14.2 Nutrient Removal: Nitrification, Denitrification & Anaerobic/Anoxic/Aerobic Zones
Key Takeaways
- Nitrification is a two-step aerobic conversion of ammonia to nitrite and then to nitrate by slow-growing autotrophic bacteria, requiring long solids retention time, dissolved oxygen of about 2 mg/L or more, warm temperature, and adequate alkalinity.
- Nitrification destroys approximately 7.14 pounds of alkalinity as calcium carbonate per pound of ammonia nitrogen oxidized, which is why nitrifying plants with soft water must monitor alkalinity and often add caustic, lime, or soda ash.
- Denitrification occurs in an anoxic zone where heterotrophic bacteria use nitrate instead of oxygen as the electron acceptor, and it returns roughly 3.57 pounds of alkalinity as calcium carbonate per pound of nitrate nitrogen reduced — about half of what nitrification consumed.
- Enhanced biological phosphorus removal requires a truly anaerobic zone with neither dissolved oxygen nor nitrate, where phosphorus-accumulating organisms release phosphorus and store volatile fatty acids, followed by aerobic luxury uptake that removes more phosphorus than the cells need.
- Biological phosphorus leaves the plant only in the wasted sludge, so consistent wasting is essential and secondary release in a clarifier blanket or thickener returns dissolved phosphorus to the head of the plant.
14.2 Nutrient Removal: Nitrification, Denitrification & Anaerobic/Anoxic/Aerobic Zones
Exam Focus: "Nutrient removal processes (e.g., anaerobic/anoxic/aerobic)" is a named Treatment Process line item, and "Nutrient removal/enhancement" appears again under chemical dosing. Ammonia limits are now common even at small plants, so nitrogen chemistry has become genuine Class I material.
1. Nitrification
Nitrification is the aerobic, two-step biological oxidation of ammonia:
Step 1: Ammonia (NH4-N) --> Nitrite (NO2-N) by ammonia-oxidizing bacteria (e.g., Nitrosomonas)
Step 2: Nitrite (NO2-N) --> Nitrate (NO3-N) by nitrite-oxidizing bacteria (e.g., Nitrobacter, Nitrospira)
The organisms responsible are autotrophs — they build cell material from inorganic carbon rather than from organic matter — and they are slow growers. Everything difficult about nitrification follows from that slow growth rate.
What Nitrifiers Require
| Requirement | Typical Target | Why It Matters |
|---|---|---|
| Dissolved oxygen | 2.0 mg/L or more in the aerobic zone | Nitrifiers compete poorly for oxygen against heterotrophs; below roughly 1 mg/L nitrification slows sharply |
| Solids retention time (MCRT) | Long enough that nitrifiers are not washed out — commonly on the order of 10 days or more at moderate temperature, and substantially longer in cold weather | Slow growers must be retained longer than they take to reproduce |
| Temperature | Warm favors nitrification strongly | Nitrification rate falls markedly as temperature drops, which is why ammonia limits are hardest to meet in late winter |
| pH | Roughly 7.2 to 8.0 | Nitrification slows outside this band and is severely inhibited below about pH 6.5 |
| Alkalinity | Maintain a residual in the effluent, commonly targeted at 50 to 100 mg/L as CaCO3 | Nitrification consumes alkalinity; running out crashes pH and stops the process |
| Absence of inhibitors | — | Nitrifiers are more sensitive to metals, cyanide, and many organics than heterotrophs, so they fail first under a toxic load |
The Two Numbers Worth Memorizing
- Oxygen demand: approximately 4.6 pounds of oxygen per pound of ammonia nitrogen oxidized — over and above the oxygen required for carbonaceous BOD. Turning on nitrification substantially increases aeration demand.
- Alkalinity destruction: approximately 7.14 pounds of alkalinity as CaCO3 per pound of ammonia nitrogen oxidized.
The classic nitrification failure. A plant in a soft-water region begins nitrifying, alkalinity is consumed faster than the influent supplies it, mixed liquor pH falls below 6.5, and nitrification stops — which then lets ammonia rise, alkalinity partially recover, pH rise, nitrification restart, and the cycle repeat. The fix is to monitor effluent alkalinity as a routine process control test and supplement with caustic soda, lime, or soda ash to hold a residual.
2. Denitrification
Denitrification is the anoxic conversion of nitrate to nitrogen gas:
Nitrate (NO3-N) --> Nitrite --> Nitric oxide --> Nitrous oxide --> Nitrogen gas (N2)
The organisms are ordinary heterotrophic bacteria — the same ones doing BOD removal — operating in a zone that has nitrate but no free dissolved oxygen. Given a choice they will always use oxygen, which is why an anoxic zone must genuinely exclude it.
Requirements
- Nitrate present — you cannot denitrify what you have not first nitrified.
- Essentially zero dissolved oxygen. This is why anoxic zones are mixed mechanically, never with air (Section 10.2).
- A carbon source. Raw influent BOD is the cheapest, which is why anoxic zones are usually placed first, receiving raw influent and a nitrate-rich internal recycle. Where nitrate must be removed after the aerobic zone, a supplemental carbon source such as methanol is fed.
What Denitrification Gives Back
- Alkalinity recovery: approximately 3.57 pounds as CaCO3 per pound of nitrate nitrogen reduced — roughly half of what nitrification destroyed. A plant that both nitrifies and denitrifies has a far easier alkalinity balance than one that only nitrifies.
- Oxygen credit: roughly 2.86 pounds of oxygen equivalent recovered per pound of nitrate nitrogen reduced, because the nitrate itself supplies the oxidizing power that would otherwise come from blower air.
Denitrification in the wrong place. Nitrate that reaches a secondary clarifier blanket and sits there will denitrify, and the nitrogen gas bubbles float sludge to the surface — the rising sludge covered in Section 3.4. The distinction matters: denitrification in an anoxic zone is the process working; denitrification in the clarifier is a problem, corrected by increasing RAS rate to shorten blanket detention time.
3. Common Zone Arrangements
| Configuration | Zone Order | Purpose |
|---|---|---|
| MLE (Modified Ludzack-Ettinger) | Anoxic → Aerobic, with a large internal mixed liquor recycle carrying nitrate from the aerobic zone back to the anoxic zone, plus RAS returned to the anoxic zone | Nitrogen removal using influent BOD as the carbon source. The workhorse arrangement. |
| A2O (anaerobic/anoxic/aerobic) | Anaerobic → Anoxic → Aerobic | Nitrogen removal plus biological phosphorus removal |
| Four-stage Bardenpho | Anoxic → Aerobic → Anoxic → Aerobic | Deeper nitrogen removal; the second anoxic zone polishes remaining nitrate |
| Oxidation ditch | Single loop with alternating aerobic and anoxic regions around the circuit | Simultaneous nitrification and denitrification in one basin |
| SBR | Time-sequenced anoxic/aerobic phases in one tank | Nutrient removal by cycling conditions rather than moving water between zones |
4. Enhanced Biological Phosphorus Removal
Phosphorus-accumulating organisms (PAOs) can store phosphorus far in excess of their metabolic needs, but only if they are cycled through the right sequence:
- Anaerobic zone — no dissolved oxygen AND no nitrate. PAOs take up volatile fatty acids from the influent and store them as internal polymers, and to power that uptake they release phosphorus into solution. Soluble phosphorus therefore rises in the anaerobic zone; this is normal and necessary.
- Aerobic zone. PAOs metabolize their stored polymers and take phosphorus back up in excess of what they released — the phenomenon called luxury uptake.
- Wasting. The phosphorus is now inside the cells, so it leaves the plant only in the wasted sludge.
Operating implications that get tested:
- The anaerobic zone must exclude nitrate as well as oxygen. Nitrate arriving with RAS lets denitrifiers consume the volatile fatty acids that PAOs need, and biological phosphorus removal collapses. This is why plants with combined nitrogen and phosphorus removal manage where nitrate-bearing RAS is returned.
- Waste consistently. Skipping wasting keeps phosphorus in the system.
- Secondary release occurs whenever phosphorus-laden sludge sits under anaerobic conditions without volatile fatty acids present — in a deep clarifier blanket, a gravity thickener, or a sludge holding tank. The phosphorus goes back into solution and returns to the head of the plant in the side stream. Keep blankets thin and side streams managed.
5. Chemical Phosphorus Removal
Where biological removal is absent or insufficient, phosphorus is precipitated chemically with a metal salt — alum, ferric chloride, or ferrous salts — or with lime.
- Dosing points include ahead of the primary clarifier, into the aeration basin or its effluent, and ahead of a tertiary filter for final polishing.
- Metal salt addition consumes alkalinity and depresses pH, which interacts directly with the nitrification alkalinity budget above.
- Chemical addition increases sludge production, and that additional chemical sludge loads thickening, digestion, and dewatering.
- Multiple dosing points at lower total dose usually outperform a single large dose at one location.
A plant with soft influent water begins meeting a new ammonia limit, then experiences a cycle in which nitrification stops, ammonia rises, and nitrification later restarts on its own. Mixed liquor pH is found to swing between 6.2 and 7.4. What is the underlying cause and the appropriate control test?
An operator observes that soluble phosphorus concentration is higher leaving the anaerobic zone of a biological phosphorus removal plant than it was entering. What does this indicate?
Why is the anoxic zone in an MLE configuration placed ahead of the aerobic zone rather than after it?