotational symmetry about z ^ .
Use the canonical momenta, not m x ˙ .
p x = ∂ x ˙ ∂ L = m x ˙ − 2 q B y , p y = ∂ y ˙ ∂ L = m y ˙ + 2 q B x .
Why this step? Mistake 2 in the parent: the Noether charge uses p i = ∂ L / ∂ q ˙ i , which here carries a vector-potential piece.
Assemble the charge.
Q = p x δ x + p y δ y = ( m x ˙ − 2 q B y ) ( − y ) + ( m y ˙ + 2 q B x ) ( x )
= m ( x y ˙ − y x ˙ ) + 2 q B ( x 2 + y 2 ) .
Verify: Set q = 0 : Q → m ( x y ˙ − y x ˙ ) = L z , the ordinary angular momentum — correct limit. With B = 0 , the conserved "canonical angular momentum" gains the 2 q B r 2 term, which is why cyclotron orbits have a fixed guiding center. Units: each term is kg⋅m 2 / s (note [ q B ] = kg/s , times m 2 ). ✓
Worked example Cyclic angle in the limit of vanishing torque
A particle in a potential L = 2 1 m ( r ˙ 2 + r 2 ϕ ˙ 2 ) − α ϕ , where α is a small constant "torque" parameter.
Study the conservation of p ϕ as α → 0 .
Forecast: With α = 0 the coordinate ϕ appears in L . Is p ϕ conserved? What happens as α → 0 ?
Test whether ϕ is cyclic. L contains the term − α ϕ , so ∂ ϕ ∂ L = − α = 0 (for α = 0 ). Not cyclic.
Why this step? Any explicit appearance of the coordinate breaks the exact shift symmetry.
Euler–Lagrange for ϕ . Using d t d p ϕ = ∂ ϕ ∂ L ,
d t d p ϕ ( m r 2 ϕ ˙ ) = − α ⇒ d t d p ϕ = − α .
Why this step? This quantifies the breakage: p ϕ drifts at constant rate − α , like a constant applied torque.
Take the limit α → 0 . Then d t d p ϕ → 0 , and p ϕ = m r 2 ϕ ˙ becomes conserved again.
Verify: Integrate: p ϕ ( t ) = p ϕ ( 0 ) − α t . At α = 0 this is a flat line (constant) — the symmetry, and its conservation law, are recovered continuously in the limit. This is the honest way "zero input" behaves: no discontinuity, just the torque switching off. ✓
Worked example Ice-skater pulling in her arms
A skater spins freely (no friction torque). She pulls her arms in, halving her moment of inertia from I 0 to I 0 /2 . Starting angular speed ω 0 = 3 rad/s . What is her final angular speed, and which symmetry guarantees the answer?
Forecast: Guess her final spin rate before doing any algebra.
Identify the symmetry. Ice is frictionless and space is empty around her: nothing in the physics picks out a preferred direction of rotation about the vertical → rotational symmetry about z ^ .
Why this step? Noether: rotational symmetry ⇒ angular momentum L z conserved . This is the law we will use, not "energy" (she does work pulling arms in, so energy is not conserved).
Write L z = I ω = const .
I 0 ω 0 = 2 I 0 ω f .
Why this step? L z = I ω is the rigid-body version of the single-particle Noether charge m r 2 ϕ ˙ from Ex 1, summed over the whole body. Conservation means the value before equals the value after.
Solve for ω f . Cancel I 0 : ω 0 = 2 1 ω f , so
ω f = 2 ω 0 = 2 × 3 = 6 rad/s .
Why this step? Halving the inertia must double the spin to keep the product I ω fixed — the familiar skater speed-up.
Verify: Angular momentum before = I 0 ⋅ 3 = 3 I 0 ; after = 2 I 0 ⋅ 6 = 3 I 0 — equal. ✓ Sanity on energy: K E = 2 1 I ω 2 goes from 2 1 I 0 ( 3 ) 2 = 4.5 I 0 to 2 1 ⋅ 2 I 0 ( 6 ) 2 = 9 I 0 — it doubled , the extra energy supplied by her muscles. Energy not conserved, angular momentum is . That difference is exactly what Noether predicts (only the symmetric quantity is frozen). ✓
Worked example Particle in a uniform gravitational field
L = 2 1 m ( x ˙ 2 + y ˙ 2 + z ˙ 2 ) − m g z , z ^ up .
Which momentum components are conserved, and which are not? (Classic "partial symmetry" trap.)
Forecast: Guess how many of p x , p y , p z are conserved.
What the figure shows: the mint double-arrow is a horizontal shift — sliding the picture left/right does not change the height energy shading (lavender bands), so horizontal translation is a genuine symmetry. The coral vertical double-arrow moves the particle to a different shade of the m g z background, i.e. changes L — so vertical translation is not a symmetry.
Scan each coordinate. L contains z (in − m g z ) but not x or y .
Why this step? Cyclic = "coordinate absent". Only the coordinates absent from L give conserved momenta.
Conclude for x , y . Both cyclic ⇒ by d t d p i = ∂ q i ∂ L = 0 ,
p x = m x ˙ = const , p y = m y ˙ = const .
Why this step? Horizontal translational symmetry is unbroken by gravity, so horizontal momentum is conserved .
Conclude for z . ∂ z ∂ L = − m g = 0 , so
d t d p z = ∂ z ∂ L = − m g = 0.
Vertical momentum is not conserved — gravity breaks vertical translation symmetry.
Verify: This is projectile motion: x ˙ , y ˙ constant (flat trajectory in the horizontal plane), while p z = m z ˙ decreases at rate m g (that's just F = − m g ). Set g = 0 and all three become conserved — the free particle. The number of conserved momenta = number of unbroken translation directions. ✓
Worked example When the machinery itself wobbles
Noether's recipe assumes two quiet things: that L gives well-defined momenta, and that the coordinate map is smooth and reversible. Two short cases show what happens when those assumptions fail.
Forecast: In each case below, does a conserved charge still exist? Guess before reading.
Case (i): non-invertible ("singular") Lagrangian.
L = x ˙ y − y ˙ x .
Compute the momenta. p x = ∂ x ˙ ∂ L = y , p y = ∂ y ˙ ∂ L = − x .
Why this step? These do not contain x ˙ , y ˙ at all — you cannot solve them for the velocities. That is exactly what "non-invertible / singular L " means: the map (velocities) → (momenta) is not one-to-one.
Is there still a symmetry charge? Rotation δ x = − y , δ y = x : check δ L . One finds δ L = 0 (the form is rotation-invariant), and the Noether charge is Q = p x δ x + p y δ y = y ( − y ) + ( − x ) ( x ) = − ( x 2 + y 2 ) .
Why this step? Noether's charge formula still outputs a quantity, but because L is singular the object is a constraint (p x − y = 0 , p y + x = 0 ), not an ordinary evolution law. Such systems need Hamiltonian Mechanics with constraints (Dirac's method), not the naive p = ∂ L / ∂ q ˙ story.
Lesson: the formula survives, the interpretation changes — always check that momenta actually depend on velocities before trusting a "conserved" charge.
Case (ii): singular coordinate transformation.
Return to polar coordinates from Ex 1. At the origin r = 0 , the angle ϕ is undefined and the map ( r , ϕ ) → ( x , y ) is not invertible (its Jacobian r vanishes).
What breaks? The conserved p ϕ = m r 2 ϕ ˙ is still perfectly conserved along the motion — but you cannot read off ϕ at r = 0 .
Why this step? A particle passing exactly through the origin has r = 0 , so p ϕ = m ⋅ 0 ⋅ ϕ ˙ = 0 ; the coordinate singularity forces the charge to 0 there, consistent with a straight line through the center carrying zero angular momentum.
Lesson: a coordinate singularity does not destroy the conservation law; it only makes that chart a bad place to describe the motion. Switch to Cartesian x , y (smooth everywhere) and L z = m ( x y ˙ − y x ˙ ) stays finite and conserved.
Verify: Case (i): d t d ( − ( x 2 + y 2 ) ) = − 2 ( x x ˙ + y y ˙ ) . The constrained equations of motion of this L give x ˙ = x , y ˙ = y is not forced; instead the constraints pin x , y so that x x ˙ + y y ˙ = 0 , keeping Q constant — the charge is consistent. Case (ii): at r = 0 , p ϕ = 0 and the Cartesian L z = m ( x y ˙ − y x ˙ ) evaluated at x = y = 0 is also 0 ; the two descriptions agree. ✓
Mnemonic The one-question workflow for ANY of these
For each candidate symmetry, ask in order:
Is the coordinate absent from L ? → conserved momentum (Ex 1, 9).
If present, does the full δ L = 0 check pass anyway? → still conserved (Ex 2, 3).
Does δ L = d t d F = 0 ? → conserved charge is ∑ p i δ q i − F (Ex 5).
Does the coordinate/time appear with nonzero slope ? → not conserved; the drift rate is ∂ L / ∂ ( coord ) (Ex 4, 7, 9).
Do the momenta actually depend on the velocities , and is the coordinate map smooth? If not, treat the "charge" as a constraint and change charts (Ex 10).
Recall Self-test clozes
A driven oscillator conserves energy only in the limit ::: F 0 → 0 (drive off), restoring time-translation symmetry.
For a boost x → x + ϵ t , the conserved charge is ::: Q = m ( x ˙ t − x ) = − m x 0 , the initial position.
A charged particle's conserved "angular momentum" gains the extra term ::: 2 q B ( x 2 + y 2 ) , because p i = ∂ L / ∂ q ˙ i includes the vector potential.
In uniform gravity the conserved momenta are ::: p x and p y (horizontal), never p z .
If the momenta don't contain the velocities (singular L ), the Noether output is ::: a constraint, not an evolution law — use constrained Hamiltonian methods.
Deeper structure of these symmetries lives in Symmetry Groups & Lie Algebras and Gauge Symmetry ; the energy charge connects to Hamiltonian Mechanics .