Article ID Journal Published Year Pages File Type
4391971 European Journal of Soil Biology 2013 9 Pages PDF
Abstract

Seasonal changes in soil nematode community structure were investigated in a 9-year pig manure experiment on an acid soil in subtropical China. The manure treatments included: 1) no manure (CK); 2) low rate with 150 kg N ha−1 y−1 (ON1); 3) high rate with 600 kg N ha−1 y−1 (ON2); 4) high rate with 600 kg N ha−1 y−1 and 3000 kg of Ca(OH)2 ha−1 3 y−1 (ON2L). The total nematode numbers ranged from 72 to 880 individuals per 100 g dry soil, represented by 27 genera, and followed a decreasing order of ON2 > ON1 > ON2L > CK. The minimum of nematode abundance was observed in April before fertilizing while the maximum in July before maize harvesting. There was a succession from Rhabditidae and Cephalobus to Protorhabditis   in the first 3 months after applying high rate manure. Nematode channel ratio and faunal analysis indicated disturbed soil food webs with bacterial decomposition under high rate manure, whereas those with fungal decomposition under low rate manure. Variation partitioning analysis showed the climatic and soil factors independently explained 17.3% and 24.7% of the variation in nematode community composition, respectively. Aggregated boosted trees analysis showed soil −NO3–NNO3−–N and/or +NH4–NNH4+–N contents had the strongest effect on most trophic groups, apart from available K on bacterivores. We concluded that soil factors had more important influence on nematode community composition than climatic factors.

Graphical abstractFigure optionsDownload full-size imageDownload as PowerPoint slideHighlights► Low rate of organic manure increases plant parasites and fungivores abundance. ► High rate manure promotes disturbed food webs with bacterial decomposition. ► Soil factor exerts more important impact than climatic factor on nematode. ► Soil NO3–N and/or NH4–N contents show strong effects on most trophic groups.

Related Topics
Life Sciences Agricultural and Biological Sciences Soil Science
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