Abstract
Changes in crop water use due to elevated CO 2 concentration ([CO 2]) must be evaluated for predicting agricultural productivity and water resource availability. We quantified the effects of elevated [CO 2] on the energy balance and canopy evapotranspiration (ET) in rice paddies. Rice ( Oryza sativa L.) was grown under both ambient [CO 2] (A-CO 2) and elevated [CO 2] (E-CO 2) imposed by free-air CO 2 enrichment (FACE) in northern Japan. Observations were made of micrometeorology and plant characteristics, including stomatal conductance and leaf area index (LAI). We estimated energy balances using a double-source model with heat transfers from the vegetation canopy and the water surface to avoid errors due to uncertainty in the measured radiative infrared (IR) temperatures. E-CO 2 reduced stomatal conductance by 13% in upper leaves and by 40% in lower leaves at the panicle initiation stage, but the reduction rates subsequently decreased. Stomata closed more in the E-CO 2 plot as vapour pressure deficit increased. Daily mean temperature of the vegetation canopy increased by 0.2–1 °C in response to stomatal closure under E-CO 2, whereas water surface temperature decreased by 1 °C before rice heading because of increased shading from the larger leaves in E-CO 2. The radiative IR temperature decreased by up to 1 °C in E-CO 2 before June, and increased by up to 0.6 °C thereafter. Latent heat flux decreased in E-CO 2, which was balanced by increased sensible heat flux and upward long-wave radiation. The decrease was greatest under dry and windy conditions. Total water use by plants throughout the growing season was 268.7 mm in A-CO 2 and 246.8 mm in E-CO 2, giving a saving of 22 mm of water in E-CO 2. Reduced transpiration (by 8.2%), combined with increased total biomass (by 9.1%), increased water use efficiency in E-CO 2 by 19%.
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