2017 ASHS Annual Conference
Effects of Interaction Between Atmospheric Humidity and Nutrient-solution Water Potential on Growth and Photosynthesis of Cucumber Seedlings Under Different Atmospheric CO2 Concentration Levels
Effects of Interaction Between Atmospheric Humidity and Nutrient-solution Water Potential on Growth and Photosynthesis of Cucumber Seedlings Under Different Atmospheric CO2 Concentration Levels
Friday, September 22, 2017: 3:00 PM
Kohala 4 (Hilton Waikoloa Village)
There have been many reports that investigate effects of atmospheric humidity on plant growth in many species, but their interactions with other factors are less well known. In the present study, we grew cucumber seedlings hydroponically under two vapor-pressure deficit (VPD) levels, two nutrient-solution water potential (Ψs) levels, and two CO2 concentration levels in controlled-environment chambers, and determined their growth and photosynthetic properties by means of growth analysis and gas-exchange measurements to reveal the potential interactions among these environmental factors. The increased VPD inhibited growth of the seedlings, but the causal factor that inhibited growth differed between Ψs and CO2 concentration levels. Under ambient CO2 concentration, increased VPD inhibited the seedlings’ growth at high Ψs due to decreased leaf expansion, versus decreased CO2 assimilation per unit leaf area at low Ψs. The decrease in intercellular CO2 concentration (Ci) with decreasing stomatal conductance (gs) caused by high VPD did not significantly limit CO2 assimilation at high Ψs, but at low Ψs the decrease in Ci occurred within the range in which CO2 assimilation is more strongly limited by Ci because of smaller gs. This difference created a VPD × Ψs interaction that limited CO2 assimilation. There was a significant VPD × Ψs interaction for leaf expansion; high VPD reduced leaf expansion only at high Ψs. At high CO2 concentration, increased VPD inhibited leaf expansion, but did not affect CO2 assimilation per unit leaf area. This is because the decrease in Ci with decreasing gs occurred where CO2 assimilation was only slightly limited by Ci because of the higher CO2 concentration level. Such complex interactions resulted from the interactions among these environmental factors on CO2 assimilation and expansion growth in complicated ways through the resulting changes in the gaseous diffusion and water balance, and through direct responses to water deficit conditions.