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应用生态学报 ›› 2002, Vol. ›› Issue (6): 693-697.

• 研究论文 • 上一篇    下一篇

湖南主要类型稻田土壤固定态铵含量及其影响因素

张杨珠, 廖继佩, 李法云, 黄运湘, 胡瑞芝, 袁正平   

  1. 湖南农业大学资源环境学院, 长沙 410128
  • 收稿日期:2000-07-17 修回日期:2000-10-13 出版日期:2002-06-15
  • 通讯作者: 张杨珠,男,1956年生,硕士,教授,主要从事土壤化学与肥力方面的研究,发表论文40余篇.Tel:0731-4618156,E-mail:Zhangyangzhu@263.net
  • 基金资助:
    国家“九五”科技攻关重中之重项目(950010103);湖南省教育厅科学基金资助项目

Fixed ammonium content of chief paddy soil types in Hunan Province and its influencing factors

ZHANG Yangzhu, LIAO Jipei, LI Fayun, HUANG Yunxiang, HU Ruizhi, YUAN Zhengping   

  1. College of Resource and Environment Science, Hunan Agricultural University, Changsha 410128
  • Received:2000-07-17 Revised:2000-10-13 Online:2002-06-15

摘要: 通过野外调查取样和室内培养试验,应用Silva和Bremner方法,研究了湖南省主要类型稻田土壤的固定态铵含量及其影响因素.结果表明,该省主要类型稻田土壤固定态铵含量为141~353mg·kg-1,平均为272±67mg·kg-1,占土壤全N的11.2%,高于湖南省以北各地区土壤和本地区地带性土壤———红壤的固定态铵含量.其含量的顺序为河沙泥>紫泥田>潮沙泥>黄泥田>红黄泥.在土壤剖面中,固定态铵含量随剖面深度的变化有4种情况:在1m深度范围内随深度增加而增加;随深度增加而减少;随深度增加而无明显变化;土壤剖面中某一土层固定态铵含量明显增加或减少.土壤固定态铵含量占土壤全N百分比随深度增加而恒增大.土壤对NH4+的固定作用在30℃下最强,高于20℃和40℃;长期淹水有利于潮沙泥、紫泥田和河沙泥对NH4+的固定作用,但干湿交替有利于黄泥田对NH4+的固定作用.相关分析表明,土壤固定态铵含量仅与<0.01mm粘粒含量呈P0.05水平的显著正相关,与有机质、全N、有机N和<0.001mm粘粒含量的相关性均不显著.

Abstract: By the method of Silva and Bremner,the fixed ammonium content of chief paddy soil types in Hunan Province and its influencing factors were studied. The results showed that the content of fixed ammonium in plough layer ranged from 141 mg·kg-1 to 353 mg·kg-1,averaged 272±67 mg·kg-1,and accounted for 112% of total soil N. The content of fixed ammonium was in order of alluvial sandy soil > purple clayey soil > newly alluvial sandy soil > yellow clayey soil > reddish yellow clayey soil. There were four distribution models of fixed ammonium in the soil profiles: 1) fixed ammonium content increased with the increase of depth in the profiles; 2) fixed ammonium content decreased with the increase of depth; 3) there was no distinct change; and 4) abrupt increase or decrease was found in the profiles. The percentage of fixed ammonium to total Nin soils always increased with the increase of depth. The fixation of NH4+ by soil was the strongest under 30℃. Long-term submergence benefited to the fixation of NH4+ in newly alluvial sandy soil,purple clayey soil,and alluvial sandy soil,while the alternation of drying and wetting contributed to the fixation of NH4+ in yellow clayey soil best. The content of fixed ammonium in tested soil was correlated with the content of clay <0.01 mm at the significant level,and not correlated with the content of clay <0.001 mm,total N,organic N,and matter.

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