CERTAIN ASPECTS OF THE RENAL REGULATION OF BODY COMPOSITION
THE pH of extracellular fluid is determined by the ratio of the plasma concentrations of bicarbonate ion to carbonic acid, as given in the classical Henderson-Hasselbach equation. [See Equation in Source Pdf] The denominator the carbonic acid concentration, [H2CO3], is proportional to the carbon dioxide tension of the blood. The carbon dioxide tension (pCO2) is primarily dependent upon respiratory function, since metabolism (hence carbon dioxide production) is relatively constant. The numerator of the equation—the bicarbonate concentration of extracellular fluid—is determined by the difference between nonvolatile cations and anions. Since there are almost limitless quantities of bicarbonate available to the organism from cell metabolism, [See Equation in Source Pdf] bicarbonate concentration must change whenever nonvolatile cation (largely sodium) is altered in relation to nonvolatile anion (largely chloride). Thus in most states extracellular bicarbonate concentration is dependent upon the ratio of sodium to chloride in extracellular fluid. The quantity of water filtered at the glomeruli and reabsorbed by the renal tubules each day is approximately 15 times the extracellular volume. The quantity of sodium chloride filtered and reabsorbed daily is approximately 15 times that contained in the extracellular space and 150 times that usually ingested and excreted each day. Therefore, the ratio of plasma sodium to chloride in any steady state is determined by the composition of the renal tubular reabsorbate, as Cushny pointed over 30 years ago. In a sense the kidney perfuses the extracellular space with large quantities of tubular reabsorbate. Tubular reasorbate—the net quantity of materials reabsorbed by the tubules. This term is analogous to glomerular filtrate—the quantity of materials filtered by the glomeruli.