Canny M
Am J Bot. 1998 Jul;85(7):897.
Some predictions of the recently proposed theory of long-distance water transport in plants (the Compensating Pressure Theory) have been verified experimentally in sunflower leaves. The xylem sap cavitates early in the day under quite small water stress, and the compensating pressure P (applied as the tissue pressure of turgid cells) pushes water into embolized vessels, refilling them during active transpiration. The water potential, as measured by the pressure chamber or psychrometer, is not a measure of the pressure in the xylem, but (as predicted by the theory) a measure of the compensating pressure P. As transpiration increases, P is increased to provide more rapid embolism repair. In many leaf petioles this increase in P is achieved by the hydrolysis of starch in the starch sheath to soluble sugars. At night P falls as starch is reformed. A hypothesis is proposed to explain these observations by pressure-driven reverse osmosis of water from the ground parenchyma of the petiole. Similar processes occur in roots and are manifested as root pressure. The theory requires a pump to transfer water from the soil into the root xylem. A mechanism is proposed by which this pump may function, in which the endodermis acts as a one-way valve and a pressure-confining barrier. Rays and xylem parenchyma of wood act like the xylem parenchyma of petioles and roots to repair embolisms in trees. The postulated root pump permits a re-appraisal of the work done by evaporation during transpiration, leading to the proposal that in tall trees there is no hydrostatic gradient to be overcome in lifting water. Some published observations are re-interpreted in terms of the theory: doubt is cast on the validity of measurements of hydraulic conductance of wood; vulnerability curves are found not to measure the cavitation threshold of water in the xylem, but the osmotic pressure of the xylem parenchyma; if measures of xylem pressure and of hydraulic conductance are both suspect, the accepted view of the hydraulic architecture of trees needs drastic revision; observations that xylem feeding insects feed faster as the water potential becomes more negative are in accord with the theory; tyloses, which have been shown to form in vessels especially vulnerable to cavitation, are seen as necessary for the maintenance of P, and to conserve the supplementary refilling water. Far from being a metastable system on the edge of disaster, the water transport system of the xylem is ultrastable: robust and self-sustaining in response to many kinds of stress.
最近提出的植物长距离水分运输理论(补偿压力理论)的一些预测已在向日葵叶片中得到实验验证。木质部汁液在白天很早的时候就在相当小的水分胁迫下形成空洞,补偿压力P(作为膨胀细胞的组织压力施加)将水推入栓塞的导管中,在活跃蒸腾期间重新填充它们。通过压力室或湿度计测量的水势不是木质部压力的度量,而是(如该理论所预测的)补偿压力P的度量。随着蒸腾作用增加,P增加以提供更快的栓塞修复。在许多叶柄中,P的这种增加是通过淀粉鞘中的淀粉水解为可溶性糖来实现的。夜间,随着淀粉重新形成,P下降。提出了一个假设,通过叶柄基本薄壁组织中水的压力驱动反渗透来解释这些观察结果。类似的过程发生在根部,并表现为根压。该理论需要一个泵将水从土壤转移到根木质部。提出了一种该泵可能起作用的机制,其中内皮层充当单向阀和压力限制屏障。木材的射线和木质部薄壁组织的作用类似于叶柄和根部的木质部薄壁组织,以修复树木中的栓塞。假定的根泵允许对蒸腾过程中蒸发所做的工作进行重新评估,从而提出在高大树木中提升水时不存在要克服的静水压力梯度。根据该理论对一些已发表的观察结果进行了重新解释:对木材水力传导率测量的有效性产生怀疑;发现脆弱性曲线不是测量木质部中水的空化阈值,而是木质部薄壁组织的渗透压;如果木质部压力和水力传导率的测量都值得怀疑,那么关于树木水力结构的公认观点就需要大幅修订;木质部取食昆虫随着水势变得更负而取食更快的观察结果与该理论一致;已证明在特别容易发生空化的导管中形成的侵填体被视为维持P以及保存补充再填充水所必需的。木质部的水分运输系统远非处于灾难边缘的亚稳态系统,而是超稳定的:在应对多种压力时稳健且自我维持。