These data indicate that the CSA monitor is a valid and reliable tool for quantifying treadmill walking and running in children.

Stewart's model of plasma acid-base balance (Can. J. Physiol. Pharmacol. 61: 1444-1461, 1983) has three weaknesses in the treatment of weak acids: 1) the combination of all weak acids into one entity, 2) inappropriate chemistry for the protein combination with H+, and 3) undocumented values for the dissociation parameters. The present study models serum albumin acid-base properties by fixed negative charges and the association of H+ with the imidazole side chain of histidine. This model has three parameters: 1) the net negative fixed charge (21 eq/mol), 2) the number of histidine residues (16/mol), and 3) the association constant for the imidazole side chain (1.77 x 10(-7) eq/l), all determined from published values. The model was compared with that of Figge, Mydosh, and Fencl (J. Lab. Clin. Med. 120: 713-719, 1992) and with the pH data of Figge, Rossing, and Fencl (J. Lab. Clin. Med. 117: 453-467, 1991). The predictions of pH were excellent, comparable to those found by Figge, Mydosh, and Fencl. The model has the advantages that its structure and parameter values are supported by the literature and that the acid-base effects of factors modifying protein can be investigated.

No abstract

Permeability-surface area products (PS) for 51Cr-EDTA, [3H]mannitol, [14C]urea, and 22Na were measured in isolated, perfused, lower hindlimb muscles of anesthetized cats. The tracers were added stepwise to the arterial inflow, and Evans blue-labeled albumin was the reference indicator. At flow rates > 70 ml.min-1.100 g-1, the PS values (+/- SE) were 5.0 +/- 0.5, 7.6 +/- 1.2, 17.8 +/- 1.4, and 21.0 +/- 1.4 (n = 7, 4, 5, and 3 animals, respectively). The ratio of simultaneous PS measurements of mannitol and urea was 0.42 +/- 0.02 (n = 9), significantly less than the free diffusion coefficient ratio (0.49), indicating the presence of restricted diffusion. PS measurements were also made during osmotic flow (4.2 +/- 0.6 ml.min-1.100 g-1) induced by 20% NaCl. The data clearly showed that osmotic transients did not alter small solute permeability. Pore models were used to show that the PS data and previously reported reflection coefficient data were consistent with a single description of the capillary wall. This model contained a water-only pathway containing 60% of the hydraulic capacity and an extracellular route modeled by pores of 4 nm radius having 21,000 cm of area per unit membrane thickness (A/delta x).