Intensity of microbiological processes in gray forest soils under the liming and plowing of crop by-products

I. Malynovska, N. Tkachenko
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引用次数: 2

Abstract

Established that liming with single dose by hydrolytic acidity (1,0 Hg) slows down the processes of organic matter mineralization in gray forest soil: without mineral fertilizers – in 2,1 times, with mineral fertilizers – in 4,1, with plowing of the seed crop biomass and the by-products of the predecessor – in 1,4 times. The mineralization of nitrogen compounds as a result of liming also proceeds slower: without mineral fertilizers – in 1,2 times, with mineral fertilizers – in 2,2 times. Confirmed patterns that were obtained in previous years of research about the impact of liming on the activity of humus mineralization – it decreases as a result of liming with full dose (1,0 Hg) without mineral fertilizers by 66,7 %, with mineral fertilizers – by 4,4 %.  The total biological activity in the soil without a mineral fertilizer increases as a result of liming by 23,0 %, with mineral fertilizers – by 42,5, at the background of exogenous organic matter (EOM) plowing – by 83,7 %. Liming allows to reduce the level of phytotoxicity of soil without mineral fertilization by 17,9 %, %, with mineral fertilizers at the background of EOM – by 12,2 %. Positive influence of liming is amplified in variants with introduction of organic matter into the soil (byproducts of predecessor and siderate). Plowing of siderate crop biomass and by-products of predecessor in crop rotation allows to slow down the processes of organic matter accumulation in soil. The application of liming and mineral fertilizers in combination with the introduction of EOM reduces the index of pedotropy in 2,1 times, only with mineral fertilizers (N60Р30К60) – in 1,5 times. Similarly, plowing of the EOM affects the intensity of other mineralization processes. The total biological activity increases as a result of EOM plowing into the soil: in the variant with the use of mineral fertilizers by 54,7 %, with mineral fertilizers and liming – by 28,9 %. Confirmed previously established laws regarding the impact of optimization of mineral nutrition on the activity of decomposition of humic substances: with an increase in the dose of mineral fertilizers in 1,5 and 2 times the activity of mineralization of humus decreases by 6.0 and 10,1 % respectively. With the improvement of mineral nutrition of plants, the amount of root extracts is increased, which is a more accessible substrate than humus acids, which leads to slowing down of the destruction of humus substances.
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作物副产物石灰化和翻耕下灰色森林土壤微生物过程强度
确定单剂量水解酸性石灰化(1,0 Hg)减缓灰色森林土壤中有机质矿化过程:不施用矿物肥料-为2.1倍,施用矿物肥料-为4.1倍,耕作种子作物生物量和前一种作物的副产品-为1.4倍。由于石灰化,氮化合物的矿化也进行得较慢:不使用矿物肥料- 1,2倍,使用矿物肥料- 2,2倍。在前几年关于石灰化对腐殖质矿化活性影响的研究中获得的证实模式-在不使用矿物肥料的情况下,使用全剂量(1.0 Hg)石灰化会使腐殖质矿化活性降低66.7%,使用矿物肥料会使其降低4.4%。在不施用矿物肥料的土壤中,由于石灰化,总生物活性增加了23.0%,而在外源有机质(EOM)耕作的背景下,施用矿物肥料增加了42.5%,增加了83.7%。石灰可以使不施用矿物肥料的土壤的植物毒性水平降低17.9%,而在EOM -背景下施用矿物肥料的土壤的植物毒性水平降低12.2%。石灰化的积极影响随着有机质(前代和伴生物的副产品)的引入而在变异中被放大。在轮作中耕作一定量的作物生物量和前代作物的副产品,可以减缓土壤中有机质的积累过程。石灰和矿质肥料的施用与EOM的引入相结合,使土壤的向土指数降低了2.1倍,仅使用矿质肥料(N60Р30К60) -降低了1.5倍。同样,东洋构造的翻耕也影响其他矿化过程的强度。EOM耕入土壤的总生物活性增加:在使用矿物肥料的变异中增加54.7%,使用矿物肥料和石灰的变异增加28.9%。证实了前人关于优化矿质营养对腐殖质分解活性影响的规律:随着矿质肥料用量增加1倍、5倍和2倍,腐殖质的矿化活性分别下降6.0%和10.1%。随着植物矿物质营养的改善,根提取物的量增加,这是一个比腐殖酸更容易接近的底物,这导致腐殖质物质的破坏速度减慢。
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