首页> 外文期刊>Soil Biology & Biochemistry >Mechanisms of soil N dynamics following long-term application of organic fertilizers to subtropical rain-fed purple soil in China
【24h】

Mechanisms of soil N dynamics following long-term application of organic fertilizers to subtropical rain-fed purple soil in China

机译:中国亚热带雨养紫色土长期施用有机肥后土壤氮动态变化机理

获取原文
获取原文并翻译 | 示例
           

摘要

In this study, a N-15 tracing incubation experiment and an in situ monitoring study were combined to investigate the effects of different N fertilizer regimes on the mechanisms of soil N dynamics from a long-term repeated N application experiment. The field study was initiated in 2003 under a wheat-maize rotation system in the subtropical rain-fed purple soil region of China. The experiment included six fertilization treatments applied on an equivalent N basis (280 kg N ha(-1)), except for the residue only treatment which received 112 kg N ha(-1): (1) UC, unfertilized control; (2) NPK, mineral fertilizer NPK; (3) OM, pig manure; (4) OM-NPK, pig manure (40% of applied N) with mineral NPK (60% of applied N); (5) RSD, crop straw; (6) RSD-NPK, crop straw (40% of applied N) with mineral NPK (60% of applied N). The results showed that long-term repeated applications of mineral or organic N fertilizer significantly stimulated soil gross N mineralization rates, which was associated with enhanced soil C and N contents following the application of N fertilizer. The crop N Make and yield were positively correlated with gross mineralization. Gross autotrophic nitrification rates were enhanced by approximately 2.5-fold in the NPK, OM, OM-NPK, and RSD-NPK treatments, and to a lesser extent by RSD application, compared to the UC. A significant positive relationship between gross nitrification rates and cumulative N loss via interflow and runoff indicated that the mechanisms responsible for increasing N loss following long-term applications of N fertilizer were governed by the nitrification dynamics. Organic fertilizers stimulated gross ammonium (NH4+) immobilization rates and caused a strong competition with nitrifiers for NH4+, thus preventing a build-up of nitrate (NO3-). Overall, in this study, we found that partial or complete substitution of NPK fertilizers with organic fertilizers can reduce N losses and maintain high crop production, except for the treatment involving application of RSD alone. Therefore, based on the N transformation dynamics observed in this study, organic fertilizers in combination with mineral fertilizer applications (i.e. OM, OM-NPK, and RSD-NPK treatments) are recommended for crop production in the subtropical rain-fed purple soils in China. (C) 2015 Elsevier Ltd. All rights reserved.
机译:在这项研究中,通过长期重复施氮实验,结合N-15示踪温育实验和原位监测研究,研究了不同氮肥施用方式对土壤氮动力学机制的影响。田间研究于2003年在中国亚热带雨养紫色土地区的小麦-玉米轮作系统下启动。该实验包括六种以等量氮为基础的施肥处理(280 kg N ha(-1)),唯一残渣处理的施肥处理为112 kg N ha(-1):(1)UC,未受精对照; (2)氮磷钾,矿物肥料氮磷钾; (3)OM,猪粪; (4)OM-NPK,猪粪(施氮量的40%)与矿物质氮磷钾(施氮量的60%); (5)RSD,农作物秸秆; (6)RSD-NPK,农作物秸秆(施氮量的40%)与矿物质氮磷钾(施氮量的60%)。结果表明,长期重复施用矿物或有机氮肥可显着刺激土壤总氮矿化速率,这与施用氮肥后土壤碳和氮含量的提高有关。作物的氮素产量和产量与矿化总量呈正相关。与UC相比,NPK,OM,OM-NPK和RSD-NPK处理的总自养硝化速率提高了约2.5倍,而RSD施用的效果则较小。总硝化速率与通过内流和径流累积的氮损失之间存在显着的正相关关系,表明长期施用氮肥后导致氮损失增加的机理受硝化动力学的控制。有机肥料刺激了总铵(NH4 +)的固定率,并与硝化剂激烈竞争NH4 +,从而防止了硝酸盐(NO3-)的积累。总体而言,在这项研究中,我们发现,除了单独施用RSD的处理外,用有机肥料部分或完全替代NPK肥料可以减少氮素损失并维持高作物产量。因此,根据本研究中观察到的氮素转化动力学,在中国亚热带雨养紫色土壤中,建议将有机肥料与矿物肥料结合使用(即OM,OM-NPK和RSD-NPK处理)用于作物生产。 。 (C)2015 Elsevier Ltd.保留所有权利。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 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