Potassium Shift Calculator (pH Correction)

Estimate true potassium after correcting for blood pH

Adjust measured serum potassium for arterial pH using the 0.6 mEq/L per 0.1 pH unit rule to estimate total body potassium status in acidaemia or alkalaemia. A browser-based nephrology and critical care calculator that runs on your device. It runs free in your browser on Gera Tools, with nothing uploaded.

Last updated Source: Gera Tools

Why does pH affect serum potassium?

Hydrogen and potassium ions exchange across cell membranes. In acidaemia, hydrogen moves into cells and potassium moves out, raising serum K+ even when total body stores are normal or low. Alkalaemia does the reverse.

Serum potassium and blood pH are tightly coupled because hydrogen (H⁺) and potassium (K⁺) ions compete for the same transport mechanisms across cell membranes. When pH is disturbed, the measured potassium can badly misrepresent the patient’s actual total-body stores. This calculator applies the standard pH-correction rule — a core bedside tool in nephrology and critical care — to estimate the underlying potassium status behind the acid-base disturbance.

The mechanism: why pH shifts potassium

In acidaemia (pH below 7.40), the rising extracellular H⁺ concentration drives hydrogen ions into cells via H⁺/K⁺ exchange. Potassium moves out to maintain electrical neutrality, raising serum K⁺ even when intracellular stores may be depleted. The measured potassium is therefore artificially elevated.

In alkalaemia (pH above 7.40), the reverse occurs: H⁺ leaves cells and K⁺ enters them, depressing the serum value below the true body store.

How the correction works

deltaPH    = measured pH − 7.40
correction = −(deltaPH / 0.1) × 0.6 mEq/L
corrected  = measured K⁺ + correction

The default shift factor is 0.6 mEq/L per 0.1 pH unit — the figure most commonly cited in clinical references — but published estimates range from about 0.2 to 0.8, reflecting that the relationship varies by the cause of the acid-base disorder and individual patient factors. The tool allows the factor to be adjusted if your institution uses a different convention.

Clinical example: diabetic ketoacidosis

DKA is the scenario where this correction matters most acutely. A patient arrives with:

  • Serum K⁺: 5.2 mEq/L (measured)
  • Arterial pH: 7.20

The pH is 0.20 units below normal. Applying the rule:
correction = −(−0.20 / 0.1) × 0.6 = −1.2 mEq/L
Corrected K⁺ ≈ 5.2 − 1.2 = ~4.0 mEq/L

That apparently normal measured potassium of 5.2 masks a body that will become hypokalaemic as insulin and fluid treatment corrects the acidaemia. The intracellular deficit can be profound. This is precisely why DKA protocols emphasise potassium replacement before insulin is started (unless the measured K⁺ is already low and ECG changes are present), even when the raw blood result looks acceptable.

Important limitations

The 0.6 mEq/L rule is a clinical approximation. Research has shown the actual shift varies substantially:

  • Metabolic acidosis from mineral acids (e.g. HCl infusion) causes a larger shift than organic acidaemias (lactic acidosis, DKA).
  • Respiratory acid-base changes cause smaller and less predictable shifts than metabolic ones.
  • The correction is most useful for metabolic acidaemia; its reliability in mixed or respiratory disorders is lower.

Treat the corrected value as a prompt to monitor and plan replacement — not as a precise number to target directly. Always interpret alongside the 12-lead ECG, the clinical picture, renal function, and serial potassium measurements as treatment progresses.