The pH Ceiling: Why Your pH Keeps Rising and What to Do About It
You add acid. pH comes back up. You add more. Eventually you grab the whole jug.
About this episode
You add acid. pH comes back up. You add more. Eventually you grab the whole jug.
Still to add: a short, direct answer written for this episode.
01Episode notes
You add acid. pH comes back up. You add more. Eventually you grab the whole jug. Then you pull up the next morning and the liner is wrinkled, across the walls and floor in that specific way that only happens one way.
This episode explains why that happens. Not with a product recommendation. Not with a different test kit. With the physics that's been governing dissolved gases in liquids since William Henry described it in 1803.
Once you understand the pH ceiling, you stop chasing. You start managing. And those are completely different things.
02Full transcript
I want to tell you about a call I get more often than I should. I pull up to a pool, step out of the truck, and before I even get to the equipment pad, I already know something happened. The liner is wrinkled. Not at the seams, not from installation. Wrinkled across the walls and floor in that specific way that only happens in one way. Somebody dumped acid. I pull out the test kit. pH is 6.2, maybe 6.4 if they caught it early. And sure enough, when I call the homeowner, the story is always the same. The pH kept drifting up. They added acid. It came back up.
They added more acid. Eventually, they got frustrated, grabbed the jug, and just poured. The whole thing. Now, a wrinkled liner isn't always a death sentence. If you catch it fast, drain the pool on a hot summer day, warm the liner up in the sun, and then revacue behind it to pull it tight, you can sometimes reset it. Sometimes. But if those wrinkles sit in low pH water long enough, the vinyl develops creases. And when you try to reset a crease liner, it cracks. And at that point, the liner is junk and people are furious. And rightfully so. All of it was preventable. Not with better products or with a different test kit, with a single concept that nobody ever explained.
Today I'm going to explain it. Because if you understand why pH keeps rising, you'll never be tempted to grab that jug again. I'm John Cooper, and whether you own a pool, service them, or run a pool company, this show is built for you. Real Chemistry, Real Answers, every Tuesday.
Before we get into the science, I want to say something directly to anyone who's been fighting pH drift for years and quietly wondering if they're the problem. You're not. PH Drift is not a management failure. It's not a sign that your chemistry is off or that you're using the wrong products or that you're somehow not doing it right. It's a physical property of water in contact with the atmosphere, and it happens in every pool, everywhere, all the time. Always has, always will. The reason it feels like a problem is that nobody ever explained what's actually causing it, and once you understand the mechanism, the frustration disappears.
You stop chasing pH and start managing it, and those are completely different things. Chasing is reactive and exhausting, and leads to that moment with the jug I described at the beginning of this episode. Managing is intentional, consistent, and boring in the best possible way. So let's understand the mechanism.
Let me introduce you to William Henry, not Wilfred Langelier this time, different scientist, different century, same world of water chemistry. William Henry was an English physician and chemist born in Manchester, England in 1774. He grew up during what historians called the Chemical Revolution, when some of the fundamental building blocks of chemistry were being discovered for the first time. He was close friends with John Dalton, the same Dalton whose work on atomic theory you probably encountered somewhere in chemistry class. In eighteen oh three, Henry published a paper in the Philosophical Transactions of the Royal Society of London. The discovery he described was elegant and simple. The amount of a gas dissolved in a liquid is directly proportional to the partial pressure of that gas above the liquid.
It became Henry's law, and it's been governing the behavior of dissolved gases in liquids ever since, including the carbon dioxide in your pool right now. Think about a carbonated beverage for a moment, a soda or a beer. Before you open it, the CO2 is dissolved in the liquid under pressure. The moment you pop the top, the pressure above the liquid drops and CO2 begins escaping. The bubbles you see are dissolved gas coming out of solution to reach a new equilibrium with the atmosphere. Henry's Law in your kitchen. Your pool works the same way, just more slowly and without bubbles you can see. Pool water contains dissolved carbon dioxide.
That CO2 exists in a natural equilibrium with the CO2 in the atmosphere above it. The water and the air are constantly reaching towards each other, trying to balance out. When CO2 leaves the water through splashing, aeration, wind across the surface, a waterfall, a spillover, the normal movement of any active pool, the carbonate chemistry shifts. Carbonic acid dissociates, bicarbonate converts to carbonate, the balance tips, and pH rises. This isn't a malfunction. This isn't something you caused or something you can prevent. This is Henry's law doing exactly what William Henry described in 1803. Your water is always moving toward its natural resting point. That resting point is what we call the pH ceiling, and that's what I want to explain next.
Before I get into the numbers, a quick note. You may have noticed that every measurement in this episode comes in two flavors, English Standard and Metric. After four episodes and several weeks on the air, we have listeners in thirty-four countries, and the very first submission to the Ask John page on the Pools Scientific website was a request to include metric equivalents. So to everyone listening from countries that went metric in the 1970s or before, and that's most of the world, here you go. We'll be doing that from now on. Now, the pH ceiling. The pH ceiling is the highest point pH will naturally rise to in your specific pool under equilibrium conditions.
It's not a target, it's not something you set. It's a physical destination that your water is always moving toward. And it's completely predictable once you understand what determines it. Two variables drive where the ceiling sits. The first is carbonate alkalinity, not carbonite, that's what Han Solo was frozen at. Carbonate alkalinity is something most pool content never explains properly. It's not the same thing as total alkalinity. Total alkalinity includes everything dissolved in your water that can neutralize acid, carbonates, bicarbonates, cyanurates, borates if you're using them. Carbonate alkalinity is specifically the carbonate and bicarbonate fraction, which is the part that actually buffers pH and determines where the ceiling lands.
In a pool with CYA, your carbonate alkalinity is lower than your total alkalinity because cyanurate is consuming some of that buffer without contributing to the pH ceiling. The Pool Scientific LSI calculator at poolsscientific.com accounts for this automatically. The Pool Math and Arenda apps do too, but it's worth understanding what it means because total alkalinity number on your test kit isn't the number that drives the ceiling. Higher carbonate alkalinity means a higher pH ceiling. At 120 parts per million carbonate alkalinity, the ceiling sits around 8.45 to 8.56 depending on water temperature. At 50 parts per million carbonate alkalinity, it drops to around 8.1 to 8.19. This is the direct science behind why we recommend salt pool operators run lower total alkalinity, 60 to 70 parts per million, rather than the standard 80 to 120 range.
Lower carbonate alkalinity means a lower ceiling, which means pH drifts less between visits, which means less acid, less chasing, and less drama. It's not a style preference, it's physics. The second variable is water temperature, and this one surprises people. Warmer water has a lower pH ceiling than colder water at the same alkalinity. A pool at 100 degrees Fahrenheit or 38 Celsius has a ceiling roughly 0.11 units lower than the same pool at 32 degrees Fahrenheit or 0 degrees Celsius. This is why your pool behaves differently in August than it does in April, even when the chemistry looks identical on paper. Same numbers, different ceiling, different drift behavior.
The season matters. Now, a quick note on something I want to address directly. Early in my career, another pool professional told me that 8.23 was the pH threshold for scaling, the point at which calcium carbonate starts dropping out of solution. I wrote it down. I used it. I believed it because it came from someone with experience and it sounded precise. Then I started noticing things in the field that didn't quite fit. Pools with pH well above 8.23 that weren't scaling. Pools closer to 8.0 that were. The number wasn't wrong exactly, but it wasn't the whole story either. So, like the nerd I am, I asked why.
Which is what I always do when field observation doesn't match the theory. Here's what the science actually says. The 8.23 figure is a real number. It represents a natural equilibrium point in the carbonate system under specific conditions. But scaling isn't triggered by a single pH number. It's driven by the saturation index, which accounts for all six variables simultaneously. Whether scaling occurs at pH 7.9 or 8.4 depends entirely on what calcium hardness, alkalinity, temperature, CYA, and TDS are doing at the same time. A fixed pH threshold oversimplifies a six variable system. The pH ceiling concept is more accurate and more useful. Know your ceiling, know your saturation index at that ceiling, and you'll know whether natural pH drift alone can cause scaling in your specific pool.
And I wouldn't have looked for that answer if I'd just kept accepting 8.23 at face value. The Orenda app displays your pH ceiling alongside the saturation index in real time. As you adjust the dials for alkalinity, temperature, and other variables, the ceiling updates automatically. The framework comes from Richard Falk's work on pool water chemistry. This is a calculable, predictable number for your pool, not a guess.
So let's come back to that wrinkled liner. The reason people grab the jug is that they've lost the relationship between cause and effect. The pH keeps drifting up, they dose acid, it comes back up, they dose more, and eventually the drift starts to feel like a personal insult, like the pool is doing it on purpose, like something is fundamentally wrong, and a bigger dose is gonna finally fix it. So they escalate. As a result, they dump a whole gallon, or 3.8 liters, of myriadic acid in all at once. And depending on the pool's alkalinity, volume, current chemistry, that dose can drop pH anywhere from 0.5 to well over a full unit, sometimes even more.
If pH was at 8.0 before they poured, it can land at 6.5 or lower. The exact number depends on too many variables to state precisely, which is exactly the problem with pouring a full gallon without doing the maths first. At a pH of 6.5, water is aggressively corrosive. Vinyl liners will wrinkle, and if the exposure is long enough, they crease. Plaster etches, metal components corrode, and the saturation index crashes into deeply negative territory, meaning your water is now actively attacking every calcium containing surface in the pool. The thing you were trying to fix just became the exact problem we're always trying to prevent, just in the other direction.
Here's what managing the ceiling looks like instead. If you know your pH ceiling is 8.2, you know pH is going to drift towards 8.2 no matter what you do between visits. You don't fight that, you work with it. A small measured dose, often as little as 8 ounces for a standard residential pool, maybe up to 16 ounces 475 milliliters, depending on volume and alkalinity. If you administer it on a regular schedule, it keeps the pH in the 7.4 to 7.6 range without the drama. You're not fighting the ceiling, you're managing the drift below it. That's a completely different relationship with the chemistry and a completely different result for your liner, your equipment, and your sanity.
Small doses on a consistent schedule. Leave the jug in the truck. Every pool drifts at a different rate, and understanding what drives yours tells you how to manage it. In episode 4, we talked about salt chlorine generators, and I attributed pH rise in salt pools to sodium hydroxide production at the cell. That's accurate. The electrolytic process does produce sodium hydroxide, and it does contribute to pH rise. That explanation is also what you'll find in most CPO training materials, and it's what the industry has pointed to for years. But there's a second mechanism that doesn't get talked about nearly as much, and it turns out to be at least as significant.
The cell also produces hydrogen gas as a byproduct of electrolysis. Hydrogen doesn't dissolve in water, it bubbles off, and those hydrogen bubbles create aeration at the cell, which drives CO2 out of the water. And it's that CO2 loss layered on top of the sodium hydroxide contribution that explains why salt pools drift as persistently as they do. Both are real, both contribute. Episode four gave you the first layer. This is the second one. This is why salt pools benefit from running alkalinity at the lower end of the range, 60 to 70 parts per million. You're lowering the ceiling and reducing the rate of CO2 outgassing simultaneously. Two mechanisms working against you means the management response has to be deliberate.
Pools with aerating features drift faster than still pools. Waterfalls, spillovers, deck jets, fountains, all of them put water and air in contact and accelerate CO2 outgassing. Same ceiling, shorter travel time to get there. A pool with a hot tub spillover is going to need more frequent pH management than a quiet flat surface with identical chemistry. This isn't a mystery, it's Henry's Law made visible. Covered pools behave differently from open ones. A pool with a solid or auto cover suppresses aeration and traps CO2 at the water surface, holding pH lower than it would naturally sit. When the cover comes off and aeration resumes suddenly, pH can spike faster than expected.
If you've ever pulled a cover off after a week away and wondered why your pH jumped, that's the mechanism. Henry's law is just reasserting itself all at once after being held back. Geography and season matter too. Altitude affects CO2 partial pressure in the atmosphere. A pool in Denver at one mile or 1.6 kilometers above sea level behaves differently from the same pool chemistry at sea level because the partial pressure of CO2 in the atmosphere is slightly lower at altitude, which affects the equilibrium the water is reaching toward. Ambient temperature shifts the ceiling through the seasons. The same pool with the same chemistry targets requires slightly different management in April than it does in August.
From episode three, we remember that pH is the most powerful lever in the saturation index. A tenth of a unit of pH movement has more impact on the index than almost any other variable in the calculation. When pH drifts towards its ceiling, the saturation index drifts positive simultaneously. Scale forming water is the predictable automatic consequence of unmanaged pH ceiling drift in any pool with meaningful calcium hardness. Your water is doing two things at once, drifting towards the ceiling and drifting towards scale forming territory. And they're the same movement. This is why carbon and alkalinity management is saturation index management. Running alkalinity at the lower end of the appropriate range for your pool type doesn't just affect how fast pH drifts.
It affects where the drift is taking you and what your water is doing to your pool surface and equipment when it gets there. Managing the pH ceiling proactively is managing the saturation index proactively. They're not two separate conversations. They're the same conversation. And now that you understand the ceiling, you can have that conversation intelligently instead of reactively.
William Henry figured all of this out in 1803. Wilfred Langelier built the saturation index in 1936. Richard Falk mapped the pH ceiling framework for pool water. More than two centuries of chemistry all pointing at the same practical truth. Your pH is going to rise. It's going to keep rising until it reaches the ceiling. That's not a problem to solve. That's a law of physics to understand. And physics, once you understand it, stops being something you fight and starts being something that you use. Small doses on a consistent schedule. Know your ceiling, know your saturation index at that ceiling. And for the love of everything holy, step away from the job.
Thank you for listening. If this episode saved someone's liner, share it. Next Tuesday, we go deeper. I'm John Cooper. This is the Pools Scientific Podcast, elevated pool care through science and technology.
03Sources
Still to add: the published sources for this episode.
04Questions people ask
Still to add: common questions about this topic, each with a plain answer.
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