Summary
The rate of dissipation of a pH gradient across the red cell membrane has been measured at pH 5.7–7.5 in a medium free of CO2 and other penetrating acids or bases. The measured rates and extents of pH movements are influenced only slightly by valinomycin-induced changes in the membrane potential. This indicates that the primary process involved is electrically silent OH−/Cl− exchange or H+/Cl− cotransport. This electrically silent pH equilibration has several characteristics which suggest the involvement of the red cell anion exchange protein.
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1.
It is strongly inhibited by phloretin and DIDS (4,4′-diisothiocyano-2,2′-stilbenedisulfonic acid).
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2.
The rates of pH equilibration depend on the halide present in the medium, the relative rates being 100, 18, and 2 in NaCl, NaBr, and NaI media, respectively.
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3.
The pH equilibration has apparent activation energies of 27 kcal/mol atT<13°C and 16 kcal/mol atT>13°C.
The pH dependence of the equilibration rate, however, is much more consistent with H+/Cl− cotransport than with OH−/Cl− exchange; the rate increases steeply with the H+, rather than the OH− concentration. It is suggested therefore that the transport event is H+/Cl− cotransport, but that this transport is mediated by the membrane protein that catalyzes anion exchange.
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Jennings, M.L. Characteristics of CO2-independent pH equilibration in human red blood cells. J. Membrain Biol. 40, 365–391 (1978). https://doi.org/10.1007/BF01874164
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DOI: https://doi.org/10.1007/BF01874164