Miller D M
Agriculture Canada, London Research Centre, University Sub Post Office, London, Ontario, Canada N6A 5B7.
Plant Physiol. 1985 Jan;77(1):168-74. doi: 10.1104/pp.77.1.168.
The volume flux, J(v), and the osmotic driving force, sigma big up tri, openpi, across excised root systems of Zea mays were measued as a function of big up tri, openP, the hydrostatic pressure difference applied across the root, using the pressure jump method previously described (Miller DM 1980 Can J Bot 58: 351-360). J(v) varied from 5.3% to 142% of its value in intact transpiring plants as a result of the application of pressure differences from -2.4 to 2.4 bar. The calculated hydraulic conductivity was 5.9 x 10(-4) cubic centimeters per second per bar per gram root and was independent of pressure. A model of root function similar to those appearing in the literature failed to provide quantitative accord with the data. A proposed model, which includes the effect of volume flux on the distribution of solutes in the symplasm, predicts accurately J(v) big up tri, openpi, and the xylem solute concentration as a function of big up tri, openP.
采用先前描述的压力阶跃法(Miller DM,1980年,《加拿大植物学杂志》58卷:351 - 360页),测量了玉米离体根系的体积通量J(v)和渗透驱动力σΔπ,它们是施加在根系上的静水压差ΔP的函数。由于施加了-2.4至2.4巴的压力差,J(v)在完整蒸腾植物中的值变化范围为其5.3%至142%。计算得出的水力传导率为5.9×10⁻⁴立方厘米每秒每巴每克根系,且与压力无关。文献中出现的类似根系功能模型未能与数据达成定量一致。一个提出的模型,包括体积通量对共质体中溶质分布的影响,准确预测了J(v)、Δπ以及木质部溶质浓度作为ΔP的函数。