H. Meinke et al., IMPROVING WHEAT SIMULATION CAPABILITIES IN AUSTRALIA FROM A CROPPING SYSTEMS PERSPECTIVE - III - THE INTEGRATED WHEAT MODEL (I-WHEAT), European journal of agronomy, 8(1-2), 1998, pp. 101-116
Previous work has identified several short-comings in the ability of f
our spring wheat and one barley model to simulate crop processes and r
esource utilization. This can have important implications when such mo
dels are used within systems models where final soil water and nitroge
n conditions of one crop define the starting conditions of the followi
ng crop. In an attempt to overcome these limitations and to reconcile
a range of modelling approaches, existing model components that worked
demonstrably well were combined with new components for aspects where
existing capabilities were inadequate. This resulted in the Integrate
d Wheat Model (I_WHEAT), which was developed as a module of the croppi
ng systems model APSIM. To increase predictive capability of the model
, process detail was reduced, where possible, by replacing groups of p
rocesses with conservative, biologically meaningful parameters. I_WHEA
T does not contain a soil water or soil nitrogen balance. These are pr
esent as other modules of APSIM. In I_WHEAT, yield is simulated using
a linear increase in harvest index whereby nitrogen or water limitatio
ns can lead to early termination of grainfilling and hence cessation o
f harvest index increase. Dry matter increase is calculated either fro
m the amount of intercepted radiation and radiation conversion efficie
ncy or from the amount of water transpired and transpiration efficienc
y, depending on the most limiting resource. Leaf area and tiller forma
tion are calculated from thermal time and a cultivar specific phylloch
ron interval. Nitrogen limitation first reduces leaf area and then aff
ects radiation conversion efficiency as it becomes more severe. Water
or nitrogen limitations result in reduced leaf expansion, accelerated
leaf senescence or tiller death. This reduces the radiation load on th
e crop canopy (i.e. demand for water) and can make nitrogen available
for translocation to other organs. Sensitive feedbacks between light i
nterception and dry matter accumulation are avoided by having environm
ental effects acting directly on leaf area development, rather than vi
a biomass production. This makes the model more stable across environm
ents without losing the interactions between the different external in
fluences. When comparing model output with models tested previously us
ing data from a wide range of agro-climatic conditions, yield and biom
ass predictions were equal to the best of those models, but improvemen
ts could be demonstrated for simulating leaf area dynamics in response
to water and nitrogen supply, kernel nitrogen content, and total wate
r and nitrogen use. I_WHEAT does not require calibration for any of th
e environments tested. Further model improvement should concentrate on
improving phenology simulations, a more thorough derivation of coeffi
cients to describe leaf area development and a better quantification o
f some processes related to nitrogen dynamics. (C) 1998 Elsevier Scien
ce B.V.