Simulations of the temporal development of leaf area index, canopy height, albedo and root depth are based on biomass, i.e. carbon content in the plant, when the switch for plant growth is “on” (refer to the Nitrogen and Carbon chapter). Simulations of the temporal development of all these plant properties always take place when growth is simulated, although these values are not further used in the abiotic part of the simulation if the temporal development of a certain plant property has been chosen as static.
When simulating temporal development by the plant growth model some empirical functions are used to convert figures on biomass to the appropriate physical attributes of the plant. Parameters for these conversions are found in a parameter table: Size and shape of growing plant.
The Leaf area index, Al, is estimated as:
where pl,sp is a parameter and Bl is the total mass of leaf (i.e. the carbon content in the leaves, CLeaf +COldLeaf). See viewing function Simulated Leaf Area Index.
The canopy height, Hp, is estimated as:
where phmax, ph1, ph2, ph3 and ph4 are parameters. Bag is the above ground biomass (i.e. the carbon content in the leaves and stem, CLeaf + COldLeaf + CStem + COldStem), ∆tpl is the time that has elapsed since the emergence day (i.e. plant age) and Cgrain is the carbon content in the grain pool. See viewing function Simulated Canopy Height.
The albedo, aveg, may be specified differently depending on if the plant is in a vegetative stage, apveg, or a grain stage, apgrain, of plant development. The growth stage index is used to interpolate between the two values in the grain filling stage:
• Grain
stage:
where:
(3.6)
and GSI is the growth
stage index described in the “Nitrogen and Carbon” chapter.
The root depth, zr, is estimated as:
where pzroot and pincroot are parameters and Br is the mass of roots (i.e. the carbon content in the roots, CRoots +COldRoots). See viewing function Simulated Root Depth.
The root length, Lr, is estimated as:
where prl.sp is a parameter and Br is the mass of roots (i.e. the carbon content in the roots, CRoots). The old root biomass is not considered since these roots are assumed to play a minor role for water uptake.