Key Idea: This topic is the experimental-skills toolkit — how you take a measurement, attach an uncertainty to it, push that uncertainty through a calculation, and turn a table of readings into a straight-line graph you can read a physics quantity off. These skills are examined as a whole paper of their own — Paper 1B (data analysis) — built around one experiment. Expect: pick the right instrument and justify it; quote and combine uncertainties; draw a best-fit line and read its gradient (with the steepest/shallowest lines for the gradient's uncertainty); linearize a law and decide whether the data support it; and evaluate the method (random vs systematic error, repeats, anomalies). The same habits — units, significant figures, ± uncertainties — also score easy marks all through Paper 2.
📋 Key rules & formulas
The multiply/divide and power propagation rules carry the data-booklet badge (look for it). The add/subtract rule, the gradient and the gradient-uncertainty are not printed — you reproduce those from the definitions.
- the absolute uncertainty — a ± value in the SAME unit as x
- the measured value
- the fractional uncertainty — a plain number, no unit
- the percentage uncertainty
- a result found by adding or subtracting measurements
- the measured quantities added or subtracted
- their absolute uncertainties (same unit as the quantity)
- the absolute uncertainty in the result (same unit)
- the calculated result (e.g. a density = m ÷ V)
- the measured quantities multiplied or divided to get y
- the fractional uncertainty in a (no unit)
- the fractional uncertainty in the result y
- the result is a raised to a power n (e.g. area = πr², so r²)
- the power (2 for a square, 3 for a cube, ½ for a square root)
- the fractional uncertainty in a (no unit)
- the fractional uncertainty in the result (no unit)
- gradient (slope) of the best-fit line — usually a physics quantity
- rise — change in the y-value between two points ON THE LINE
- run — change in the x-value over the same interval
- uncertainty in the gradient
- gradient of the STEEPEST line that still passes through all the error bars
- gradient of the SHALLOWEST such line
- the quantity plotted UP the vertical axis (chosen so the graph is straight)
- the quantity plotted ACROSS the horizontal axis
- the gradient — equals a physics constant you are trying to find
- the vertical intercept — 0 for a 'directly proportional' law
📐 Choosing the instrument (resolution)
Choose the instrument whose smallest division is small compared with what you are measuring. A 0.5 mm wire on a mm ruler is hopeless (±0.5 mm is the whole thing) but easy on a micrometer (±0.005 mm). Reading uncertainty from a single instrument = ± half its smallest division.
⚖️ The three propagation rules side by side
🎯 Random vs systematic error
A straight line alone only means the law is linear (Y = mX + c). It is directly proportional only if the line also passes through the origin (c = 0). Equivalently, the ratio Y/X is constant across every row of the table.
✏️ Worked exam-style questions
IB-style question — measure a multiple to shrink the uncertainty
A student measures the thickness of one sheet of paper. A micrometer (resolution 0.01 mm, so ±0.005 mm) on a single sheet would give a fractional uncertainty of nearly 7%. Instead they measure a stack of 80 sheets and get 8.40 mm with the same ±0.005 mm. (a) Find the thickness of one sheet. (b) Find the absolute and percentage uncertainty in the thickness of one sheet, and say why this method is better.
Solution:
(a) The stack thickness divided by the number of sheets:
(b) Dividing by an EXACT count (80) divides the absolute uncertainty by the same number:
(b) Percentage uncertainty = (Δt ÷ t) × 100%:
(a) t = 0.105 mm. (b) Δt ≈ 6 × 10⁻⁵ mm, about 0.06% — far better than the ≈7% a single sheet would give. Measuring a MULTIPLE (a stack, or 10 swings) and dividing by an exact count keeps the same small absolute reading uncertainty while making the measured value large.
IB-style question — propagate uncertainty through a density
A small cube has side L = 2.00 ± 0.01 cm and mass m = 64.0 ± 0.5 g. The density is ρ = m ÷ V, where V = L³. (a) Find the density. (b) Find its percentage uncertainty. (c) Quote ρ with its absolute uncertainty.
Solution:
(a) Volume first (a cube, so L³), then density = mass ÷ volume:
(b) ρ = m ÷ L³ is a quotient with a power, so ADD fractional uncertainties — the side counts THREE times (|n| = 3):
(b) Evaluate each term, then add, then ×100%:
(c) Absolute uncertainty = fractional × value, rounded to 1 s.f.:
(a) ρ = 8.00 g cm⁻³. (b) ≈ 2.3%. (c) ρ = 8.0 ± 0.2 g cm⁻³. The L³ makes the side's fractional uncertainty count THREE times — that power term dominates, which is why you measure the side most carefully.
IB-style question — gradient and its uncertainty from a graph
On a force-versus-extension graph the best-fit line passes through (0, 0). Two points read off THE LINE are (0.020 m, 2.4 N) and (0.080 m, 9.6 N). The steepest and shallowest lines through the error bars have gradients 124 N m⁻¹ and 116 N m⁻¹. (a) Find the spring constant from the best-fit gradient. (b) Find the uncertainty in the gradient and quote k properly.
Solution:
(a) Gradient = rise ÷ run, using the two points ON THE LINE:
(a) Evaluate — and the gradient of a force-extension line IS the spring constant k:
(b) Uncertainty = half the spread of the steepest and shallowest gradients:
(a) k = 120 N m⁻¹. (b) k = 120 ± 4 N m⁻¹. Always read the gradient off the LINE (not the data points), and get its uncertainty from the steepest/shallowest lines through the error bars — never guess it.
IB-style question — linearize a law and test it
Theory predicts the depth d a marker sinks is d = k√P, where P is the water pressure. (a) State what to plot on each axis to get a straight line through the origin, and what the gradient represents. (b) A classmate instead claims d is directly proportional to P. Using the rows (P = 4.0 kPa, d = 3.1 cm) and (P = 9.0 kPa, d = 4.6 cm), show that this claim is wrong.
Solution:
(a) Match d = k√P to Y = mX + c: Y is d, X is √P, and there is no '+ c'.
(b) If d ∝ P then the ratio d ÷ P must be CONSTANT. First row:
(b) Second row:
(b) The two ratios differ, so d ÷ P is NOT constant:
(a) Plot d (up) against √P (across); the gradient equals the constant k. (b) d ÷ P is not constant (0.78 ≠ 0.51 cm kPa⁻¹), so d is NOT directly proportional to P — it fits d ∝ √P. 'Directly proportional' always means a straight line through the origin / a constant ratio.
🧠 Quick self-check
Tap each card to reveal the answer.
🎯 Exam tips
Exam Tips
- Match the instrument's RESOLUTION to the quantity, and reading uncertainty = ± half the smallest division. To shrink it, measure a MULTIPLE (a stack of sheets, 10 swings) and divide by the exact count.
- Pick the right propagation rule by the operation: + or − → add ABSOLUTE uncertainties; × or ÷ → add FRACTIONAL/percentage uncertainties; a power aⁿ → multiply the fractional uncertainty by |n|. The last two are in the data booklet.
- In a quotient with a power (like ρ = m ÷ L³), the side's fractional uncertainty counts |n| times — here three times — so that term usually dominates. Measure the powered quantity most carefully.
- Round the absolute uncertainty to 1 significant figure, then match the value to the same decimal place: ρ = 8.0 ± 0.2 g cm⁻³, never 8.00 ± 0.23.
- Read a gradient off TWO well-separated points ON the best-fit line, not the data points. State what the gradient represents and give its units — it is always a physics quantity.
- For the gradient's uncertainty, draw the steepest and shallowest lines that still pass through all the error bars, then Δm = (mₘₐₓ − mₘᵢₙ) ÷ 2.
- Linearize by rearranging the law to Y = mX + c, then plot Y against X. 'Directly proportional' demands a straight line THROUGH THE ORIGIN (or a constant ratio across rows) — a straight line alone is only 'linear'.
- Random error scatters readings → cut it by repeating and averaging. Systematic error shifts them all the same way → averaging won't help; fix the instrument or method. Always discard a clear anomaly before averaging.
- Dimensional analysis: balance the fundamental SI units (kg, m, s, A) on both sides to find an unknown exponent, or to state the units of a constant read off a gradient (y-axis units ÷ x-axis units).