IMARCS staff course · Module 3
Saltwater Chemistry
What pH, CO2, alkalinity, calcium, magnesium, ammonia, nitrite, nitrate and phosphate are, how they connect, why stable beats perfect, and how to read the numbers on the form.
- 1. Reading the numbers
- 2. pH and carbon dioxide
- 3. Alkalinity, calcium and magnesium
- 4. Ammonia, nitrite and nitrate
- 5. Nitrate and phosphate
- 6. Deep sand beds and the Redfield ratio
- 7. Stable beats perfect
- 8. How the numbers connect
1. Reading the numbers: normal range and call limits
Every number on the System Logs form shows its normal range. Some also have call limits, which are wider. Where a reading lands tells you what to do next.
| Test | Which systems, when | Normal | Call limits |
|---|---|---|---|
| Temperature | Every system, every working day | 26 to 28 C (RACK-1: 28 to 30 C) | 26 to 30 C |
| Salinity | Every system, every working day | 32 to 35 ppt (RACK-1: 29 to 31 ppt) | 30 to 35 ppt (RACK-1: 29 to 35 ppt) |
| pH | Every system, Tuesday and Friday | 7.8 to 8.6 | 7.8 to 8.6 |
| Alkalinity | RS200-2 Tuesday and Friday, CADE-800 every working day | 7.5 to 8.5 dKH | 6.5 to 10 dKH |
| Nitrate | RS200-2 and CADE-800, Tuesday | Detectable up to 30 ppm | None |
| Phosphate | RS200-2 and CADE-800, Tuesday | Detectable up to 0.2 ppm | None |
The call limits for temperature and salinity are the livable range from Module 2. RACK-1 runs at 30 ppt, so its salinity numbers are different.
Think it throughSalinity on RACK-1 reads 29.4 ppt. Salinity on G2N-2 reads 29.4 ppt. Is the answer the same for both?
No. RACK-1 runs at 30 ppt, so 29.4 is normal there. On G2N-2, 29.4 is below the 30 ppt call limit: measure again, then call Michael now. The same number can mean different things on different systems.
Remember: Normal: log it. Outside normal: tell Michael today. Outside the call limits: measure again, call now.
2. pH and carbon dioxide
pH tells you how acidic or basic the water is. Seawater is basic, above 7. In an aquarium, the main thing that moves pH is carbon dioxide (CO2). More CO2 in the water makes it more acidic, so pH goes down. Less CO2 lets pH go up.
With the lights on, corals, clams and algae use CO2, so pH rises. With the lights off, everything keeps breathing out CO2 and nothing uses it, so pH falls. A healthy tank with nothing wrong reads differently in the morning and in the evening.
That's why tests are done in the same 13:00 to 18:00 window. A reading taken at a different time can't be compared to the last one: you can't tell a real problem from the time of day.
CO2 in the room
Indoor air often has more CO2 than outdoor air, especially in closed rooms. The water takes CO2 from the air above it, so a closed room can mean a lower pH.
CO2 media on the CADE-800
The CADE-800 skimmer pulls air through a reactor packed with CO2 absorbing media before that air goes into the tank. The media strips CO2 out of the air. When the media is used up, it stops absorbing, and the skimmer pushes CO2 straight back into the water. Used-up media looks exactly the same as fresh media, so it's changed every Friday, all of it, even if it looks fine.
Think it throughA coworker tests pH at 08:30 and gets 7.95. On Tuesday afternoon it was 8.15. They say pH is crashing. What do you say?
The readings were taken at different times of day, so they can't be compared. pH is lower in the morning on a healthy tank. Test again in the 13:00 to 18:00 window. 7.95 is inside 7.8 to 8.6 anyway.
Think it throughThe CADE-800 pH has been drifting lower for two weeks. Alkalinity is normal. The CO2 media looks the same as always. What could it be, and what's the trap?
More CO2 is getting into the water. The CO2 media is one possibility, and the trap is that used-up media looks exactly like fresh media. Check that it has really been changed every Friday. Room air is another possibility. Log the readings and tell Michael if pH goes outside normal.
Remember: More CO2, lower pH. Test pH in the same time window every time.
3. Alkalinity, calcium and magnesium
Alkalinity is the water's buffer: it holds pH steady when acid is added. The higher the alkalinity, the more it resists pH dropping. Alkalinity is measured in dKH.
Corals, clams and coralline algae build their skeletons and shells from calcium and carbonate. As they grow, they take calcium and alkalinity out of the water every day. Magnesium is used too. If nothing puts them back, the numbers fall.
Calcium and magnesium are two of the main parts of seawater. At 35 ppt, natural seawater has about 410 ppm calcium and about 1,300 ppm magnesium (Module 6, section 1). They aren't on the daily form.
AFR is a powder mixed with RO water and dosed by a pump. It supplies calcium, magnesium, alkalinity and trace elements. On the CADE-800 it's dosed from a 5 liter reservoir. RS200-2 also has AFR, but it doses only a few milliliters a day. Dosing pumps are covered in detail in Module 8.
Alkalinity and nutrient levels
Alkalinity and nutrients are linked. As a general rule, lower nutrient levels (nitrate and phosphate) need lower alkalinity.
Think it throughThe CADE-800 AFR reservoir read 3.4 L yesterday and 3.4 L today. The dosing pump is humming. Is it fine?
No. The level has to go down every day. The same number means the doser isn't delivering, even if it hums. Call Michael the same day. If nothing is done, the corals and the clam get nothing and nobody finds out until dKH has already dropped.
Remember: Corals and clams use calcium and alkalinity every day. AFR puts them back. Check that it's actually going in.
4. Ammonia, nitrite and nitrate
Fish waste, uneaten food and anything that dies and rots make ammonia. In a working system, bacteria turn ammonia into nitrite, then nitrite into nitrate. Module 5 covers the bacteria.
Ammonia comes in two forms. The un-ionized form (NH3) is about 100 times more toxic to fish than the ionized form (NH4+). Higher pH and higher temperature push more of the ammonia into the toxic form. The same ammonia reading is more dangerous in warmer water, or at a higher pH.
Where nitrate goes
Nitrate leaves the water in two ways. Water changes take it out. And where there's no oxygen, anaerobic bacteria turn nitrate into nitrogen gas, which leaves the water. Many IMARCS systems have deep sand beds, and they pull nitrate down.
How a deep sand bed removes nitrate
A deep sand bed is a thick layer of fine sand. Near the top, water moves through the sand, and bacteria there use oxygen. Deeper down, the water barely moves, so the oxygen that gets used up isn't replaced. Below a certain depth there's almost no oxygen at all.
Some bacteria can live there anyway. With no oxygen to breathe, they use nitrate instead. As they use it, the nitrate is turned step by step into nitrogen gas, which bubbles out of the sand and leaves the water. This is called denitrification. It only happens where there's no oxygen, which is why the sand has to be deep: a thin layer of sand has oxygen all the way through.
Ammonia and nitrite aren't on the daily form. Nitrate is (section 5).
Think it throughTwo tanks have the same small amount of ammonia. One is 26 C at pH 7.9. The other is 29 C at pH 8.4. Which is more dangerous for the fish?
The 29 C, pH 8.4 tank. Higher temperature and higher pH both push more of the ammonia into the toxic NH3 form.
Remember: Ammonia, then nitrite, then nitrate. Nitrate leaves with water changes, or as gas from a deep sand bed.
5. Nitrate and phosphate: food, in the right amount
Nitrate and phosphate build up from food and waste. On the reef systems, RS200-2 and CADE-800, they're tested every Tuesday.
Zero is harmful
Nitrate and phosphate aren't just waste. Organisms in the tank consume them as a food source. When they read zero, those organisms are starving. That's why 0 isn't normal.
What phosphate is
Phosphate is the form of phosphorus found in the water. Every living thing needs it. It's part of DNA, part of ATP, the molecule that carries energy in every cell, and part of every cell membrane.
Why too much phosphate is bad
Too much phosphate fuels algae, which can take over a tank. It also slows calcifying corals taking up calcium, so they grow more slowly. That matters most in aquariums with animals that build shells and skeletons.
Watch the decimal point. 0.2 ppm phosphate is normal. 2 ppm is ten times higher. A big change from last week usually means a test error: wrong sample size, or reading the color card wrong. Test again before you write it down.
Think it throughA coworker says zero nitrate and zero phosphate is perfect, because they're waste. What do you say?
Zero isn't normal. Organisms in the tank consume nitrate and phosphate as a food source, so at zero they're starving. Tell Michael today.
Think it throughCADE-800 phosphate was 0.06 ppm last Tuesday. Today the card reads 0.6 ppm. What do you do before you write it down?
Check the decimal and test again. A tenfold jump in one week usually means a test error. If the retest agrees, record it: 0.6 is above 0.2, so it's outside normal. Tell Michael today.
Remember: Detectable, not zero. Nitrate up to 30 ppm, phosphate up to 0.2 ppm. Water changes, not binders.
6. Deep sand beds and the Redfield ratio
Living things use nitrogen and phosphorus in a fairly steady proportion. In ocean plankton it's about 106 carbon to 16 nitrogen to 1 phosphorus. This is called the Redfield ratio. The part to remember: about 16 nitrogen for every 1 phosphorus.
A deep sand bed pulls nitrate down, but it does nothing to phosphate. Phosphate keeps arriving with food and waste, so it builds up quickly. Nitrate goes down, phosphate goes up, and the balance between them is soon far from 16 to 1.
In most tanks this isn't a big deal. It matters in aquariums with calcareous organisms: corals, clams and other animals that build shells and skeletons. That's where high phosphate does damage (section 5), and water changes are how it comes back out.
Think it throughA tank with a deep sand bed shows nitrate falling week after week while phosphate climbs. A coworker suggests adding phosphate binder. What do you say?
The deep sand bed is pulling nitrate down and doing nothing to phosphate, so the balance is moving away from 16 to 1. IMARCS doesn't use phosphate binding material as a general rule: phosphate comes out with water changes. Log the numbers and tell Michael if they're outside normal.
Remember: Deep sand beds take nitrate out, not phosphate. Water changes take phosphate out.
7. Stable beats perfect
A number that isn't ideal but is stable is far less harmful than constantly chasing the ideal number and causing swings. Animals can adapt, and even thrive, under numbers that aren't ideal, as long as those numbers are stable.
Every "fix" is a change. Fixing a small difference today, then fixing the overshoot tomorrow, gives the animals a new number every day. That's what does the damage. This is also why you never try to fix a reading yourself: log it, and follow the form.
Think it throughdKH on a tank has read 7.3 for three weeks. The animals look healthy. Someone wants to bring it up to 8.0 today. Good idea?
No. 7.3 is outside normal, so it's logged and Michael is told, but the number is stable and the animals are doing well. A sudden change is a bigger risk than a stable number that's a little low. Never fix a reading yourself.
Remember: Stable and not ideal beats ideal and swinging.
8. How the numbers connect
These numbers are linked. When one moves, others can move with it. Finding the cause means looking at all of them together, not one at a time.
Think it throughRS200-2: pH 7.85 and dKH 6.9 on Friday. On Tuesday it was pH 8.10 and dKH 7.9. What's the first thing to check, and why?
Both are falling together, and alkalinity is what holds pH up. First retest dKH, since it moved more than 0.5. If it agrees, check whether alkalinity is being replaced: the RS200-2 AFR tube clear at the sump end, and the dosing level dropping. dKH 6.9 is outside normal: tell Michael today.
Remember: One number moving can move others. Look at what moved with it.
9. What you see, and what it means
| pH lower in the morning than in the afternoon | Normal day and night cycle. Compare readings from the same time window. |
| pH low, alkalinity normal | More CO2: closed room air, or CO2 media used up (CADE-800). |
| pH and alkalinity both falling | Alkalinity isn't being replaced. Check the AFR is actually going in. |
| CADE-800 AFR level same as yesterday | The doser isn't delivering. Call Michael the same day. |
| dKH moved more than 0.5 since the last test | Test again before writing it down. |
| dKH 8.6 to 10, or 6.5 to 7.4 | Outside normal, inside the call limits. Tell Michael today. |
| Nitrate or phosphate reads 0 | Not normal: organisms that feed on it are starving. Tell Michael today. |
| Nitrate low, phosphate climbing week after week | A deep sand bed is pulling nitrate down while phosphate builds. Water changes take phosphate out. |
| Phosphate ten times higher than last week | Check the decimal, test again. If it agrees, it's outside normal: tell Michael today. |
| A number a little off ideal but steady for weeks | Stable. Don't chase it. Log it and follow the form. |
| A reading outside the call limits | Measure again, then call Michael now. |
10. Words to know
| pH | How acidic or basic the water is. Below 7 is acidic, above 7 is basic. Seawater is basic. |
| Carbon dioxide (CO2) | A gas that animals breathe out. In water it makes acid and lowers pH. |
| CO2 media | Material that absorbs CO2 from the air going into the CADE-800 skimmer. Used-up media looks the same as fresh. |
| Offset label | A label on a pen or meter that reads a little off. Add the offset to what it shows before you enter the number. |
| Alkalinity (dKH) | The water's buffer that holds pH steady. Used up by corals and clams. |
| Buffer | Something that resists a change. Alkalinity resists pH dropping. |
| Calcium | One of the main parts of seawater. Corals and clams use it to build skeletons and shells. |
| Magnesium | One of the main parts of seawater, about 1,300 ppm at 35 ppt. |
| AFR | A powder mixed with RO water and dosed by pump. Supplies calcium, magnesium, alkalinity and trace elements. |
| Ammonia | Waste from animals and rotting matter. Its NH3 form is very toxic. |
| Nitrite | The middle step: bacteria make it from ammonia, then turn it into nitrate. |
| Nitrate | The end step. A food source for organisms in the tank. Normal at IMARCS: detectable up to 30 ppm. |
| Phosphate | A nutrient every living thing needs. Too much fuels algae and slows calcifying corals. Normal at IMARCS: detectable up to 0.2 ppm. |
| Anaerobic | Without oxygen. Anaerobic bacteria turn nitrate into nitrogen gas. |
| Denitrification | Bacteria with no oxygen breathing nitrate instead, turning it into nitrogen gas that leaves the water. |
| Deep sand bed | A thick sand layer whose deep parts have no oxygen. It pulls nitrate down, but not phosphate. |
| Redfield ratio | The steady proportion of nitrogen to phosphorus in living things: about 16 to 1. |
| Normal range | Where a reading should be. Outside it: tell Michael today. |
| Call limits | The wider limits. Outside them: measure again, then call Michael now. |
Sources
- IMARCS How-To Guides (ops.imarcs.org/guides): testing, pH, dKH retest rule, AFR, CO2 media
- Randy Holmes-Farley: the relationship between alkalinity and pH
- UF/IFAS: Ammonia in aquatic systems (FA16)
- Tropic Marin All-For-Reef product description
- Deep sand bed (Wikipedia)
- Denitrification (Wikipedia)
- Redfield ratio (Wikipedia)
- EarthDate: P is for Life (why living things need phosphorus)
- AquaNerd: Phosphates in your reef aquarium, part 1
The quiz for this module opens when quiz grading goes live.