Verifying measuring devices - method comparison

Knowledge base · June 27, 2026

You buy a new online probe, switch laboratories, or want to replace an expensive lab analysis with a cheaper field measurement. Each case raises the same question: can the new method be trusted as much as the old one? The answer isn’t a gut feeling or a correlation coefficient - it’s a structured method comparison.

Correlation is not agreement

The most common mistake: “the sensor correlates with the lab at 0.99, so it’s fine.” It isn’t enough. A high Pearson r only tells you that both methods rise and fall together - yet the sensor may be systematically high by a fixed amount or a fixed percentage. Correlation won’t catch that. Assessing interchangeability of methods calls for different tools.

The toolkit that actually answers the question

  • Deming regression - a fit line that, unlike ordinary OLS regression, assumes error on both axes. When neither method is the absolute truth, this is the right choice. A slope ≈ 1 and intercept ≈ 0 mean no proportional and no constant error.
  • Identity line (y = x) - the “perfect agreement” reference. The closer the points lie to it, the better.
  • Bias (mean difference) and bias % - how far, on average, the test method departs from the reference. This is the measure of systematic error.
  • Bland-Altman plot - the difference between methods against their mean, with limits of agreement (±1.96 SD). It shows whether the discrepancy is constant or grows with concentration, and how large the differences realistically get.
  • RMSE - the typical error magnitude in measurement units.
  • N - the number of paired measurements; without enough pairs the conclusions are fragile.

What it looks like in practice

Below: verification of an online optical probe (test method) against a laboratory BOD₅ determination (reference method) on the same treated-wastewater sample:

Method comparison in LimnoLog: Deming regression and Bland-Altman plot for an optical probe versus laboratory BOD5
Method comparison in LimnoLog - Deming regression and Bland-Altman plot.

How to read it: a Deming slope of 1.01 (ideal = 1) and a bias of a few tenths of mg O₂/L mean the probe has no meaningful proportional or constant error. On the Bland-Altman plot ~95% of the differences fall within narrow limits of agreement - the methods are effectively interchangeable. Had the points been tilted or the limits wide, that would signal the cheaper method cannot safely stand in for the reference.

The decision: when are methods interchangeable

There is no single threshold - it depends on what the data are used for. Helpful questions:

  • Are the limits of agreement narrower than a difference that would matter in practice (e.g. a decision threshold or a standard)?
  • Is the bias small enough to ignore - and if not, is it constant and therefore correctable?
  • Does the discrepancy not grow with concentration (no tilt on the Bland-Altman plot)?

If the answers are “yes”, you can adopt the cheaper/faster method with a clear conscience.

In LimnoLog

The app handles this in Charts → Method comparison. All you need is to record both the test and the reference result in the same sample (session + station) - for example a telemetry-probe parameter alongside a lab determination. LimnoLog pairs the measurements automatically and computes the Deming regression, bias, limits of agreement and Bland-Altman. It’s a natural complement to sound QA/QC practice and broader statistical analysis; for continuous measurements themselves, see Telemetry and online sensors.

Start a project in LimnoLog and verify your equipment on your own data.

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