长期施肥对灰化土腐殖质转化的影响

Ievgen Skrylnyk, O. М. Puznyak, А. Kutova, K. S. Artemyeva, B. P. Moskalenko
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摘要

本文以乌克兰西部波利西亚地区灰化土砂质壤土为背景,通过田间试验研究了长期施肥过程中不同结构组织层次腐殖质转化规律的研究结果。发现灰化土腐殖质组成中化学活性有机物含量低是由腐殖质形成的地带性特征引起的,可以通过施用肥料积极纠正。长期施用有机肥和矿物肥加剧了腐植酸新形成及其流动形态的形成过程,在不施用化肥的对照中,Cha-1 / Cfa-1的比值为0.28,在石灰化背景下,不同施肥条件下Cha-1 / Cfa-1的比值为0.33-0.88。在有机矿肥体系下,有机质腐殖化形成了最有利的条件,但在石灰化背景下,腐殖质类型仍为富营养盐型,对照型的Cha / Cfa比值为0.93,而石灰化背景下的Cha / Cfa比值为0.41。此外,施肥对腐植酸多分散性的再分配也有影响,其特征是疏水分子聚集体组成的异质性降低。在1800 cm-1 ~ 2500 cm-1的宽范围内,土壤腐植酸在CaCO3作用下的积分谱线从左向右发生了变化,这与分子参数的变化有关。根据色谱分析结果,确定了灰化土腐殖酸的分子分布剖面与腐殖质物质类相对应。第一部分的特点是形成极性组成的大分子的离子缔合物。腐植酸的恢复主要是由于其高分子结构,对施用肥料最为敏感。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Effect of long-term application of fertilizers on the humus substances transformation in podzolic soil
The article reflects the results of a study of the regularities of the transformation of humic substances at different levels of structural organization during long-term fertilization against the background of liming of podzolic sandy loamy soil in a field experiment in Western Polissya of Ukraine. It was found that the low content of chemically active organic substances in the humus composition of podzolic soils, caused by the zonal features of humus formation, can be positively corrected by applying fertilizers. Long-term use of organic and mineral fertilizers intensifies the process of new formation of humic acids and the formation of their mobile forms – the ratio of Cha-1 / Cfa-1 is 0.28 in the control without fertilizers and 0.33–0.88 in the variants of fertilization against the background of liming. With an organo-mineral fertilizer system, the most favorable conditions are formed for the humification of organic substances however, the type of humus remained fulvate – the Cha / Cfa ratio is 0.93 in the control variant and 0.41 – against the background of liming. Also, the application of fertilizers had an effect on the redistribution of the polydispersity of humic acids, which was characterized by a decrease in the heterogeneity of the composition of hydrophobic molecular aggregates. In a wide range of 1800 cm-1 to 2500 cm-1, a change in the direction of the line of the integral spectrum of soil humic acids under the application of CaCO3 from left to right was found, which is associated with a change in molecular parameters. Based on the results of chromatographic analysis, it was established that the profiles of the molecular distribution of humic acids podzolic soil correspond to the humus substances class. The first fraction is characterized by the formation of ion associates of larger molecules of polar composition. The recovery of humic acids occurred mainly due to high-molecular structures, which is the most sensitive to the application of fertilizers.
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