Jd. Bisognano et al., PROTON (OR HYDROXIDE) FLUXES AND THE BIPHASIC OSMOTIC RESPONSE OF HUMAN RED-BLOOD-CELLS, The Journal of general physiology, 102(1), 1993, pp. 99-123
Upon exposure of human red blood cells to hypertonic sucrose, the fluo
rescence of the potentiometric indicator 3,3'-dipropylthiadicarbocyani
ne iodide, denoted diS-C3(5), displays a biphasic time course indicati
ng the rapid development of an inside-positive transmembrane voltage,
followed by a slow DIDS (4,4'-diisothiocyano-2,2'-disulfonic acid stil
bene)-sensitive decline of the voltage. In addition to monitoring memb
rane potential, proton (or hydroxide) fluxes were measured by a pH sta
t method, cell volume was monitored by light scattering, and cell elec
trolytes were measured directly when red cells were shrunken either wi
th hypertonic NaCl or sucrose. Shrinkage by sucrose induced an initial
proton efflux (or OH- influx) of 5.5 mueq/g Hb.min and a Cl shift of
21-31 mueq/g Hb in 15 min. Upon shrinkage with hypertonic NaCl, the ce
lls are initially close to Donnan equilibrium and exhibit no detectabl
e shift of Cl or protons. Experiments with the carbonic anhydrase inhi
bitor ethoxzolamide demonstrate that for red cell suspensions exposed
to air and shrunken with sucrose, proton fluxes mediated by the Jacobs
-Stewart cycle contribute to dissipation of the increased outward Cl c
oncentration gradient. With maximally inhibitory concentrations of eth
oxzolamide, a residual proton efflux of 2 mueq/g Hb.min is insensitive
to manipulation of the membrane potential with valinomycin, but is co
mpletely inhibited by DIDS. The ethoxzolamide-insensitive apparent pro
ton efflux may be driven against the electrochemical gradient, and is
thus consistent with HCI cotransport (or Cl/OH exchange). The data are
consistent with predictions of equations describing nonideal osmotic
and ionic equilibria of human red blood cells. Thus osmotic equilibrat
ion after shrinkage of human red blood cells by hypertonic sucrose occ
urs in two time-resolved steps: rapid equilibration of water followed
by slower equilibration of chloride and protons (or hydroxide). Under
our experimental conditions, about two-thirds of the osmotically induc
ed apparent proton efflux is mediated by the Jacobs-Stewart cycle, wit
h the remainder being consistent with mediation via DIDS-sensitive HCl
cotransport (or Cl/OH exchange).