Turner Neil C, Schulze E -D, Gollan T
Lehrstuhl für Pflanzenökologie, Universität Bayreuth, Postfach 3008, D-8580, Bayreuth, Federal Republic of Germany.
CSIRO Dryland Crops and Soils Research Program, Private Bag, P.O., 6014, Wembley, W.A., Australia.
Oecologia. 1985 Feb;65(3):348-355. doi: 10.1007/BF00378908.
The responses of leaf water potential, leaf conductance, transpiration rate and net photosynthetic rate to vapour pressure deficits varying from 10 to 30 Pa kPa were followed in Helianthus annuus as the extractable soil water decreased. With a vapour pressure deficit of 25 Pa kPa around the entire plant as the soil water content decreased, the leaf conductance and transpiration rate showed a strong closing response to leaf water potential at a value of-0.65 MPa, whereas with a vapour pressure deficit of 10 Pa kPa around the entire plant, the rate of transpiration and leaf conductance decreased almost linearly as the leaf water potential decreased from-0.4 to-1.0 MPa. Increasing the vapour pressure deficit from 10 to 30 Pa kPa in 5 Pa kPa steps decreased the leaf conductance by a similar proportion at all extractable soil water contents. At high soil water contents, the decrease in conductance with leaf water potential was greater when the vapour pressure deficit was increased than when it was not, indicating a direct influence of vapour pressure deficit on the stomata. The rate of net photosynthesis decreased to a smaller degree than the leaf conductance when the vapour pressure deficit around the leaf was varied. Overall, the net photosynthetic rate decreased almost linearly from 20 to 25 μmol m s at-0.3 MPa to 5 μmol m s at-1.2 MPa. As the soil water decreased, the internal carbon dioxide partial pressure was maintained between 14 and 25 Pa.No unique relationship between leaf conductance, transpiration rate or photosynthetic rate and leaf water potential was observed, but in all experiments leaf conductance and the rate of net photosynthesis decreased when about two-thirds of the extractable water in the solid had been utilized irrespective of the leaf water potential. We conclude that soil water status, not leaf water status, affects the stomatal behaviour and photosynthesis of H. annuus.
随着可提取土壤水分的减少,研究了向日葵叶片水势、叶片导度、蒸腾速率和净光合速率对10至30 kPa蒸汽压亏缺变化的响应。当土壤含水量降低,整株植物周围蒸汽压亏缺为25 kPa时,叶片导度和蒸腾速率在叶片水势为-0.65 MPa时对叶片水势表现出强烈的关闭响应,而当整株植物周围蒸汽压亏缺为10 kPa时,随着叶片水势从-0.4降至-1.0 MPa,蒸腾速率和叶片导度几乎呈线性下降。以5 kPa的步长将蒸汽压亏缺从10 kPa增加到30 kPa,在所有可提取土壤含水量下,叶片导度均以相似的比例降低。在高土壤含水量条件下,当蒸汽压亏缺增加时,导度随叶片水势的降低幅度大于蒸汽压亏缺未增加时,这表明蒸汽压亏缺对气孔有直接影响。当叶片周围的蒸汽压亏缺变化时,净光合速率的降低程度小于叶片导度。总体而言,净光合速率从-0.3 MPa时的20至25 μmol m⁻² s⁻¹几乎呈线性下降至-1.2 MPa时的5 μmol m⁻² s⁻¹。随着土壤水分减少,叶片内部二氧化碳分压维持在14至25 Pa之间。未观察到叶片导度、蒸腾速率或光合速率与叶片水势之间存在独特关系,但在所有实验中,无论叶片水势如何,当土壤中约三分之二的可提取水分被利用时,叶片导度和净光合速率都会降低。我们得出结论,土壤水分状况而非叶片水分状况影响向日葵的气孔行为和光合作用。