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Active Extrusion of Protons into Deionized Water by Roots of Intact Maize Plants ¹

Institute of Plant Nutrition, Justus Liebig-University, Suedanlage 6, D - 6300 Giessen, Federal Republic of Germany

The investigations were focussed on the question as to whether roots of intact maize plants (Zea mays L. cv Blizzard) release protons into deionized H₂O. Plants in the six to seven leaf stage depressed the pH of deionized H₂O from 6 to about 4.8 during an experimental period of 4 hours. Only one-third of the protons released could be ascribed to the solvation of CO₂ in H₂O. The main counter anions released were Cl^–, NO₃^–, and SO₄^2–. At low temperature (2°C), the H⁺ release was virtually blocked while a relatively high amount of K⁺ was released. The presence of K⁺, Na⁺, Ca²⁺, and Mg²⁺ in the external solution increased the H⁺ secretion significantly. Addition of vanadate to the outer medium inhibited the H⁺ release while fusicoccin had a stimulating effect. Substituting the nutrient solution of deionized H₂O resulted in a substantial increase of the membrane potential difference from –120 to –190 millivolts. The experimental results support the conclusion that the H⁺ release by roots of intact maize plants is an active process driven by a plasmalemmalocated ATPase. Since the net H⁺ release was not associated with a net uptake of K⁺, it is unlikely to originate from a K⁺/H⁺ antiport.

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