Modelling the residual N effect of slurry applied to maize land on dairy farms in the Netherlands

J. Schröder, H. Keulen
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引用次数: 18

Abstract

The decomposition rate of soil organic N was estimated from data of a long-term field experiment and used in a simulation model. Subsequently, the model was used to estimate the effects of Dutch manuring practice on maize land. The time course of the N mineralization rate was estimated for three scenarios: (i) following actual manure applications which have declined with time (scenario A); (ii) assuming continuous applications in accordance with the present and anticipated legislation (scenario P); (iii) assuming annual applications of 200 kg mineral fertilizer N/ha only (scenario M). The actual mineralization rate (following scenario A) in 1995 was estimated at 23-31 kg N/ha higher than when manure had been applied at moderate rates (following scenario P). Corresponding estimates for the year 2005 were 18-19 kg N/ha per year. The calculations suggest that it may be difficult to maintain soil organic N pools with mineral fertilizer only. Consequently, the mineralization rate following scenario M decreased with time as did the yields of silage maize. The magnitude of the residual effect indicates that there is need and scope for fine tuning of N fertilizer recommendations. The simple model used seems suitable for exploring the magnitude of the residual effect of manures.
模拟荷兰奶牛场玉米地施用浆液的残氮效应
利用长期田间试验资料估算了土壤有机氮的分解速率,并建立了模拟模型。随后,该模型被用于估计荷兰施肥对玉米地的影响。在三种情况下估算了氮矿化率的时间过程:(i)在实际施肥后,随着时间的推移而下降(情景A);(ii)假设按照现行及预期的法例持续申请(方案P);(iii)假设每年只施用200公斤矿物肥料N/ha(情景M)。1995年的实际矿化率(情景A)估计为23-31公斤N/ha,高于以中等比率施用粪肥的情况(情景P)。2005年的相应估计为每年18-19公斤N/ha。计算结果表明,单施矿肥可能难以维持土壤有机氮库。因此,情景M下的矿化率随着时间的推移而降低,青贮玉米的产量也是如此。剩余效应的大小表明,有必要和范围微调氮肥建议。所使用的简单模型似乎适合于探索肥料残留效应的大小。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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