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Kinetics of ammonium and nitrate uptake by eucalypt roots and associated proton fluxes measured using ion selective microelectrodes

机译:使用离子选择性微电极测量桉树根吸收铵和硝酸盐的动力学以及相关的质子通量

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Ion-selective microelectrodes were used non-invasively to measure the concentration dependence of NH4+ and NO3- fluxes around the roots of intact solution-cultured Eucalyptus nitens (Deane & Maiden) Maiden. In addition, NH4+ and H+ fluxes were measured simultaneously at a range of NH4+ concentrations, and NO3- and H+ fluxes were measured simultaneously at a range of NO3- concentrations. Nitrogen concentrations ranged from 10-250 muM, i.e. in the range corresponding to the high affinity transport system (HATS). Both NH4+ and NO3- fluxes exhibited saturating Michaelis-Menten-style kinetics. The K-m was 16 muM for NH4+ and 18 muM for NO3-. Values of V-max were 53 nmol m(-2) s(-1) for NH4+ and 37 nmol m(-2) s(-1) for NO3-. Proton fluxes were highly correlated with NH4+ and NO3- fluxes, but the relationships were different. Proton efflux increased with increasing NH4+ concentration and mirrored the changing NH4+ fluxes. The ratio between NH4+ and H+ fluxes was 1:-1.6. Proton influx was evident with initial exposure to NO3-, with the flux stoichiometry for NO3-: H+ being 1:1.4. Subsequent increases in NO3- concentration caused a gradual increase in H+ efflux such that the flux stoichiometry for NO3-: H+ became 1:-0.8. The presence of 100 muM NH4+ greatly reduced NO3- fluxes and caused a large and constant H+ efflux. These results are evidence that E. nitens has a preference for NH4+ as a source of N, and that the fluxes of NH4+ and NO3- are quantitatively linked to H+ flux.
机译:离子选择性微电极用于非侵入式测量完整溶液培养的桉树(Deane&Maiden)少女的根周围的NH4 +和NO3-通量的浓度依赖性。另外,在一定的NH4 +浓度范围内同时测量了NH4 +和H +通量,并且在一定的NO3浓度范围内同时测量了NO3-和H +通量。氮浓度范围为10-250μM,即在对应于高亲和力转运系统(HATS)的范围内。 NH4 +和NO3-通量均表现出饱和的Michaelis-Menten式动力学。 NH4 +的K-m为16μM,NO3-的K-m为18μM。对于NH4 +,V-max的值为53 nmol m(-2)s(-1),对于NO3-为37 nmol m(-2)s(-1)。质子通量与NH4 +和NO3-通量高度相关,但关系不同。质子外流随NH4 +浓度的增加而增加,并反映了NH4 +通量的变化。 NH4 +和H +通量之比为1:-1.6。最初暴露于NO3-时质子大量涌入,NO3-:H +的通量化学计量比为1:1.4。随后NO3-浓度的增加导致H +外排量的逐渐增加,使得NO3-:H +的通量化学计量比变为1:-0.8。 100μMNH4 +的存在大大降低了NO3-的通量,并导致大量且恒定的H +流出。这些结果证明,大肠埃希氏菌优先选择NH4 +作为氮源,并且NH4 +和NO3-的通量与H +通量定量相关。

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