How REALice works

Great ice starts with better floodwater

Rinks flood with hot water for one reason that matters: it holds almost no trapped air. For decades the rule has been hot floodwater on cold ice. Hot water spreads well and freezes clear, and it earned its place. But every 140–160°F flood also puts heat and moisture into a building that is working hard to stay cold and dry, and the refrigeration plant then has to take all of it back out. The traditional method solves a water-quality problem by creating a refrigeration problem. REALice separates the two: it gives the water the properties that made hot water useful, without the heat.

THE OLD RULEHot floodwater + cold ice = good ice
→
WITH REALICEConditioned floodwater + warmer set points = better ice
No powerPowered by water pressure only (minimum 45 psi static for the R10X, 55 psi for the R12X)
No moving partsNothing to wear, service or replace
No chemicalsNot a filter, not a softener
Made in SwedenDeveloped, 3D-printed and quality-controlled by Watreco AB. Five-year warranty.

Water without trapped air

What hot water was doing

Tap water carries undissolved air as micro bubbles. Freeze it as it comes and the bubbles stay in the ice: it turns cloudy and brittle, chips under skates and needs more floods to repair. Heating the water drives that air out, which is why hot floods freeze clear and hard. The heat is not what makes good ice; the air removal is. A rink pays twice: once to heat the water, once to pull that heat back out of the slab.

What REALice does instead

REALice removes the same micro bubbles with water pressure instead of heat, in a unit on the fill line to the resurfacer; the three stages are described below. The water that reaches the ice is de-aerated, slightly less viscous, and no warmer than it needs to be: cold tap water, tempered if the rink prefers, but never above 68°F.

Cold water alone makes poor ice. Operators who tried it before have the cloudy sheets to prove it. The point is not cold water; it is water without trapped air.

What REALice is not

  • Not a water softener or reverse-osmosis system. It does not remove minerals; it removes trapped micro air bubbles. Hard source water still needs its own treatment, though REALice changes how the hardness behaves. Effects on hard water →
  • Not a chemical additive. Nothing is added to the water, and nothing is taken out except the trapped air.
  • Not a filter. There is no medium to clog or replace.
  • Not a reason to run the plant colder. The electricity saving comes from running the brine warmer, not colder.

How the system conditions the water

The vortex forming in a clear tube.
REALice system cut open, showing the preformer, vortex chamber and outlet
The system cut open: preformer, vortex chamber and outlet.

REALice uses water pressure to remove the micro air bubbles from the floodwater before it reaches the resurfacer. It does this in three stages:

  1. The preformer guides incoming water into a tornado-like rotation and splits it into channels, each shaped to form its own vortex.
  2. The vortex chamber winds those vortices into one strong, stable vortex, the way a rope is spun from threads. Along its axis the pressure drops sharply.
  3. Deaeration. The undissolved micro-bubbles are drawn into the low-pressure core, where they expand and merge into larger bubbles that separate from the water downstream. A sight glass after the system shows them collected into a visible central stream.

Where the air goes →

The three-part penalty of hot water

Every flood gives the refrigeration plant three jobs. One of them is the same for any water. The other two get bigger the hotter the flood is and the colder the rink is kept.

1Cooling the flood to freezing

A 160°F flood has to be brought all the way down to 32°F before any ice can form. The hotter the water, the bigger this job.

2Freezing it

Turning 32°F water into 32°F ice. This takes the same energy for hot or cold water, so it doesn't change.

3Chilling the ice to rink temperature

The new ice then has to be pulled down to the operating set point. The colder the set point, the bigger this job.

Cold conditioned water almost removes job one: there's no hot flood to cool down. And because the ice it makes is harder, the rink can run a warmer set point, so job three gets smaller too. Less work for the compressors means less electricity, on top of the gas that no longer heats the water.

Measured

What changes in the water

The Polymer Technology Group at Eindhoven University of Technology tested REALice-treated water against untreated water from the same supply, in three batches:

  • Viscosity: 3–17% lower, depending on the batch, with the strongest result in freshly treated water.
  • Heat capacity: about 5% higher.
  • Electrical conductivity: about 3% higher, consistent with the air being removed.
  • Surface tension: unchanged.

Lower viscosity is why treated cold water spreads and levels the way hot water does. Fewer undissolved bubbles is why it freezes with fewer tiny air pockets. Together they replace the two things hot water was being used for.

The conditioned state holds for about a day. Fill the resurfacer at the end of the night and it's ready in the morning; there's no need to dump and refill. Water that sits for days or gets moved around picks up air again, which is why REALice belongs at the fill station, not upstream of a storage tank, and why the resurfacer shouldn't be trickle-filled.

PTG Eindhoven, 2011. Vortex Process Technology brief (PDF)

Measured

What changes in the ice

Crystal structure. Treated and untreated municipal water from the same supply were frozen side by side and thin slices examined under cross-polarized light, with the imaging done at Luleå University of Technology. The untreated sample was fragmented and irregular; the REALice sample showed larger, more uniform, more consolidated crystals. The report was written by the manufacturer, Watreco.

Hardness. Southern California Edison tested two rinks with a Schmidt hammer before and after REALice. Readings were as good or better after, and far more uniform across the sheet. The hammer measures rebound hardness, not density; the result is consistent with denser ice but doesn't measure it. The evidence in full →

Ice crystals under cross-polarized light: untreated water on the left, REALice-treated water on the right
Untreated (left) and REALice (right). Imaging at Luleå University of Technology, 2011.
In progress

Further independent measurement of REALice-treated water and ice is under way at the University of Massachusetts Amherst. Results will be published here when released.

The new operating philosophy: REALice ice needs to run warmer

The biggest electricity saving comes from the set point: warmer brine, fewer compressor hours. Years of hot-water flooding have taught technicians that 22–24°F is the ceiling for hockey ice, and with hot water it is. De-aerated water changes that. The ice is harder and more consolidated to start with, so it can run warmer and be better for it; O.R.F.A. puts the best blade-to-ice glide at 28°F. A warmer set point isn't weaker ice. Once the rink is dialled in, it's the correct temperature for a stronger sheet.

The crew finds the sweet spot by raising the set point in small steps over several days and watching the ice; once found, it's the baseline for the following season. That change in habit is the real work of the first weeks, and it is the one that has to happen: leave the set point where it was and the ice is too hard and chips, and most of the electricity saving never appears. Operator training and certification comes with every system, for the whole crew and for the people who replace them.

Carleton Place Arena found 26°F with a 1°F differential too cold and 27°F too warm, and their controls only moved in whole degrees. They ran 26°F with a 2°F return differential instead and got the ice they wanted. REALice doesn't replace the technician's judgement; it rewards it.

Operator tests

Signs the ice is still too cold

The rink tells you. If the set point is still too low for conditioned water, you'll see:

  • Heavy snow from normal skating
  • Easy scarring and surface scratching
  • Ridges between resurfacer pass lanes, because the first pass freezes before the next overlaps it
  • A cold puck that slows too quickly and won't run cleanly to the far end
  • Dry shavings like artificial snow that won't form a snowball

Each of these is a reason to go up a step, not down. Conditioned water freezes readily, and kept too cold it flash-freezes; the symptoms above are what that looks like.

What this means in the rink

What operators seeWhat's behind itBasis
Water spreads and levels differentlyLower viscosity: the flood spreads evenly without heat.Measured (PTG)
Ice feels harderFewer air pockets and larger, more uniform crystals make a more compact layer.Measured (SCE); imaging (Luleå)
Less snow, fewer scars, faster recoveryA stronger surface breaks down less under blades, once the set point is at the sweet spot.Operator-observed
Clear ice; lines and logos sharpNo micro-bubbles in the water to scatter light in the ice.Measured (PTG) and observed
Less humidity, fog and frostNo hot-water moisture spike at every flood; the dehumidifier and ventilation have less to do.Operator-observed
Brine set point 3–5°F warmer with no loss of qualityCold floods put far less heat into the slab, and the ice is harder to begin with.Operator-observed; metered as electricity savings
No scale in nozzles, lines or tankHardness minerals form loose aragonite crystals that wash through, instead of calcite scale that bonds to pipes and nozzles.Water chemistry; observed. Hard water →

That is the mechanism. For what it produced in real rinks — FortisBC's ten-rink verification, Uxbridge's sub-metered twin pad, Caledon, Kitchener — with the method behind every number, see measured results.

Why less snow matters

Snow isn't just an ice-quality issue. Every shovel of snow the resurfacer removes is surface that has to be replaced with new floodwater, which has to be frozen again, which is plant load, water, operator time and blade wear. Harder ice at the right temperature sheds less, so the resurfacer takes less off and puts less back. Better water makes better ice, better ice makes less snow, less snow needs less replacement water, and less replacement water is less refrigeration. The energy saving is the end of that loop, not the start of it.

Ice cleans with cold water

One adjustment: conditioned cold water doesn't melt snow and debris out of scars the way hot water does. Use the resurfacer's wash-water function on every ice clean so the scars are flushed before the new flood goes down. If the machine has no wash water, cut slightly more ice during the clean to remove that material mechanically. It's a small change in practice, and it's the one that matters most in the first weeks.

Installation and operating requirements

  • Installed inline on the resurfacer fill line, on both the cold and hot water lines with a mixing valve or ball valves, so warmer water stays available for other tasks around the bay. A plumber does it in a day.
  • Powered by water pressure only; no electrical connection at the system. Minimum static pressure at the fill station: 45 psi for the R10X, 55 psi for the R12X; a booster pump covers rinks that fall short. The pipe after the REALice must be the same size as the pipe going in.
  • No filtration needed with potable water. If a sediment pre-filter is already in place, keep it, installed upstream of the REALice.
  • One system can serve a twin pad on a shared feed.

Best practice

  • Use treated water for all floodwater, and don't trickle-fill the resurfacer.
  • Raise the ice temperature gradually after installation and watch snow, scarring, pass-lane ridging, puck glide and shavings.
  • Use wash water on every ice clean.
  • Keep ice thickness in the target range; thick ice insulates the surface from the plant and feels soft regardless of the water.
  • All of the above is covered in the REALice Ice Meister course, included with every system.
  • If cloudy or milky water appears on older equipment, inspect the tank for legacy scale before blaming the water. Why that happens →

Common objections

"Cold water makes brittle ice."

Untreated cold water does, if it's simply swapped for hot without changing anything else. Conditioned water is different and needs a warmer set point. Snow, scarring and pass-lane ridges after the switch mean the rink hasn't reached its sweet spot yet, not that the water is wrong.

"It needs a perfect rink."

No two rinks are alike: old barns, poor insulation, air leaks, humidity, slab condition. REALice doesn't need ideal conditions; it gives the operator better water and a clear way to adjust the rink around it.

"Some rinks still need warmer water."

Some use lukewarm water during transition, in very cold buildings, or where towel freezing is a concern. That still saves most of the energy of a 160°F flood. The direction of travel is toward the lowest floodwater temperature the rink supports.

"Hot water melts the surface so the new layer bonds."

It does melt a skin, and that skin refreezes with the flood. But a layer bonds when the flood freezes into the surface rather than on top of it, and what prevents that is ice that is too cold: the flood flash-freezes before it has spread, the same cause as pass-lane ridges. De-aerated water spreads thinner and more evenly, and at the warmer set point it freezes into the sheet. Flush the scars with wash water on every clean and the layers bond.

"Operators lose control."

The opposite. The technician still controls thickness, set points, cut depth, water volume, wash water and blade condition. REALice improves the input so those decisions produce better ice with less energy.

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