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首页> 外文期刊>Nutrient Cycling in Agroecosystems >Estimating net N mineralization under unfertilized winter wheat using simulations with NET N and a balance approach
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Estimating net N mineralization under unfertilized winter wheat using simulations with NET N and a balance approach

机译:利用NET N和平衡法模拟估算未施肥冬小麦的净N矿化度。

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摘要

Eliminating uncertainty in soil N supply could reduce fertilizer input, but the amount of N mineralized during plant growth is usually still unknown. We aimed to test the relatively simple two-pool net N mineralization model NET N that uses site-specific temperature and soil water functions as well as pedotransfer functions for deriving the pool sizes and was developed for NW Germany. The objectives were to (1) evaluate, if field net N mineralization under unfertilized winter wheat could be satisfactorily simulated, and to (2) examine the variation in time patterns of net N mineralization within years and sites and from two functional N pools: a rather small, fast mineralizable N pool (N-fast) and a much greater, slowly mineralizable N pool (N-slow). NET N simulations for 36 site-year-combinations and up to five dates within the growing season were evaluated with detailed N balance approaches (calculated from: soil mineral N contents, plant N uptake using estimates of green area index, simulated N leaching). Simulated net N mineralization was highly significantly correlated (r(2) = 0.58; root mean square error = 24.2 kg N ha(-1)) to estimations from the most detailed balance approach, with total simulated net N mineralization until mid August ranging from 62.1 to 196.5 kg N ha(-1). It also became evident that N mineralization from pool N-slow-in contrast to pool N-fast-was considerably higher for loess soils than for sandy or loamy soils. The results suggest that NET N was adequate for simulations in unfertilized winter wheat. However, further field studies are necessary for proving its applicability under fertilized conditions
机译:消除土壤氮供应的不确定性可以减少肥料的投入,但是在植物生长过程中矿化的氮含量通常仍然未知。我们的目标是测试相对简单的两池净N矿化模型NET N,该模型使用特定地点的温度和土壤水分功能以及pedotransfer函数来推导出水池的大小,并且是为德国西北地区开发的。目的是为了(1)评估是否可以令人满意地模拟未施肥的冬小麦下的田间净氮矿化,以及(2)研究年份和地点以及两个功能性氮库中净氮矿化时间模式的变化:较小的快速矿化N池(N快)和较大的缓慢矿化N池(N慢)。使用详细的氮平衡方法(通过以下方法进行的NET N模拟)对36个站点-年份组合和最多5个生长期的N平衡方法进行了评估(计算依据:土壤矿物质N含量,使用绿地指数的估计值对植物N的吸收,模拟的N淋洗)。模拟净氮矿化与最详细的平衡法估算值高度相关(r(2)= 0.58;均方根误差= 24.2 kg N ha(-1)),至8月中旬为止,模拟净氮矿化总量为62.1至196.5 kg N ha(-1)。与黄壤土相比,N-慢池与N-快池形成的氮矿化明显高于沙质或壤土。结果表明,NET N足以模拟未施肥的冬小麦。但是,有必要进行进一步的田间研究以证明其在受精条件下的适用性。

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