Infer velocity from a position graph with uncertainty
An interval-average velocity is the slope joining two points on a position–time graph: (x₂−x₁)/(t₂−t₁). Instantaneous velocity is the local slope. A graph can sit above zero yet slope downward: positive position and negative velocity are perfectly compatible. Screen angle alone is not a velocity; read axis scales and units.
Learning outcome: Hold acceleration at 1 m/s². Compare half-windows 1, 0.5 and 0.25 s; record the velocity estimate and worst-case bound. Explain why the exact midpoint velocity stays fixed while the measured estimate changes. Repeat with negative acceleration and retain the same error signs.
Starting recap
Use signed quantities, algebraic substitution, graph slopes and areas. State the system, coordinate axes and units before calculating.
All lessons are open directly. Your saved experiments remain when you leave and return.
Try
For a=1 m/s² and h=0.5 s, true positions at 1.5 and 2.5 s are 4.125 and 8.125 m. The assigned observations are 4.025 and 8.225 m. Their slope is 4.2 m/s; the true midpoint velocity is 4 m/s. The 0.2 m/s error equals ε/h=0.1/0.5.
Open the experimentPredict
Will halving the time window always improve this measured slope? Separate the exact quadratic from the observation errors.
Experiment
Hold acceleration at 1 m/s². Compare half-windows 1, 0.5 and 0.25 s; record the velocity estimate and worst-case bound. Explain why the exact midpoint velocity stays fixed while the measured estimate changes. Repeat with negative acceleration and retain the same error signs.
Estimate a local slope with bounded position error
Worked teaching model · synthetic values · Synthetic x=2t+0.5at² m. Each endpoint has an assigned position error bounded by 0.10 m. The displayed left endpoint error is −0.10 m and right is +0.10 m: a deliberately adverse realization, not random noise. Times are exact.
Reset keeps your prediction, captures and practice history.
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 |
|---|---|---|
| Left observed position | 4.025 | m |
| Right observed position | 8.225 | m |
| Secant velocity estimate | 4.2 | m/s |
| True midpoint velocity | 4 | m/s |
| Worst-case velocity error bound | 0.2 | m/s |
Accessible plot coordinates
| time (s) | position (m) |
|---|---|
| 0 | 0 |
| 0.25 | 0.53125 |
| 0.5 | 1.125 |
| 0.75 | 1.78125 |
| 1 | 2.5 |
| 1.25 | 3.28125 |
| 1.5 | 4.125 |
| 1.75 | 5.03125 |
| 2 | 6 |
| 2.25 | 7.03125 |
| 2.5 | 8.125 |
| 2.75 | 9.28125 |
| 3 | 10.5 |
| 3.25 | 11.78125 |
| 3.5 | 13.125 |
| 3.75 | 14.53125 |
| 4 | 16 |
| time (s) | position (m) |
|---|---|
| 1.5 | 4.025 |
| 2.5 | 8.225 |
A smaller interval need not give a better experimental velocity estimate: fixed position error is divided by a smaller time interval.
For this quadratic trajectory the exact symmetric secant equals midpoint velocity. The displayed positive bias is entirely the deliberately adverse endpoint error, not curvature bias. Solid: exact trajectory; dashed: observed secant.
A smaller interval need not give a better experimental velocity estimate: fixed position error is divided by a smaller time interval.
For this quadratic trajectory the exact symmetric secant equals midpoint velocity. The displayed positive bias is entirely the deliberately adverse endpoint error, not curvature bias. Solid: exact trajectory; dashed: observed secant.
Captures preserve recipes and replay their calculated results. They are synthetic model evidence, not physical measurements.
Understand
Apply
Public practice checks a specific claim. It does not establish independent mastery.
How could you reduce error without merely shrinking the interval? Consider calibration, image resolution and fitting several observations.
Continue
Completion requires a saved prediction, at least one capture and a reflection. Presence checks do not grade your reasoning.
Skipping retains experiments and awards no mastery.
Save a science backup or import one
Science work is stored locally in this browser, separately from mathematics and AI. It does not sync automatically. Use this science-only backup; this checkout's older all-subject export does not include science.
A legacy file is available only when the complete snapshot fits the 36 MB limit. For larger snapshots, prepare a complete file set below; never discard notebooks to make a smaller file.
Matching imported notebook drafts replace their current drafts. Omitted lessons and known first attempts remain. Export your current work first if you want to retain both drafts.
Complete file sets and course backups
A file set can hold more work than one science file. Keep its manifest and every part together. Each file is limited to 36 MB. This format needs this version of LearnAI or a compatible newer version; older versions can use only the legacy single-file backup above.
The set includes every saved science course and global continuation at this moment. Later edits need a new export. A conflicting tab exports its own visible work, which may differ from saved work in another tab.
0 file(s) selected. File order and filenames do not determine identity. Missing, changed or conflicting parts block the entire restore; no good part is applied by itself.
Science storage: loading. No account or remote computation is required.