Botany Department, University of British Columbia, Vancouver, British Columbia, Canada V6T 2B1.
Plant Physiol. 1983 Sep;73(1):100-4. doi: 10.1104/pp.73.1.100.
A computer-controlled multichannel data acquisition system was employed to obtain continuous measurements of net nitrate or chlorate uptake by roots of intact barley plants (Hordeum vulgare cv Betzes) using nitrate-specific electrodes. Plants, previously grown in solutions maintained at 10 or 200 micromolar NO(3) (-) (low N or high N conditions, respectively), were provided with 200 micromolar NO(3) (-) or ClO(3) (-) during the uptake period. Initial rates of NO(3) (-) uptake were several times higher in low N plants than in high N plants. Within 10 min, uptake in the former plants declined to a new steady rate which was sustained for the remainder of the experiment. No such time-dependent changes were evident in the high N plants. Rates and patterns of net chlorate uptake exhibited almost identical dependence upon previous nitrate provision. NO(3) (-) ((36)ClO(3) (-)) influx, by contrast, appeared to be independent of NO(3) (-) pretreatment prior to influx determination. Nitrate efflux, estimated by several different methods, was strongly correlated with internal nitrate concentration of the roots.
采用计算机控制的多道数据采集系统,利用硝酸盐特异性电极,对完整大麦植株(Hordeum vulgare cv Betzes)根系净硝酸盐或氯酸盐摄取进行连续测量。这些植物先前在 10 或 200 微摩尔 NO3-(-)(低氮或高氮条件,分别)溶液中生长,在摄取期间提供 200 微摩尔 NO3-(-)或 ClO3-(-)。在低氮植物中,NO3-(-)摄取的初始速率比高氮植物高几倍。在 10 分钟内,前者的摄取速率下降到一个新的稳定速率,并在实验的剩余时间内持续。在高氮植物中没有明显的这种时间依赖性变化。净氯酸盐摄取的速率和模式几乎与先前硝酸盐供应的依赖性相同。相比之下,NO3-(-)((36)ClO3-(-))内流似乎与内流测定之前的 NO3-(-)预处理无关。通过几种不同的方法估算的硝酸盐外排与根系内部硝酸盐浓度强烈相关。