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从吸盘数据中浸出硝酸盐:排水计算方法和浓度插值的影响。

Nitrate leaching from suction cup data: Influence of method of drainage calculation and concentration interpolation.

机构信息

Department of Agroecology, Aarhus University, Blichers Allé 20, 8830, Tjele, Denmark.

Department of Mathematics, Aarhus University, Ny Munkegade 118, 8000, Aarhus, Denmark.

出版信息

J Environ Qual. 2020 Mar;49(2):440-449. doi: 10.1002/jeq2.20020. Epub 2020 Feb 18.

Abstract

The use of suctions cups is a common practice for estimating nitrate (NO -N) leaching under agricultural systems despite the various uncertainties associated with the approach. One major uncertainty is water flux, which is required for calculating NO -N leaching loads from measured concentrations. Another problem is the interpolation of NO -N concentrations between measurement days. We investigated how differences in water flux, obtained from two different models (EVACROP and APSIM), affect NO -N leaching loads. The effect of interpolation of NO -N concentrations based on days or drainage was also addressed. The models were set up according to a 2-yr field experiment with spring barley (Hordeum vulgare L. Quinch) with different levels of N fertilization rates on a loamy soil at Flakkebjerg, Denmark. Due to small differences in measured NO -N concentrations between sequential samplings, the method of interpolation did not significantly affect NO -N leaching in the two periods investigated. Although there is no standard against which leaching losses from different approaches can be tested, results highlight that the modeling of water uptake as affected by N supply influences the amount of drainage and thus calculated NO -N leaching. Therefore, for experiments with varying N fertilization levels, the APSIM model, which accounts for N nutrition on crop water use, is likely more accurate. For common fertilization rates, the simpler EVACROP seems appropriate. Thus, when using suction cup data for testing models or for evaluating mitigation options for nitrate leaching, the use of an appropriate model for estimating water fluxes is important.

摘要

尽管吸力杯法在农业系统中估计硝酸盐(NO3-N)淋失具有各种不确定性,但它仍是一种常用方法。一个主要的不确定性是水通量,它是从测量浓度计算 NO3-N 淋失负荷所必需的。另一个问题是在测量日之间插值 NO3-N 浓度。我们研究了从两种不同模型(EVACROP 和 APSIM)获得的水通量差异如何影响 NO3-N 淋失负荷。还探讨了基于天数或排水量插值 NO3-N 浓度的影响。根据在丹麦 Flakkebjerg 的壤土上进行的为期 2 年的春大麦(Hordeum vulgare L. Quinch)田间试验,设置了这些模型,该试验具有不同水平的氮肥施用量。由于连续采样之间测量的 NO3-N 浓度差异较小,因此插值方法在两个研究期间均未显著影响 NO3-N 淋失。尽管没有可以用来测试不同方法淋失损失的标准,但结果表明,受氮供应影响的水分吸收模型会影响排水量,从而计算出的 NO3-N 淋失量。因此,对于具有不同氮肥施用量的实验,考虑作物水分利用对氮营养的 APSIM 模型可能更准确。对于常见的施肥率,较简单的 EVACROP 似乎更合适。因此,在使用吸力杯数据来测试模型或评估硝酸盐淋失缓解措施时,使用合适的模型来估算水通量非常重要。

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