• Minhtri K Nguyen, Vahram Ornekian, Anthony W Butch, and Ira Kurtz.
• Departments of Medicine, University of California, Los Angeles, California 90095, USA. mtnguyen@mednet.ucla.edu
• Am. J. Physiol. Renal Physiol. 2007 May 1; 292 (5): F1652-6.

AbstractPseudohyponatremia is a clinical condition characterized by an increased fraction of protein or lipid in plasma, thereby resulting in an artificially low plasma sodium concentration ([Na(+)](p)). Since the automated method of measuring [Na(+)](p) in most laboratories involves the use of an indirect ion-selective electrode (I-ISE), this method does not correct for elevated protein or lipid concentrations. In I-ISE, the plasma sample is diluted before the actual measurement is obtained, and the [Na(+)](p) is determined based on the assumption that plasma is normally composed of 93% plasma water. Therefore, the [Na(+)](p) as determined by I-ISE will be artificially low in clinical conditions when the plasma water content (PWC) is <93%. In contrast, the plasma is not diluted when the [Na(+)](p) is measured using direct ISE (D-ISE). This method directly measures Na(+) activity in plasma water and is therefore unaffected by the proportion of plasma occupied by water. In this study, we report a novel quantitative method for determining the PWC utilizing I-ISE and D-ISE. To validate this new method experimentally, we altered the PWC in vitro by dissolving varying amount of salt-free albumin in human plasma. We then measured PWC gravimetrically in each sample and compared the gravimetrically determined PWC with the ISE-determined PWC. Our findings indicate that the PWC can be accurately determined based on differences in the [Na(+)](p) as measured by I-ISE and D-ISE and that this new quantitative method can be a useful adjunct in the analysis of the dysnatremias.

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