文献类型： 外文期刊

作者： Wu, TY ¹ ; Schoenau, JJ ² ; Li, FM ² ; Qian, PY ² ; Malhi, SS ³ ; Shi, YC;

作者机构： 1.Univ Saskatchewan, Dept Soil Sci, Saskatoon, SK S7N 5A8, Canada

2.Univ Saskatchewan, Dept Soil Sci, Saskatoon, SK S7N 5A8, Canada; Lanzhou Univ, State Key Lab Arid Agroecol, Lanzhou 730070, Peoples R China; Gansu Agr Acad Sci, Soil Sci & Fertilizer Inst, Lanzhou 730070, Peoples R China; Agr & Agri Food Canada, Res Farm, Melfort, SK S0E 1A0, Canada

3.Univ Saskatchewan, Dept Soil Sci, Saskatoon, SK S7N 5A8, Canada; Lanzhou Univ, State Key Lab Arid Agroec

关键词： soil organic carbon;particle-size fractionation;organo-mineral complex;tillage and rotation system

期刊名称：BIOLOGY AND FERTILITY OF SOILS （ 影响因子：6.432； 五年影响因子：6.332 ）

ISSN： 0178-2762

年卷期： 2006 年 42 卷 4 期

页码：

收录情况： SCI

摘要： The effects of several dominant tillage and rotation systems on soil organic C content of different particle-size fractions were studied in Chernozemic soils from southwestern and east-central Saskatchewan, Canada. In an Orthic Brown Chernozem in southwestern Saskatchewan, 7 years of no-till cereal-fallow, imposed on a long-term tillage fallow-wheat rotation soil, resulted in 0.1 Mg C ha(-1) more organic C mass in the sand + organic matter (OM) fraction of the 0- to 5-cm layer, whereas organic C associated with coarse silt (CS), fine silt (FS), coarse clay, and fine clay of 0- to 5- and 5- to 10-cm layers was less than that of the comparable tilled cereal-fallow system. Conversion of tilled fallow-wheat rotation soil to continuous cropping had a slight effect, whereas the organic C mass in all the size fractions was significantly increased in both 0- to 5- and 5- to 10-cm layers after alfalfa was introduced on tilled fallow-wheat as perennial forage for 10 years. In an Orthic Black Chernozem in east-central Saskatchewan that was cultivated and tilled using a cereal-fallow rotation for 62 years, organic C mass decreased in sand + OM, CS, and FS of 0- to 10-cm depth. Conversion of the tilled cereal-fallow cropland soil back to seeded grassland resulted in significantly more soil organic C in sand + OM fraction after 12 years of grass seed-down. The sand + OM fraction appears to be the size fraction pool initially most sensitive to adoption of management practices that are liable to sequester carbon in the soil.