Renal excretion of divalent ions in response to chronic acidosis: evidence that systemic pH is not the controlling variable.

Although metabolic acidosis produces calciuric, phosphaturic, and magnesiuric effects, the consequences of chronic respiratory acidosis are unclear. To examine the role of systemic pH on renal divalent metabolism, 4-day balance studies were performed in rats with both metabolic acidosis induced by adding 1.5% NH4Cl to the drinking water, and respiratory acidosis produced by exposure to 10% atmospheric CO2 in an environmental chamber, and in controls pair-fed with each group. By the fourth day, blood pH had decreased to an identical degree with both chronic metabolic and respiratory acidosis and averaged 7.28. As anticipated, chronic metabolic acidosis resulted in significant calciuria, magnesiuria, and phosphaturia. However, despite the similar decrement in blood pH, calcium, phosphorus, and magnesium excretion was similar to that in the pair-fed controls with chronic respiratory acidosis. These findings indicate that a low systemic pH, per se, does not account for the modifications in urinary divalent ion handling that accompany chronic metabolic acidosis. However, additional observations suggest that differences in the intracellular pH of the proximal tubular epithelium may be an important regulatory variable.