What it is: Bicarbonate (HCO₃) is a natural buffer that regulates water's pH and contributes to alkalinity. It's formed when carbon dioxide dissolves in water and reacts with carbonate minerals.
Why it matters: Bicarbonate gives water its "softness" and smooth mouthfeel. It's the signature component of famous mineral waters and may aid digestion by neutralizing stomach acid after meals.
Natural sources: Dissolves from limestone, dolomite, and chalk as groundwater moves through rock. Volcanic and geothermal waters often have elevated bicarbonate. Deep aquifers typically have more than surface water.
Optimal range (100–300 mg/L): Water in this range has a pleasant, slightly sweet taste and silky texture. Classic European mineral waters like Evian and Volvic fall here. Good for everyday hydration.
Too high (>600 mg/L): Creates highly alkaline water with a distinct mineral taste. Waters like Vichy or Gerolsteiner have very high bicarbonate. Best consumed occasionally rather than as primary hydration.
Too low (<50 mg/L): Water may taste flat or slightly acidic. Less buffering capacity means pH can fluctuate more. Common in rain-fed surface water and heavily treated municipal supplies.