摘要
通过3 a 6季作物收获后测定不同施肥方式下潮土1 m土层中的硝态氮,结果表明无论是0~20 cm、80~100 cm还是0~100 cm土层,其硝态氮含量顺序均是N>NK>NP>NPK>SNPK>MNPK;0~20 cm土层中硝态氮相对值随降雨量增大而减小,降水量大则硝态氮向下淋溶较多;施有机肥或秸秆还田有减轻淋溶的作用。0~60 cm土层中硝态氮相对值在测定时期及处理之间差异均不显著。
The content of NO3--N in 0~100 cm Chao soil after harvest with different fertilizer treatment through 3 years were analyzed. The results indicated that the NO3--N content in 0~20 cm, 80~100 cm and 0~100 cm soil layers was decreased in the order: N> NK> NP> NPK> SNPK > MNPK. The NO3--N content in 0~20 cm layer decreased with precipitation, that was to say precipitation could accelerate NO3--N leaching down, but manure and straw could reduce the leaching. The percentage of NO3--N distributed in 0~60 cm soil layer varied little in different fertilizer treatments.
出处
《土壤与环境》
CSCD
2000年第3期201-203,共3页
Soil and Environmental Sciences
基金
农业部重点科研计划"高新技术与基础研究"项目!(95农-高科-17-03-02)