There is no single 'damp meter' that reads true moisture everywhere. Different instruments measure different things — electrical resistance, dielectric properties, air humidity, true water content — and each is reliable only within its limits. Competent moisture investigation combines several methods and reads them against each other, rather than trusting one number.

Moisture measurement methods compared
MethodWhat it measuresKey limitation
Resistance (pin) meterElectrical resistance (relative)False-high on hygroscopic salts; relative on masonry
Capacitance meterDielectric response (relative)Shallow depth; affected by density/metals
Calcium carbide (CM) testTrue total moisture contentDestructive (drilled sample)
Gravimetric (oven-dry)True moisture content + salt analysisLab method; sampling required
RH / temperature loggerAir humidity & temperature over timeMeasures air, not the wall
Interstitial probeT/RH inside the constructionRequires drilling / embedding
Thermal imagingSurface temperatureLocates, doesn't quantify moisture

Resistance (pin / conductivity) moisture meters

The familiar two-pin meter measures the electrical resistance between its pins — wetter material conducts better, so lower resistance reads as higher moisture. It is genuinely useful in timber, for which these meters are calibrated and where they give a reasonable estimate of moisture content. But used on masonry and plaster, the readings are relative indicators, not true moisture content, and they have a notorious failure mode:

Capacitance (non-invasive) moisture meters

Capacitance (or dielectric) meters press a flat sensor against the surface and measure the material's dielectric response, which varies with moisture — without pins, so no damage. They are excellent for quickly mapping the relative distribution of moisture across a surface (finding where it's wetter), and for non-destructive scanning. Their limits: they read only a shallow depth, they're affected by the material's density and by metals/foils behind the surface, and like resistance meters they give relative comparisons, not absolute moisture content. Use them to map, not to quantify.

Reference tests: carbide and gravimetric

When you need the true moisture content of masonry — for example to confirm or refute a rising-damp diagnosis — you take a physical sample and use a reference method:

  • Calcium carbide (CM / 'speedy') test: a drilled sample is mixed with calcium carbide in a sealed pressure vessel; water reacts to produce acetylene gas, and the pressure indicates the moisture content. It's a recognised on-site method giving true total moisture content, unaffected by salts.
  • Gravimetric (oven-dry) test: a sample is weighed, oven-dried to constant mass and reweighed; the weight loss is the water. This is the laboratory reference standard for moisture content — and, with further analysis, can distinguish capillary moisture from hygroscopic (salt-held) moisture, which is decisive in diagnosing rising damp.

RH and temperature data loggers

For condensation and mould problems, the most important measurements aren't of the wall at all — they're of the air. Logging room air temperature and relative humidity over a representative period (days, capturing the cooking/showering/sleeping cycle) characterises the indoor environment, reveals humidity spikes, and — combined with surface temperatures — lets us calculate dew point and surface RH. A single spot RH reading is almost worthless because humidity swings constantly; the logged trend is what tells the story.

Interstitial probes and embedded sensors

To investigate moisture inside a construction, sensors can be placed within the build-up: temperature and RH probes inserted into drilled holes, or wood-moisture and relative-humidity sensors embedded at the cold face of insulation or in sensitive timber. On monitored retrofits these provide real, long-term, in-situ data on whether a wall is wetting up or drying out — the ground-truth that validates (or challenges) the hygrothermal model.

Thermal imaging — locating, not quantifying

A thermal camera measures surface temperature, not moisture directly — but it's invaluable in moisture work. Evaporating moisture cools a surface, so damp areas often show as cooler patches; cold spots reveal the thermal bridges where condensation forms; and under blower-door depressurisation, air-leakage paths (which carry moisture) light up. Thermal imaging finds the where and the why quickly across a whole surface, which you then confirm and quantify with the contact methods above. (See the Thermal Imaging guide.)

The combined approach