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首页> 外文期刊>Soil Science Society of America Journal >Impacts of soil amendment history on nitrogen availability from manure and fertilizer.
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Impacts of soil amendment history on nitrogen availability from manure and fertilizer.

机译:土壤改良史对肥料和肥料中氮素利用率的影响。

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摘要

Repeated, long-term additions of organic materials not only increase stocks of mineralizable soil N, but also bring about changes in soil characteristics that influence N dynamics. We conducted an aerobic incubation to explore how soil amendment history affects the transformation and availability of recently added N. Soil was collected from plots under contrasting amended and nonamended soil management systems in a 13-yr cropping systems experiment. Nitrogen source treatments were: no added N (control), NH4+ fertilizer (Fert), a net mineralizing manure (MManure), and a net immobilizing manure (IManure). Soil NH4+ and NO3- concentrations were monitored for 282 d. A two-pool, first-order model with fixed rate parameters was fitted to the NO3- accumulation data. When no N was added, net mineralization in the historically amended soil was twice that in the historically nonamended soil, mostly due to differences in soil total N stocks. When N sources were added, NH4+ consumption, net N mineralization, and estimated N pools were affected by both soil amendment history and N source, with a significant interaction between the two factors. Historically amended soil reduced the availability of recently added N relative to the nonamended soil. This reduction occurred in the active pool (N1) for MManure and in the slow pool (N2) for Fert. It appeared to be related to the timing of C availability. Future work modelling N availability should consider soil amendment history not only for its effects on soil N supply capacity, but also for its effects on the availability of recently added N sources..
机译:长期反复添加有机材料不仅增加了可矿化土壤氮的储量,而且还带来了影响氮动力学的土壤特性变化。我们进行了有氧培养,以探索土壤改良历史如何影响最近添加的N的转化和可用性。在13年的种植系统实验中,在经过对比的修正和非修正土壤管理系统下,从地块中收集土壤。氮源处理为:不添加氮(对照),NH4 +肥料(Fert),净矿化肥料(MManure)和净固肥(IManure)。监测土壤NH4 +和NO3-浓度282 d。将具有固定速率参数的两池一阶模型拟合到NO3-累积数据中。如果不添加氮,则历史改良土壤中的净矿化度是历史非改良土壤中的净矿化度的两倍,这主要是由于土壤总氮储量的差异。当添加氮源时,土壤改良剂的历史和氮源都影响着NH4 +的消耗,净氮矿化和估计的氮库,而这两个因素之间存在显着的相互作用。历史上修改过的土壤相对于未修改过的土壤减少了最近添加的N的可用性。对于MManure,此减少发生在活动池(N1)中,对于Fert,发生在慢池(N2)中。它似乎与C可用性的时间有关。未来对氮素有效性进行建模的工作不仅应考虑土壤改良剂的历史,因为其对土壤氮素供应能力的影响,还应考虑其对最近添加的氮源的有效性的影响。

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