Acid-base regulation during nitrate assimilation in Hydrodictyon africanum

Abstract The acid-base balance during NO₃^? assimilation in Hydrodictyon africanum has been investigated during growth from (1) an analysis of the elemental composition of the cells, (2) the alkalinity of the ash and (3) the net H⁺ changes in the medium during growth. These investigations agree in showing that some 0.25 excess organic negative charges are generated per N assimilation from No₃^? as N-source and C02 as C-source; the excess OH^? (0.75 OH^? per NO₃^? assimilated) appears in the medium. Approximately half of the excess organic negative charge is attributable to cell wall uronates; the remainder is intracellular. All of the excess OH^? appearing in the medium must have crossed the plasmalemma (as net downhill H⁺ influx or OH^? efflux). Previous work has shown that the value of ψco is more negative than ψ_K⁺ during NO₃^? assimilation, suggesting that the active electrogenic H⁺ extrusion pump is still operative despite the net downhill H⁺ influx. The interpretation of this in terms of H⁺?NO₃^? symport which causes the entry of more H⁺ than is consumed in NO₃^? metabolism, with extrusion of the excess H⁺via the active, electrogenic H⁺ pump, was tested by measuring short-term H⁺ influx upon addition of NO^?₃. A net H⁺ influx occurs before NOa assimilation (as indicated by additional O₂ evolution in the light) has commenced, suggesting a mechanistic relation of H⁺ and NO₃^? influxes. This is consistent with the interpretation suggested above. Determinations of cytoplasmic pH showed no significant effect of NO₃^? assimilation, suggesting that cytoplasmic pH changes sufficient to change the ‘pH-regulating’ H⁺ fluxes are smaller than the errors in the determination of cytoplasmic pH.