Soil degradation under cropping and its influence on wheat yield on a weakly structured New Zealand silt loam

Citation
Gs. Francis et al., Soil degradation under cropping and its influence on wheat yield on a weakly structured New Zealand silt loam, AUST J SOIL, 39(2), 2001, pp. 291-305
Citations number
27
Categorie Soggetti
Environment/Ecology
Journal title
AUSTRALIAN JOURNAL OF SOIL RESEARCH
ISSN journal
00049573 → ACNP
Volume
39
Issue
2
Year of publication
2001
Pages
291 - 305
Database
ISI
SICI code
0004-9573(2001)39:2<291:SDUCAI>2.0.ZU;2-4
Abstract
Results from the first phase of a long-term experiment showed that, after 6 years under pasture, several soil quality attributes had improved compared with soil cropped annually. The objectives of this study were to quantify the effects of pasture-induced increases in structural stability and organi c matter (N fertility) on wheat grown in 3 successive seasons following pas ture cultivation. Growing winter wheat after the ploughing of land that had previously grown perennial grass resulted in gradual reductions in soil or ganic C and total N. Reductions in soil microbial biomass C and earthworm p opulations were much more rapid. Soil aggregate stability declined rapidly in the first year after ploughing, but more slowly after that. Soil macropo rosity increased after ploughing, mainly due to the relief of compaction ca used by sheep treading during grazing. The contrasting soil conditions that existed at the end of the first experimental phase significantly affected the harvest yield of the first and second wheat crops, with yields 2-3 t/ha greater after perennial grasses than after annual crops. Variations in har vest yield and N uptake were explained by differences in soil N fertility a nd soil structural conditions. Treatment effects on yield were not detected in the third wheat crop. For the structural condition and N fertility of t his soil, the extent of improvement during 3 years under perennial pasture was similar to the extent of decline under 3 years of cropping. This sugges ts that similar lengths of pastoral and arable cropping are needed in crop rotations for the long-term maintenance of these properties in weakly struc tured silt loam soils in New Zealand.