Biology Department, Vassar College, Poughkeepsie, New York 12601.
Plant Physiol. 1967 May;42(5):685-90. doi: 10.1104/pp.42.5.685.
Steady state effluxes of potassium and sodium ions were measured on Pisum sativum var. Alaska root segments excised from seedlings which had grown in a nutrient solution containing the major inorganic ions and either (86)Rb as a tracer for K or (22)Na as a tracer for Na. Fluxes appeared to be from 2 cellular compartments, a small compartment with a high flux rate and a larger compartment with a slow flux rate. Cell wall exchange fluxes are believed to have been negligible. Efflux rates for 11.3% and 88.7% of cellular potassium ions were 6 x 10(-7) and 1.32 x 10(-7) respectively; rates for 33.7% and 66.3% of cellular sodium ions were 1.48 x 10(-7) and 3.83 x 10(-8) respectively, (equivalents per gram fr wt per hr). The sodium flux measurements, with previous measurements of ionic concentrations and transmembrane potentials, support the theory that sodium is transported actively from Pisum roots.
用含主要无机离子的营养液培养豌豆幼苗,切取根段进行实验,测定钾离子和钠离子的稳态流出。实验结果表明,钾离子和钠离子分别经两个细胞区室流出,一个区室的流出速度快,另一个区室的流出速度慢。细胞壁交换通量可以忽略不计。11.3%和88.7%的细胞钾离子流出速度分别为 6×10(-7)和 1.32×10(-7);33.7%和 66.3%的细胞钠离子流出速度分别为 1.48×10(-7)和 3.83×10(-8),(每克鲜重每小时当量数)。钠离子的流出速度以及之前测量的离子浓度和跨膜电位支持这样一种理论,即钠离子从豌豆根中主动运输。