Abstract
Estimates of net soil sulfur (S) mineralisation of grazed pastures in New
Zealand were made using the New Zealand Ministry of Agriculture (MAF) S model
and a recently developed simple mass-balance S model. Quantitative estimates
of S inputs and outputs in the MAF S model were also compared with those
obtained in recent field trials. Results obtained showed that the MAF S model
was reasonably accurate in estimating S inputs and outputs and long-term
maintenance pasture S requirements but not short-term pasture S requirements,
due to the parameters used not accounting for the effects of major factors
affecting soil organic S mineralisation. Net annual soil S mineralisation
under high-producing pastures estimated by the simple mass-balance model was
substantial, ranging from 17·7 to 29·1 kg S/ha ·
year, thus showing that the mineralisation of soil organic S can be a
significant source of S for pasture plant growth. The inclusion of the MAF
soil organic S test into the MAF S model may improve short-term S
requirements, but the soil organic S test needs to be calibrated with net soil
S mineralisation potential, soil types, management practices, and pasture
production. Although some of the excreta S that has been transferred to stock
camps may be returned to the main grazing area, this excretal S and sulfate
leaching losses were found to be major S outputs of the main grazing area. The
results suggested that the mineralisation of soil organic S may not be
sufficient to replace S losses indefinitely when S fertiliser applications are
withheld.
Subject
General Agricultural and Biological Sciences
Cited by
9 articles.
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