An elemental S oxidation model has been developed which combines a max
imum S release rate with modifiers for temperature and soil moisture c
onditions. This model has been combined with a pasture growth and CNSP
nutrient cycling model to match S oxidation rate to pasture S demand.
In two Southern Australian enviroments, 100 mu m elemental S was supe
rior to 200 mu m particles whilst in Northern Australia the 200 mu m p
articles were superior. These models can be used to match S release to
plant demand.