Distinguish an origin error from a failed projectile model
A model prediction and a sensor readout can disagree for different reasons. A constant horizontal origin error shifts every position by the same amount. A change in horizontal acceleration instead changes curvature over time. The supplied comparison is designed to distinguish those two explanations under explicitly exact timing and fixed spatial scale.
Learning outcome: Compare a=0 and1 at offset 0.1 m, then change offset to −0.2 m. Retain raw, corrected and residual coordinates. Predict the second difference before checking and propose a separate timing/perspective test that the packet cannot supply.
Starting recap
Use SI units, signed components, algebraic ratios and graph coordinates. Identify the measurement rule and distinguish a record from an interpolated model.
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Try
For a=1 and o=0.1 m, initial horizontal readout 0.1 m identifies the offset in this packet. The corrected second difference is −0.04 m over a 0.2 s step, giving acceleration −1 m/s². Origin correction leaves that curvature intact.
Open the experimentPredict
Can subtracting the first position reading eliminate a true quadratic residual?
Experiment
Compare a=0 and1 at offset 0.1 m, then change offset to −0.2 m. Retain raw, corrected and residual coordinates. Predict the second difference before checking and propose a separate timing/perspective test that the packet cannot supply.
Distinguish curvature from a position-origin error
Worked teaching model · synthetic values · Synthetic packet at0,.2,.4,.6,.8 s: x=4t−a t²/2+offset,y=2+2t−5t². Times and vertical scale exact. Constant horizontal deceleration is an assigned alternative, NOT a physical aerodynamic drag law; the displayed packet remains above ground.
Reset keeps your prediction, captures and practice history.
Raw and origin-corrected horizontal records
Unlike graph quantities rescale independently; read units and values, not screen angles. 1: raw readings (open markers).2: origin-corrected readings (filled markers).3: no-horizontal-acceleration comparison (dotted). Joined curves show the supplied model, not additional observations.
Equivalent numerical coordinates for Raw and origin-corrected horizontal records
raw readings
| time (s) | horizontal coordinate (m) |
|---|---|
| 0 | 0.1 |
| 0.2 | 0.88 |
| 0.4 | 1.62 |
| 0.6 | 2.32 |
| 0.8 | 2.98 |
At most 82 representative computed coordinates including endpoints; the plotted curve can use a finer grid. A table of a revealed generator is not independent measurement evidence.
origin-corrected readings
| time (s) | horizontal coordinate (m) |
|---|---|
| 0 | 0 |
| 0.2 | 0.78 |
| 0.4 | 1.52 |
| 0.6 | 2.22 |
| 0.8 | 2.88 |
At most 82 representative computed coordinates including endpoints; the plotted curve can use a finer grid. A table of a revealed generator is not independent measurement evidence.
no-horizontal-acceleration comparison
| time (s) | horizontal coordinate (m) |
|---|---|
| 0 | 0 |
| 0.2 | 0.8 |
| 0.4 | 1.6 |
| 0.6 | 2.4 |
| 0.8 | 3.2 |
At most 82 representative computed coordinates including endpoints; the plotted curve can use a finer grid. A table of a revealed generator is not independent measurement evidence.
Residual after removing origin offset
Unlike graph quantities rescale independently; read units and values, not screen angles. 1: observed minus constant-velocity comparison (solid). Joined curves show the supplied model, not additional observations.
Equivalent numerical coordinates for Residual after removing origin offset
observed minus constant-velocity comparison
| time (s) | position residual (m) |
|---|---|
| 0 | 0 |
| 0.2 | -0.02 |
| 0.4 | -0.08 |
| 0.6 | -0.18 |
| 0.8 | -0.32 |
At most 82 representative computed coordinates including endpoints; the plotted curve can use a finer grid. A table of a revealed generator is not independent measurement evidence.
| Quantity | Value | Unit |
|---|---|---|
| Indicated horizontal origin | 0.1 | m |
| Horizontal second difference | -0.04 | m |
| Inferred signed horizontal acceleration | -1 | m/s² |
| Final residual from constant4 m/s model | -0.32 | m |
| Final height of sampled packet | 0.4 | m |
| Known generator horizontal deceleration | 1 | m/s² |
A constant origin error shifts all positions, whereas the stipulated horizontal acceleration changes their curvature.
Second differences remove a constant offset and a linear velocity term. Under the exact timing/position assumptions, curvature rejects this no-horizontal-acceleration comparison, but does not identify physical drag. Perspective distortion, clock error, changing scale or other forces require independent checks. All five vertical positions remain above the ground; no post-impact data are fit.
Predict before inspecting the values. Save contrasting records with assumptions and one alternative explanation. This virtual display does not certify practical measurement technique.
A constant origin error shifts all positions, whereas the stipulated horizontal acceleration changes their curvature.
Second differences remove a constant offset and a linear velocity term. Under the exact timing/position assumptions, curvature rejects this no-horizontal-acceleration comparison, but does not identify physical drag. Perspective distortion, clock error, changing scale or other forces require independent checks. All five vertical positions remain above the ground; no post-impact data are fit.
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.
Why does rejecting one ballistic assumption not by itself measure an air-drag coefficient?
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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.
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