The short-lived radio-isotope nitrogen-13 (half-life 10 min) was used as a tracer in studying fluxes of N in the roots of intact barley plants. After supplying the plants with 13N-nitrate for 30 min, efflux of 13N into an unlabelled (wash) solution was followed under steady-state conditions for a further 10 min. Tests with ion exchange resins suggested that all of the 13N released during this period was in the form of nitrate. In addition to nitrate from a surface film of solution and from the free space of the roots, efflux from another compartment was detected, tentatively identified as the cytoplasmic nitrate pool. In plants grown with nitrate as the only external N-source, efflux from this compartment decreased with a rate constant about 0·17 min−1 (half-time ∼4 min). Adding ammonium sulphate to the wash solution alone did not significantly affect either the initial rate, or the rate constant, of efflux of 13N from these roots. However, 13N efflux decreased more rapidly (rate constant about 0·32 min−1, half-time ∼2·2 min) in roots grown in, and subsequently washed with, solution containing ammonium nitrate. In barley plants grown with 1·5 mol m−3 nitrate, the cytoplasmic nitrate pool was estimated to contain about 2% of the total nitrate in the roots, corresponding to a cytoplasmic nitrate concentration ∼26 mol m−3. Nitrate efflux was equivalent to almost 40% of nitrate influx in the roots of these plants.