Factors Associated with Determination of Root ²²Na⁺ Influx in the Salt Accumulation Halophyte Suaeda maritima

Abstract

Salinity is an increasing problem for agricultural production worldwide. The result of low-affinity Na⁺ uptake is toxic to the cytoplasm of most crop plants. Nevertheless, the pathways for this low-affinity Na⁺ uptake are still uncertain. In this work we used ²²Na⁺ isotope tracing technology to investigate factors associated with determination of root ²²Na⁺ influx in the salt accumulation halophyte Suaeda maritima. We found that a 2 min of exposure to the ²²Na⁺ labeled uptake solution was optimal for determining ²²Na⁺ influx into excised roots of S. maritima and that 7 min of blotting is suitable in ²²Na⁺ influx experiments. ²²Na⁺ influx did not increase linearly with the increasing external Na⁺ concentration, in the range tested, of 2 to 300 mM NaCl. But root ²²Na⁺ influx and root Na⁺ concentration were well correlated. ²²Na⁺ influx into excised roots of S. maritima was not, however, well correlated with the plant size. All the above results indicated further that this ²²Na⁺ isotope influx procedure is a good method for quantify Na⁺ uptake rate by the roots of the salt accumulation halophyte.