Modern commercial soilless cultivation demands dynamic irrigation triggers derived from real-time crop transpiration rather than static time-clock timers. Under-irrigation induces localized rootzone matric stress and electrical conductivity (EC) spikes, while over-irrigation saturates root pore space, causing rhizosphere anoxia and pythium root rot. The hourly Penman-Monteith model provides the physical standard for partitioning radiative and aerodynamic transpirational demand.
The Penman-Monteith formula computes hourly reference evapotranspiration (\(ET_0\)) by coupling net radiation (\(R_n\)) with vapor pressure deficit (\(VPD\)) and aerodynamic aerodynamic resistance (\(r_a\)) and canopy stomatal resistance (\(r_s\)):
ET_0 = [ Δ·(R_n - G) + ρ_a·c_p·(e_s - e_a) / r_a ] ÷ [ Δ + γ·(1 + r_s / r_a) ] [mm/h]
ET_c = K_c × ET_0 [mm/h]
Where \(\Delta\) represents the slope of the saturation vapor pressure curve, \(R_n - G\) is net canopy radiation minus ground heat flux, \( ho_a\) is air density, \(c_p\) is specific heat of moist air, \(e_s - e_a\) is vapor pressure deficit, \(\gamma\) is the psychrometric constant, and \(K_c\) is the crop coefficient scaled by Leaf Area Index (LAI).