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Growth-induced Water Potentials in Plant Cells and Tissues

机译:植物细胞和组织中生长诱导的水势

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摘要

A physical analysis of water movement through elongating soybean (Glycine max L. Merr.) hypocotyls was made to determine why significant water potentials persist in growing tissues even though the external water potentials were zero and transpiration is virtually zero. The analysis was based on a water transport theory modified for growth and assumed that water for growing cells would move through and along the cells in proportion to the conductivity of the various pathways.Water potentials calculated for individual cells were nearly in local equilibrium with the water potentials of the immediate cell surroundings during growth. However, water potentials calculated for growing tissue were 1.2 to 3.3 bars below the water potential of the vascular supply in those cells farthest from the xylem. Only cells closest to the xylem had water potentials close to that of the vascular supply. Gradients in water potential were steepest close to the xylem because all of the growth-sustaining water had to move through this part of the tissue. Average water potentials calculated for the entire growing region were −0.9 to −2.2 bars depending on the tissue diffusivity.For comparison with the calculations, average water potentials were measured in elongating soybean hypocotyls using isopiestic thermocouple psychrometers for intact and excised tissue. In plants having virtually no transpiration and growing in Vermiculite with a water potential of −0.1 bar, rapidly growing hypocotyl tissue had water potentials of −1.7 to −2.1 bars when intact and −2.5 bars when excised. In mature, nongrowing hypocotyl tissue, average water potentials were −0.4 bar regardless of whether the tissue was intact or excised.The close correspondence between predicted and measured water potentials in growing tissue indicates that significant gradients in water potential are required to move growth-associated water through and around cells over macroscopic distances. The presence of such gradients during growth indicates that cells must have different cell wall and/or osmotic properties at different positions in the tissue in order for organized growth to occur. The mathematical development used in this study represents the philosophy that would have to be followed for the application of contemporary growth theory when significant tissue water potential gradients are present.
机译:进行了通过伸长大豆下胚轴的水分运动的物理分析,以确定为什么即使外部水势为零且蒸腾量实际上为零,生长的组织中仍然存在大量水势。该分析基于为生长而改良的水运移理论,并假设用于生长细胞的水将根据各种途径的电导率成比例地通过和沿细胞运动。单个细胞计算出的水势几乎与水处于局部平衡生长期间直接细胞周围环境的潜力。但是,计算得出的生长组织的水势比最远离木质部的那些细胞的血管供应水势低1.2至3.3 bar。只有最靠近木质部的细胞才具有接近血管供应的水势。水势的梯度最接近木质部,因为所有维持生长的水都必须穿过组织的这一部分。根据组织的扩散率,整个生长区域的平均水势为-0.9至-2.2 bar。为了与计算结果进行比较,使用等度热电偶干湿计对完整和切除的组织测量了伸长的大豆下胚轴的平均水势。在几乎没有蒸腾作用且在Ver石中生长且水势为-0.1 bar的植物中,快速生长的胚轴组织在完整时的水势为-1.7至-2.1 bar,在切除时的水势为-2.5 bar。在成熟的,不生长的下胚轴组织中,无论组织是完整的还是切除的,平均水势均为-0.4 bar。生长组织中预测的和测量的水势之间的紧密对应关系表明,与生长相关的水势需要显着的水势梯度。穿过宏观距离的细胞和细胞周围的水。在生长过程中这种梯度的存在表明细胞必须在组织中的不同位置具有不同的细胞壁和/或渗透特性,以便发生有组织的生长。当存在显着的组织水势梯度时,本研究中使用的数学发展表示必须遵循的理论才能应用现代生长理论。

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