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AVAILABILITY AND MOBILITY OF NUTRIENTS IN ACID FOREST SOIL TREATED WITH FAST AND SLOW-RELEASE NUTRIENTS

机译:速释与缓释养分对酸性森林土壤养分的有效性和流动性

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摘要

The effects of slow and fast-release fertilizers (P, K, Mg) on the movement and availability of nutrients in acid forest soil were studied. Fast-release superphosphate, potassium chloride and magnesium sulphate and slow-release apatite (P) and biotite (K, Mg) were applied alone or together with urea or urea+limestone. The nutrient content in the organic horizon was determined one growing season and three growing seasons after the application, and in the mineral layer after one growing season. The movement of nutrient ions in the organic horizon was studied by an ion exchange resin bag method during a 5-month period following application. The fast-release salts immediately increased the soluble P and exchangeable K and Mg contents in the organic and mineral soils and in the resin bags. After three growing seasons the effect of K application in the organic layer was non-detectable and that of P had clearly diminished. Apatite gradually increased soluble P content in the organic layer, but biotite had only a minor effect on the K and Mg contents. The nutrients from the fast-release fertilizers had clearly become available and mobile in the year of application and were thus susceptible to leaching. The rate of nutrient release from apatite and biotite is slower and the added nutrients are retained in the organic horizon. Slow-release compounds, like apatite and biotite, might be potential fertilizers for counteracting acidic deposition and subsequent nutrient losses.
机译:研究了缓释和速释肥料(磷,钾,镁)对酸性森林土壤中养分的迁移和有效性的影响。速释过磷酸钙,氯化钾和硫酸镁以及缓释磷灰石(P)和黑云母(K,Mg)可以单独使用,也可以与尿素或尿素+石灰石一起使用。施用后一个生长季节和三个生长季节确定有机层中的营养成分含量,一个生长季节后确定矿物层中的营养成分含量。在施用后的5个月内,通过离子交换树脂袋法研究了有机层中营养离子的运动。速释盐立即增加了有机和矿物土壤以及树脂袋中的可溶性P以及可交换的K和Mg含量。在三个生长季节后,无法检测到钾在有机层中的作用,而磷的作用已明显减弱。磷灰石逐渐增加了有机层中的可溶性P含量,但黑云母对K和Mg含量的影响很小。在施肥的那一年,速释肥料中的养分显然已经变得可用和流动,因此很容易浸出。磷灰石和黑云母释放养分的速度较慢,添加的养分保留在有机层中。缓释化合物,如磷灰石和黑云母,可能是抵消酸性沉积和随后养分流失的潜在肥料。

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