Department of Soil Science, North Carolina State University, 27607, Raleigh, NC, USA.
Planta. 1976 Jan;132(2):149-56. doi: 10.1007/BF00388896.
Wheat (Triticum vulgare L., cv. Blueboy) seedlings, grown with 0.25, 1.0 and 15 mM nitrate in complete nutrient solutions, were transferred 10 days after germination to 1.0 mM K(15)NO3 (∼99 A% (15)N) plus 0.1 mM CaSO4 at pH 6.0. The solutions were replaced periodically over a 6-h period (5 mW cm(-2); 23°). Changes in the [(15)N]- and [(14)N]nitrate in the solution were determined by nitrate reductase and mass-spectrometric procedures and potassium by flame photometry. Influx of [(15)N]nitrate was depressed in plants grown at 1.0 mM nitrate relative to those grown at 0.25 mM, but there was no appreciably difference in [(14)N]nitrate efflux. Prior growth at 15 mM further restricted [(15)N]nitrate influx which, together with a substantial increase in [(14)N]nitrate efflux, resulted in no net nitrate uptake during the course of the experiment. Efflux of [(14)N]nitrate occurred to solutions containing no nitrate but it was significantly enhanced upon exposure to [(15)N]nitrate in the external solution. Influx of [(15)N]nitrate was more restricted at 5°, relative to 23°, than was [(14)N]nitrate efflux. The nitrate concentrations of the root tissue immediately before exposure to the K(15)NO3 solutions did not give a precise indication of the subsequent [(15)N]nitrate influx rates nor of the [(14)N]nitrate efflux rates. Net K(+) uptake was related to the magnitude of the net nitrate uptake, not to the initial K(+) concentration in the roots. The data are interpreted as indicating that [(15)N]nitrate influx and [(14)N]nitrate efflux are largely independent processes, subject to different controls, and that net nitrate uptake provides the driving force for net potassium uptake.
小麦(Triticum vulgare L.,cv. Blueboy)幼苗在完全营养液中分别用 0.25、1.0 和 15mM 硝酸盐培养 10 天后,在发芽后第 10 天转移到 1.0mM K(15)NO3(约 99A%(15)N)加 0.1mM CaSO4,pH 值为 6.0。在 6 小时的时间内定期更换溶液(5mW cm(-2);23°)。通过硝酸盐还原酶和质谱程序以及火焰光度法确定溶液中[(15)N]-和[(14)N]硝酸盐的变化。与在 0.25mM 硝酸盐中生长的植物相比,在 1.0mM 硝酸盐中生长的植物中[(15)N]硝酸盐的流入受到抑制,但[(14)N]硝酸盐的流出没有明显差异。先前在 15mM 下的生长进一步限制了[(15)N]硝酸盐的流入,这与[(14)N]硝酸盐的大量流出一起,导致实验过程中没有净硝酸盐吸收。[(14)N]硝酸盐的流出发生在不含硝酸盐的溶液中,但暴露于外部溶液中的[(15)N]硝酸盐会显著增强其流出。与[(14)N]硝酸盐的流出相比,在 5°时,[(15)N]硝酸盐的流入受到更大的限制,而不是在 23°时。暴露于 K(15)NO3 溶液之前,根组织中的硝酸盐浓度不能准确指示随后的[(15)N]硝酸盐流入速率或[(14)N]硝酸盐流出速率。净 K(+)吸收与净硝酸盐吸收的幅度有关,而与根中的初始 K(+)浓度无关。这些数据表明,[(15)N]硝酸盐流入和[(14)N]硝酸盐流出是两个很大程度上独立的过程,受不同的控制,净硝酸盐吸收为净钾吸收提供了驱动力。