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首页> 外文期刊>Journal of plant nutrition and soil science >Impact of urease and nitrification inhibitor on NH4+ and NO3- dynamic in soil after urea spring application under field conditions evaluated by soil extraction and soil solution sampling
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Impact of urease and nitrification inhibitor on NH4+ and NO3- dynamic in soil after urea spring application under field conditions evaluated by soil extraction and soil solution sampling

机译:尿素春季施用土壤萃取和土壤溶液采样评价下尿素春季施工后脲酶和硝化抑制剂对土壤NH4 +和NO3-动态的影响

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The application of mineral nitrogen (N) fertilizers is one of the most important management tools to ensure and increase yield in agricultural systems. However, N fertilization can lead to various ecological problems such as nitrate ( NO3 - ) leaching or ammonia and nitrous oxide emissions. The application of N stabilizers (i.e., inhibitors) combined with urea fertilization offers an effective option to reduce or even prevent N losses due to their regulatory effect on ammonium ( NH4 + ) and NO3 - release into the soil. The present field experiment therefore aimed at soil N speciation dynamics after urea spring fertilization (225 kg N ha(-1)) in the presence of a urease inhibitor (UI), a nitrification inhibitor (NI), both inhibitors (UI+NI) or when no inhibitor was applied at all. The study focused on the distribution of N species among soil matrix and soil solution. Plant cultivation was completely omitted in order to avoid masking soil N turnover and speciation by plant N uptake and growth dynamics. Application of UI clearly delayed urea hydrolysis in the top soil, but a complete hydrolysis of urea took place within only 10 days after fertilization (DAF). Nitrification was significantly reduced by NI application, leading to higher NH4 + - N and lower NO3 - - N concentrations in treatments with NI. Due to sorption of NH4 + to the soil matrix a significantly larger fraction of NH4 + was always detected in the soil extracts compared to soil solution. However, while in soil extracts the impact of NI application was less apparent and delayed, in soil solution a quick response to NI application was observed as revealed by significantly increased soil solution concentrations of NH4 + . Because of the "asymmetric" soil phase distribution soil solution NH4 + was predominant over NO3 - only initially after fertilization even in inhibitor treatments (approximate to 8 to 10 DAF). Nevertheless, inhibitor application tended towards closer ratios of NH4 + to NO3 - concentration i
机译:矿物氮(N)肥料的应用是确保和增加农业系统收益的最重要的管理工具之一。然而,N施肥可以导致各种生态问题,如硝酸盐(NO3 - )浸出或氨和氧化二氮排放。 N稳定剂(即,抑制剂)的应用与尿素施肥相结合,提供了减少或甚至预防由于其对铵(NH4 +)和NO3​​ - 释放到土壤的调节作用而降低损失的有效选择。因此,本场实验旨在尿素抑制剂(UI)存在尿素抑制剂(UI),硝化抑制剂(Ni),抑制剂(UI + Ni)的存在下的土壤n形状动力学(225kg n(-1))或者根本没有抑制剂。该研究侧重于土壤基质和土壤溶液中N种的分布。完全省略了植物培养,以避免通过植物N吸收和生长动态掩盖土壤N营业额和形态。 UI在顶部土壤中清楚地延迟尿素水解,但在受精后仅在10天内完成尿素的完全水解(DAF)。 Ni施用显着降低了硝化,导致Ni治疗的NH 4 + - N和下部NO3 - N浓度。由于NH4 +的吸附到土壤中,与土壤溶液相比,在土壤提取物中始终在土壤提取物中检测到明显较大的NH 4 +。然而,虽然在土壤提取物中,Ni施用的影响不太明显和延迟,但在土壤溶液中,观察到对Ni施用的快速反应,如NH 4 +的土壤溶液浓度显着增加的土壤溶液浓度显着增加。由于“不对称”土相分布土壤溶液NH4 +在NO 3上占主导地位 - 甚至在抑制剂处理中的施肥之后仅在施用(近似为8至10个DAF)。然而,抑制剂应用趋向于NH4 +至NO3 - 浓度I的更接近比率

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