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POTENTIAL FOR AGRICULTURAL BIOMASS PRODUCTION



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FAO land evaluation a-a1080e
40 2019 ND-CP 413905
POTENTIAL FOR AGRICULTURAL BIOMASS PRODUCTION 
Agro-ecological zoning
The Agro-Ecological Zones (AEZ) approach is an example of indicator modelling. 
It is a GIS-based modelling framework that combines land evaluation methods with 
socio-economic and multiple-criteria analysis to evaluate spatial and dynamic aspects 
of agriculture within a broader environmental context (FAO 1996). The methodology 
involves the representation of land in layers of spatial information and combination 
of these layers using a Geographic Information System. The combination of layers 
produces agro-ecological cells with georeferenced land resources information. The 
results of an AEZ assessment are estimated by grid cell and aggregated to national, 
regional or global scale. The results include identification of areas with specific climate, 
soil, and topographic constraints to crop production; estimation of the location, 
extent and productivity of rainfed and irrigated cultivable land and their potential for 
expansion; quantification of cultivation potential of land currently in forest ecosystems; 
and impacts of climate change on food production potential, geographical shifts of 
cultivable land, and implications for food security (Fischer et al., 2002). Such national-
level information with global coverage is critical for knowledge-based decision making 
for sustainable agricultural development.
Plant growth modelling
Plant growth modelling is process-based and typically involves the calculation of 
three components: plant water requirements, biomass production and plant litter 
decomposition. Plant growth models are essentially point-oriented and may be linked 
with a GIS through multiple model runs for a representative range of points across the 
grid surface. 
Plant water requirements
The major driver for a plant water balance is the reference evapotranspiration. Five 
major steps can be identified in a water balance: 
1. calculation of the reference evapotranspiration, 
2. determination of the plant growth characteristics and plant parameters
3. calculation of the actual evapotranspiration, 
4. calculation of plant-available water capacity and 
5. calculation of the water balance. 


Annex 3 – Tools for land evaluation
93
Allen et al., (1998) present an updated procedure for calculating reference and 
actual evapotranspiration from meteorological data and crop coefficients. In addition 
to the method of using a single coefficient to calculate the actual evapotranspiration 
(Doorenbos and Pruitt 1977), Allen et al., (1998) recommend the use of two factors 
to separately describe evaporation and transpiration. A further revision and update 
provides details on the Penman-Monteith combination method as a new standard for 
reference evapotranspiration and advises on procedures for calculating the various 
parameters and estimating missing climatic data. 

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