Biomass Production
The amount of daily solar radiation intercepted by the leaf area of the plant is calculated using Beer’s law (Monsi and Saeki, 1953):
Hphosyn=0.5∗Hday∗(1−exp(−k□∗LAI)) 5:2.1.1
where Hphosyn is the amount of intercepted photosynthetically active radiation on a given day (MJ m−2), Hday is the incident total solar (MJ m−2), 0.5∗Hday is the incident photosynthetically active radiation (MJ m−2), k□ is the light extinction coefficient, and LAI is the leaf area index.
Photosynthetically active radiation is radiation with a wavelength between 400 and 700 mm (McCree, 1972). Direct solar beam radiation contains roughly 45% photosynthetically active radiation while diffuse radiation contains around 60% photosynthetically active radiation (Monteith, 1972; Ross, 1975). The fraction of photosynthetically active radiation will vary from day to day with variation in overcast conditions but studies in Europe and Israel indicate that 50% is a representative mean value (Monteith, 1972; Szeicz, 1974; Stanhill and Fuchs, 1977).
Radiation-use efficiency is the amount of dry biomass produced per unit intercepted solar radiation. The radiation-use efficiency is defined in the plant growth database and is assumed to be independent of the plant’s growth stage. The maximum increase in biomass on a given day that will result from the intercepted photosynthetically active radiation is estimated (Monteith, 1977):
Δbio=RUE∗Hphosyn 5:2.1.2
where Δbio is the potential increase in total plant biomass on a given day (kg/ha), RUE is the radiation-use efficiency of the plant (kg/ha⋅(MJ/m2)−1 or 10−1 g/MJ), and Hphosyn is the amount of intercepted photosynthetically active radiation on a given day (MJ m−2). Equation 5:2.1.2 assumes that the photosynthetic rate of a canopy is a linear function of radiant energy.
The total biomass on a given day, d, is calculated as:
bio=∑i=1dΔbioi 5:2.1.3
where bio is the total plant biomass on a given day (kg ha−1), and Δbioi is the increase in total plant biomass on day i (kg/ha).
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