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首页> 外文期刊>Plant and Soil >The fate of residual 15N-labelled fertilizer in arable soils: its availability to subsequent crops and retention in soil
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The fate of residual 15N-labelled fertilizer in arable soils: its availability to subsequent crops and retention in soil

机译:耕作土壤中残留15 标记肥料的命运:其对后续作物的可用性和在土壤中的保留

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摘要

An earlier paper (Macdonald et al., 1997; J. Agric. Sci. (Cambridge) 129, 125) presented data from a series of field experiments in which 15N-labelled fertilizers were applied in spring to winter wheat, winter oilseed rape, potatoes, sugar beet and spring beans grown on four different soils in SE England. Part of this N was retained in the soil and some remained in crop residues on the soil surface when the crop was harvested. In all cases the majority of this labelled N remained in organic form. In the present paper we describe experiments designed to follow the fate of this `residual' 15N over the next 2 years (termed the first and second residual years) and measure its value to subsequent cereal crops. Averaging over all of the initial crops and soils, 6.3% of this `residual' 15N was taken up during the first residual year when the following crop was winter wheat and significantly less (5.5%) if it was spring barley. In the second year after the original application, a further 2.1% was recovered, this time by winter barley. Labelled N remaining after potatoes and sugar beet was more available to the first residual crop than that remaining after oilseed rape or winter wheat. By the second residual year, this difference had almost disappeared. The availability to subsequent crops of the labelled N remaining in or on the soil at harvest of the application year decreased in the order: silty clay loam>sandy loam>chalky loam>heavy clay. In most cases, only a small proportion of the residual fertilizer N available for plant uptake was recovered by the subsequent crop, indicating poor synchrony between the mineralization of 15N-labelled organic residues and crop N uptake. Averaging over all soils and crops, 22% of the labelled N applied as fertilizer was lost (i.e., unaccounted for in harvested crop and soil to a depth of 100 cm) by harvest in the year of application, rising to 34% at harvest of the first residual year and to 35% in the second residual year. In the first residual year, losses of labelled N were much greater after spring beans than after any of the other crops.
机译:较早的一篇论文(Macdonald等,1997; J。Agric。Sci。(剑桥)129,125)提供了一系列田间试验的数据,其中在春季对冬小麦施用了15 N标记的肥料。 ,东南油英格兰的四种不同土壤上种植的冬季油菜,土豆,甜菜和春豆。收获农作物时,该氮的一部分保留在土壤中,有些残留在土壤表面的农作物残渣中。在所有情况下,大多数这种标记的N保持有机形式。在本文中,我们描述了旨在遵循此“残留” 15 N在接下来的两年(称为第一和第二残留年)中的命运并衡量其对随后谷物作物的价值的实验。在所有初始农作物和土壤上平均,在剩余的第一个年份中,随后的作物是冬小麦,占“残留” 15 N的6.3%,而如果是春季大麦,则显着减少(5.5%)。 。最初施用后的第二年,又回收了2.1%,这次是大麦。马铃薯和甜菜后残留的标记氮比油菜或冬小麦后残留的氮含量更高。到第二个剩余年份,这种差异几乎消失了。在施用年收获时残留在土壤中或土壤上的标记氮对后续作物的有效性按以下顺序降低:粉质粘土壤土>沙质壤土>白垩质壤土>重质粘土。在大多数情况下,后续作物只能回收一小部分可用于植物吸收的残留肥料氮,这表明15 N标记的有机残留物的矿化与作物吸收氮之间的同步性差。在所有土壤和农作物上,施肥当年平均损失了22%的氮作为肥料流失(即,未收割的农作物和土壤深度达100 cm的氮),在施肥的当年上升到34%。第一个剩余年份,第二个剩余年份达到35%。在剩余的第一年中,春季豆后标记的N的损失要比其他任何作物后的损失都要大。

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