Simple pendulum

Every grandfather clock, every metronome, and the earliest reliable timekeepers ever built all lean on one small, elegant fact: a bob swinging on a string keeps remarkably steady time. This is the simple pendulum — the third strand of the "Measurements and Experimentation" chapter, after you have already learnt to measure length and mass precisely. Here you learn how time is measured, using nothing more exotic than a string, a bob, and a stopwatch. The syllabus keeps things focused: know what time period and frequency mean, use the formula T=2πl/gT = 2\pi\sqrt{l/g} directly in numericals (its derivation is not required), and understand why plotting ll against T2T^2 gives a straight line whose slope hands you the local value of gg. This article expands on that ground with a fuller picture of the physics, a graph-based derivation of gg, and extra worked practice — but stays exactly within this scope.

The core insight

A simple pendulum's time period depends only on its length and on gg, following T=2πl/gT = 2\pi\sqrt{l/g}, and this lets a length-versus-T2T^2 graph be used to measure gg experimentally.

The core idea

A simple pendulum is an idealised system: a small, heavy bob hung from one end of a light, inextensible string, with the other end fixed, free to swing back and forth in a vertical plane. "Light" means the string's mass is negligible compared to the bob's, and "small" means the bob can be treated as a single point of mass — these idealisations are what make the formula below clean and simple. One complete oscillation (or vibration) is the bob's journey from its starting position, through the mean position to one extreme, back through the mean position to the other extreme, and back again to the start. Two useful quantities describe this repeating motion: The time period (TT) is the time taken for one complete oscillation, in seconds. The frequency (ff) is the number of complete oscillations in one second, in hertz (Hz). They are reciprocals of each other:

f=1Tf = \frac{1}{T}

where: ff is frequency in Hz and TT is time period in seconds. For small angles of swing (a few degrees), the time period depends only on the pendulum's length ll and the local acceleration due to gravity gg:

T=2πlgT = 2\pi\sqrt{\frac{l}{g}}

where: TT is the time period (s), ll is the length of the pendulum measured from the point of suspension to the centre of the bob (m), and gg is the acceleration due to gravity (m/s²). Notice what is missing from the right side: the mass of the bob, and (for small swings) the amplitude. A heavy bob and a light bob of the same length, released from the same small angle, keep exactly the same time. Squaring the formula turns it into something you can test on a graph:

T2=4π2g lT^2 = \frac{4\pi^2}{g}\,l

This is a straight line through the origin when T2T^2 (y-axis) is plotted against ll (x-axis), with slope 4π2g\dfrac{4\pi^2}{g}. A student measures TT for several different lengths ll, plots the points, draws the best-fit line, and reads off its slope — turning a swinging string into a gravity-measuring instrument.

Figure
A straight line graph of T squared on the vertical axis against length l on the horizontal axis passing through the origin, with a right triangle marked on the line showing rise over run equal to the slope four pi squared over g
Graph of l versus T squared — slope gives g length l (m) T squared (s squared) run rise slope = 4 pi squared / g origin
Derivation AGetting g from the slope of the l–T² graph

The goal is to start from the given relation T=2πl/gT = 2\pi\sqrt{l/g}, turn it into the straight-line form actually plotted in the laboratory, and show precisely how the measured slope of that line hands you the local acceleration due to gravity — the calculation the syllabus expects you to carry out even though the pendulum formula itself is not derived.

Step 1. Begin with the given formula and remove the square root by squaring both sides. Starting from T=2πl/gT = 2\pi\sqrt{l/g}, squaring gives T2=(2π)2×lg=4π2g lT^2 = (2\pi)^2 \times \dfrac{l}{g} = \dfrac{4\pi^2}{g}\,l. This single algebraic step converts an equation with a square root — awkward to plot directly — into one that is linear in ll and T2T^2.

Step 2. Recognise the linear form. Compare T2=4π2g lT^2 = \dfrac{4\pi^2}{g}\,l with the general equation of a straight line through the origin, y=mxy = mx. Here yy is T2T^2, xx is ll, and the constant multiplying xx — the slope mm — is 4π2g\dfrac{4\pi^2}{g}. Because gg is treated as constant at a given place on Earth, this slope is a fixed number, and the line must pass through the origin (when l=0l = 0, T2=0T^2 = 0).

Step 3. Connect the algebra to the experiment. In the lab, a student measures the time period TT for several different pendulum lengths ll, squares each TT, and plots T2T^2 against ll. The points lie on a straight line through the origin, exactly as Step 2 predicts. Measuring the slope of the best-fit line — rise in T2T^2 divided by run in ll — gives a numerical value for 4π2g\dfrac{4\pi^2}{g}.

Step 4. Rearrange to isolate gg. Since slope =4π2g= \dfrac{4\pi^2}{g}, cross-multiplying gives g×slope=4π2g \times \text{slope} = 4\pi^2, so

g=4π2slopeg = \frac{4\pi^2}{\text{slope}}

This is the working rule: measure the slope experimentally, then divide 4π24\pi^2 by it to obtain gg. The Worked example below applies this exact rule to real numbers.

Worked example

Question: A simple pendulum has a length of 1.0 m. Find its time period and frequency. This same pendulum is one of several lengths used to plot a T2T^2 (y-axis) against ll (x-axis) graph, which comes out as a straight line through the origin with slope 4.02 s2/m4.02\text{ s}^2/\text{m}. Find the value of gg this experiment gives. (Take π=3.14\pi = 3.14.)

Step 1. Substitute into the time period formula for the 1.0 m pendulum.

T=2πlg=2×3.14×1.09.8T = 2\pi\sqrt{\frac{l}{g}} = 2 \times 3.14 \times \sqrt{\frac{1.0}{9.8}}

Step 2. Evaluate the square root and complete the calculation.

1.09.8=0.102≈0.319⇒T=2×3.14×0.319≈2.0 s\sqrt{\frac{1.0}{9.8}} = \sqrt{0.102} \approx 0.319 \quad\Rightarrow\quad T = 2 \times 3.14 \times 0.319 \approx 2.0\text{ s}

Step 3. Find the frequency from f=1/Tf = 1/T.

f=12.0=0.5 Hzf = \frac{1}{2.0} = 0.5\text{ Hz}

Step 4. Now use the measured graph slope, applying g=4π2/slopeg = 4\pi^2/\text{slope} from the derivation above.

g=4π2slope=4×(3.14)24.02=39.444.02≈9.8 m/s2g = \frac{4\pi^2}{\text{slope}} = \frac{4 \times (3.14)^2}{4.02} = \frac{39.44}{4.02} \approx 9.8\text{ m/s}^2

Answer: The time period is approximately 2.0 s\mathbf{2.0\text{ s}}, the frequency is 0.5 Hz\mathbf{0.5\text{ Hz}}, and the slope of 4.02 s2/m4.02\text{ s}^2/\text{m} on the ll–T2T^2 graph gives back g≈9.8 m/s2\mathbf{g \approx 9.8\text{ m/s}^2}, matching the standard value — a check that both parts of the question are physically consistent.

Competitive stretch

If the same pendulum were taken to a place where the measured slope of the ll–T2T^2 graph is 4.20 s2/m4.20\text{ s}^2/\text{m}, what value of gg would this indicate?

Step 1. Apply g=4π2/slopeg = 4\pi^2/\text{slope} directly: g=39.44/4.20≈9.39 m/s2g = 39.44 / 4.20 \approx 9.39\text{ m/s}^2.

Answer: This location has a lower effective g≈9.39 m/s2g \approx 9.39\text{ m/s}^2 — a larger slope on the ll–T2T^2 graph always signals a smaller gg, since slope and gg are inversely related.

Common traps

  • Mixing up which axis is which — depending on how a question phrases the graph (ll vs T2T^2 or T2T^2 vs ll), the slope formula flips between g4π2\dfrac{g}{4\pi^2} and 4π2g\dfrac{4\pi^2}{g}; always check the axes stated in the question first.
  • Believing a heavier bob swings faster or slower — the formula shows TT depends only on ll and gg, never on the bob's mass.
  • Miscalculating 4π24\pi^2 as 4π4\pi, a common arithmetic slip when finding gg from the slope.
  • Trying to derive T=2πl/gT = 2\pi\sqrt{l/g} itself from first principles — the syllabus gives this formula directly; only the graph-to-gg working (as shown above) is expected of you.

Ask the tutor: Want more practice turning an ll–T2T^2 graph slope into a value of gg, or a quick refresher on rearranging T=2πl/gT = 2\pi\sqrt{l/g}? Ask the AI tutor for guided problems on this topic.

Why does the mass of the bob not affect the time period at all?

It seems surprising until you notice that in the formula T=2πl/gT = 2\pi\sqrt{l/g}, mass simply does not appear — only length and gravity do. Physically, a heavier bob needs a larger force to accelerate it through the swing, but gravity also pulls it down with proportionally more force, and the two effects exactly cancel. So a lead bob and a wooden bob of the same size and length, released from the same small angle, complete each swing in identical time.

Does the amplitude of the swing change the time period?

Only if the amplitude is large. The formula T=2πl/gT = 2\pi\sqrt{l/g} is derived under the assumption of a small swing angle (typically under about 10 degrees), and within that range the time period is independent of amplitude — a small swing and a slightly larger small swing take the same time. For large angles, this approximation breaks down and the true time period increases slightly with amplitude, but this lies outside the ICSE Class 9 syllabus, which only expects the small-angle case.

Why do we plot l against T squared instead of l against T directly?

Because T=2πl/gT = 2\pi\sqrt{l/g} is not a straight-line relation between ll and TT — it involves a square root, so a graph of TT against ll would be a curve, which is hard to read a precise slope from. Squaring both sides gives T2=(4π2/g) lT^2 = (4\pi^2/g)\,l, a genuine straight line through the origin. Straight lines are far easier to draw accurately and to extract a reliable slope from, which is exactly why the experiment is designed around T2T^2 rather than TT.

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Where this leads