Aslam M., Travis R. L., Huffaker R. C.
Department of Agronomy and Range Science, University of California, Davis, California 95616.
Plant Physiol. 1994 Dec;106(4):1293-1301. doi: 10.1104/pp.106.4.1293.
The inhibitory effect of NH4+ on net NO3- uptake has been attributed to an enhancement of efflux and, recently, to an inhibition of influx. To study this controversy, we devised treatments to distinguish the effects of NH4+ on these two processes. Roots of intact barley (Hordeum vulgare L.) seedlings, uninduced or induced with NO3- or NO2-, were used. Net uptake and efflux, respectively, were determined by following the depletion and accumulation in the external solutions. In roots of both uninduced and NO2- -induced seedlings, NO3- efflux was negligible; hence, the initial uptake rates were equivalent to influx. Under these conditions, NH4+ had little effect on NO3- uptake (influx) rates by either the low- or high-Km uptake systems. In contrast, in plants preloaded with NO3-, NH4+ and its analog CH3NH3+ decreased net uptake, presumably by enhancing NO3- efflux. The stimulatory effect of NH4+ on NO3- efflux was a function of external NH4+ and internal NO3- concentration. These results were corroborated by the absence of any effect of NH4+ on NO2- uptake unless the roots were preloaded with NO2-. In this case NH4+ increased efflux and decreased net uptake. Hence, the main effect of NH4+ on net NO3- and NO2- uptake appears to be due to enhancement of efflux and not to inhibition of influx.
NH₄⁺对净硝酸盐(NO₃⁻)吸收的抑制作用归因于外流的增强,最近又归因于内流的抑制。为了研究这一争议,我们设计了一些处理方法来区分NH₄⁺对这两个过程的影响。使用了完整大麦(Hordeum vulgare L.)幼苗的根系,这些幼苗未诱导或用NO₃⁻或NO₂⁻诱导。分别通过跟踪外部溶液中的消耗和积累来测定净吸收和外流。在未诱导和NO₂⁻诱导的幼苗根系中,NO₃⁻外流可以忽略不计;因此,初始吸收速率等同于内流。在这些条件下,NH₄⁺对低亲和力或高亲和力吸收系统的NO₃⁻吸收(内流)速率几乎没有影响。相比之下,在预先加载了NO₃⁻的植物中,NH₄⁺及其类似物CH₃NH₃⁺降低了净吸收,可能是通过增强NO₃⁻外流实现的。NH₄⁺对NO₃⁻外流的刺激作用是外部NH₄⁺和内部NO₃⁻浓度的函数。除非根系预先加载了NO₂⁻,否则NH₄⁺对NO₂⁻吸收没有任何影响,这证实了上述结果。在这种情况下,NH₄⁺增加了外流并降低了净吸收。因此,NH₄⁺对净NO₃⁻和NO₂⁻吸收的主要影响似乎是由于外流的增强,而不是内流的抑制。