Pump-leak sodium fluxes in low salt corn roots

Summary The influx and efflux of sodium from 4-hr washed, low salt corn roots (Zea mays L.) has been studied for characterization of passive and active components. Initial Na⁺ content of the roots is very low, 2.25±0.4 mol/g fresh weight. Na⁺ influx in the presence of 0.2mm Ca²⁺ and 0.002 to 20mm K⁺ is passive (a leak) based upon Goldman-type models, being determined by Na⁺ and cell potential (). Na⁺ was not transported by the K⁺ carrier and influx was unaffected by 50 m dicyclohexylcarbodiimide (DCCD). Permeability of the cells to Na⁺ was of the same order asP _k.Efflux of Na⁺ was by an efficient and rapid active transport system (a pump), thus accounting for the failure of these roots to accumulate high levels of Na⁺. In short-term loading and efflux experiments, internal Na⁺ turnover had a half-time of about 5 min. Sodium efflux was unaffected by DCCD. Net H⁺ flux was zero in the presence of DCCD regardless of sodium efflux, indicating absence of Na⁺/H⁺ antiport. Efflux of Na⁺ was equally rapid into medium containing no Na⁺ and only 0.002mm K⁺. K⁺ influx accounted for less than 4% of Na⁺ efflux, prompting the hypothesis that the Na⁺ (or cation?) efflux pump is the second electrogenic system previously defined based upon electrophysiological measurements.