The Bicarbonate Calculator determines bicarbonate concentration from water alkalinity and pH using carbonate equilibrium equations. Essential for aquaculture, swimming pool chemistry, drinking water treatment, and any application where carbonate-bicarbonate buffering capacity must be quantified.
182.5
mg/L
0.3
mg/L
9.3
mg/L
6.6
%
93.3
%
0.1
%
141.1
mg/L as CO2
182.5
mg/L
0.3
mg/L
9.3
mg/L
6.6
%
93.3
%
0.1
%
141.1
mg/L as CO2
Alkalinity and bicarbonate are not the same thing — though in many natural waters they are nearly equivalent. Alkalinity measures a water's total capacity to neutralize acids (contributed by bicarbonate, carbonate, hydroxide, and other bases), while bicarbonate concentration quantifies the specific HCO₃⁻ species. At the pH range of most natural waters (6.5–8.5), bicarbonate dominates alkalinity so completely that the two are nearly interchangeable; but in swimming pools, industrial process water, or unusual natural settings, the distinction matters significantly. The bicarbonate calculator resolves this using the full carbonate equilibrium system.
In water, dissolved carbon dioxide exists as three interconverting species depending on pH:
CO₂(aq) + H₂O ⇌ H₂CO₃* ⇌ HCO₃⁻ + H⁺ ⇌ CO₃²⁻ + 2H⁺
The relative proportions of these three species depend entirely on pH, through the two carbonate equilibrium constants:
In the pH range 6.5–8.5 (virtually all natural freshwaters and drinking waters), bicarbonate (HCO₃⁻) is the dominant carbonate species. The fraction as bicarbonate: f_HCO₃ = [H⁺]Ka₁ / ([H⁺]² + [H⁺]Ka₁ + Ka₁Ka₂). At pH 7.5: f_HCO₃ > 99.9%. Use this online calculator to convert your alkalinity measurement to bicarbonate concentration. The alkalinity calculator performs the complementary conversion.
Alkalinity is measured by acid titration — typically to an endpoint of pH 4.3–4.5 (the "total alkalinity" or "M alkalinity" in water analysis). Common units and conversion factors:
Bicarbonate concentration (KH — "carbonate hardness" in the aquarium hobby) is critical for fish and coral health:
The water hardness calculator and water chemistry calculators provide complementary aquatic chemistry tools.
In clinical medicine, bicarbonate is the primary metabolic acid-base buffer in blood. Normal serum bicarbonate: 22–26 mEq/L (mmol/L). Bicarbonate deviates in acid-base disorders: metabolic acidosis (HCO₃⁻ below 22 mEq/L) — diabetic ketoacidosis, lactic acidosis, renal failure; metabolic alkalosis (HCO₃⁻ above 26 mEq/L) — prolonged vomiting, diuretic use, primary hyperaldosteronism. The Henderson-Hasselbalch equation relates pH, bicarbonate, and partial CO₂ pressure in blood: pH = 6.1 + log([HCO₃⁻] / (0.0307 × pCO₂_mmHg)), enabling calculation of any one variable from the other two in clinical acid-base interpretation.
In most natural waters (pH 6.5–8.5), bicarbonate is the dominant species, comprising over 95% of total carbonate. At pH 7.5, bicarbonate constitutes about 97% of alkalinity species. Carbonate becomes significant only above pH 8.3 (the phenolphthalein alkalinity endpoint). Free CO₂ is important for corrosion — dissolved CO₂ lowers pH and attacks metal pipes and concrete. For the Langelier Saturation Index, individual carbonate species are needed. In aquaculture, free CO₂ above 10 mg/L can stress fish, while bicarbonate provides the essential buffering that maintains stable pH for aquatic life.
Inputs
Results
At pH 7.5, nearly all alkalinity exists as bicarbonate (181 mg/L). Carbonate is negligible (0.3 mg/L), and free CO₂ is low (4.2 mg/L).
Inputs
Results
At pH 9.5, significant carbonate (27 mg/L) appears alongside bicarbonate. Free CO₂ is essentially zero, indicating non-corrosive conditions.
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