There is no single right purity for chamber water. The number you need flips depending on which humidifier sits behind it. Getting it backwards either dusts the chamber or kills the boiler.
A specification for humidifier water usually reads as one line: deionised water below five microsiemens per centimetre. The line is correct for two of the three common humidifiers. For the third it is a recipe for a dead machine. The purity a chamber needs is not a property of the chamber at all. It is a property of the humidifier inside it, since one type relies on the very minerals the others must shed. Reading the spec without reading the humidifier behind it leads a laboratory to feed pure water into a boiler that cannot use it, or hard water into an atomiser that throws the minerals straight onto the specimen.
Pure water barely conducts electricity. Its conductivity comes almost entirely from dissolved ions, the calcium, magnesium, sodium, chloride that ordinary water carries, so a conductivity reading is a direct measure of how much mineral the water holds. The cleaner the water, the fewer the ions, the lower the conductivity. This makes a single cheap meter a stand-in for a full chemical assay.
The figure is quoted in microsiemens per centimetre. Tap water reads a few hundred of those units, carrying its full mineral load. Deionised water for a humidifier runs below five. Ultrapure water, the kind a semiconductor fab uses, reaches 0.055 microsiemens per centimetre, the conductivity of water with almost nothing dissolved in it at all. The span from tap to ultrapure covers four orders of magnitude, all of it readable on one instrument.
A worked reading makes the scale tangible. A hard tap supply at 400 microsiemens carries roughly 250 parts per million of dissolved solids, a heavy mineral load by any humidifier’s standard, since dissolved solids run near two-thirds of the conductivity figure. The same water through a deioniser leaves at under five microsiemens, a drop of nearly a hundredfold, carrying a few parts per million at most. The meter shows that cut in a single reading, the proof the treatment worked before any water reaches the chamber. A reading that fails to fall is a deioniser already spent.
The mineral that conductivity counts is the same mineral that builds scale. Hardness counts the calcium with the magnesium, quoted as parts per million of calcium carbonate, the figure a water report leads with. Soft water runs under 60 parts per million, hard water above 120, the hardest supplies well past 300. Every one of those parts becomes a candidate for scale wherever the water is heated or evaporated.
Scale forms because heating drives a chemical shift. Warm water holds less dissolved carbon dioxide, so heating tips dissolved calcium bicarbonate into solid calcium carbonate, the hard crust that lines a boiler element. The hotter the surface, the faster the crust grows, which is why a steam generator scales hardest at its element. A millimetre of scale insulates that element, forcing it hotter to hold output, shortening its life. The hardness figure on the water report predicts that crust before a single litre boils.
Engineers put a sharper number on the tendency with the Langelier Saturation Index, a figure computed from the water’s hardness, its alkalinity, its pH, its dissolved solids, read at the working temperature. A positive index marks water that tends to deposit scale, a negative index water that tends to dissolve it, a zero sitting at balance. A humidifier fed water with a strongly positive index crusts its element fast. The index turns a water report into a forecast of how hard a given supply will scale a boiler before that boiler ever runs.
Conductivity has a mirror image called resistivity, the same property read the other way round. Where conductivity counts how easily current passes, resistivity counts how strongly the water resists it, so the two are reciprocals: one microsiemens per centimetre equals one megohm-centimetre. The five-microsiemens humidifier spec is therefore the same as a resistivity of 0.2 megohm-centimetre. Ultrapure water at 0.055 microsiemens reads 18.2 megohm-centimetre, the figure a purity datasheet usually quotes.
The reading carries a temperature trap worth knowing. Water conductivity climbs steeply as the water warms, by a couple of percent for every degree, so a sample read warm shows a higher number than the same water read cool. A meaningful figure is always quoted at 25 degrees, the reference temperature, with a good meter compensating automatically back to it. A conductivity number with no temperature behind it is missing half its meaning.

The deionised-water spec turns on its head the moment an electrode steam generator is involved. An electrode boiler makes steam by passing mains current through the water itself, using the water’s own resistance to heat it, so the water has to conduct for the machine to function at all. The current it draws, the steam it makes, both depend directly on the conductivity of the water filling the cylinder. Such a boiler is designed to run on water in a conductive band, on the order of 125 to 1250 microsiemens per centimetre, ordinary potable or lightly treated water that carries enough ions to pass current. The boiler even tracks that conductivity as the water level rises, modulating its steam output by how much electrode surface the water covers, the entire control scheme built on the water carrying current. Feed it deionised water below five microsiemens, almost no current flows. The boiler sits cold, drawing a trickle, making little or no steam, a machine rendered inoperable by water that is too clean. This is the trap the one-line spec sets: a maintenance engineer reads deionised below five, installs a deioniser to protect the chamber, stopping the humidifier dead. The minerals the deioniser strips out are the very thing the electrode boiler needed. For this humidifier the right water is the opposite of pure, clean enough to limit scale, conductive enough to boil, a middle band away from either extreme. Get the type wrong here, no amount of purity helps, because purity itself is the fault.
A resistive steam generator works the other way. It heats the water with an immersed electric element, much like a kettle, raising the water to its boil by radiant heat regardless of what the water carries. Its steam output does not depend on conductivity at all, so it runs the same on deionised water, on reverse-osmosis water, on potable water. The ion content is irrelevant to how it boils.
This freedom is why a resistive boiler accepts the pure-water spec without trouble. Running it on deionised water below five microsiemens brings a real reward, since the absence of minerals means almost no scale builds on the element, stretching the interval between descaling tasks. The pure-water line that kills an electrode boiler is exactly the line a resistive boiler prefers. The same words, the opposite outcome, decided entirely by which boiler reads them.

The ultrasonic atomiser makes the purest-water demand of the three. It does not boil the water, so it cannot leave minerals behind in a vessel. It throws the water into the air as a fog of fine droplets, carrying whatever the water holds along with them. When a droplet evaporates, its dissolved minerals stay airborne as a fine white dust that settles across the chamber, onto the specimen, into the surfaces a test is reading.
For this source the deionised-water spec is a condition of validity, not a refinement. Run an ultrasonic bath on tap water, it powders the chamber within hours, ruining any test that depends on a clean specimen surface. The five-microsiemens line keeps the dust away, the lower the figure the cleaner the result. An ultrasonic source is the one humidifier where even the standard spec is a ceiling worth beating.
Match the water to the humidifier, never the humidifier to the water, because one boiler needs the ions the others have to lose.
Conductivity is a strong proxy, not a complete one. It reads ionised content well, the dissolved salts that carry current, so it catches the minerals that scale a boiler or dust a chamber. It stays blind to several things that still matter. Dissolved silica carries almost no charge, so a water can read low on conductivity. It can still hold silica that bakes into a glassy scale of its own on a hot element.
Two more contaminants slip past the meter. Organic matter, measured separately as total organic carbon, adds little conductivity. It still feeds the microbial growth that fouls a standing supply. Fine particulate passes a conductivity check untouched, then blocks the small orifices of an injection line or an ultrasonic bath. A laboratory chasing the lowest conductivity sometimes forgets these three, so a careful water spec names silica, organic carbon, particulate alongside the headline microsiemens figure. The single number is necessary, far from sufficient.
A common confusion sits between softening and deionising, two treatments that do unlike jobs. A softener swaps the hardness ions, the calcium, the magnesium, for sodium, so it pulls out the scale-forming minerals. It leaves the sodium behind in their place, so the water stays fully conductive, its total ion content barely changed. Softened water reads almost the same conductivity as the hard water it came from.
That difference decides which humidifier each treatment suits. An electrode boiler runs happily on softened water, the sodium carrying its current as the softening holds back the worst of the scale, a clean match. An ultrasonic source gains nothing from softening, since the sodium left behind still flies into the chamber as dust, so an ultrasonic bath calls for deionising in its place. Reading softened water as deionised water is the error that scales an electrode boiler under the wrong cure, or dusts a chamber someone believed protected.
Two processes produce the water a humidifier spec calls for. Ion exchange runs the water through resin beds that swap its mineral ions for hydrogen and hydroxide, which combine into pure water. A cation resin trades the metal ions, the calcium, magnesium, sodium, for hydrogen. An anion resin trades the acid ions, the chloride, sulphate, carbonate, for hydroxide. A mixed bed packs both resins together, driving the conductivity down toward the single digits the spec calls for. Reverse osmosis takes a different route, forcing the water through a semi-permeable membrane under pressure, the membrane holding back the bulk of the dissolved solids, a good unit rejecting well over 95 percent of them in one pass. A polishing ion-exchange stage after reverse osmosis reaches the lowest figures where a test demands them.
Reverse osmosis splits its feed into two streams, the clean permeate that passes the membrane, the concentrate that carries the rejected solids to drain. A typical unit recovers perhaps half to three-quarters of its feed as permeate, sending the rest down the drain with the minerals. That reject ratio is the running cost of the method, water spent to make water clean. A site weighs it against the resin a pure ion-exchange plant would burn through otherwise, the cheaper route depending on how hard the feed water starts.
The choice between them follows the duty. Reverse osmosis suits a steady bulk demand, running continuously to a storage tank, its membranes lasting years on a clean feed. Ion exchange suits a smaller or sharper demand, its resin recharged or replaced as it exhausts. Many laboratories run reverse osmosis first, ion exchange second, the membrane carrying the bulk load while the resin polishes the last of the ions out.
The water spec only matters at the volume a real test consumes, which is larger than most expect. A chamber holding a high humidity at a warm temperature evaporates water continuously, the moisture leaking out through seals, through the door on every opening, through the load itself. A mid-size chamber running an 85-degree, 85-percent soak can drink on the order of one to a few litres an hour, every hour, for the length of the test. A thousand-hour humidity test then runs through thousands of litres of treated water.
That volume sets the deioniser, not the chamber. A treatment sized for a quick top-up exhausts its resin partway through a long test, its outlet conductivity climbing while the test still has weeks to run. Sizing the supply against the chamber’s hourly draw, multiplied by the longest test it serves, keeps the water in spec from the first hour to the last. A laboratory that sizes the deioniser to the bottle, ignoring the duty, runs out of pure water before the specimen runs out of test.
The purity demand climbs with the severity of the test. An ordinary damp heat soak forgives a little drift in the water. A pressurised test punishes it, since the harshest humidity methods concentrate whatever the water carries. Highly accelerated stress testing, the HAST method that runs near 130 degrees at 85 percent humidity under pressure, drives water hard into a sealed vessel where any mineral content has nowhere to escape, settling onto the specimen or into the chamber walls.
These methods specify deionised water for a reason beyond housekeeping. At their temperatures, under pressure, a trace of mineral that a mild test would ignore plates out as a visible deposit, corrupting a semiconductor package the test is meant to qualify. The water purity becomes part of the test’s validity, written into the method, audited with the result. A HAST run on doubtful water is a HAST run worth repeating.
Deionised water does not stay deionised on its own. The resin in an ion-exchange bed holds a finite capacity, so as it fills with the ions it has captured, its output conductivity climbs back up, the water leaving it growing steadily less pure. A bed run past its capacity passes minerals straight through, feeding the humidifier water that no longer meets the spec, the label on the tank still reading deionised.
The guard against this is a conductivity monitor on the outlet. A meter reading the water as it leaves the treatment, alarming when the figure crosses the spec, catches an exhausting bed before it contaminates a run. A laboratory that trusts a deioniser without watching its outlet learns of the exhaustion only when a specimen shows dust or a boiler shows scale, long after the water went out of spec. The meter turns purity from an assumption into a measured, logged fact.
The resin gives warning if the meter is watched. A mixed bed does not fail all at once; its outlet conductivity holds flat for most of its life, then climbs through a knee as the last capacity fills, the rise steepening toward exhaustion. An outlet meter trended over time shows that knee approaching, letting the resin change land before the spec breaks at all. The cost of a resin charge is small set against a long test scrapped for dust.
A humidity test that depends on water purity has to record that purity to stand up. The conductivity at the supply, logged at the start of a run, then through it, becomes part of the test record, the proof that the water met spec while the specimen sat in the chamber. An auditor reading the result later can see the water held its purity, the dust risk ruled out by a logged number.
This record matters most where the result is contested. A specimen that failed under test, its maker arguing the chamber dusted it, is answered by a conductivity log showing clean water throughout. A specimen that passed, its purity later doubted, is defended the same way. The water log sits beside the temperature and humidity traces as a third line of evidence, cheap to keep, decisive when a result is questioned.
Pure water is an aggressive solvent, hungry for the ions it lacks. Run it through copper or brass, it leaches metal from the pipe, picking up the very contamination the deioniser removed, so a deionised supply piped in copper arrives at the humidifier dirtier than it left the treatment. The metal it dissolves also corrodes the pipe from the inside, a slow failure born of the water being too clean.
The cure is inert plumbing. Stainless steel holds up well against pure water, as do several plastics, polypropylene, PVDF among them, so a deionised line runs in one of these from treatment to humidifier. The storage tank follows the same rule, a sealed plastic or stainless vessel, no metal drum. Designing the wetted path in inert materials keeps the water at the purity the spec promised, all the way to the point it turns into vapour.
Particulate gets its own guard. Conductivity passes fine solids without seeing them, so a supply clean on ions can still carry grit that blocks an injection orifice or an ultrasonic bath. A filter on the line catches it, a few microns rating for ordinary particles, down to a 0.2 micron rating where a method also needs the water close to sterile. The filter sits after the storage tank, near the humidifier, so it traps whatever the tank shed as well as whatever the treatment missed. Clean ions are one spec, clean particles a second, met by two devices.
Pure water is chemically restless, pulling contamination out of whatever it touches. Left standing open to the air, deionised water absorbs carbon dioxide from the atmosphere, the gas dissolving into carbonic acid that raises the conductivity back up over hours, over days. Water that left the deioniser at one microsiemens can read several after a spell in an open tank, drifting out of spec without anyone adding a thing.
Stagnation brings a second problem. Still water at room temperature grows microbial film over time, even water this clean, since a few organisms find enough to live on, seeding a population that the humidifier then sprays into the chamber. A supply held in a sealed tank, turned over regularly, drawn fresh, stays closer to its rated purity than a drum left open between tests. Fresh water beats stored water on every count the spec measures.
Where a supply has to sit, a guard against biology pays for itself. An ultraviolet lamp on the line kills the organisms a stagnant tank breeds, a recirculation loop keeps the water moving so none settles in a dead leg. This matters most for an ultrasonic source, which sprays whatever the water grows straight onto the specimen, a biological contamination layered on top of the mineral one. A sealed tank, a UV lamp, a moving loop together hold the supply clean across the gaps between tests.
The entire specification collapses into one decision: identify the humidifier first, then set the water to suit it. An electrode boiler takes conductive water in its design band, on the order of 125 to 1250 microsiemens, so a deioniser feeding it is a fault to strip out, mislabelled an upgrade. The water for this machine is clean potable or lightly softened water, well away from the deionised line.
A resistive boiler or an ultrasonic source takes the pure water the common spec describes, deionised below five microsiemens, the lower the better for the ultrasonic case. For these two the deioniser is essential, its outlet monitored, its water kept fresh. A chamber that mixes humidifier types across a fleet needs its water spec written per machine, one line for each humidifier across the fleet.
The cost of getting this wrong runs in both directions. Pure water in an electrode boiler stops the steam, a fault that reads as a humidifier failure until someone checks the conductivity. Hard water in an ultrasonic source dusts the specimen, a fault that reads as a strange test result until someone checks the water. Both trace back to a water spec set without naming the humidifier it was meant to feed.
The cost of the wrong water shows up in hard figures. A scaled boiler element overheats, failing early, a replacement part, the downtime to fit it as well. A dusted test is scrapped outright, its weeks of chamber time lost, its specimens consumed for nothing. A deioniser left to exhaust feeds both faults at once, unseen, until the damage surfaces. Set against those losses, the price of right-sized treatment, a conductivity meter, a fresh supply, reads as the cheap side of the ledger.
Deionised water below five microsiemens per centimetre is the right answer for a resistive steam generator, for an ultrasonic atomiser too, the two humidifiers that want their water free of minerals. It is the wrong answer for an electrode boiler, which needs the conductivity that deionising removes, running on water in the 125-to-1250-microsiemens band. The number on the spec sheet means nothing until it is read next to the name of the humidifier it feeds. A laboratory that writes the water spec against the machine, monitors the conductivity at the outlet, keeps the supply fresh, gives every humidifier in its fleet the water that machine was built to turn into vapour. Read the machine first, the spec follows without guesswork, the one-line figure either right or ruinous by what it feeds.
It depends on the humidifier. A resistive steam generator or an ultrasonic atomiser needs deionised water below five microsiemens per centimetre, equal to a resistivity of 0.2 megohm-centimetre, since both work best free of minerals. An electrode steam boiler needs the opposite, conductive water in the band of roughly 125 to 1250 microsiemens, because it relies on the water’s ions to carry the current that boils it. One spec does not fit all three machines.
Because it boils the water by passing electric current through it, using the water’s own resistance as the heating element. The current, the steam with it, depends on the water conducting. Deionised water below five microsiemens carries almost no ions, so almost no current flows, the boiler sitting cold, making little or no steam. The minerals a deioniser strips out are exactly the ones the electrode boiler needs to function.
They are reciprocals, the same purity read two ways. One microsiemens per centimetre equals one megohm-centimetre, so a humidifier spec of five microsiemens is the same as 0.2 megohm-centimetre. Ultrapure water reads 0.055 microsiemens, or 18.2 megohm-centimetre. Conductivity meters suit dirtier water, resistivity meters suit very pure water. Both describe the identical property.
Because water conductivity changes steeply with temperature, climbing by a couple of percent for each degree of warming. A sample read warm shows a higher number than the same water read cool, so a figure with no temperature attached is ambiguous. Twenty-five degrees is the reference point, a good meter compensating its reading back to it automatically, letting one number mean the same thing every time.
By ion exchange, by reverse osmosis, or by the two in series. Ion exchange runs the water through resin that swaps mineral ions for hydrogen, for hydroxide, driving conductivity into the single digits. Reverse osmosis forces the water through a membrane that holds back most dissolved solids. Many laboratories run reverse osmosis first for the bulk removal, then add an ion-exchange polish to reach the lowest figures a test demands.
Because pure water pulls contamination from its surroundings. Open to the air, it absorbs carbon dioxide that dissolves into carbonic acid, raising the conductivity over hours, over days. Standing still, it grows a little microbial film even at this purity. Fresh from the deioniser the water might read one microsiemens, then several after a spell in an open tank, which is why a humidifier supply is kept sealed, turned over, drawn fresh.