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Urine anion and osmolal gaps in metabolic acidosis

Michael Emmett, MD
Section Editor
Richard H Sterns, MD
Deputy Editor
John P Forman, MD, MSc


Measurement of the urine anion gap (UAG) and/or urine osmolal gap (UOG) may be helpful in the evaluation of patients with a normal anion gap (hyperchloremic) metabolic acidosis by providing an estimate of urinary ammonium (NH4) excretion (table 1) [1-5]. The normal renal response to metabolic acidosis is to increase urinary NH4 excretion. (See "Approach to the adult with metabolic acidosis".)

The clinical use of the urine anion and osmolal gaps will be reviewed here. Issues related to use of the serum anion and osmolal gaps are discussed separately. (See "The delta anion gap/delta HCO3 ratio in patients with a high anion gap metabolic acidosis" and "Serum osmolal gap".)


Ingestion of a typical Western diet generates approximately 50 to 100 meq of hydrogen ions (nonvolatile acid: ie, acids other than CO2) per day. To maintain acid balance, these hydrogen ions must be excreted in the urine in a process that includes the following:

Reabsorption of filtered bicarbonate, since bicarbonate loss is equivalent to the generation of hydrogen ions.

Excretion of the daily nonvolatile acid load. Only trivial amounts of free hydrogen can be excreted since, at a urine pH of 4.5, the free hydrogen ion concentration is less than 0.04 meq/L. Thus, urine hydrogen ions are either bound to buffers (such as phosphate) or to ammonia (NH3) to form ammonium (NH4).


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Literature review current through: Jan 2017. | This topic last updated: Thu Nov 17 00:00:00 GMT 2016.
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