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The ice-point check

A properly made ice bath gives 0 °C to within a few millikelvin — a cheap, repeatable way to watch a PRT for drift between calibrations.

CalibrationValiTrac AI editorialUpdated 2026-09-173 min read

An ice point is a slurry of shaved ice made from clean water, in an insulated container, with just enough water to fill the gaps and no free water at the bottom. Made carefully it realises 0 °C closely enough for most industrial purposes.

Using it

  • Immerse the probe to sufficient depth in the slurry, away from the walls, and allow it to stabilise.
  • Compare with the value recorded at the last calibration (or with the certificate's 0 °C correction).
  • A shift larger than the check's uncertainty indicates drift or damage and should trigger investigation.

The check does not replace calibration — it tests one point — but a PRT that holds its ice point is unlikely to have drifted grossly elsewhere, and a record of checks strengthens the case for the calibration interval.

Making one that is actually at 0 °C

The ice point is cheap and repeatable, and it is also easy to make badly. A glass of water with ice cubes floating in it is not an ice point; it is stratified water somewhere between 0 and 4 °C, and a probe in it can read half a degree high. The difference between a good bath and a bad one is entirely in the preparation.

What matters, and what happens if you skip it
StepWhyError if skipped
Shaved or finely crushed ice, not cubesSmall particles pack without voids and keep the whole volume at the transitionUp to several tenths of a degree
Pure water for the ice — distilled or deionisedDissolved solids depress the freezing point0.01–0.1 °C, more with tap water
Insulated container (a Dewar)Slows melting and stops the outside warming the slurryDrift over the measurement
Pack tightly, then add just enough cold water to fill voidsAir pockets are insulators; free water is not at 0 °C0.1 °C or more
No free water at the bottomDenser water at 4 °C collects there and the probe sits in itUp to 0.4 °C, and always in the same direction
Adequate immersion, away from the wallsStem conduction from a 20 °C roomTenths of a degree with a short probe
What matters, and what happens if you skip it

Made properly the ice point realises 0 °C to within a few millikelvin, which is better than almost any working reference in the building, for the cost of a Dewar and some ice.

Reading it as a trend

A single ice-point reading proves very little. The value comes from charting it: the same probe, the same procedure, monthly, plotted. A drift then becomes visible as a trend long before the annual certificate reports it, and the chart is also the evidence for extending or shortening the calibration interval.

Set a decision threshold in advance. A shift larger than the certificate uncertainty at 0 °C is the usual trigger to investigate; a shift approaching the tolerance is a trigger to withdraw the instrument and recalibrate. Deciding the threshold after seeing a worrying reading is the same mistake as choosing a decision rule after seeing a borderline result.

What it does and does not tell you

  • It tests one point. A PRT that holds its ice point is unlikely to have drifted grossly elsewhere, but unlikely is not evidence for a certificate.
  • It is a check, not a calibration: no uncertainty is evaluated and no traceability link is created. It cannot extend an interval by itself.
  • It catches the failures that matter most — a knock, a thermal shock, moisture ingress — because those move the ice point first.
  • For a thermocouple it is far less informative, since the reference junction and the wire's thermal history dominate and an ice point exercises neither.

Frequently asked questions

How do you make an ice point?
Shave or crush ice made from distilled or deionised water, pack it in an insulated container, add just enough cold clean water to fill the gaps, and immerse the probe deeply, away from the walls, until stable.
How accurate is an ice point check?
A careful ice bath is within about 0.002–0.005 °C of 0 °C. Common errors — tap water, large cubes, free water, shallow immersion — can add tens of millikelvin.

References

  1. [1]ISO/IEC 17025:2017 — General requirements for the competence of testing and calibration laboratories

General technical guidance written against the cited sources. It is not regulatory or legal advice and does not replace the applicable standard, guideline or a qualified reviewer's judgement.

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