Convert GPR biophysical outputs into NNI inputs (low-level helper)
Source:R/estimate_biophysical.R
biophysical_to_NNI_inputs.RdLow-level helper that turns LAI, Cm and a canopy-N raster
into the two layers consumed by compute_NNI: the
aboveground dry biomass W (t DM ha\(^{-1}\)) and the plant N
concentration N_actual (pct DM).
Usage
biophysical_to_NNI_inputs(
lai_rast,
cm_rast,
cnc_rast,
alpha_leaf = 0.35,
k_NChl = NULL,
w_min = 1
)Arguments
- lai_rast
RasterLayer or terra SpatRaster with leaf area index.
- cm_rast
RasterLayer or terra SpatRaster with leaf dry-matter content (g cm\(^{-2}\)).
- cnc_rast
RasterLayer or terra SpatRaster with canopy nitrogen: either
CNC_Cprot(g N m\(^{-2}\), protein path) orCNC_Cab(g Chl m\(^{-2}\), chlorophyll path - in that case supplyk_NChl).- alpha_leaf
Leaf-to-total aboveground biomass allocation coefficient (default 0.35; use
crop_params_NNIfor crop-specific values).- k_NChl
When
cnc_rastcontains CNC_Cab (g Chl m\(^{-2}\)), the canopy-level N:Chl ratio used to convert it to g N m\(^{-2}\) (defaultNULL= protein path, no conversion).- w_min
Minimum biomass (t DM ha\(^{-1}\)) below which pixels are masked (default 1.0).
Value
A named list with two SpatRaster layers, W and
N_actual, ready to be passed to compute_NNI.
Details
Most users should rather call the end-to-end
compute_NNI_from_S2 wrapper, which handles crop-specific
parameters, FVC / SCL masking and zone classification in a single call.
This function is exposed for advanced workflows that need direct
control over the conversion.
The conversions follow
$$W_{leaf}\ (\mathrm{g\ m^{-2}}) = LAI \cdot C_m \cdot 10^4$$
$$W\ (\mathrm{t\ DM\ ha^{-1}}) = W_{leaf} / (100 \cdot \alpha_{leaf})$$
(leaf-to-total aboveground allocation coefficient \(\alpha_{leaf}\),
~0.30-0.45 depending on crop and phenology), and
$$N_{actual}(\% DM) = 100 \cdot N_{total} / W_{leaf} \cdot \alpha_{leaf}^{-1}$$
with \(N_{total}\) either equal to CNC_Cprot (g N m\(^{-2}\))
or k * CNC_Cab when the chlorophyll path is used.
Pixels where W < w_min are set to NA because the
critical-N dilution curve is not defined below that biomass.