We compared influxes and internal transport in soybean plants (Glycine max cv. Kingsoy) of labelled N from external solutions where either ammonium or nitrate was labelled with tbe stable isotope'-'^N and the radioactive i.sotope'''N. The objective was to see whether mass spectrometric determinations of tissue '^N content were sufficiently sensitive to measure influxes accurately over short time periods. Our findings were as follow.s. (1) There was a close quantitative correspondence between estimates of N influx of individual plants using """^N or '"'N niea.surements with either NO," or NH/ at 4 or 2 mol m"\ respectively in the external solution.(2) Transport to the shoot of N from NO, absorbed over a 5-15 min period could be monitored when the external NO," concentration ranged from 0-05 to 4 mol m""\ NH/ as the N source labelled shoot tissue more slowly, and estimates of the transport between root and shoot could be made only with '"^N. (3) Influx of NO," into root tissue could be measured by "'N enricbment after 5-10 min at concentrations approaching the probable AM of the high-aninity transport system. (4) There was some indication of isotope discrimination, especially with respect to the movement of labelled N to the shoot, when NO," is the N source. For many purposes, '"''N tracing can be used satisfactorily to estimate influxes of both NO," and NH/ in soybean roots. Use of the short-lived radionuclide ' N remains the method of cli«)ice for more refined measurements of Internal distribution and a.ssimilation.