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Conductivity Temperature Compensation Calculator

Conductivity rises about 2 % per °C in most water samples. Convert a measured value to the standard 25 °C reference, or predict the raw reading at another temperature.

Reference 25 °CLinear coefficientµS/cmWater analysis
µS/cm
°C
% per °C
°C
Conductivity at 25 °C1,000 µS/cm
In mS/cm1
Compensation factor1.2
How this result was calculated
  1. Factor = 1 + α × (T − Tref) = 1 + 0.02 × 10 = 1.2
  2. κref = κT ÷ factor = 1,000 µS/cm
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Linear Temperature Compensation

κ25 = κT ÷ [1 + α × (T − 25)]

α is about 1.9 to 2.1 %/°C for most natural waters and salt solutions. Acids, alkalis and ultrapure water have different and nonlinear coefficients.

Worked example

1200 µS/cm measured at 35 °C with α = 2 %/°C corresponds to 1200 ÷ 1.2 = 1000 µS/cm at 25 °C.

Key insight: for pure water below about 1 µS/cm the coefficient can exceed 5 %/°C and is strongly nonlinear; use the analyser’s ultrapure water compensation mode instead of a linear α.
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Frequently Asked Questions

Why is conductivity referenced to 25 °C?

Conductivity changes about 2 % per °C, so readings must be referred to a standard temperature to be compared.

How do I find α for my sample?

Measure the raw conductivity at two temperatures and calculate α = (κ₂ − κ₁) ÷ [κ₁ × (T₂ − T₁)] relative to the reference.

Does compensation affect accuracy?

Yes. A wrong α causes an error that grows with the difference between sample and reference temperature.

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