Electrical conductivity (EC) measures the ability of a water sample to carry an electrical current. It is expressed in microsiemens per centimeter (µS/cm) or millisiemens per centimeter (mS/cm). The more ions dissolved in water (e.g., sodium, calcium, chloride, sulfate), the higher the conductivity.
Conductivity is the reciprocal of resistivity. Ultra-pure water has resistivity around 18.2 MΩ·cm (conductivity ≈ 0.055 µS/cm). Tap water ranges from 100–800 µS/cm, while seawater can exceed 50 mS/cm due to high Na⁺ and Cl⁻ concentrations.
Conductivity is a rapid, cost‑effective indicator for:
A conductivity meter consists of a sensor (electrode) and a transmitter / main unit that processes the signal. The principle is based on Ohm’s law: measure the resistance between two electrodes immersed in the sample, then convert to conductivity.
But raw conductance depends on electrode geometry — that’s where the cell constant (K) comes in.
Conductivity (γ) = measured conductance (G) × cell constant (K). K = distance between electrodes (L) / effective area (A), unit cm⁻¹. Different K values suit different ranges:
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Most meters allow calibration with standard KCl solutions and automatic cell constant recognition.
The tiny electrode current is converted to voltage (I/V converter), then rectified, filtered, and often phase‑sensitive detected to eliminate capacitive interference. After ADC conversion, a microprocessor applies temperature compensation and displays the value normalized to 25°C.
Based on your application:
🧪 Pro tip: Always calibrate with fresh standard solution; keep electrodes clean and hydrated. For ultra‑pure water, use a flow‑cell to prevent CO₂ absorption from air, which raises conductivity.
Water conductivity is a fast, reliable proxy for total ion content — essential for industries from pharmaceuticals to environmental science. Behind every accurate reading is a conductivity meter that cleverly applies AC excitation, advanced electrode design, and precise signal processing to turn a simple electrical measurement into a meaningful water quality parameter. Understanding its working principle helps you choose the right instrument, interpret data correctly, and maintain your sensor for years of reliable service.
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