Anion gap with albumin correction and delta ratio, corrected sodium for hyperglycaemia, corrected calcium for albumin, calculated osmolality with the osmolar gap, and the urine anion gap. SI or US units.
Anion gap. AG = NaβΊ β (Clβ» + HCOββ»). Including potassium, (NaβΊ + KβΊ) β (Clβ» + HCOββ»), which adds about 4. The commonly quoted reference range is 8β16 mmol/L without potassium, but modern ion-selective-electrode analysers report chloride lower than older flame-photometry methods did, and many laboratories now quote 3β11. Always use your own laboratory's range; a gap of 14 is normal in one lab and raised in another. Both forms are shown here.
Albumin-corrected anion gap. Albumin is the main unmeasured anion, so a low albumin hides a gap. Corrected AG = observed AG + 2.5 Γ (4.0 β albumin in g/dL), which in SI is observed AG + 0.25 Γ (40 β albumin in g/L). At an albumin of 20 g/L this adds 5 mmol/L β enough to turn an apparently normal gap into a high one in a critically ill patient.
Delta ratio. Ξ ratio = (AG β reference AG) Γ· (24 β HCOββ»), using your laboratory's midpoint gap. Under 0.4 suggests a hyperchloraemic normal-gap acidosis; 0.4β0.8 a mixed high-gap and normal-gap acidosis; 0.8β2.0 a pure high-gap acidosis; above 2.0 a high-gap acidosis on top of a pre-existing high bicarbonate (metabolic alkalosis, or compensation for chronic respiratory acidosis).
Corrected sodium. Hyperglycaemia pulls water out of cells and dilutes sodium. Katz (1973): add 1.6 mmol/L for every 5.6 mmol/L (100 mg/dL) of glucose above 5.6 mmol/L. Hillier (1999) measured a larger effect and argued for 2.4 mmol/L per 5.6 mmol/L; both are shown because the correction matters most in DKA and HHS, exactly where the choice changes whether you call the sodium normal.
Corrected calcium. Payne's formula: corrected calcium (mmol/L) = measured calcium + 0.02 Γ (40 β albumin in g/L), or in mg/dL, measured + 0.8 Γ (4.0 β albumin in g/dL). About half of plasma calcium is protein-bound, so a low albumin lowers total calcium without changing the ionised fraction that actually matters β which is why an ionised calcium is the better test whenever the correction is large or the patient is unwell.
Osmolality. Calculated osmolality = 2 Γ NaβΊ + glucose + urea (all mmol/L). Osmolar gap = measured β calculated, normally under 10 mmol/kg. A raised gap raises the possibility of an unmeasured osmole β ethanol, methanol, ethylene glycol, isopropanol, acetone, or mannitol β but the calculated figure ignores potassium, calcium, magnesium and protein, so a gap of 10β15 on its own is weak evidence.
Urine anion gap. Urine (NaβΊ + KβΊ) β Clβ», used in a normal-gap metabolic acidosis to separate the causes. A negative gap means the kidney is excreting ammonium appropriately, pointing to a gastrointestinal bicarbonate loss such as diarrhoea; a positive gap means it is not, pointing to a renal tubular acidosis. It is invalid in volume depletion, ketonuria (where the unmeasured anion is the ketone) and renal impairment.
Worked panel. Na 130, K 4.0, Cl 100, HCOββ» 12, albumin 25 g/L, glucose 28 mmol/L, urea 8 mmol/L, calcium 2.10 mmol/L. Anion gap = 130 β (100 + 12) = 18; with potassium, 134 β 112 = 22. Albumin correction adds 0.25 Γ (40 β 25) = 3.75, giving a corrected gap of 21.8. Delta ratio = (18 β 12) Γ· (24 β 12) = 0.50 β a mixed high-gap and normal-gap acidosis, so there is a hyperchloraemic component alongside the gap. Corrected sodium = 130 + 1.6 Γ (28 β 5.6) Γ· 5.6 = 136.4 by Katz and 139.6 by Hillier, so the apparent hyponatraemia is largely dilutional. Corrected calcium = 2.10 + 0.02 Γ (40 β 25) = 2.40 mmol/L β normal total calcium was masking a genuinely raised corrected value. Calculated osmolality = 260 + 28 + 8 = 296 mmol/kg.
Traps. The gap is only as good as the chloride: a chloride reported from a different sample, or a lipaemic or icteric sample, produces a gap that does not exist. Bromide, iodide and nitrate falsely raise chloride and so falsely lower the gap; lithium and some paraproteins do the opposite. Correcting sodium for glucose does not correct it for the osmotic shift of mannitol, IVIG or contrast. Payne's formula assumes a normal acid-base state β acidosis itself lowers protein-bound calcium, so in a sick patient with a low albumin the correction is doubly unreliable and an ionised calcium should be measured instead. All of these corrections are estimates about a single blood sample, not about the patient.
Disclaimer. Arithmetic for qualified clinicians β not medical advice and not a diagnosis. Interpret against your laboratory's own reference ranges. Sources: Kraut & Madias on the anion gap and delta ratio (Nature Reviews Nephrology) Β· Katz, Diabetes Care 1973 Β· Hillier et al., American Journal of Medicine 1999 Β· Payne et al., Lancet 1973 Β· Rodriguez-Soriano on the urine anion gap. Last reviewed: 2026-09-21.