Alkalinity Titration Calculator
Turn bench titration volumes into alkalinity as CaCO3: total alkalinity plus the hydroxide / carbonate / bicarbonate split from the two endpoints.
Alkalinity (as CaCO3)
| Species (as CaCO3) | mg/L |
|---|
How the calculation works
APHA 2320 B — titration to pH 4.5
Alkalinity (mg/L as CaCO3) = titrant (mL) × N × 50,000 ÷ sample (mL)
(50,000 mg/eq is the equivalent weight of CaCO3.)
Alkalinity (mg/L as CaCO3) = titrant (mL) × N × 50,000 ÷ sample (mL)
(50,000 mg/eq is the equivalent weight of CaCO3.)
Speciation from the two endpoints (P = alkalinity to pH 8.3, T = total alkalinity, all as CaCO3)
P = 0 → bicarbonate = T
2P < T → carbonate = 2P, bicarbonate = T − 2P
2P = T → carbonate = T
2P > T → hydroxide = 2P − T, carbonate = 2(T − P)
P = T → hydroxide = T
Notes & limitations
Method and speciation relationships per APHA Standard Methods for the Examination of Water and Wastewater, Method 2320 B (Alkalinity — Titration Method). Results are conventionally reported as mg/L as CaCO3.
- The pH 8.3 endpoint marks conversion of carbonate to bicarbonate; the pH 4.5 endpoint marks conversion of bicarbonate to carbonic acid. Use a calibrated pH meter rather than color indicators for the most defensible endpoints.
- Interferences: soaps, oily matter, suspended solids, and precipitates can blur the endpoints; phosphates and silicates contribute to the titration. See Method 2320 for the full interference discussion.
- The speciation table assumes the sample contains only hydroxide, carbonate, and bicarbonate contributors. If borates, silicates, or phosphates are significant, the split is approximate.
- Titrant normality must be standardized and current — an old normality is the most common source of error.
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