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SCIENCE · INVESTIGATE AND EXPLAIN

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 experiment

Predict

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.

Reset keeps your prediction, captures and practice history.

Mass indications with common offset

indicated mass (g)volume (cm³)02001620

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)
02
56
1010
1514
2018
2522
3026
3530
4034
4538
5042
5546
6050
6554
7058
7562
8066
8570
9074
9578
10082
10586
11090
11594
12098
125102
130106
135110
140114
145118
150122
155126
160130
165134
170138
175142
180146
185150
190154
195158
200162

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
Selected mass indication82g
Reference mass indication at 200 cm³162g
Single-sample inferred density820kg/m³
Two-volume slope density800kg/m³
Inferred additive offset2g

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.

Captures preserve recipes and replay their calculated results. They are synthetic model evidence, not physical measurements.

Understand

Declare the fluid, reference and evidence

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.

Build the algebraic model

In this original synthetic packet the true density is 800 kg/m³, equivalent to 0.8 g/cm³. The balance adds a common offset b grams after the assumed container tare. Its reading at volume V cm³ is 0.8V+b. Dividing one reading by volume therefore gives 0.8+b/V g/cm³, which depends on sample size even though the liquid does not change.

Check the original numerical packet

Use two volumes to separate slope and intercept. At 100 cm³ with a +2 g offset the indication is 82 g; at 200 cm³ it is 162 g. Their difference divided by the 100 cm³ volume difference is 0.8 g/cm³, and the inferred offset is 2 g. Retain another volume as a check: 50 cm³ should read 42 g. That check tests this disclosed linear model; it is not independent evidence of an unknown real liquid.

Challenge the assumptions and transfer

Pressure is normal force per area, a different quantity from density. A separate 20 N normal force distributed uniformly over 4 cm² produces 50000 Pa because 4 cm² is 0.0004 m². Halving that area at fixed force doubles pressure; doubling the liquid sample volume does not by itself double its density. A common multiplicative volume calibration error would not cancel from the two-volume slope as the additive mass offset does.

Worked original case

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.

Bounded investigation

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.

Changed-case numerical practice

Try the changed case before feedback

A liquid gives indicated masses 66 g at 80 cm³ and 146 g at 180 cm³, with a common additive offset. Find its density in kg/m³.

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.

Sources and limits

Original content checked 30 October 2026 against OpenStax College Physics 2e. All records are supplied or generated educational evidence. No pressure rigs, liquid handling, bodily measurements or physical exposure protocols are requested. Virtual admissibility does not certify real equipment safety, practical skill or independent mastery.

Apply

A common additive mass offset is removed by:

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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