In high-intensity commercial crop production, light and carbon dioxide represent the primary substrates for the Calvin-Benson cycle. Ambient atmospheric CO₂ (~420 ppm) is biochemically rate-limiting for C3 greenhouse crops (tomatoes, cucumbers, peppers, strawberries). Supplying supplemental carbon dioxide up to 800–1,200 ppm elevates net CO₂ assimilation (\(A_{net}\)) by 25–40%, provided canopy stomata remain open and photosynthetically active.
The biochemical model of Farquhar, von Caemmerer, and Berry (FvCB) establishes that net carbon assimilation is limited by either Rubisco enzyme kinetics (\(W_c\)) or RuBP regeneration via electron transport (\(W_j\)):
A_net = min(W_c, W_j) - R_d [μmol/m²·s]
W_c = V_cmax × [ (C_i - Γ*) ÷ (C_i + K_c·(1 + O_i / K_o)) ]
g_s = g_0 + a_1 × [ (A_net × RH) ÷ C_s ] [mol/m²·s]
The Ball-Berry model couples stomatal conductance (\(g_s\)) directly with carbon assimilation (\(A_{net}\)), relative humidity (\(RH\)), and surface CO₂ concentration (\(C_s\)). Under high CO₂ concentrations, guard cells naturally decrease aperture to conserve water, yet internal intercellular carbon (\(C_i\)) remains high, drastically elevating instantaneous Water Use Efficiency (WUE).