Simple harmonic motion

Push a swing gently and let go, and it does not wander off in some random wobble — it settles into a smooth, repeating to-and-fro that looks the same on every cycle. Pluck a guitar string, drop a mass on a spring, watch the balance wheel of an old mechanical watch: all of them, if you strip away friction and air resistance, obey the very same mathematics. That shared mathematics has a name — simple harmonic motion, or SHM — and it is the single most important idea in the entire chapter on oscillations. What makes SHM special is not just that the motion repeats. Lots of motion repeats — a bouncing ball, a person pacing a room — without being SHM. SHM is the specific repeating motion whose displacement traces out a pure sine or cosine curve against time, and whose restoring force always pulls exactly in proportion to how far the object has strayed from its resting point. That one restriction, a=−ω2xa = -\omega^2 x, turns out to be extraordinarily powerful: once you know a system obeys it, you can predict its position, velocity and acceleration at any instant, its time period without ever running the experiment, and how its energy sloshes between two forms as it swings. This article builds the core SHM equation from the ground up, connects it to the familiar picture of a point going round a circle at constant speed, derives the two headline CBSE results — the loaded spring's T=2πm/kT = 2\pi\sqrt{m/k} and the simple pendulum's T=2πL/gT = 2\pi\sqrt{L/g} — and works through the energy bookkeeping that ties displacement, velocity and total mechanical energy together in one tidy picture.

Key takeaways
  • SHM is defined by one equation. A particle is in SHM if a=−ω2xa = -\omega^2 x: acceleration is always directed toward the mean position and proportional to displacement from it.
  • The displacement is a pure sinusoid. x(t)=Acos⁡(ωt+ϕ)x(t) = A\cos(\omega t + \phi), with amplitude AA, angular frequency ω\omega, and phase constant ϕ\phi fixing the starting condition.
  • SHM is the shadow of circular motion. The projection of a point moving on a circle of radius AA at constant angular speed ω\omega onto any diameter executes SHM with that same ω\omega.
  • A linear restoring force always gives SHM. Whenever F=−kxF = -kx, Newton's second law forces a=−(k/m)xa = -(k/m)x, so ω=k/m\omega = \sqrt{k/m} and the period is T=2πm/kT = 2\pi\sqrt{m/k}.
  • The simple pendulum is SHM only for small angles. For θ\theta small enough that sin⁡θ≈θ\sin\theta \approx \theta, a pendulum obeys the same restoring-force pattern and gives T=2πL/gT = 2\pi\sqrt{L/g}.
  • Energy trades continuously between kinetic and potential. KE=12mω2(A2−x2)KE = \tfrac12 m\omega^2(A^2-x^2) and PE=12mω2x2PE = \tfrac12 m\omega^2 x^2 always add to the constant total E=12mω2A2E = \tfrac12 m\omega^2 A^2.
  • Key idea: any system whose restoring force is directly proportional to displacement, F = -kx, is forced by Newton's second law into the sinusoidal motion x = A cos(ωt + φ) with ω = √(k/m), and its energy oscillates between kinetic and potential while their sum stays fixed at ½mω²A².
The core insight

Simple harmonic motion is the periodic motion produced whenever a restoring force is directly proportional to displacement and opposite in direction, F=−kxF = -kx, which forces the displacement to follow x=Acos⁡(ωt+ϕ)x = A\cos(\omega t+\phi) with ω=k/m\omega = \sqrt{k/m}, links to uniform circular motion as its shadow on a diameter, and conserves a total energy E=12mω2A2E = \tfrac12 m\omega^2A^2 that is continuously exchanged between kinetic and potential forms.

Where it fits in the syllabus

SHM is the centrepiece of the CBSE Class 11 Physics chapter "Oscillations," sitting right after periodic motion and displacement-as-a-function-of-time (built in the prerequisite article) and right before the formal link to uniform circular motion (the next article in this sequence). The prescribed scope here is precise: the SHM equations x=Acos⁡(ωt+ϕ)x=A\cos(\omega t+\phi), v=−Aωsin⁡(ωt+ϕ)v=-A\omega\sin(\omega t+\phi) and a=−ω2xa=-\omega^2x; the restoring force law F=−kxF=-kx and the loaded-spring period T=2πm/kT=2\pi\sqrt{m/k}; the simple pendulum's T=2πL/gT=2\pi\sqrt{L/g}; and energy in SHM. Damped, forced and driven oscillations and resonance have been removed from the 2025-26 CBSE prescription — they are mentioned only in passing below as "studied in Class 12 / higher classes," never developed.

The physical picture

The defining equation of SHM describes displacement as a single sinusoid in time. For a particle oscillating about a mean position taken as the origin,

x(t)=Acos⁡(ωt+ϕ)x(t) = A\cos(\omega t + \phi)

where: x(t)x(t) is the displacement from the mean position at time tt; AA is the amplitude, the maximum displacement on either side; ω\omega is the angular frequency in radians per second, related to the time period TT and ordinary frequency ν\nu by ω=2π/T=2πν\omega = 2\pi/T = 2\pi\nu; and ϕ\phi is the phase constant, fixing where in the cycle the motion starts at t=0t=0. The quantity (ωt+ϕ)(\omega t+\phi) itself is called the phase of the motion at time tt — it tells you exactly which point of the repeating cycle the particle occupies. Differentiating once gives the velocity, and again gives the acceleration:

v(t)=dxdt=−Aωsin⁡(ωt+ϕ)v(t) = \frac{dx}{dt} = -A\omega\sin(\omega t+\phi)
a(t)=dvdt=−Aω2cos⁡(ωt+ϕ)=−ω2x(t)a(t) = \frac{dv}{dt} = -A\omega^2\cos(\omega t+\phi) = -\omega^2 x(t)

The last step is the heart of the whole chapter: a=−ω2xa = -\omega^2x. Acceleration is always directed back toward the mean position (the minus sign) and its size grows in direct proportion to how far the particle has moved away (the xx). This single relation is both necessary and sufficient for SHM — any motion obeying it is SHM, and any true SHM must obey it. A physical reading helps fix the picture. At the extreme positions x=±Ax=\pm A, the particle is momentarily at rest (v=0v=0) but is being pulled back with the largest possible acceleration, amax=ω2Aa_{max}=\omega^2A. At the mean position x=0x=0, the pull vanishes (a=0a=0) but the particle is moving at its fastest, vmax=Aωv_{max}=A\omega. Everywhere in between, speed and acceleration trade off smoothly — as one grows the other shrinks — which is exactly why the motion keeps overshooting the mean position, decelerating, stopping at the far extreme, and reversing, cycle after cycle.

Figure
A displacement time graph and its matching velocity and acceleration graphs for one full cycle of simple harmonic motion, showing displacement as a cosine curve starting at the positive extreme, velocity as a shifted sine curve that is zero at the extremes and maximum at the mean position, and acceleration as an inverted cosine curve that is largest at the extremes and zero at the mean position
x, v and a over one cycle of SHM x(t) = A cos(wt) v(t) = -Aw sin(wt) a(t) = -Aw^2 cos(wt) mean position, T/4 extreme, T/2

Watch a peg fixed on the rim of a turntable spinning at a steady angular speed ω\omega, but instead of watching the peg itself, watch only its shadow cast on a screen along one diameter. That shadow does not sweep round smoothly — it slows at the two edges and speeds up in the middle, oscillating back and forth exactly like a mass on a spring. If the turntable has radius AA and the peg starts at angle ϕ\phi from the reference diameter, the shadow's position along that diameter is precisely x=Acos⁡(ωt+ϕ)x = A\cos(\omega t + \phi) — the SHM equation, with no extra assumptions. This is why ω\omega in SHM is called angular frequency even though nothing is visibly rotating in a swinging pendulum or a bobbing spring: it is literally the angular speed of the imaginary reference circle whose projection reproduces the same x(t)x(t).

The restoring force and the loaded spring

Derivation AThe period of a mass on a spring, T = 2π√(m/k)

The goal is to show that any system obeying Hooke's law — a restoring force directly proportional to displacement and opposite in direction, F=−kxF=-kx — is automatically forced into simple harmonic motion by Newton's second law, and to extract the exact time period in terms of the mass mm and the spring's force constant kk, without assuming the answer in advance.

Step 1. Write down the restoring force. For a block of mass mm attached to a spring of force constant kk, displaced by xx from its natural (mean) length, Hooke's law gives the force the spring exerts back on the block as F=−kxF = -kx. The minus sign says the force always opposes the displacement — pulling the block back when stretched, pushing it back when compressed.

Step 2. Apply Newton's second law. The net force on the block equals mama, so ma=−kxma = -kx, which rearranges to a=−kmxa = -\dfrac{k}{m}x.

Step 3. Compare with the definition of SHM. The defining relation of SHM, established above, is a=−ω2xa = -\omega^2x. Matching the two expressions for aa term by term forces ω2=k/m\omega^2 = k/m, so ω=k/m\omega = \sqrt{k/m}. Because this angular frequency came purely from Newton's second law and Hooke's law, with no restriction on how large the displacement xx was, a spring-mass system obeys SHM exactly (as long as the spring itself stays within its elastic, Hooke's-law regime), not just approximately.

Step 4. Convert to the time period. Since ω=2π/T\omega = 2\pi/T, substituting ω=k/m\omega=\sqrt{k/m} gives 2π/T=k/m2\pi/T = \sqrt{k/m}, so

T=2πmkT = 2\pi\sqrt{\frac{m}{k}}

Step 5. Read the physics of the formula. A heavier block (mm larger) oscillates more sluggishly — the period grows with m\sqrt{m}. A stiffer spring (kk larger) snaps the block back faster — the period shrinks with 1/k1/\sqrt{k}. Neither the amplitude AA nor the acceleration due to gravity gg appears anywhere in the formula: a spring-mass system's period is the same whether it oscillates gently or with a large swing, and the same whether it hangs vertically or lies on a smooth horizontal table (gravity only shifts the mean position, it never changes kk or mm).

Energy in SHM

A particle in SHM continuously exchanges energy between kinetic and potential forms, but the sum of the two is fixed for a given amplitude. Since v=−Aωsin⁡(ωt+ϕ)v = -A\omega\sin(\omega t+\phi) and x=Acos⁡(ωt+ϕ)x=A\cos(\omega t+\phi), using sin⁡2+cos⁡2=1\sin^2+\cos^2=1 gives v2=ω2(A2−x2)v^2 = \omega^2(A^2-x^2), so the kinetic energy at displacement xx is

KE=12mv2=12mω2(A2−x2)KE = \frac12 mv^2 = \frac12 m\omega^2(A^2-x^2)

The restoring force F=−kx=−mω2xF=-kx=-m\omega^2x (using k=mω2k=m\omega^2) is conservative, and the potential energy stored against it, taken as zero at the mean position, works out to

PE=12mω2x2PE = \frac12 m\omega^2 x^2

where: mm is the oscillating mass, ω\omega its angular frequency, AA the amplitude and xx the instantaneous displacement. Adding the two, the x2x^2 terms cancel:

E=KE+PE=12mω2A2E = KE + PE = \frac12 m\omega^2 A^2

The total mechanical energy is constant throughout the motion, proportional to the square of the amplitude and to the square of the angular frequency — double the amplitude and the energy quadruples. At the mean position (x=0x=0) all the energy is kinetic (KE=EKE=E, PE=0PE=0); at either extreme (x=±Ax=\pm A) all of it is potential (PE=EPE=E, KE=0KE=0); everywhere in between the two share the fixed total, tracing out complementary parabolas when plotted against xx.

Figure
A graph of kinetic energy and potential energy plotted against displacement x from minus A to plus A, potential energy rising as an upward parabola from zero at the mean position to a maximum at both extremes, kinetic energy as a downward parabola that is maximum at the mean position and zero at both extremes, with their sum shown as a flat horizontal line equal to the constant total energy
Kinetic and potential energy versus displacement in SHM +A -A 0 PE = (1/2) m w^2 x^2 KE = (1/2) m w^2 (A^2 - x^2) Total energy E = (1/2) m w^2 A^2, constant

The simple pendulum

A simple pendulum — a point mass mm on a light, inextensible string of length LL — is not an ideal spring, yet for small swings it obeys the very same a=−ω2xa=-\omega^2x pattern, and hence is SHM to a very good approximation. When the string makes a small angle θ\theta with the vertical, gravity's component along the arc is −mgsin⁡θ-mg\sin\theta, restoring the bob toward the bottom. For angles small enough that θ\theta is measured in radians and sin⁡θ≈θ\sin\theta \approx \theta (true to better than one per cent below about 1010 degrees), the restoring force becomes proportional to the arc-length displacement x=Lθx = L\theta, giving a=−(g/L)xa = -(g/L)x. Matching this against a=−ω2xa=-\omega^2x gives ω=g/L\omega=\sqrt{g/L} and hence the CBSE headline result

T=2πLgT = 2\pi\sqrt{\frac{L}{g}}

Notice this period depends only on the length LL and on gg — not on the mass of the bob and not on the amplitude of swing (as long as the small-angle condition holds), which is exactly why pendulum clocks kept reliable time for centuries regardless of small changes in how hard they were wound.

Worked examples

Board level - amplitude, angular frequency and displacement at a given time

A particle executes SHM with amplitude 0.2 m0.2\ \text{m} and angular frequency 5 rad/s5\ \text{rad/s}. At t=0t=0 the particle is at its mean position moving in the positive direction. Write the equation for x(t)x(t), and find the displacement, velocity and acceleration at t=0.3 st=0.3\ \text{s}.

Step 1. Choose the correct form. Since x(0)=0x(0)=0 with v(0)>0v(0)>0, using x=Asin⁡(ωt)x = A\sin(\omega t) satisfies both: x(0)=0x(0)=0, and v(0)=Aωcos⁡(0)=Aω>0v(0)=A\omega\cos(0)=A\omega>0. So x(t)=0.2sin⁡(5t) mx(t) = 0.2\sin(5t)\ \text{m}, equivalent to Acos⁡(ωt+ϕ)A\cos(\omega t+\phi) with ϕ=−π/2\phi=-\pi/2.

Step 2. Displacement at t=0.3 st=0.3\ \text{s}: x=0.2sin⁡(5×0.3)=0.2sin⁡(1.5 rad)x = 0.2\sin(5\times0.3) = 0.2\sin(1.5\ \text{rad}). Since sin⁡(1.5)≈0.997\sin(1.5) \approx 0.997, x≈0.2×0.997≈0.199 mx \approx 0.2\times0.997 \approx 0.199\ \text{m} — almost at the extreme A=0.2 mA=0.2\ \text{m}.

Step 3. Velocity at the same instant: v=Aωcos⁡(5t)=0.2×5×cos⁡(1.5)=1.0×0.0707≈0.071 m/sv = A\omega\cos(5t) = 0.2\times5\times\cos(1.5) = 1.0\times0.0707 \approx 0.071\ \text{m/s}, small, consistent with the particle being nearly stationary near an extreme.

Step 4. Acceleration: a=−ω2x=−(5)2×0.199≈−4.98 m/s2a=-\omega^2x = -(5)^2\times0.199 \approx -4.98\ \text{m/s}^2, close to the maximum magnitude ω2A=25×0.2=5 m/s2\omega^2A = 25\times0.2=5\ \text{m/s}^2, directed back toward the mean position. Answer: x(t)=0.2sin⁡(5t) mx(t)=0.2\sin(5t)\ \text{m}; at t=0.3 st=0.3\ \text{s}, x≈0.199 mx\approx0.199\ \text{m}, v≈0.071 m/sv\approx0.071\ \text{m/s}, a≈−4.98 m/s2a\approx-4.98\ \text{m/s}^2.

Competitive level - spring-mass period, maximum speed and energy split

A block of mass 0.5 kg0.5\ \text{kg} is attached to a spring of force constant k=200 N/mk = 200\ \text{N/m} and set oscillating with amplitude A=0.10 mA = 0.10\ \text{m} on a smooth horizontal table. Find (a) the angular frequency and time period, (b) the maximum speed, and (c) the kinetic and potential energy when the block is at x=0.05 mx = 0.05\ \text{m}.

Step 1. Angular frequency from ω=k/m=200/0.5=400=20 rad/s\omega=\sqrt{k/m} = \sqrt{200/0.5} = \sqrt{400} = 20\ \text{rad/s}. Time period T=2πm/k=2π/ω=2π/20≈0.314 sT = 2\pi\sqrt{m/k} = 2\pi/\omega = 2\pi/20 \approx 0.314\ \text{s}.

Step 2. Maximum speed occurs at the mean position: vmax=Aω=0.10×20=2.0 m/sv_{max} = A\omega = 0.10\times20 = 2.0\ \text{m/s}.

Step 3. Total energy: E=12mω2A2=12×0.5×400×(0.10)2=12×0.5×400×0.01=1.0 JE = \tfrac12 m\omega^2A^2 = \tfrac12\times0.5\times400\times(0.10)^2 = \tfrac12\times0.5\times400\times0.01 = 1.0\ \text{J}.

Step 4. At x=0.05 mx=0.05\ \text{m} (half the amplitude): PE=12mω2x2=12×0.5×400×0.0025=0.25 JPE = \tfrac12 m\omega^2x^2 = \tfrac12\times0.5\times400\times0.0025 = 0.25\ \text{J}, and by conservation KE=E−PE=1.0−0.25=0.75 JKE = E-PE = 1.0-0.25 = 0.75\ \text{J}. Answer: ω=20 rad/s\omega=20\ \text{rad/s}, T≈0.314 sT\approx0.314\ \text{s}, vmax=2.0 m/sv_{max}=2.0\ \text{m/s}, and at x=0.05 mx=0.05\ \text{m}: PE=0.25 JPE=0.25\ \text{J}, KE=0.75 JKE=0.75\ \text{J} (total 1.0 J1.0\ \text{J}). Timing note: under ninety seconds once the pattern is drilled. Get ω\omega from k/m\sqrt{k/m} first — everything else (period, vmax=Aωv_{max}=A\omega, total energy 12mω2A2\tfrac12m\omega^2A^2) follows directly by substitution, and the energy split at any xx is just EE minus 12mω2x2\tfrac12m\omega^2x^2; there is no need to ever go back to solving the equation of motion from scratch.

Common traps

  • Calling any repeating motion SHM. A motion is SHM only if it is a pure sine/cosine of time and, equivalently, only if a=−ω2xa=-\omega^2x holds exactly — a bouncing ball or a person pacing back and forth is periodic but not SHM.
  • Writing x=Acos⁡(ωt)x=A\cos(\omega t) by habit and dropping ϕ\phi. That special case is only correct if the particle starts at the positive extreme; general starting conditions (like starting at the mean position, as in the board example above) need a nonzero phase constant.
  • Confusing angular frequency ω\omega (rad/s) with ordinary frequency ν\nu (Hz) — they are related by ω=2πν\omega=2\pi\nu, and mixing them up throws every numerical answer off by a factor of 2π2\pi.
  • Believing the loaded-spring period depends on gg or on amplitude. It does not — T=2πm/kT=2\pi\sqrt{m/k} contains only mm and kk; gravity merely relocates the mean position when the spring hangs vertically.
  • Applying T=2πL/gT=2\pi\sqrt{L/g} at large swing angles. The formula is only valid for small θ\theta (roughly under 1010 degrees, where sin⁡θ≈θ\sin\theta\approx\theta); at large amplitude the period actually increases slightly, a correction outside this syllabus.
  • Sign errors differentiating cos⁡\cos to get vv and aa: remember ddtcos⁡(ωt+ϕ)=−ωsin⁡(ωt+ϕ)\frac{d}{dt}\cos(\omega t+\phi)=-\omega\sin(\omega t+\phi), not +ωsin⁡(⋅)+\omega\sin(\cdot).

You should be able to…

  • Write and interpret x=Acos⁡(ωt+ϕ)x=A\cos(\omega t+\phi), identifying amplitude, angular frequency and phase constant from an equation or a physical situation.
  • Derive v=−Aωsin⁡(ωt+ϕ)v=-A\omega\sin(\omega t+\phi) and a=−ω2xa=-\omega^2x by differentiation, and explain why a=−ω2xa=-\omega^2x is the defining test for SHM.
  • Explain SHM as the projection of uniform circular motion onto a diameter.
  • Derive T=2πm/kT=2\pi\sqrt{m/k} from F=−kxF=-kx and Newton's second law, and state which quantities the period does and does not depend on.
  • Derive T=2πL/gT=2\pi\sqrt{L/g} for a simple pendulum under the small-angle approximation, and know why the approximation is needed.
  • Compute KE=12mω2(A2−x2)KE=\tfrac12m\omega^2(A^2-x^2), PE=12mω2x2PE=\tfrac12m\omega^2x^2 and the constant total E=12mω2A2E=\tfrac12m\omega^2A^2 at any displacement.

Ask the tutor: Not sure how to pick the right form of x(t)x(t) (sine vs. cosine, and the correct phase constant ϕ\phi) from a word problem's starting conditions, or want to see the pendulum's small-angle approximation checked numerically? Ask the AI tutor to walk through a few initial-condition and energy-split problems with you.

If a graph of x versus t just looks wavy, how do I know for sure it is SHM and not some other periodic motion?

A wavy-looking graph is not proof by itself — plenty of periodic motions have curvy graphs without being SHM. The rigorous check is algebraic: work out the acceleration (from the force law, or by differentiating the given x(t)x(t) twice) and see if it comes out as a=−ω2xa=-\omega^2x, a constant times minus the displacement, with no other terms. If the graph is explicitly labelled as a pure sine or cosine curve with constant amplitude and constant period, you can trust it is SHM; if it is some other repeating shape (triangular, sawtooth, or a sine with changing amplitude from friction), it is periodic but not simple harmonic.

Why does the period of a spring not depend on how far I pull it before letting go?

This feels wrong at first because pulling farther clearly means more distance to cover, so you would expect a longer time. But it also means a bigger restoring force at every point (since F=−kxF=-kx scales with xx), which gives a proportionally bigger speed everywhere along the path. The two effects — more distance and proportionally more speed — cancel exactly for a Hooke's-law spring, which is precisely why T=2πm/kT=2\pi\sqrt{m/k} has no AA in it. This "independence of period from amplitude" is a special signature of ideal SHM, not a general property of all periodic motion.

Is the small-angle approximation for the pendulum just a simplification for students, or does it matter in real life?

It genuinely matters, not just for exams. A pendulum swung through a large angle (say 40 or 50 degrees) really does take slightly longer per swing than 2πL/g2\pi\sqrt{L/g} predicts, because sin⁡θ\sin\theta falls short of θ\theta as the angle grows, weakening the restoring force at large displacement. Precision pendulum clocks are deliberately built to swing through only a few degrees so that the small-angle formula stays accurate to many decimal places; the exact large-angle period is a genuinely harder problem (elliptic integrals) that is well beyond this syllabus.

I have heard of damped and forced oscillations and resonance — will those be tested with SHM in this chapter?

Not in the current CBSE Class 11 syllabus (2025-26) — damped oscillations, forced oscillations and resonance have been removed from the prescribed chapter and are studied only in Class 12 or higher classes, if at all in your stream. Everything examined here assumes an idealised, undamped oscillator: no friction, no air resistance, no external driving force, so the amplitude and energy stay exactly constant forever. Keep your board-exam answers confined to the ideal case unless a question explicitly says otherwise.

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