文章摘要
刘振东,李贵春,周 颖,杨晓梅,尹昌斌,南云不二男.无机肥配施粪肥对华北褐土团聚体分布及有机碳含量的影响[J].农业环境科学学报,2013,32(11):2239-2245.
无机肥配施粪肥对华北褐土团聚体分布及有机碳含量的影响
The Effect of Fertilizer Management Practices on Distribution of Aggregates and SOC
  
DOI:10.11654/jaes.2013.11.019
中文关键词: 褐土  团聚体稳定性  平均重量直径  几何平均直径  有机碳
英文关键词: cinnamon soil  aggregate stability  MWD  GMD  organic carbon
基金项目:
作者单位
刘振东 中国农业科学院农业资源与农业区划研究所 农业部面源污染控制重点实验室 北京 100081 
李贵春 中国农业科学院农业环境与可持续发展研究所 农业部面源污染控制重点实验室 北京 100081 
周 颖 中国农业科学院农业资源与农业区划研究所 农业部面源污染控制重点实验室 北京 100081 
杨晓梅 中国农业科学院农业资源与农业区划研究所 农业部面源污染控制重点实验室 北京 100081 
尹昌斌 中国农业科学院农业资源与农业区划研究所 农业部面源污染控制重点实验室 北京 100081 
南云不二男 日本国际农林水产业研究中心 
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中文摘要:
      为研究无机肥配施粪肥对华北褐土团聚体分布、稳定性及对土壤有机碳(Soil organic carbon, SOC)保护性机制的影响,于2012年采自河北省徐水县试验站冬小麦-夏玉米定位试验田进行了试验。设置1个空白对照CK,1个单施化肥处理N10,4个粪肥与化肥配施处理M1N9、M2N8、M3N7、M5N5,采集0~20 cm耕层土样,测定土样团聚体稳定性和SOC含量。结果表明:单施化肥不能明显提升土壤中SOC含量;配施粪肥能显著地提高R0.25和大团聚体中OC(Organic carbon)的含量。M3N7处理能显著提高团聚体平均重量直径(Mean weight diameter,MWD)、几何平均直径(Geometric mean diameter,GMD)和各级团聚体中OC的含量。M2N8、M3N7、M5N5处理中SOC主要分布在2~0.25 mm的大团聚体上,CK处理中SOC主要分布在微团聚体上,大团聚体含量较低,说明微团聚体比大团聚体形成的早,稳定性高于大团聚体,验证了微团聚体通过胶结作用形成大团聚体的层次性机制。该褐土的团聚体-SOC相互作用说明大团聚体的层次性形成和稳定性对SOC的保护具有关键作用。
英文摘要:
      The research is about influences of aggregate size distribution and stability and soil organic carbon protective mechanism in cinnamon soil in organic and chemical fertilizer management practices. Soil samples ,which were collected from Xushui station long-term positioning experiment field in Hebei Province, includes 6 treatments:chemical fertilizer(N10), four fertilizer management practices which combinated chemical fertilizer with manure, CK. The aggregate size classes were got by dry sieving methods. The results indicated that N10 didn′t significantly increase the capacity of organic carbon in soil, Organic fertilizer could significantly improve the R0.25 and organic carbon content in large-aggregate. The treat of M3N7 can significantly improve MWD, GMD and organic carbon content in all levels of aggregates, showing the significance of organic fertilizer on forming and maintaining soil aggregates. Organic carbon are mainly distributed in the 2~0.25 mm aggregate size classes and organic carbon content in CK treatment of micro-aggregate is highest. That the formation and stability of micro-aggregate is earlier than large-aggregate, verified the mechanism of large-aggregate forming from micro-aggregate through the cementation. The cinnamon soil aggregate-organic carbon interaction is the key factor that the large-aggregate stability and forming with stratification mechanism, which protect the organic carbon.
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