Renal Stone Risk Index Calculator

Urinary supersaturation indices for calcium oxalate and uric acid

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Recurrent kidney stones are driven by urinary supersaturation: when the concentration of stone-forming ions exceeds their solubility, crystals nucleate and grow. Simplified indices let a clinic quantify that risk from a 24-hour urine collection without a full thermodynamic model.

How it works

The Tiselius AP-CaOx index estimates calcium oxalate crystallisation probability:

AP-CaOx = 1.9 x Ca^0.84 x Ox / ( Cit^0.22 x Mg^0.12 x Vol^1.03 )

where calcium, oxalate, citrate, and magnesium are in mmol/day and volume is in litres/day. Calcium and oxalate raise the index, while citrate, magnesium, and dilution lower it. Uric acid risk is governed almost entirely by urine pH through the dissociation of uric acid:

soluble fraction = 1 / (1 + 10^(pKa - pH)),  pKa ~= 5.35

A low soluble fraction with a high uric acid load signals high uric acid stone risk.

Interpretation and notes

For the AP-CaOx index, values below about 1.0 are low risk, above about 1.7 high risk, and in between intermediate. For uric acid, raising urine pH toward 6.5 dramatically increases the soluble fraction and is the basis of alkalinising therapy. These are screening estimates from published simplified formulae and do not replace full thermodynamic software such as EQUIL or Lithorisk, nor specialist metabolic assessment. Always interpret indices alongside the complete 24-hour profile and the patient’s stone composition.

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