Nano Bubble Oxidation Technology
The whole platform rests on one physical fact: a small enough bubble stops leaving.
Put air through a diffuser at the bottom of a pond and you get a rising curtain of bubbles. Most of that gas reaches the surface and returns to the atmosphere. The bubble is a delivery vehicle with a few seconds in the water, and its surface area is small relative to the gas it carries.
Shear the same gas volume into bubbles below roughly a micron and the behavior changes completely. Buoyancy stops dominating. The bubbles carry a negative surface charge — measured in the literature at around −34 to −45 mV for oxygen nanobubbles — which keeps them from coalescing back into large bubbles. They stay in suspension. And because surface area scales against the cube of radius while volume scales against it directly, dividing a bubble into ever smaller bubbles multiplies the interface across which gas can cross into water.
The measured consequence is the number that matters. Work published in Science of the Total Environment on nanobubble aeration found the gas–liquid mass transfer coefficient rose roughly elevenfold against conventional bubbles for the same delivered gas volume.
That is the entire commercial argument for putting the equipment on a boat. You are not carrying enough gas to brute-force a bay. You are carrying gas that actually dissolves.
The stage, in order
- Intake and characterization Water is drawn in and read before anything acts on it — temperature, salinity, pH, dissolved oxygen, turbidity, and the organic load that decides how much of a pass gets spent doing nothing useful.
- Gas conditioning Oxygen, for the duty this hull is named after. A mission that needs oxidation runs under the HABslayer or ChemSlayer name and carries the discharge standard that goes with it. On a full program the gases sit inside the subscription rather than in a procurement the client has to run.
- Nanobubble generation The gas is sheared into the sub-micron range in-line. This is the step that decides whether the oxygen ends up in the water or in the air above the vessel.
- Oxidation, where a mission calls for it For organic load — bloom material, biofilm, dissolved organics — an oxidative stage does work that oxygenation alone cannot. It runs inside the reactor, on water that never stops moving, and it is operated to meet the standard set on what leaves.
- Discharge into the layer that needs it Treated, oxygen-enriched water goes back into the water it was taken from, at the depth the deficit sits at. A surface treatment on a stratified estuary in August is theater; the deficit is under the thermocline.
- Verification Inline instruments read the treatment as it runs and can cut an oxidant on their own. In-situ profiling reads what actually changed in the water, and the result feeds the next pass rather than a report written in November.
The plant moves. The water stays.
That sequence is easy to misread, so here it is flatly. Nothing is stored on a SeaBreather. Water is not collected, not held, and not carried off somewhere quieter to be dealt with. A hull of this class is specified at around 5,000 gallons a minute, which is a rate rather than a load — and at a rate like that, nothing is sitting still.
Then the part worth taking away. Treated water goes back where it came from: the same basin, the same layer, improved. Smaller and larger vessel systems are built and get deployed where a particular water calls for them, and whichever one arrives, that does not change.
So containment is a statement about the reaction rather than about the water's liberty. Enclosing a reaction is what makes a discharge figure mean anything, because a reaction with a wall around it has an inlet and an outlet somebody can put an instrument on. It was never a claim that a bay had been penned.
Bromide is the reason the treatment happens inside a hull
Ozone in seawater is not ozone in fresh water. Bromide is present at meaningful concentration and ozone reacts with it roughly eighty-three times faster than with chloride. The hypobromite that results can go on to form bromate, which is a regulated concern rather than an academic one.
How much of it forms is a property of the water, though, not a constant. Meaningful bromate needs bromide above a threshold, and salt and brackish water do not always carry one. Ozone is also indiscriminate: every dissolved carbon compound in that column competes for the same oxidant, so bromide is one demand among many. Formation conditions are therefore assessed for the water body itself, before a hull is committed to it.
Whose limit applies, and where it is written down
No standing bromate figure is published on this platform, and the omission is the point. A drinking-water rule was written for a public supply piped to a tap. Your bay is not that. Carry the number across anyway and you have answered the wrong question — including for the case people worry about most, since a desalination plant already runs equipment that handles bromate at its own intake.
So the governing value is the one that applies to the receiving water in front of you. It is set case by case with the authority consenting the work, and it goes into the service level agreement before a system is deployed. A figure printed here would become the standing commitment for every water body on earth, and it would be wrong in most of them.
Inline instruments govern the treatment while it runs and can cut an oxidant automatically. What they cannot see is a stable end-product, so periodic independent laboratory analysis confirms bromate instead. The two are complementary and neither substitutes for the other. Bromate is straightforward to read in near real time, and treatment is modulated or stopped on that reading.
Results go to the regulator that issued the consent, on the schedule that consent sets, and the oversight institution reads the same record as it lands. So does the client. Under the service level agreement the client and its qualified authorized agents may put an active deployment on hold on any suspected infraction, and it stays on hold until the concern is cleared. Rigor written into a contract beats a number printed on a website.
Which is also the answer to what happens on the harder duties, where a toxin bloom or oxidative oil work tightens the envelope. Nothing is impounded aboard while somebody signs for it, because there is no storage aboard to impound it in. The assurance sits earlier: conservative settings at the source, instruments that cut the oxidant or shut the intake before an out-of-specification discharge can form, and a laboratory confirming afterward what the probes could not see. A mission run that way does not deliver the hull's full rate. Better you hear that here than discover it in month two.
Where the science is still arguing
A 2020 study from Moleaer and Arizona State University reported that injected nanobubbles produce reactive oxygen species including hydroxyl radicals. A controlled study published in ACS ES&T Engineering in 2023 by Chae, Kim, Kim and Fortner found hydroxyl radical generation from nanobubbles to be minimal, if it occurred at all, under the ambient conditions they tested.
Both are real. They disagree. Programs are built on the mass-transfer result, which is not in dispute, and on the oxidation stage, which is engineered and instrumented. Radical generation is not in the dose model and it is not in the price.
Controls and data
A dose is a decision, and the decision is instrumented.
Fleet routing, water-column telemetry and earth observation are not a dashboard bolted on at the end. They decide where a hull goes tomorrow.
All four of these get better the longer a program runs, which is a plain argument for running one continuously. A record that only starts once the water is already bad has nothing to measure against, and a forecast built on one summer is a guess.
Hyperspectral and earth observation
Satellite and airborne ocean-color work identifies where the water is changing before a shore-side sample would. It sets the search area; it does not set the dose.
In-situ monitoring
Water-column profiles at the point of treatment. Dissolved oxygen, temperature, salinity, pH and turbidity through depth, before and after each pass.
Predictive analytics
Risk surfaces for the coming days across the service zone, so a Deep Strike goes to forming water rather than to yesterday's headline.
Fleet routing
Vessel hours are the scarce resource in any program. Routing is the difference between a fleet that covers a coastline and one that chases it.
Questions we get asked
Straight answers
What is a nanobubble?
A gas-filled bubble below roughly 1,000 nanometers in diameter. At that scale bubbles stop rising and bursting: they carry a negative surface charge, remain suspended for long periods, and present an enormous combined surface area for gas to cross into the water.
How much better is nanobubble aeration than conventional aeration?
A peer-reviewed study of nanobubble aeration measured the gas–liquid mass transfer coefficient rising approximately elevenfold against conventional bubbles for the same delivered gas volume. Site conditions vary. The mechanism does not.
Source: Science of the Total Environment — mass transfer of nanobubble aeration
Do nanobubbles generate hydroxyl radicals?
Genuinely unsettled, and the disagreement is between two serious pieces of work. A 2020 Moleaer and Arizona State University study reported reactive oxygen species including hydroxyl radicals from injected nanobubbles. A controlled 2023 study by Chae and colleagues in ACS ES&T Engineering found hydroxyl radical generation from nanobubbles was minimal, if present at all, under the ambient conditions tested.
We do not price a program on radical chemistry we cannot demonstrate on site.
Does ozonating seawater create bromate?
It can. Ozone reacts with bromide far faster than with chloride, and what that produces can go on to become bromate.
How much depends on the water. Quantity needs bromide above a threshold, which salt and brackish water do not reliably supply, and ozone spends itself on all the dissolved carbon present rather than on bromide alone. Those conditions get assessed for your water body before a hull is committed to it.
The limit that governs is then the receiving water's own, settled with the authority consenting the work and written into the service level agreement ahead of deployment. Alarivean publishes no fixed ceiling, because a drinking-water rule was not written for a bay and a figure fixed here would be the wrong one somewhere else. Monitoring runs live, an independent laboratory confirms the stable end-product, and you can put an active deployment on hold on any suspected infraction until it is cleared.
Does the treatment harm marine life in the treated water?
NOAA's National Centers for Coastal Ocean Science validated an ozone nanobubble aeration system on an eight-acre pond near Fort Myers Beach in 2018 and reported complete elimination of algae within 48 hours, with proper reoxygenation and no apparent harm to aquatic life. A separate NCCOS-affiliated evaluation of a nanobubble ozone ballast-water system found no statistically significant adverse residual toxicity in receiving water.
Both studies name other operators' equipment, not SeaBreather. They establish the mechanism and its safety at those scales. Performance on your own water is settled in the calibration phase.
Sources: NOAA NCCOS, 2018 · NOAA NCCOS, 2020
Can this replace fixing the catchment?
No, and nothing here is offered as a substitute for it. Upstream reduction is the twenty-year answer and it should be started now. What in-water treatment buys is the seasons in between — the fisheries, the beaches, the intakes and the reef that would otherwise be written off while the upstream work is legislated, funded and built.
Next step
Bring us a water column, not a brief.
Depth profiles, season, what you have already tried. Alarivean returns a read on whether this platform is the right tool for that water — including when it is not.