What §6.5 actually says

ISO/IEC 17025:2017 §6.5.1 requires that the laboratory establish metrological traceability for its measurements 'through a documented unbroken chain of calibrations, each contributing to the measurement uncertainty'. For pH, the chain usually reads: NIST or NRC primary standard → certified buffer lot → your calibration procedure → your electrode → your sample.

The clause most CALA assessors focus on is §6.5.3: the uncertainty must be documented with sufficient detail to understand what contributes to it. 'Sufficient detail' means a budget that enumerates each contribution, shows how it was estimated, and combines them according to the GUM (Guide to the expression of Uncertainty in Measurement).

This is where the gap lives. Most lab uncertainty statements for pH cover four components: buffer uncertainty, electrode slope drift, temperature compensation, and repeatability. They omit — or implicitly set to zero — the residual liquid junction potential contribution. For many sample matrices, that omitted term is larger than the other four combined.

The real budget, sorted by dominance

Figure 1. Uncertainty budget for pH measurement in an Alberta wastewater matrix (OSPW). Junction potential dominates the expanded uncertainty.
Figure 1. Uncertainty budget for pH measurement in an Alberta wastewater matrix (OSPW). Junction potential dominates the expanded uncertainty.

Five components, combined via quadrature per GUM §5.1.2, yield an expanded uncertainty of ±0.115 pH at k=2 (95 % coverage). The individual contributions:

Componentu(pH)Source
Buffer certificate (NRC, k=2)±0.005CoA from buffer supplier, converted to standard u by dividing by k
Electrode slope drift±0.008Observed variation in slope between calibrations
Temperature compensation±0.012Residual after ATC correction; ±1 °C sample/buffer temperature mismatch
Repeatability±0.006Short-term SD of 10 replicate measurements
Junction potential (sample)±0.055Estimated from matrix type — see Fig. 2

Combining: uc = √(0.005² + 0.008² + 0.012² + 0.006² + 0.055²) = 0.058 pH. Expanded U = k × uc = 2 × 0.058 = 0.115 pH. Without the junction potential term, the number would be 0.016 → U = 0.032 pH. The difference is not small. It is 3.5×.

Why the junction potential term changes so dramatically with matrix

The liquid junction is where the calibration buffer (typically 3 M KCl inside the reference) meets the sample. Ideally the two solutions would be identical in ionic composition. They never are. The resulting asymmetric ion diffusion across the junction creates a potential that the Nernst equation does not predict — the residual liquid junction potential (RLJP).

RLJP scales with how different the ionic environment of the sample is from the buffer environment. For pure NIST-style buffers (high KCl, dilute, low ionic strength), RLJP is effectively zero. For real samples, it ranges from small to dominant:

Figure 2. Residual junction potential contribution to pH uncertainty, by sample matrix.
Figure 2. Residual junction potential contribution to pH uncertainty, by sample matrix.

For drinking water and dilute effluent, RLJP is small — the sample is close to the buffer in ionic composition. For oil sands process water (OSPW), tailings pond water, and high-chloride brines, RLJP becomes the dominant uncertainty term by a wide margin.

Operational consequenceIf your laboratory reports pH for Alberta tailings pond water with ±0.03 expanded uncertainty, that number is structurally indefensible. The sample matrix alone injects ±0.06 to ±0.08 pH via RLJP. Your certificate may pass a cursory review, but a CALA technical assessor who understands electrochemistry will write it up.

How to estimate RLJP without specialized equipment

You do not need a Harned cell or a reference-grade Pt-H₂ electrode to estimate RLJP for routine work. Two pragmatic approaches:

Method A — Matrix-matched buffers

Prepare a secondary buffer set in which the background salt matches your sample. Example: for high-chloride brine samples, make secondary buffers in 3 M KCl background rather than nominal ionic strength. Calibrate with the NIST primary buffers, then measure the matrix-matched secondaries. The offset is your RLJP estimate. Publication by Baucke (2002) and Spitzer & Meinrath (2007) document the method; it is accepted for ISO 17025 uncertainty estimation.

Method B — Dilution series

For samples where you cannot prepare matched buffers, measure the sample at full strength and at 1:5 dilution in deionized water. The apparent pH shift minus the true pH shift (from activity coefficient correction) gives an RLJP estimate. Less rigorous than Method A; acceptable for routine matrices with small RLJP contributions.

Writing it up: the certificate language CALA wants

CALA technical assessors have become specific about pH uncertainty language. Avoid 'traceable to NIST via [buffer supplier]'. Instead, write:

Recommended text'pH measurements are traceable to the International System of Units (SI) through NRC (or NIST) primary pH reference solutions, via [buffer supplier] certified secondary buffers, lot [XXXX], dated [YYYY-MM]. Expanded uncertainty U = ±X.XXX pH (k=2, approximately 95 % coverage) includes contributions from: buffer certificate, electrode slope drift, temperature compensation, repeatability, and residual liquid junction potential estimated for the sample matrix [matrix type].'

That sentence is audit-survivable. It names the chain, the buffer lot, the traceability route, and the dominant uncertainty term — including the matrix dependence that a thorough assessor will ask about.

Summary