Contents: gravimetric method → convert water temperature to density → air buoyancy correction → accuracy vs precision, systematic vs random error. (Hand-drawn animation) Open on YouTube →
Six scenes: predict → TC/TD last drop → read the scale → weigh to get volume → significant ≠ failing → class forest plot; answer correctly to unlock the next scene. Open the lab in a new tab ↗
Testing labs must calibrate volumetric glassware regularly under ISO/IEC 17025 (the international accreditation standard for the competence of testing and calibration laboratories). The international standard ISO 4787 specifies how to calibrate glass volumetric ware by the “gravimetric method”.
Today you will verify for yourself whether your own pipette and burette are truly “accurate”.
| Instrument | Grade | Tolerance | Standard |
|---|---|---|---|
| 10 mL volumetric pipette | Class A | ±0.02 mL | ASTM E969 |
| 50 mL burette | Class A | ±0.05 mL (full length) | ASTM E287 |
| Same-capacity glassware | Class B | Tolerance is about 2× that of Class A | — |
ρair=0.0012 g/mL ρweights=8.0 g/mL ρw is obtained from the Tanaka (2001) equation — the internationally accepted “density–temperature” formula for pure water, from which the table below was calculated.
| Water temp. (°C) | 20 | 22 | 24 | 25 | 26 | 28 |
|---|---|---|---|---|---|---|
| ρw (g/mL) | 0.998207 | 0.997773 | 0.997299 | 0.997047 | 0.996786 | 0.996235 |
Mean bias and 95% CI range (floating bars) for 5 illustrative students; dashed lines are the ±0.02 mL tolerance — illustrative data, not real measurements.
| Systematic error (determinate error) | Random error (indeterminate error) | |
|---|---|---|
| Direction | Always off to the same side (always high or always low) | Sometimes positive, sometimes negative, no fixed direction |
| Cause | A specific cause can be found: instrument, method, operating habit | Many tiny variations add up; no single cause can be named |
| Which metric it affects | Mean departs from the true value → bias (accuracy) | Data scatter → SD, RSD% (precision) |
| Does repeating cancel it? | No; even the average of 100 runs is still off | The mean becomes steadier and the CI narrower, but each run still fluctuates |
| What to do | Find it → calibrate or correct (e.g., buoyancy correction Fb) | Increase replicates and describe with SD and 95% CI |
| What to calculate | Excel function | In plain words |
|---|---|---|
| Mean | =AVERAGE(range) | Add the 10 values and divide by 10 |
| SD | =STDEV(range) | The “typical” distance of each value from the mean |
| RSD% | =SD/mean*100 | SD as a percentage of the mean |
| t value | =TINV(0.05,9) | Look up n=10 to get 2.262 |
| CI half-width | =t*SD/SQRT(10) | Mean ± this number = 95% CI |
Pipette 0.2 mL, water at 32 °C, V = m×Fb/ρw (ρw=0.99503, Fb=1.0011), n=10, measured 2026-09-29.
P2:W2 (8 cells), missing X and Y.=mean/0.9956, which is just the volume conversion of mass divided by density, unrelated to the confidence interval (and it omits Fb too).Tap to tick — make sure you really can do it.