CONCENTRATION AND FLUX OF CO2, TURBULENCE FLUXES AND RADIATION BALANCE IN THE NEAR SURFACE LAYER OVER WHEAT FIELD

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  • The gradient of CO2 concentration, photosynthetically active radiation(PAR). net radiation.soil heat flux, profiles of wind speed, and air temperature and humidity were measured above a wheat field during May and June 1985 at Beijing Agro-Ecosystems Experimental Station. Beijing,China. Fluxes of carbon dioxide, sensible heat, latent heat and momentum were calculated by using the aerodynamic method. The observation site. equipment, calibration techniques, the errors associated with the measurement, and the computational procedures are described. The results show that the diurnal variations of amplitude of CO2 concentrations were 103.8 to 27. 0.86. 3 to 22.8 and 69.8 to 11.6 ppm:the average CO2 concentrations were 331.5. 339.9 and 364.6 ppm for the photosynthesis type, and 369.6. 364.0 and 375.2 ppm for the respiration type at 1. 2 and 10 m above surface, respectively, from May 14 to June 15. In the daytime, transfer direction of the CO2 fluxes and gradients is from air to crop canopy, and at noon(1100 to 1300 BT(Beijing Time)) the transfer rate reaches negative maximum value. At night, transfer of CO2 fluxes and gradients is in the reversed direction and reaches positive maximum in the early morning(0400 to 0600 BT). There are strong negative correlations between CO2 flux and the net radiation(Rn),available energy(H+LE). photosynthetically active radiation(PAR) and momentum flux(τ).
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