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The distribution of soil nitrifiers and efficacy of 3,4-dimethylpyrazole phosphate changes with soil depth and calcium carbonate application

机译:土壤氮化物的分布与3,4-二甲基吡唑磷酸盐变化的疗效和碳酸钙磷酸钙

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The nitrification inhibitor 3,4-dimethylpyrazole phosphate (DMPP) is used to limit nitrogen (N) losses incurred following nitrification of applied N fertilisers. Inhibitor efficacy changes with soil conditions including pH and organic matter (OM) content, both of which can be stratified down the soil profile. An incubation study was conducted using acidic soil that exhibited pH stratification. Soil samples were collected from the field in 2 cm depth increments to a depth of 10 cm. Two liming treatments were applied to each depth where the pH(Ca) was raised above 6 or left in its initial acidic state. Nitrogen treatments (urea ammonium nitrate (UAN) with and without DMPP) were applied to each liming treatment per depth and incubated for four weeks. Destructive sampling for mineral N, DMPP concentration and pH occurred every week. The abundance of nitrifiers was determined using semi-quantitative real-time polymerise chain reaction (PCR) targeting the amoA gene at weeks 0, 1 and 4. Liming significantly increased nitrification rates and bacterial amoA gene abundance. Results showed the top 0-2 cm recorded the largest population of bacterial nitrifiers. Changes in pH influenced the composition of nitrifiers present in the soil. Bacterial nitrifiers were absent from the 8-10 cm soil layer in unlimed soils (pH(Ca) 4.25) but liming caused an increase in gene abundance. Archaeal amoA gene abundance was highest in unlimed plots at 4-8 cm depth although populations decreased over the incubation period and also with lime application. DMPP effectively inhibited nitrification in limed plots, however no significant difference existed between UAN and DMPP treatments for unlimed treatments. DMPP successfully decreased bacterial amoA gene abundance in all depths that were limed but not in unlimed soils. Decreases in inhibitor concentrations occurred within one week in the 0-2 cm layer possibly due to bacterial decomposition associated with greater OM concentration at the soil surface. This study highlighted that DMPP use is more effective in relatively neutral soils and liming will change the abundance and distribution of nitrifiers within the top 10 cm of soil.
机译:硝化抑制剂3,4-二甲基吡唑磷酸盐(DMPP)用于限制硝化施用的施用后产生的氮气(n)损失。抑制剂功效随着土壤条件而变化,包括pH和有机物质(OM)含量,两者都可以分层在土壤剖面下分层。使用表现出pH分层的酸性土壤进行孵育研究。将土壤样品以2cm深度增量从场上收集到10厘米的深度。将两个跛行处理施加到每个深度,其中pH(CA)在60升或留在其初始酸性状态以上。将氮气处理(尿素硝酸铵(UAN)与含有和不含DMPP)的每个深度的每个跛行处理施加并孵育四周。每周发生矿物质N,DMPP浓度和pH的破坏性取样。使用半定量实时聚合链反应(PCR)测定含有半定量的实时聚合链反应(PCR),靶向AmoA基因在数周0,1和4.估计显着提高硝化率和细菌氨基氨基型丰度。结果表明,顶部0-2厘米记录了最大的细菌氮群。 pH的变化影响了土壤中存在的氮气组成。在无赖的土壤中的8-10cm土层中没有细菌氮化剂(pH(CA)4.25),但拟肢引起基因丰富的增加。虽然孵化期和石灰施用,但群体在4-8厘米深度深度下,抗原氨基氨基基因丰富在4-8厘米的深度中最高。 DMPP在跛行地块中有效地抑制了硝化,但UAN和DMPP治疗没有显着差异,用于无赖处理。 DMPP在所有深度中成功降低了细菌氨基氨基基因丰富,而不是在无赖的土壤中。抑制剂浓度的降低可能导致0-2cm层的一周内可能是由于在土壤表面处的较大OM浓度相关的细菌分解。本研究强调,DMPP在相对中性的土壤中更有效,估计将改变氮气在氮气前10厘米内的丰度和分布。

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