1971
DOI: 10.1085/jgp.57.3.326
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The Kinetics of Sodium Transport in the Toad Bladder

Abstract: A compartmental model of toad bladder sodium content has been developed, whereby it is possible to measure the four unidirectional fluxes across the opposite faces of the transport compartment, as well as the amount of sodium in the compartment. 24Na is added to the mucosal medium of a short-circuited bladder mounted between halves of a chamber in which the fluid is stirred by rotating impellers. After a steady state is reached, nonradioactive medium is flushed through both sides of the chamber, collected, and… Show more

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Cited by 37 publications
(60 citation statements)
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“…Note that there is a significant increase in J,,, the influx from the mucosal medium into the transport pool, and ksl, the rate coefficient for the efflux from the pool to the serosal medium, the "pump rate constant." Values for the pool and the other unidirectional fluxes are not given, since calculation of these values, as shown in the accompanying paper (Finn and Rockoff, 1971), requires a steady state for total sodium. Since the short-circuit current is not stable during the wash period (as the effect of vasopressin is waning despite the continued presence of the hormone) this may not be a valid assumption.…”
Section: Resultsmentioning
confidence: 99%
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“…Note that there is a significant increase in J,,, the influx from the mucosal medium into the transport pool, and ksl, the rate coefficient for the efflux from the pool to the serosal medium, the "pump rate constant." Values for the pool and the other unidirectional fluxes are not given, since calculation of these values, as shown in the accompanying paper (Finn and Rockoff, 1971), requires a steady state for total sodium. Since the short-circuit current is not stable during the wash period (as the effect of vasopressin is waning despite the continued presence of the hormone) this may not be a valid assumption.…”
Section: Resultsmentioning
confidence: 99%
“…One may therefore calculate the relative amount of isotope in the pool by comparing the computer-determined values of P 1 (0) with the amount of tracer present in the loading solution, PM(O). Definitions and symbols are as in the accompanying paper (Finn and Rockoff, 1971), and are shown in Fig. 1.…”
Section: Resultsmentioning
confidence: 99%
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