Temporal variation of C and N mineralization, microbial biomass and extractable organic pools in soil after oilseed rape straw incorporation in the field

被引:131
作者
Jensen, LS
Mueller, T
Magid, J
Nielsen, NE
机构
[1] Plant Nutr. and Soil Fertil. Lab., Department of Agricultural Sciences, Roy. Vet. and Agric. University, Thorvaldsensvej 40
关键词
D O I
10.1016/S0038-0717(97)00014-X
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The temporal variation of soil microbial biomass C and N, extractable organic C and N, mineral N and soil-surface CO2 flux in situ in two arable soils (a sandy loam and a coarse sandy soil) was examined periodically for a full year after field incorporation of 0, 4 or 8 t dry mass ha(-1) of oilseed rape straw in late summer. Both unlabelled and N-15-labelled straw were applied. Soil-surface CO2 flux, used as an index of soil respiration, was up to 2-fold higher in the straw-amended treatments than in the unamended treatment at both sites during the first 6-8 wk, but the general temporal pattern was mainly controlled by soil temperature and soil water content. Microbial biomass C and N increased very rapidly after the straw amendments and the 31-49% difference from the unamended treatment persisted throughout the winter. Temporal variations in soil microbial biomass C and N were only within +/-13-22% of the mean at both sites and in all straw treatments over the ly period. Microbial biomass C-to-N ratios were not significantly different between straw treatments and were relatively constant over time. Extractable organic C and N were slightly higher in the straw-amended treatments and were higher in spring and summer than in autumn and winter. More than 90% of the added straw N could be accounted for initially and there was no loss of straw N over the winter period, in spite of a winter rainfall that was twice the 25 y average. Between 52 and 80% of the initial increase in microbial biomass N was derived from the straw N, with up to 27% of the straw N being incorporated into the microbial biomass. Rapid immobilization of soil mineral N occurred simultaneously and the sum of this and the straw-derived microbial biomass N on day 7 exceeded the total increase in microbial biomass N, indicating a very rapid turnover of microbial biomass in the first few days. Significant differences in microbial biomass C and N between the straw treatments were still found after nearly ly and the decay constant of straw-derived microbial biomass N was estimated to be ca. 0.26 y(-1). (C) 1997 Elsevier Science Ltd.
引用
收藏
页码:1043 / 1055
页数:13
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