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Measurement of urine to blood (U-B) carbon dioxide tension (P(CO2)) gradient during alkalinization of the urine has been suggested to assess distal H(+) secretion. A fact that has not been considered in previous studies dealing with urinary P(CO2) is that dissolution of HCO(3) in water results in elevation of P(CO2) which is directly proportional to the HCO(3) concentration. To investigate the interrelationship of urinary HCO(3) and urinary acidification, we measured U-B P(CO2) in (a) the presence of enhanced H(+) secretion and decreased concentrating ability i.e., chronic renal failure (CRF), (b) animals with normal H(+) secretion and decreased concentrating ability, Brattleboro (BB) rats, and (c) the presence of both impaired H(+) secretion and concentrating ability (LiCl treatment and after release of unilateral ureteral obstruction). At moderately elevated plasma HCO(3) levels (30-40 meq/liter), normal rats achieved a highly alkaline urine (urine pH &gt; 7.8) and raised urine HCO(3) concentration and U-B P(CO2). At similar plasma HCO(3) levels, BB rats had a much higher fractional water excretion and failed to raise urine pH, urine HCO(3) concentration, and U-B P(CO2) normally. At a very high plasma HCO(3) (&gt;50 meq/liter), BB rats raised urine pH, urine HCO(3) concentration, and U-B P(CO2) to the same levels seen in normals. CRF rats failed to raise urine pH, urine HCO(3), and U-B P(CO2) normally at moderately elevated plasma HCO(3) levels; at very high plasma HCO(3) levels, CRF rats achieved a highly alkaline urine but failed to raise U-B P(CO2). Dogs and patients with CRF were also unable to raise urine pH, urine HCO(3) concentration, and U-B P(CO2) normally at moderately elevated plasma HCO(3) levels. In rats, dogs, and man, U-B P(CO2) was directly related to urine HCO(3) concentration and inversely related to fractional water excretion. At moderately elevated plasma HCO(3) levels, animals with a distal acidification defect failed to raise U-B P(CO2); increasing the plasma HCO(3) to very high levels resulted in a significant increase in urine HCO(3) concentration and U-B P(CO2). The observed urinary P(CO2) was very close to the P(CO2) which would be expected by simple dissolution of a comparable amount of HCO(3) in water. These data demonstrate that, in highly alkaline urine, urinary P(CO2) is largely determined by concentration of urinary HCO(3) and cannot be used as solely indicating distal H(+) secretion.

The Critical Importance of Urinary Concentrating Ability in the Generation of Urinary Carbon Dioxide Tension