首页> 中文期刊>土壤学报 >不同轮作模式下氮肥用量对土壤有机氮组分的影响

不同轮作模式下氮肥用量对土壤有机氮组分的影响

     

摘要

A 3 a field experiment,consisting of 6 croppings,was conducted to investigate effects of N fertilizationon content and fractionation of soil organic N relative to N application rate and crop rotation mode,paddy/upland(rice/rapeseed,RR)rotation and upland(cotton/rapeseed,CR)rotation. Results show that after the 3 years of crop rotations cultivations,soil total N content in the 0~20 cm soil layer increased remarkably in plots more than 300 kg hm-2 in N input. Compared with CK(No N fertilization, N0-0),soil total N content increased by 13.6%~23.5% and 15.0%~23.0%,respectively,in the treatments 300 kg hm-2 and 375 kg hm-2 in N application rate under either RR or CR rotation. The increase in soil total acidolysable N content accounted for most of the increase in soil total N. Although no significant difference in soil total acidolysable N content was observed between plots under RR and CR rotations,fractionation of the soil acidolysable N varied between plots. The proportion of soil acidolysable ammonium N increased by 33.8% in the plots under RR rotation,much lower than that(53.9%)in the plots under CR rotation,but the increment of unidentified soil acidolysable N in proportion was higher in plots under RR rotation(36.0%) than that(16.6%)in the plots under CR rotation. To sum up,reasonable N fertilization may significantly increase soil organic N content. Fractionation of the soil organic N pool varies sharply between plots under RR and CR rotations. It is,therefore,of important significance to optimize N fertilization for high crop yield and high N utilization efficiency in the light of the characteristics of soil organic N transformation under different rotation systems.%通过三年六季的田间定位试验,对比研究了水旱轮作(水稻/油菜)和旱地轮作(棉花/油菜)下氮肥用量对土壤有机氮含量及其组分的影响.结果表明,经过三年轮作后,周年轮作氮肥投入超过300 kg hm-2(以纯氮计,下同)的处理0~20 cm土壤全氮含量明显增加.与不施氮处理相比,周年氮肥用量为300 kg hm-2和375 kg hm-2水旱轮作处理0~20 cm土壤全氮含量增加了13.6%~23.5%,而旱地轮作处理则增加了15.0%~23.0%,土壤酸解态氮含量增加是土壤全氮变化的主要原因.两种轮作模式下土壤酸解态氮含量无显著差异,但土壤酸解态氮各组分的变化却不相同.水旱轮作中酸解铵态氮增加的比例(33.8%)低于旱地轮作(53.9%),但其酸解未知态氮含量增加的比例(36.0%)高于旱地轮作(16.6%).综上所述,周年氮肥合理施用能明显提高土壤有机氮含量,水旱和旱地轮作下土壤酸解态氮库各组分变化差异明显.根据不同轮作模式下土壤有机氮库转化特点,优化氮肥施用对于提高作物产量和氮肥利用率具有重要意义.

著录项

  • 来源
    《土壤学报》|2017年第6期|1547-1558|共12页
  • 作者单位

    华中农业大学资源与环境学院,农业部长江中下游耕地保育重点实验室,武汉 430070;

    华中农业大学资源与环境学院,农业部长江中下游耕地保育重点实验室,武汉 430070;

    华中农业大学资源与环境学院,农业部长江中下游耕地保育重点实验室,武汉 430070;

    华中农业大学资源与环境学院,农业部长江中下游耕地保育重点实验室,武汉 430070;

    华中农业大学资源与环境学院,农业部长江中下游耕地保育重点实验室,武汉 430070;

    华中农业大学资源与环境学院,农业部长江中下游耕地保育重点实验室,武汉 430070;

    华中农业大学资源与环境学院,农业部长江中下游耕地保育重点实验室,武汉 430070;

    华中农业大学资源与环境学院,农业部长江中下游耕地保育重点实验室,武汉 430070;

  • 原文格式 PDF
  • 正文语种 chi
  • 中图分类 有机成分;
  • 关键词

    氮肥; 水旱轮作; 旱地轮作; 全氮; 土壤酸解态氮;

相似文献

  • 中文文献
  • 外文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号