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水分通过玉米根的运输:利用双压力探针技术同时测量细胞水平和根水平的水流

Water Transport across Maize Roots : Simultaneous Measurement of Flows at the Cell and Root Level by Double Pressure Probe Technique.

作者信息

Zhu G L, Steudle E

机构信息

Lehrstuhl für Pflanzenökologie, Universität Bayreuth, Universitätsstrasse 30, D-8580 Bayreuth, Federal Republic of Germany.

出版信息

Plant Physiol. 1991 Jan;95(1):305-15. doi: 10.1104/pp.95.1.305.

Abstract

A double pressure probe technique was used to measure simultaneously water flows and hydraulic parameters of individual cells and of excised roots of young seedlings of maize (Zea mays L.) in osmotic experiments. By following initial flows of water at the cell and root level and by estimating the profiles of driving forces (water potentials) across the root, the hydraulic conductivity of individual cell layers was evaluated. Since the hydraulic conductivity of the cell-to-cell path was determined separately, the hydraulic conductivity of the cell wall material could be evaluated as well (Lp(cw) = 0.3 to 6.10(-9) per meter per second per megapascal). Although, for radial water flow across the cortex and rhizodermis, the apoplasmic path was predominant, the contribution of the hydraulic conductance of the cell-to-cell path to the overall conductance increased significantly from the first layer of the cortex toward the inner layers from 2% to 23%. This change was mainly due to an increase of the hydraulic conductivity of the cell membranes which was Lp = 1.9.10(-7) per meter per second per megapascal in the first layer and Lp = 14 to 9.10(-7) per meter per second per megapascal in the inner layers of the cortex. The hydraulic conductivity of entire roots depended on whether hydrostatic or osmotic forces were used to induce water flows. Hydrostatic Lp(r) was 1.2 to 2.3.10(-7) per meter per second per megapascal and osmotic Lp(r) = 1.6 to 2.8.10(-8) per meter per second per megapascal. The apparent reflection coefficients of root cells (sigma(s)) of nonpermeating solutes (KCI, PEG 6000) decreased from values close to unity in the rhizodermis to about 0.7 to 0.8 in the cortex. In all cases, however, sigma(s) was significantly larger than the reflection coefficient of entire roots (sigma(sr)). For KCI and PEG 6000, sigma(sr) was 0.53 and 0.64, respectively. The results are discussed in terms of a composite membrane model of the root.

摘要

在渗透实验中,采用双压力探针技术同时测量玉米(Zea mays L.)幼苗单个细胞和离体根的水流及水力参数。通过追踪细胞和根水平上的初始水流,并估算根中驱动力(水势)的分布,评估了单个细胞层的水力传导率。由于细胞间途径的水力传导率是单独测定的,因此细胞壁材料的水力传导率也可得以评估(Lp(cw)=0.3至6.10(-9)每米每秒每兆帕斯卡)。尽管对于穿过皮层和根表皮的径向水流而言,质外体途径占主导,但细胞间途径的水力传导率对总传导率的贡献从皮层的第一层到内层显著增加,从2%增至23%。这种变化主要是由于细胞膜水力传导率的增加,在皮层的第一层中Lp = 1.9.10(-7)每米每秒每兆帕斯卡,而在皮层内层中Lp = 14至9.10(-7)每米每秒每兆帕斯卡。整个根的水力传导率取决于使用静水力还是渗透力来诱导水流。静水力Lp(r)为1.2至2.3.10(-7)每米每秒每兆帕斯卡,渗透力Lp(r)=1.6至2.8.10(-8)每米每秒每兆帕斯卡。非渗透性溶质(KCI、PEG 6000)的根细胞表观反射系数(sigma(s))从根表皮中接近1的值降至皮层中的约0.7至0.8。然而,在所有情况下,sigma(s)均显著大于整个根的反射系数(sigma(sr))。对于KCI和PEG 6000,sigma(sr)分别为0.53和0.64。根据根的复合膜模型对结果进行了讨论。

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本文引用的文献

1
Axial and Radial Hydraulic Resistance to Roots of Maize (Zea mays L.).
Plant Physiol. 1989 Oct;91(2):719-26. doi: 10.1104/pp.91.2.719.
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Pressure probe technique for measuring water relations of cells in higher plants.
Plant Physiol. 1978 Feb;61(2):158-63. doi: 10.1104/pp.61.2.158.
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Determination of hydraulic and osmotic properties of soybean root systems.
Plant Physiol. 1977 Jun;59(6):1013-20. doi: 10.1104/pp.59.6.1013.
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Interaction between Osmotic- and Pressure-induced Water Flow in Plant Roots.
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