Test whether agreement between methods is independent evidence
Two methods that agree can still share the same error. A freefall timing method infers gravity fromg=2h/t²; a small-angle pendulum infersg=4π²L/T². Their mechanisms differ, but if both use the same miscalibrated clock, their resulting estimates are not fully independent. The purpose of this capstone is to design evidence that could expose such a shared cause.
Learning outcome: Compare c=1 and1.05 with lagzero, then introduce lag0.05 at fixedc. Save both method estimates and the multiheight fall packet. Propose a genuinely independent calibration and predict how its evidence would differ under clock-scale versus fall-lag explanations. Specify how length error could confound the comparison.
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With clock scale1.05 and no added fall lag, fall time is0.42 s and both methods infer10/1.05²≈9.0703 m/s². Their difference iszero, but both differ from the generator truth. With an added fall lag0.05 s, fall time is0.47 s and fall gravity becomes1.6/0.47²≈7.2431 m/s²; the pendulum estimate remains9.0703. This contrast challenges a fall-specific assumption but does not itself certify the clock.
Open the experimentPredict
Can agreement between two different physical methods prove that their shared timing scale is correct?
Experiment
Compare c=1 and1.05 with lagzero, then introduce lag0.05 at fixedc. Save both method estimates and the multiheight fall packet. Propose a genuinely independent calibration and predict how its evidence would differ under clock-scale versus fall-lag explanations. Specify how length error could confound the comparison.
Test whether agreement is independent evidence
Worked teaching model · synthetic values · Two original supplied-data methods share a clock: freefall from rest and small-angle pendulum. Trueg10, exact lengths/heights, no drag; elapsed readings are scaled by a, with additional b only on fall timing. This prescribed bias model is not a real calibration or confidence interval. No physical dropping or suspension activity.
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Axes rescale with settings; compare numerical values, not screen angles or apparent lengths. Solid/points show the selected model relationship or observations; the dashed comparison is explained below.
| Quantity | Value | Unit |
|---|---|---|
| Observed fall time for height0.8 m | 0.42 | s |
| Observed period for length1 m | 2.08626 | s |
| Fall-method inferred gravity | 9.07029 | m/s² |
| Pendulum-method inferred gravity | 9.07029 | m/s² |
| Difference between inferred gravities | 0 | m/s² |
| True gravity in supplied generator | 10 | m/s² |
| Common clock scale | 1.05 | ratio |
| Fall-only added lag | 0 | s |
Accessible plot coordinates
| fall height (m) | observed fall time squared (s²) |
|---|---|
| 0.2 | 0.0441 |
| 0.4 | 0.0882 |
| 0.6 | 0.1323 |
| 0.8 | 0.1764 |
| 1 | 0.2205 |
| fall height (m) | observed fall time squared (s²) |
|---|---|
| 0.2 | 0.04 |
| 0.4 | 0.08 |
| 0.6 | 0.12 |
| 0.8 | 0.16 |
| 1 | 0.2 |
The two inferred gravities agree despite any common clock-scale bias: agreement is not independent calibration.
For zero added lag, both methods infer gtrue/clockScale². A second method sharing the same calibration is not fully independent. The solid graph is the supplied fall-time-squared packet; dashed is the generator’s unbiased reference. A real investigation would not know the hidden true values without independent reference evidence.
The two inferred gravities agree despite any common clock-scale bias: agreement is not independent calibration.
For zero added lag, both methods infer gtrue/clockScale². A second method sharing the same calibration is not fully independent. The solid graph is the supplied fall-time-squared packet; dashed is the generator’s unbiased reference. A real investigation would not know the hidden true values without independent reference evidence.
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