Conditions controlling relative uptake of potassium and rubidium by plants from soils

Abstract

Earlier studies have demonstrated close inverse relationships between Rb⁺ concentrations in plants and pH or base (including K⁺) saturation of soils. This study aims at elucidating conditions in soils influencing plant uptake of Rb⁺. Growth experiments with Carex pilulifera L. were performed, modifying the acidity and K⁺ supply of acid soils and solutions. We were unable to assess any reduction in Rb⁺ uptake by adding precipitated CaCO₃ to acid soil unless pH was raised to near neutrality. Though not fully compensating the loss of soil solution K⁺and exchangeable K⁺ from uptake by the growing plants, soil treated with 0.5 mM K⁺ (as KCl) reduced the Rb⁺ concentration in the shoots by 40% without measurably changing soil pH. Experiments varying the pH and K⁺ concentration of a nutrient solution (20% Hoagland), spiked with 6 uM Rb⁺, clearly demonstrated that plant uptake of Rb⁺ and K⁺ was unaffected by acidity in the pH range 3.6–5.0 tested, whereas Rb⁺ uptake was reduced by ca. 50%, when K⁺ concentration was increased from 1.2 to 3.6 mM. The sensitivity of this reaction indicates that shortage or low availability of K⁺ controls Rb⁺ uptake from acid soils, being probably more important than soil acidity per se. Secondary effects of high soil acidity, such as leaching losses of K⁺, might also be of importance in accounting for the high uptake of Rb⁺ from such soils. It is suggested that leaf analysis of Rb⁺ may be used as a method to assess early stages of K⁺ deficiency in plants on acid soils.