Response of a Scots pine (Pinus sylvestris) stand to application of phosphorus, potassium, magnesium and lime. 1. Soil data

G. Arnold, A. Diest
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引用次数: 8

Abstract

In 1985-1988, a 25-yr-old Scots pine forest in Netherlands was limed and fertilized with P, K and Mg in a 24 factorial design and in an experiment with 5 liming levels, in order to alleviate potential nutrient deficiencies as a result of high N depositions (ca. 40 kg ha-1 yr-1). In this paper, effects of fertilization and liming on nutrients in forest floor and mineral soil are discussed as a basis for explanation of foliar nutrient concentrations and tree performance. Of all treatments, liming showed the widest array of effects, especially in forest floor: raised pH and lowered extractable Al in forest floor, and after 4 yr those in 0-50 cm mineral soil. These effects, except for that on forest floor pH, were stronger with increasing lime dosages. Liming showed transient effects on amounts of soil inorganic N (Ni). Until 1989, Ni in forest floor was lowered and that in mineral soil was raised by liming. This could be attributed to the formation of NO3, which is more mobile than NH4. Plots limed with 3 t lime/ha appeared to have higher Ni concentrations in the whole sampled profile than those limed with >3 t/ha or unlimed plots, the reason for which is unclear. Liming removed extractable K and Mg from forest floor probably by exchange against Ca. Residence time of added P and possibly Mg in forest floor was increased by liming, probably by solubility of added fertilizers. Added K was poorly retained in forest floor and probably quickly leached to soil layers deeper than 50 cm.
苏格兰松对磷、钾、镁和石灰施用的反应。1. 土壤数据
1985-1988年,在24因子设计和5个石灰水平试验中,对荷兰一处25年树龄的苏格兰松林施用石灰,并施用磷、钾和镁,以减轻高氮沉积(约40 kg hm -1 -1)造成的潜在营养缺乏。本文讨论了施肥和石灰对森林底土和矿质土养分的影响,为解释叶面养分浓度和树木生长性能提供了依据。在所有处理中,石灰化表现出最广泛的影响,特别是在森林地面:提高森林地面的pH值,降低可提取铝,4年后在0-50 cm的矿物土中也是如此。除了对森林地面pH值的影响外,这些影响随着石灰用量的增加而增强。石灰对土壤无机氮(Ni)含量的影响是短暂的。1989年以前,森林地面的镍含量降低,矿质土壤的镍含量通过石灰化提高。这可能是由于NO3的形成,它比NH4更具流动性。在整个采样剖面中,石灰浓度为3吨/公顷的地块似乎比石灰浓度为30吨/公顷或未石灰的地块具有更高的Ni浓度,其原因尚不清楚。石灰化可能通过与Ca的交换使可提取的K和Mg从森林地面上消失。石灰化可能通过添加的肥料的溶解度延长了添加的P和可能的Mg在森林地面上的停留时间。添加的钾在森林地面的保留很差,可能很快淋滤到50厘米以下的土层。
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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