Gravimetric Air Content

Also known as air content by density · gravimetric air method · theoretical density air content · air content concrete · entrained air percent · ASTM C138 air content · air void content fresh concrete

A=TDTA = \dfrac{T - D}{T}

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Learning zone

Air content is one of the two things that decide whether concrete survives a Canadian winter — the other being the water-cement ratio — and this is the way to measure it with nothing but a scale. Work out what the concrete would weigh per unit volume if it contained no air at all, from the batch weights and the specific gravities; measure what it actually weighs; and the shortfall is air.

Why air matters is worth understanding rather than memorising. When water in a saturated paste freezes it expands by about nine percent, and if it has nowhere to go it generates hydraulic pressure in the capillary system that exceeds the tensile strength of the paste. The concrete cracks a little. It thaws, water refills the cracks, and it freezes again. Over a few dozen cycles the surface scales off and the concrete disintegrates from the outside in — and strength does not save it. A 50 MPa mix with no entrained air will fail a freeze-thaw exposure that a 25 MPa air-entrained mix shrugs off for fifty years. Entrained air is a system of tiny, closely spaced bubbles that gives the freezing water somewhere to expand into before the pressure builds. The relevant parameter is not really the volume of air at all; it is the spacing factor, the distance any point in the paste is from the nearest bubble.

That distinction matters because it is where a passing air content can still be a failing air-void system. Total air content — which is all this equation, or any pressure meter, can see — counts two quite different things. Entrained air is the deliberate, admixture-produced population of very small stable bubbles, and it is what buys durability. Entrapped air is large irregular voids that mixing folded in and vibration is supposed to remove; it costs strength and buys nothing. A mix can hit its total air target while having a poor bubble distribution, and the only measurement that distinguishes them is a hardened air-void analysis on a polished section.

The weakness of the gravimetric method is the theoretical density. The measured density is a direct weighing and it is as good as the technician. The theoretical density is calculated from the batch weights and the specific gravities, so every error in a mix design lands squarely in the answer — a wrong aggregate specific gravity, a moisture correction that did not happen, a batch weight that differs from the design. That is why the pressure method is the field standard for accepting a load, and this one is the check on the pressure method rather than its replacement.

Where the two disagree, the disagreement is information rather than a nuisance. A pressure meter needs an aggregate correction factor determined for the specific aggregate in use, and if that factor is stale the meter reads consistently off. More seriously, a pressure meter reads nonsense on a porous or lightweight aggregate, because it cannot distinguish air in the paste from air inside the stone — the very case where the gravimetric method still works. And every percent of air costs a few percent of compressive strength, so an over-aired mix is giving away strength that somebody paid for. Air content is the one specification where both directions are genuinely expensive.

Gravimetric Air Content
A=TDTA = \dfrac{T - D}{T}
TDA
Where
  • AA= Air content (%)
  • TT= Theoretical air-free density (kg/m³)
  • DD= Measured fresh density (kg/m³)
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