Lehrstuhl für Pflanzenökologie, der Universität Bayreuth, Universitätsstrasse 30, D-8580 Bayreuth, Federal Republic of Germany.
Plant Physiol. 1992 Mar;98(3):840-52. doi: 10.1104/pp.98.3.840.
To evaluate the possible role of solute transport during extension growth, water and solute relations of cortex cells of the growing hypocotyl of 5-day-old castor bean seedlings (Ricinus communis L.) were determined using the cell pressure probe. Because the osmotic pressure of individual cells (pi(i)) was also determined, the water potential (psi) could be evaluated as well at the cell level. In the rapidly growing part of the hypocotyl of well-watered plants, turgor increased from 0.37 megapascal in the outer to 1.04 megapascal in the inner cortex. Thus, there were steep gradients of turgor of up to 0.7 megapascal (7 bar) over a distance of only 470 micrometer. In the more basal and rather mature region, gradients were less pronounced. Because cell turgor approximately pi(i) and psi approximately 0 across the cortex, there were also no gradients of psi across the tissue. Gradients of cell turgor and pi(i) increased when the endosperm was removed from the cotyledons, allowing for a better water supply. They were reduced by increasing the osmotic pressure of the root medium or by cutting off the cotyledons or the entire hook. If the root was excised to interrupt the main source for water, effects became more pronounced. Gradients completely disappeared and turgor fell to 0.3 megapascal in all layers within 1.5 hours. When excised hypocotyls were infiltrated with 0.5 millimolar CaCl(2) solution under pressure via the cut surface, gradients in turgor could be restored or even increased. When turgor was measured in individual cortical cells while pressurizing the xylem, rapid responses were recorded and changes of turgor exceeded that of applied pressure. Gradients could also be reestablished in excised hypocotyls by abrading the cuticle, allowing for a water supply from the wet environment. The steep gradients of turgor and osmotic pressure suggest a considerable supply of osmotic solutes from the phloem to the growing tissue. On the basis of a new theoretical approach, the data are discussed in terms of a coupling between water and solute flows and of a compartmentation of water and solutes, both of which affect water status and extension growth.
为了评估溶质运输在延伸生长过程中的可能作用,使用细胞压力探针测定了 5 天大的蓖麻幼苗(Ricinus communis L.)伸长胚轴的皮层细胞的水和溶质关系。由于还确定了单个细胞的渗透压(pi(i)),因此也可以在细胞水平上评估水势(psi)。在水分充足的植物胚轴快速生长的部分,膨压从外皮层的 0.37 兆帕增加到内皮层的 1.04 兆帕。因此,在仅 470 微米的距离内,膨压存在高达 0.7 兆帕(7 巴)的陡峭梯度。在更基底部和相当成熟的区域,梯度不那么明显。由于细胞膨压大约等于 pi(i),psi 大约等于 0 穿过皮层,因此组织中也没有 psi 的梯度。当从子叶中去除胚乳时,细胞膨压和 pi(i)的梯度增加,从而可以更好地供水。当增加根介质的渗透压或切断子叶或整个钩时,它们会减少。如果切除根以中断水的主要来源,则效果更加明显。梯度完全消失,在 1.5 小时内,所有层的膨压降至 0.3 兆帕。当通过切割表面以压力将 0.5 毫摩尔氯化钙溶液注入切下的胚轴时,可以恢复或甚至增加膨压梯度。当通过加压木质部测量单个皮层细胞的膨压时,会记录到快速响应,并且膨压的变化超过施加的压力。通过磨损角质层也可以在切下的胚轴中重新建立梯度,从而从潮湿的环境中获得供水。膨压和渗透压的陡峭梯度表明韧皮部向生长组织供应相当数量的渗透溶质。基于新的理论方法,根据水和溶质流动的耦合以及水和溶质的分区化,讨论了数据,这两者都影响水状态和延伸生长。