Formation of soil structure in long-term fertilised sandy soil: Role of the manganese oxides

Pub Date : 2019-12-01 DOI:10.2478/bgeo-2019-0012
V. Šimanský, J. Jonczak
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引用次数: 1

Abstract

Abstract We investigated the role of Mn oxides on the soil structure (contents of dry and water-stable aggregates) of sandy soil under a controlled long-term fertilisation experiment. We examined two experiments: a 94-year-term experiment with: no fertilisers, NPK fertilisers, and CaNPK fertilisers; and a 25-year-term experiment that included: farmyard manure and no mineral fertilisation, farmyard manure + NPK fertilisers, and farmyard manure + CaNPK fertilisers. The results showed that in the 94-year-term trial, Mn oxides were increased in CaNPK treatment. In the 25-year-term experiment, the farmyard manure combined with NPK decreased total Mn and its oxides. In the 94-year-term experiment, the content of dry-sieved macro-aggregates (DSAma) and water-stable macro-aggregates increased due to fertilisation. The result of our study suggests that Mn oxides had positive effects mainly on higher size classes of DSAma and did not have any effect on water-stable aggregate contents.
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长期施肥沙质土壤中土壤结构的形成:锰氧化物的作用
摘要在长期对照施肥条件下,研究了氧化锰对沙土土壤结构(干团聚体和水稳性团聚体含量)的影响。我们研究了两个试验:一个94年的试验:不施肥、不施用氮磷钾和不施用磷磷钾;以及一项为期25年的试验,包括:农家肥和无矿物肥,农家肥+氮磷钾肥料,农家肥+氮磷钾肥料。结果表明,在94年的试验中,CaNPK处理增加了锰氧化物。在25年的试验中,农家肥配施氮磷钾降低了总锰及其氧化物。在94年的试验中,由于施肥,干筛大团聚体(DSAma)和水稳性大团聚体的含量增加。我们的研究结果表明,锰氧化物主要对高粒径的DSAma有积极影响,而对水稳性团聚体含量没有任何影响。
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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