United States Department of Agriculture-Agricultural Research Service, Crops Research Laboratory, Colorado State University, Fort Collins, Colorado 80523.
Plant Physiol. 1983 Apr;71(4):810-7. doi: 10.1104/pp.71.4.810.
A treatment of water flow into and through plants to the evaporating surface of the leaves is presented. The model is driven by evaporation from the cell wall matrix of the leaves. The adsorptive and pressure components of the cell wall matric potential are analyzed and the continuity between the pressure component and the liquid tension in the xylem established. Continuity of these potential components allows linking of a root transport function, driven by the tension in the xylem, to the leaf water potential. The root component of the overall model allows for the solvent-solute interactions characteristic of a membrane-bound system and discussion of the interactions of environmental variables such as root temperature and soil water potentials. A partition function is developed from data in the literature which describes how water absorbed by the plant might be divided between transpiration and leaf growth over a range of leaf water potentials.Relationships between the overall system conductance and the conductance coefficients of the various plant parts (roots, xylem, leaf matrix) are established and the influence of each of these discussed.The whole plant flow model coupled to the partition function is used to simulate several possible relationships between leaf water potential and transpiration rate. The effects of changing some of the partition function coefficients, as well as the root medium water potential on these simulations is illustrated.In addition to the general usefulness of the model and its ability to describe a wide range of situations, we conclude that the relationships used, dealing with bulk fluid flow, diffusion, and solute transport, are adequate to describe the system and that analogically based theoretical systems, such as the Ohm's law analogy, probably ought to be abandoned for this purpose.
本文介绍了一种将水流入和流经植物并到达叶片蒸发表面的处理方法。该模型由叶片细胞壁基质的蒸发驱动。分析了细胞壁基质势的吸附和压力分量,并建立了压力分量与木质部液体张力之间的连续性。这些潜在分量的连续性允许将由木质部张力驱动的根运输功能与叶片水势联系起来。整体模型的根部分允许对环境变量(如根温、土壤水势)的相互作用进行讨论,这些相互作用具有膜结合系统的溶剂-溶质相互作用的特征。从文献中的数据开发了一个分配函数,该函数描述了植物吸收的水分在蒸腾和叶片生长之间可能如何分配,其范围涵盖了一系列叶片水势。建立了整个系统传导率与各种植物部分(根、木质部、叶片基质)传导率系数之间的关系,并讨论了每一部分的影响。将整体植物流动模型与分配函数耦合,以模拟叶片水势和蒸腾速率之间的几种可能关系。说明了改变分配函数系数以及根介质水势对这些模拟的影响。除了模型的一般用途及其描述广泛情况的能力之外,我们得出的结论是,所使用的关系,涉及到整体流体流动、扩散和溶质传输,足以描述该系统,而且类似地基于理论的系统,如欧姆定律类比,可能应该为此目的而被放弃。