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SCIENCE · INVESTIGATE AND EXPLAIN

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.

All lessons are open directly. Your saved experiments remain when you leave and return.

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 experiment

Predict

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

horizontal coordinate (m)time (s)00.83.20

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)
00.1
0.20.88
0.41.62
0.62.32
0.82.98

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)
00
0.20.78
0.41.52
0.62.22
0.82.88

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)
00
0.20.8
0.41.6
0.62.4
0.83.2

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

position residual (m)time (s)00.80-0.32

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)
00
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.

Calculated quantities under the declared measurement model
QuantityValueUnit
Indicated horizontal origin0.1m
Horizontal second difference-0.04m
Inferred signed horizontal acceleration-1m/s²
Final residual from constant4 m/s model-0.32m
Final height of sampled packet0.4m
Known generator horizontal deceleration1m/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

Begin with a measurement question

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.

Build the algebraic model

The synthetic packet uses x=4t−at²/2+o and y=2+2t−5t² at times 0,0.2,0.4,0.6,0.8 s. The parameter a is a stipulated constant horizontal deceleration magnitude, not an aerodynamic drag law. The origin offset o can be removed by subtracting the initial readout. That subtraction does not remove the quadratic term.

Check a concrete implication

After origin correction, compare the positions with the no-horizontal-acceleration prediction x=4t. Residual is−at²/2, which curves downward when a is positive. Equal-time second differences are−aΔt², so division by the squared time step gives signed horizontal acceleration. A residual pattern rejects the stated constant-horizontal-velocity comparison under the assumptions; it does not identify which physical force or imaging failure caused the discrepancy.

Challenge the evidence boundary

At a=1 m/s², the final residual at 0.8 s is −0.32 m regardless of offset. All five vertical points remain above ground, ending at 0.4 m, so the fit does not include post-contact positions. Perspective distortion, changing scale, clock error or unmodeled force could still mimic aspects of the pattern in a real record. Design an independent calibration or changed observation before naming a mechanism.

Worked original case

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.

Predict and investigate

Can subtracting the first position reading eliminate a true quadratic residual? 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.

Changed numerical practice

Try the changed case before feedback

At times 0,0.2,0.4 s, horizontal positions are0.1,0.88,1.62 m. Infer signed horizontal acceleration in m/s² assuming constant acceleration and exact times.

This practice is public and unsaved. A matching number does not verify understanding. Retain your explanation, assumptions and changed-case evidence in the separate course workspace.

Reflect and source-check

Why does rejecting one ballistic assumption not by itself measure an air-drag coefficient?

Original explanations, synthetic records and models; checked 30 October 2026 against OpenStax College Physics 2e. The guided calculation is algebra-based; no calculus prerequisite is assumed. All activity is virtual. No physical launch, drop, water crossing, machinery operation or medical decision is requested. A public answer or saved capture does not verify independent mastery or actual measurement technique.

Apply

With exact equal-time samples, subtracting a fixed position offset changes the second difference by:

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?

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.

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