Vesala Timo, Sevanto Sanna, Grönholm Tiia, Salmon Yann, Nikinmaa Eero, Hari Pertti, Hölttä Teemu
Department of Physics, University of HelsinkiHelsinki, Finland; Department of Forest Sciences, University of HelsinkiHelsinki, Finland; Viikki Plant Science Centre, University of HelsinkiHelsinki, Finland.
Earth and Environmental Sciences Division, Los Alamos National Laboratory Los Alamos, NM, USA.
Front Plant Sci. 2017 Feb 6;8:54. doi: 10.3389/fpls.2017.00054. eCollection 2017.
The pull of water from the soil to the leaves causes water in the transpiration stream to be under negative pressure decreasing the water potential below zero. The osmotic concentration also contributes to the decrease in leaf water potential but with much lesser extent. Thus, the surface tension force is approximately balanced by a force induced by negative water potential resulting in concavely curved water-air interfaces in leaves. The lowered water potential causes a reduction in the equilibrium water vapor pressure in internal (sub-stomatal/intercellular) cavities in relation to that over water with the potential of zero, i.e., over the flat surface. The curved surface causes a reduction also in the equilibrium vapor pressure of dissolved CO, thus enhancing its physical solubility to water. Although the water vapor reduction is acknowledged by plant physiologists its consequences for water vapor exchange at low water potential values have received very little attention. Consequences of the enhanced CO solubility to a leaf water-carbon budget have not been considered at all before this study. We use theoretical calculations and modeling to show how the reduction in the vapor pressures affects transpiration and carbon assimilation rates. Our results indicate that the reduction in vapor pressures of water and CO could enhance plant water use efficiency up to about 10% at a leaf water potential of -2 MPa, and much more when water potential decreases further. The low water potential allows for a direct stomatal water vapor uptake from the ambient air even at sub-100% relative humidity values. This alone could explain the observed rates of foliar water uptake by e.g., the coastal redwood in the fog belt region of coastal California provided the stomata are sufficiently open. The omission of the reduction in the water vapor pressure causes a bias in the estimates of the stomatal conductance and leaf internal CO concentration based on leaf gas exchange measurements. Manufactures of leaf gas exchange measurement systems should incorporate leaf water potentials in measurement set-ups.
水分从土壤向叶片的拉动使得蒸腾流中的水处于负压状态,导致水势降至零以下。渗透浓度也会导致叶片水势降低,但程度要小得多。因此,表面张力大约被负压引起的力所平衡,从而在叶片中形成凹形弯曲的水 - 气界面。水势降低导致内部(气孔下/细胞间)腔室中的平衡水汽压相对于水势为零的水面(即平面)上的平衡水汽压降低。弯曲表面还会使溶解的二氧化碳的平衡蒸气压降低,从而提高其在水中的物理溶解度。尽管植物生理学家认识到了水汽压的降低,但其对低水势值下水汽交换的影响却很少受到关注。在本研究之前,增强的二氧化碳在水中的溶解度对叶片水分 - 碳平衡的影响根本没有被考虑过。我们使用理论计算和建模来展示水汽压降低如何影响蒸腾速率和碳同化速率。我们的结果表明,在叶片水势为 -2 MPa 时,水和二氧化碳的蒸气压降低可使植物水分利用效率提高约 10%,当水势进一步降低时提高幅度更大。低水势甚至在相对湿度低于 100% 时也允许气孔直接从周围空气中吸收水汽。仅这一点就可以解释例如加利福尼亚海岸雾带地区的海岸红杉所观察到的叶片吸水速率,前提是气孔充分开放。忽略水汽压的降低会导致基于叶片气体交换测量对气孔导度和叶片内部二氧化碳浓度估计的偏差。叶片气体交换测量系统的制造商应在测量设置中纳入叶片水势。