Infer liquid density without confusing it with a balance offset
A fluid changes shape under sustained shear rather than supporting a fixed shear deformation like an ideal elastic solid. Liquids and gases both qualify, but an incompressible-liquid approximation treats density as unchanged across the selected pressure range. Density is mass per volume, not weight per volume. A sample can have larger mass without being a denser material.
Learning outcome: Compare two offsets across three volumes. Save one-sample ratios and two-volume slope estimates, reserve the third volume as a check, and identify which calibration error the method cancels and which it does not.
Starting recap
Declare density, pressure reference, flow regime and admissible force constraints. Convert area and volume units before balancing forces, mass or energy.
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Try
With 150 cm³ and offset −4 g, the indication is 116 g and the one-sample density is 773.333 kg/m³. Comparing with 156 g at 200 cm³ recovers 800 kg/m³.
Open the experimentPredict
A common additive mass offset is removed by:
Experiment
Compare two offsets across three volumes. Save one-sample ratios and two-volume slope estimates, reserve the third volume as a check, and identify which calibration error the method cancels and which it does not.
Separate density from balance offset
Worked teaching model · synthetic values · Synthetic incompressible liquid density 800 kg/m³. Exact volume; every mass reading has the same additive offset. No container mass remains after ideal tare. Compare the selected sample with one of volume 200 cm³.
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Mass indications with common offset
Unlike graph quantities rescale independently; read units and values, not screen angles. 1: synthetic scale (solid). Joined curves show the supplied model, not additional observations.
Equivalent numerical coordinates for Mass indications with common offset
synthetic scale
| volume (cm³) | indicated mass (g) |
|---|---|
| 0 | 2 |
| 5 | 6 |
| 10 | 10 |
| 15 | 14 |
| 20 | 18 |
| 25 | 22 |
| 30 | 26 |
| 35 | 30 |
| 40 | 34 |
| 45 | 38 |
| 50 | 42 |
| 55 | 46 |
| 60 | 50 |
| 65 | 54 |
| 70 | 58 |
| 75 | 62 |
| 80 | 66 |
| 85 | 70 |
| 90 | 74 |
| 95 | 78 |
| 100 | 82 |
| 105 | 86 |
| 110 | 90 |
| 115 | 94 |
| 120 | 98 |
| 125 | 102 |
| 130 | 106 |
| 135 | 110 |
| 140 | 114 |
| 145 | 118 |
| 150 | 122 |
| 155 | 126 |
| 160 | 130 |
| 165 | 134 |
| 170 | 138 |
| 175 | 142 |
| 180 | 146 |
| 185 | 150 |
| 190 | 154 |
| 195 | 158 |
| 200 | 162 |
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 |
|---|---|---|
| Selected mass indication | 82 | g |
| Reference mass indication at 200 cm³ | 162 | g |
| Single-sample inferred density | 820 | kg/m³ |
| Two-volume slope density | 800 | kg/m³ |
| Inferred additive offset | 2 | g |
An additive mass offset biases a mass-to-volume ratio but cancels from a two-volume difference.
rho=m/V requires consistent units: 1 g/cm³=1000 kg/m³. A slope of mass versus volume separates a constant offset from density, provided the liquid, tare offset and volume calibration remain unchanged. Two points do not independently test linearity; retain a third volume as a check.
Predict before inspecting the values. Save contrasting records with assumptions and one alternative explanation. This virtual display does not certify practical measurement technique.
An additive mass offset biases a mass-to-volume ratio but cancels from a two-volume difference.
rho=m/V requires consistent units: 1 g/cm³=1000 kg/m³. A slope of mass versus volume separates a constant offset from density, provided the liquid, tare offset and volume calibration remain unchanged. Two points do not independently test linearity; retain a third volume as a check.
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Understand
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Public practice checks a specific claim. It does not establish independent mastery.
Why does an additive balance offset have a larger relative effect on a small sample?
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