Department of Botany, Hebrew University of Jerusalem, Israel.
Plant Physiol. 1966 Jan;41(1):39-44. doi: 10.1104/pp.41.1.39.
CO(2) depresses water influx into sunflower hypocotyl segments of low water potential; by contrast, it stimulates flux into segments of high water potential. When segments of high potential were placed in a series of mannitol concentrations and allowed to achieve steady rates of water uptake, influx into CO(2)-treated tissue in a solution of 3 atm equalled that into control tissue in water. Reasons are given for deducing that a change in internal osmotic concentration (pi(i)) of the order of 40% would be necessary to account for this result on the basis of pi(i). Direct measurements (by cryoscopy and by the minimum volume method) detected no difference in the steady state value for pi(i) as between CO(2)-treated and control tissue. It was therefore concluded that CO(2) had caused some reduction in turgor pressure.Water uptake into tissue treated with CO(2) for only the first 2 minutes of a 30-minute period was equal to that into tissue treated continuously with CO(2), i.e. 3 times the control value. Ten seconds' CO(2) treatment produced a significant stimulation. When the cycles of treatment were repeated the samples receiving flashes of CO(2) maintained a rate of water uptake superior to that of the control, whereas influx into continuously treated tissue fell below the control value after 1 hour.CO(2) treatment applied in a moist air chamber stimulated subsequent water influx when the tissue was transferred to water. Fifteen seconds' treatment was sufficient to produce a marked effect. Even when a transition period of 30 minutes in the moist chamber was interposed between CO(2) treatment (5 minutes) and transfer to water, a stimulation was observed. The CO(2) effect could be achieved at zero degrees; 5 minutes' treatment in the moist chamber at zero degrees, followed by a 15-minute transition period at the same temperature, substantially increased subsequent water uptake at 25 degrees .
二氧化碳抑制低水势下的向日葵下胚轴切段的水分流入;相反,它刺激高水势下的水分流入。当高水势的切段被放置在一系列甘露醇浓度中,并允许它们达到稳定的水分吸收速率时,在 3 个大气压的二氧化碳处理组织中的流入量等于在水中的对照组织中的流入量。有理由推断,根据渗透势(pi(i)),内部渗透浓度的变化(pi(i))需要达到约 40%,才能解释这一结果。直接测量(冰点法和最小体积法)未检测到二氧化碳处理和对照组织之间 pi(i)稳态值的差异。因此得出结论,二氧化碳导致膨压降低。在 30 分钟的处理期间仅对组织进行 2 分钟的二氧化碳处理,吸收的水量等于连续用二氧化碳处理的组织,即达到对照值的 3 倍。10 秒的二氧化碳处理会产生明显的刺激。当处理周期重复时,接收二氧化碳闪烁的样本保持高于对照的水分吸收速率,而连续处理的组织的流入量在 1 小时后低于对照值。在潮湿空气室中应用二氧化碳处理刺激组织转移到水后随后的水分流入。15 秒的处理足以产生明显的效果。即使在二氧化碳处理(5 分钟)和转移到水之间插入 30 分钟的潮湿室过渡期,也观察到了刺激。二氧化碳的作用可以在 0 度下实现;在 0 度的潮湿室中处理 5 分钟,然后在相同温度下进行 15 分钟的过渡期,可大大增加在 25 度下的后续水分吸收。