Paper 5 - Constants, uncertainty and conclusions

Paper 5 - Constants, uncertainty and conclusions

Learn to turn fitted gradients and intercepts into physical constants with correct units. Propagate uncertainty through those equations, report results at justified precision and state exactly what agreement with a model or reference value establishes.

Recovering physical constants from fitted numbers

Two graphs of the same experiment can have different numerical gradients. Can they still give the same physical constant? Yes: the axes may use different scale factors. A fitted number becomes physics only after the equation, units and axis scales are restored.

Begin with the supplied model and your stated axes. Derive expressions for the gradient and intercept, then rearrange with the required physical constant as the subject. Use the fitted line rather than substituting one arbitrary pair of raw readings: the line uses the whole trend and supplies its own uncertainty estimate.

For the supplied spring-system model

T2=4π2km+4π2mekT^2=\frac{4\pi^2}{k}m+\frac{4\pi^2m_{\mathrm e}}{k}

a plot of T2T^2 against mm gives G=4π2/kG=4\pi^2/k and c=Gmec=Gm_{\mathrm e}. Therefore k=4π2/Gk=4\pi^2/G and me=c/Gm_{\mathrm e}=c/G. Here period is in seconds, mass in kilograms, GG in s2 kg−1\mathrm{s^2\,kg^{-1}}, cc in s2\mathrm{s^2}, kk in N m−1\mathrm{N\,m^{-1}} and mem_{\mathrm e} in kilograms. The model is supplied for the investigation, not a new recall requirement.

[DIAGRAM: asset_name: Numerical gradients depend on the axis scale; asset_slug: practical-a2-scaled-gradient; caption: The two numerical gradients describe the same physical slope after the axis factors are restored; description: Two plots show the identical line T squared equals 0.800 times m plus 0.0400 in SI units. One plots T squared over seconds squared against m over kilograms and labels numerical gradient 0.800. The other plots the same vertical quantity against m divided by 0.10 kilogram and labels numerical gradient 0.0800. Both derive physical gradient 0.800 seconds squared per kilogram.]
The two numerical gradients describe the same physical slope after the axis factors are restored

On an axis headed m/(0.10 kg)m/(0.10\,\mathrm{kg}), an increase of one plotted unit is 0.10 kg0.10\,\mathrm{kg}, not 1 kg1\,\mathrm{kg}. A numerical gradient of 0.08000.0800 against this axis corresponds to

G=0.08001 s20.10 kg=0.800 s2 kg−1G=0.0800\frac{1\,\mathrm{s^2}}{0.10\,\mathrm{kg}} =0.800\,\mathrm{s^2\,kg^{-1}}

The constant is then k=4π2/0.800=49.3 N m−1k=4\pi^2/0.800=49.3\,\mathrm{N\,m^{-1}}. With c=0.0400 s2c=0.0400\,\mathrm{s^2}, me=0.0500 kgm_{\mathrm e}=0.0500\,\mathrm{kg}. If the horizontal axis were mass in grams, its physical slope would instead be 0.000800 s2 g−10.000800\,\mathrm{s^2\,g^{-1}}: converting the mass unit restores the same result.

Units are a useful independent check. Since N m−1=kg s−2\mathrm{N\,m^{-1}}=\mathrm{kg\,s^{-2}}, the reciprocal of GG's unit has the correct spring-constant unit. An intercept with unit s2\mathrm{s^2} cannot be substituted as a mass. For a dimensionless log axis, the intercept itself is dimensionless; inverse logarithms and the stated reference units recover the physical amplitude.

Watch out

A slope read from scaled numerical axes is not automatically an SI gradient. Attach the vertical scale unit divided by the horizontal scale unit before using it in a physical equation.

Uncertainty follows the equation for the constant

The uncertainty in a physical constant is not necessarily just the percentage uncertainty in the gradient. Read its derived equation: every uncertain input that affects the result must be accounted for, using absolute or fractional uncertainties in the appropriate place.

Use the conservative small-uncertainty rules recalled from earlier lessons. For sums and differences, add the absolute uncertainties. For products and quotients, add fractional uncertainties. A power multiplies the fractional uncertainty by the magnitude of its exponent. These are estimated bounds, not a claim that all errors have a known statistical distribution; do not replace them by a different statistical rule unless instructed.

For example, subtracting densities (8050±60) kg m−3(8050\pm60)\,\mathrm{kg\,m^{-3}} and (1250±40) kg m−3(1250\pm40)\,\mathrm{kg\,m^{-3}} gives (6800±100) kg m−3(6800\pm100)\,\mathrm{kg\,m^{-3}}. Add the absolute uncertainties before converting the difference's uncertainty into a fraction, 100/6800100/6800. Subtracting the uncertainties would incorrectly suggest that subtracting two uncertain measurements makes their difference exact.

For the spring example, take G=(0.800±0.040) s2 kg−1G=(0.800\pm0.040)\,\mathrm{s^2\,kg^{-1}} and c=(0.0400±0.0060) s2c=(0.0400\pm0.0060)\,\mathrm{s^2}. Since k=4π2/Gk=4\pi^2/G, its fractional uncertainty is 0.040/0.800=0.0500.040/0.800=0.050, or 5.0%5.0\%. Thus k=(49.3±2.5) N m−1k=(49.3\pm2.5)\,\mathrm{N\,m^{-1}}, to consistent precision. The exact factor 4π24\pi^2 and exact unit conversions add no measurement uncertainty.

For me=c/Gm_{\mathrm e}=c/G, the stated conservative estimate is

Δmeme≈Δc∣c∣+ΔG∣G∣=0.00600.0400+0.0400.800=0.20\frac{\Delta m_{\mathrm e}}{m_{\mathrm e}} \approx\frac{\Delta c}{|c|}+\frac{\Delta G}{|G|} =\frac{0.0060}{0.0400}+\frac{0.040}{0.800}=0.20

so me=(0.050±0.010) kgm_{\mathrm e}=(0.050\pm0.010)\,\mathrm{kg}. The slope and intercept have separate graphical uncertainty estimates. Do not assume their percentages are equal. Where a task specifies an extreme-value method, use the compatible limiting fitted values and show the substitutions; gradient and intercept from one fitted line are linked, so do not describe every arbitrary combination as a possible actual line.

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