Response of a Scots pine (Pinus sylvestris) stand to application of phosphorus, potassium, magnesium and lime: 2. Soil solution composition.

G. Arnold, I. L. Sweers, A. Diest
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引用次数: 4

Abstract

In 1985-88, a 25-yr-old Scots pine forest in Netherlands was limed (5 levels) and fertilized with P, K and Mg in a factorial design. This paper discusses the influence of P, K and Mg addition (as one treatment) and liming, on solute concentrations at depths of 30 cm, i.e. in the root zone (monitored September 1989 - April 1992) and 100-150 cm, i.e. below the root zone (April 1991). Liming increased NO3 concentrations at both depths. At 30 cm this effect of liming gradually vanished during the study period, concurrently with declining soil solution pH, while an increasing effect of PKMg on NO3 developed. Probably it took several years for nitrifying microflora to adapt to improved nutrient availability, while the effect of liming was instantaneous. These data show that besides liming, fertilization may increase NO3 leaching. NH4 was not affected by any treatment. Applied K and Mg compounds were easily soluble, and their soil solution concentrations were increased at both depths in PKMg-amended plots. Probably slow-release fertilizers would allow for a more efficient incorporation of K and Mg into the system's biomass. Reducing effects of liming on soluble Al were weak (30 cm) or absent (100-150 cm). Al at 30 cm did not reach concentrations known to be harmful to Scots pine, but Ca:Al ratios were critical in unlimed plots. No evidence was found for enhanced cation leaching caused by increased formation of nitric acid in limed plots.
苏格兰松(Pinus sylvestris)对磷、钾、镁和石灰施用的反应:2。土壤溶液组成。
1985- 1988年,采用因子设计对荷兰一处25年树龄的苏格兰松林进行石灰化处理(5个水平),并施用磷、钾和镁。本文讨论了磷、钾和镁的添加(作为一个处理)和石灰化对30厘米深,即根区(1989年9月至1992年4月监测)和100-150厘米深,即根区以下(1991年4月)溶质浓度的影响。石灰化增加了两个深度的NO3浓度。在30 cm处,石灰的作用逐渐消失,同时土壤溶液pH下降,而PKMg对NO3的作用逐渐增强。硝化微生物群可能需要几年的时间来适应改善的养分有效性,而石灰化的效果是瞬间的。这些数据表明,除石灰外,施肥也会增加硝态氮的淋溶。NH4不受任何处理的影响。施用钾和镁的化合物易于溶解,在pkmg改良的地块中,其土壤溶液浓度在两个深度都有所增加。也许缓释肥料能使钾和镁更有效地结合到系统的生物量中。石灰对可溶性铝的还原作用较弱(30 cm)或无还原作用(100-150 cm)。30厘米处的铝没有达到已知的对苏格兰松有害的浓度,但Ca:Al比在未限定的地块上是至关重要的。没有证据表明石灰地块中硝酸的形成增加导致阳离子浸出的增强。
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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