水蚀条件下不同土壤氮素和有机质流失规律


Autoria(s): 张兴昌; 邵明安
Data(s)

2000

Resumo

人工模拟放水冲刷试验研究结果表明 ,随放水冲刷强度的增大 ,不同土壤硝态氮、铵态氮、有机质和全氮流失加剧 ,泥沙全氮和有机质富集程度减少 ;当给不同土壤施等量的硝酸铵时 ,发现随径流流失化肥的铵态氮和硝态氮分别占施入量的 0 .9%~ 3 .5 %和 8.2 %~ 19.7% ,硝酸铵主要随径流流失 ,以泥沙颗粒流失量甚微 ;土壤侵蚀、有机质和全氮流失量与 >2 0 μm团聚体相关系数分别为 -0 .893 5、-0 .792 8和 -0 .815 1,2 0 μm直径的团聚体是区分土壤有机质和全氮流失的标准

The results of artificial water scoured experiment show that with the increase of water scoured intensity,the losses of nitrate and ammonium in runoff ,and those of organic matter and total N in sediment increased greatly,while the enrichment ratios of organic matter and total N in sediment reduced correspondingly.When the soils in gully hilly loess region were fertilized with same amount of NH\-4NO\-3,the ammonium and nitrate loss in runoff was respectively 0\^9~3\^5% and 8\^2~19\^7% of the application ...

Identificador

http://ir.iswc.ac.cn/handle/361005/691

http://www.irgrid.ac.cn/handle/1471x/140414

Idioma(s)

中文

Fonte

张兴昌, 邵明安.水蚀条件下不同土壤氮素和有机质流失规律.应用生态学报,2000,2:231-234

Tipo

期刊论文