Aluminum‐dependent dynamics of ion transport in Arabidopsis: specificity of low pH and aluminum responses

Low‐pH and Al³⁺ stresses are the major causes of poor plant growth in acidic soils. However, there is still a poor understanding of plant responses to low‐pH and Al³⁺ toxicity. Low‐pH or combined low‐pH and Al³⁺ stress was imposed in order to measure rhizosphere pH, ion fluxes, plasma membrane potential and intracellular H⁺ concentration in distal elongation and mature zones (MZs) along the longitudinal axis of Arabidopsis thaliana roots. Low‐pH stress facilitated H⁺ influx into root tissues and caused cytoplasmic acidification; by contrast, combined low‐pH/Al³⁺ treatment either decreased H⁺ influx in the distal elongation zone (DEZ) or induced H⁺ efflux in the MZ, leading to cytoplasmic alkalinization in both zones. Low‐pH stress induced an increase in rhizosphere pH in the DEZ, whereas combined low‐pH/Al³⁺ stress resulted in lower rhizosphere pH in both root zones compared with the low‐pH treatment alone. Low‐pH stress facilitated K⁺ efflux; the presence of Al³⁺ diminished K⁺ efflux or favored K⁺ influx into root tissues. In both zones, low‐pH treatment induced plasma membrane (PM) depolarization, which was significantly diminished (P≤ 0.05) when combined stresses (low‐pH/100 µM Al³⁺) were imposed. After 60 min of exposure, low pH caused PM depolarization, whereas low pH/100 µM Al³⁺ caused PM hyperpolarization. Thus, low pH and Al³⁺ toxicity differentially affect root tissues and, consequently, the rhizosphere, which might underpin the differential mechanisms of plant adaptation to these abiotic stresses.