• ISSN 1008-505X
  • CN 11-3996/S

基于长期氮肥示踪试验评估氮肥利用率算法的合理性

Evaluation of the rationality of nitrogen use efficiency approaches based on long-term fate of nitrogen fertilizer tracing experiments

  • 摘要: 氮肥利用率是衡量氮肥被作物利用的一个指标,常规采用的计算方法为差减法和15N示踪法,主要是通过作物吸收的氮量来计算氮肥利用率。由于这两种方法没有考虑氮肥在土壤中的残留和后效,显著低估了施用氮肥的实际效应。为此,国内外研究者一直在探索更实际的氮肥利用率计算法。不同的改进方法以不同的表现形式包含了氮肥的遗留效应,弥补了差减法和15N示踪法在短期试验中对实际氮肥利用率的严重低估,基本接近于实际氮肥利用率,但远高于常规差减法或15N示踪法估算值。在本文中定义的实际氮肥利用率(ANUE)为:在土壤残留示踪氮被完全消耗的条件下,作物地上部吸收肥料氮占施氮量的百分比。法国28年旱地作物的氮肥叠加利用率为61.3%~65.3%,中国太湖地区17年的水旱轮作体系示踪氮肥试验中氮肥叠加利用率为38.6%~43.0%。本研究采用Origin 2021的图形数字化工具,获取这两个长期定位试验数据,包括每季作物吸收15N、土壤残留15N数据,分别以耗竭耕层(0—20 cm)、1 m、2 m土体中的氮素残留量来计算氮肥利用率。以此为参照标准,评估土壤氮素平衡法和氮肥有效率法计算结果的合理性。基于2 m土体残留肥料氮的土壤氮素平衡法和氮肥有效率法,会高估旱地作物的氮肥利用率;而以耕层土壤残留肥料氮作为估计参数时,则与旱地实际氮肥利用率基本一致(61%~74%);而氮肥有效率(41%~52%)可以很好地估算我国太湖地区水旱轮作体系的实际氮肥利用率。因此,跨地块或作物系统的氮肥利用率比较,应选择适当的计算方法,以避免由不同方法导致的不可比性而产生误解。氮肥有效率法(将作物吸收和土壤残留氮均视为有效部分)可以通过短期试验获得接近实际的氮肥利用率,具有广泛的应用价值。

     

    Abstract: Nitrogen use efficiency (NUE) is a key indicator for evaluating the crop uptake of nitrogen (N) fertilizer applied to cropland. The principal approaches for quantifying NUE include N difference and 15N tracer. However, these approaches significantly underestimated the actual efficiency of N fertilizer, as these approaches failed to consider the residual and legacy effects of N fertilizer in soil. Therefore, researchers all over the world have been investigating the more actual NUE. The NUE calculated by improvement methods is analogous to the actual NUE, but higher than the N difference or the 15N tracer approaches. This can be attributed to the differing forms in which various improvement methods incorporate the legacy effects of N fertilizer, thereby compensating for the underestimation of NUE using the N difference or the 15N tracer approaches in short-term experiments. In this review, the actual NUE is defined as the percentage of N fertilizer uptake by the crop aboveground to the amount of N fertilizer inputs, while completely consuming the residual N fertilizer in soil. The accumulative N recovery efficiency is 61.3%−65.3% of a 28-year upland cropping system in France, and 38.6%−43.0% of a 17-year paddy-upland rotation system in the Taihu Lake region of China. We obtained the data from the two long-term field experiments using the Digitizer tool of Origin 2021, including the crop 15N uptake and the residual 15N in soil. The NUE was calculated based on the N residual in the topsoil (0−20 cm), 1 m, and 2 m soil, respectively. We analyzed and evaluated the rationality of the computed results of the soil N balance and N fertilizer efficiency approaches by comparing them to the actual NUE. The soil N balance and N fertilizer efficiency approaches significantly overestimated NUE when calculated by two meters of residual N in the soil. The surface (0−20 cm) soil residual N was found as a calculation parameter for estimating the actual NUE in these two approaches (61%−74%). However, the N fertilizer efficiency (41%−52%) was the only approach that accurately estimated the actual NUE in the Taihu Lake region of China. Therefore, the comparison of NUE across plots or crop systems should be based on a consistently chosen quantification approach to avoid inherent biases introduced by different approaches. In general, the N fertilizer efficiency approach (both crop absorption and soil residual nitrogen are considered to be utilized) achieves near the actual NUE in short-term experiments, demonstrating extensive application value.

     

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