Institute of Soils and Water, Agricultural Research Organization, The Volcani Center, Bet Dagan 50250 Israel.
Plant Physiol. 1991 Oct;97(2):515-22. doi: 10.1104/pp.97.2.515.
Cotton (Gossypium hirsutum L. cv Acala SJ2) plants were exposed to three levels of osmotic or matric potentials. The first was obtained by salt and the latter by withholding irrigation water. Plants were acclimated to the two stress types by reducing the rate of stress development by a factor of 4 to 7. CO(2) assimilation was then determined on acclimated and nonacclimated plants. The decrease of CO(2) assimilation in salinity-exposed plants was significantly less in acclimated as compared with nonacclimated plants. Such a difference was not found under water stress at ambient CO(2) partial pressure. The slopes of net CO(2) assimilation versus intercellular CO(2) partial pressure, for the initial linear portion of this relationship, were increased in plants acclimated to salinity of -0.3 and -0.6 megapascal but not in nonacclimated plants. In plants acclimated to water stress, this change in slopes was not significant. Leaf osmotic potential was reduced much more in acclimated than in nonacclimated plants, resulting in turgor maintenance even at -0.9 megapascal. In nonacclimated plants, turgor pressure reached zero at approximately -0.5 megapascal. The accumulation of Cl(-) and Na(+) in the salinity-acclimated plants fully accounted for the decrease in leaf osmotic potential. The rise in concentration of organic solutes comprised only 5% of the total increase in solutes in salinity-acclimated and 10 to 20% in water-stress-acclimated plants. This acclimation was interpreted in light of the higher protein content per unit leaf area and the enhanced ribulose bisphosphate carboxylase activity. At saturating CO(2) partial pressure, the declined inhibition in CO(2) assimilation of stress-acclimated plants was found for both salinity and water stress.
棉花(Gossypium hirsutum L. cv Acala SJ2)植株暴露于三种渗透或基质势水平下。第一种通过盐获得,第二种通过断水获得。通过将两种胁迫类型的胁迫发展速度降低 4 到 7 倍,植物适应这两种胁迫。然后,对适应和非适应植物进行 CO(2)同化测定。与非适应植物相比,盐胁迫下 CO(2)同化的下降在适应植物中显著较小。在环境 CO(2)分压下,在水分胁迫下未发现这种差异。在适应 -0.3 和 -0.6 兆帕盐胁迫的植物中,净 CO(2)同化与细胞间 CO(2)分压的关系的初始线性部分的斜率增加,但在非适应植物中没有增加。在适应水分胁迫的植物中,斜率的这种变化并不显著。叶片渗透势在适应植物中降低得更多,因此即使在 -0.9 兆帕时也能保持膨压。在非适应植物中,膨压压力在约 -0.5 兆帕时达到零。盐适应植物中 Cl(-)和 Na(+)的积累完全解释了叶片渗透势的降低。在盐适应和水分胁迫适应植物中,有机溶质浓度的升高仅占溶质总增加的 5%和 10%至 20%。这种适应是根据单位叶面积的更高蛋白质含量和增强的核酮糖二磷酸羧化酶活性来解释的。在饱和 CO(2)分压下,发现盐胁迫和水分胁迫适应植物的 CO(2)同化抑制下降。