Dalton Concrete ProsConcrete in Dalton, GACall (770) 285-0629

Why concrete driveways flake in north Georgia

Flaking is freeze thaw scaling. Water sits in the surface pores, expands each time it freezes, and lifts the top few millimetres away in sheets. North Georgia runs sixty to eighty freeze thaw cycles a year, and the mix that resists it has to be ordered air entrained before the pour.

What is actually happening to the surface?

Water is freezing inside the concrete, not on top of it.

Concrete is porous. A finished slab looks solid but the surface holds a network of tiny voids, and those voids fill with water every time it rains. When the temperature drops below freezing, that water expands by roughly nine percent. It has to go somewhere, and in a dense unentrained surface there is nowhere for it to go except outward, against the concrete around it.

One cycle does nothing you can see. The pressure opens the pores fractionally and the thaw relaxes it again. Repeat that sixty to eighty times a year, which is what north Georgia does, and the surface layer gradually loses its bond with the concrete beneath it.

Eventually it comes away. Usually as flakes and thin sheets a few millimetres thick, often starting in the areas that stay wet longest. The trade word is scaling, and it is a surface failure rather than a structural one.

The slab underneath is frequently fine. That is the good news and the reason this is worth diagnosing properly rather than replacing on sight.

Why does it happen here and not everywhere?

Because the number of cycles matters more than how cold it gets.

People assume this is a northern problem. It is not. What damages concrete is the transition across freezing, not the depth of the cold, and a climate that crosses that line repeatedly does more damage than one that freezes hard in December and stays frozen until March.

North Georgia is close to a worst case for this. Winters here swing above and below freezing repeatedly, day to night, week to week. Sixty to eighty crossings a year is a great many opportunities for water in a slab to expand.

Add the local ground to it. Whitfield County is red clay with pockets of chert and weathered shale, and clay holds water rather than draining it away. A slab on clay with a thin base stays wetter for longer, which means more water in the pores when the temperature drops.

What actually prevents it?

Air entrainment, decided at the concrete order.

An air entrained mix carries four to seven percent microscopic air bubbles distributed through it. When water in the surface freezes and expands, it pushes into the nearest bubble instead of against the concrete. The pressure has somewhere to go, so the bond between surface and slab is never broken.

It is a small specification with a large effect. It adds very little to the cost of a load, it does not change how the concrete looks, and it is the difference between a driveway that looks tired at five years and one that looks fine at twenty five.

It also cannot be added afterwards. Air entrainment is a property of the mix, not a treatment applied to a finished surface. A driveway poured without it will scale eventually, and nothing applied on top changes that.

If you are having flatwork poured in this part of Georgia, ask one question. Is the mix air entrained? The answer is yes or no, and it separates people who pour flatwork here from people who pour flatwork.

Should I reseal, resurface or replace?

It depends on whether the slab moves, and there is a test you can run yourself.

Stand with one foot either side of the worst crack and shift your weight. If the two sides stay level, the slab is stable and only the surface has failed. If one side moves, or already sits lower than the other, the base underneath has failed and that is a different problem.

On a stable slab, sealing is sensible maintenance. It keeps water out of the pores, which is the mechanism doing the damage. The choice of sealer matters more than people expect: a film forming sealer gives the wet look most people want, but a film that does not breathe can trap moisture underneath, and when that freezes it lifts the film and sometimes the surface with it. A breathable penetrating sealer trades some gloss for not doing that.

Resurfacing a stable slab also works. A bonded overlay of one to two inches over properly prepared concrete lasts a long time. Over a slab that moves it fails at the same lines by the second spring, because two inches cannot hold a working crack shut.

Replacement is the answer where the base has gone. A slab in pieces at different heights has nothing sound to build on, and repouring on the same base buys the same failure again a few years later.

What should a replacement get right?

The four things the original almost certainly got wrong.

An air entrained mix at four to seven percent. Four to six inches of compacted graded aggregate base, so water drains away from the underside instead of standing against it. Adequate thickness for the load, meaning four inches for cars and five or six where a work truck or trailer parks. And control joints at sensible intervals so the inevitable shrinkage cracking follows a line somebody chose.

All four are cheap while the machine is already on site and impossible once the concrete has set. Removal of the old slab runs $2 to $6 a square foot, and the new pour $8 to $16, so this is not a small job and it is worth getting the specifications named in writing.

Drainage is the fifth item and the one most often left out. A slab that holds standing water will scale faster whatever the mix, so where the water goes deserves a deliberate answer rather than whatever the grade happens to do.

Get a quote

Call (770) 285-0629, or send this.

Call (770) 285-0629