Nitrogen-carbon circulation in agrocenoses with different fertilization systems

IF 0.4 Q4 AGRICULTURE, MULTIDISCIPLINARY
O. Demydenko, V. Velychko
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引用次数: 2

Abstract

Aim. To compare nitrogen-carbon circulation in organic and intense fertilization system in agrocenosis of a short crop rotation with grain and intertilled crops on podzolic highly-regraded low-humus chernozem in the Central Forest-Steppe of Ukraine. Methods. Summarization of the study results in the permanent fi eld experiment, statistical method, dispersion method, correlation analysis of performance parameters, structures of phytomass, quality and quantity items of carbon and nitrogen balance. Results. In the organic system of fertilization, the removal of N increased to 0.25 units per capacity unit of nitrogen balance, which is 1.47 times higher, and the total loss of N increased 1.1 times (0.31 units per capacity unit of nitrogen balance) regarding the intense system of fertilization, but with lower values of balance items for nitrogen in the agrocenosis. Direct and strong correlation relationships were revealed between the yield of fodder units and the content of organic carbon in the structural components of the total phytomass: with organic carbon in the main products and root mass – R = 0.86–0.88 ± 0.02; R^2 = 0.74–0.77, and with the content of organic carbon in by-products and non- commodity total phytomass the relation to the yield of fodder units was on the level of direct mean correlation: R = 0.58–0.65 ± 0.02; R^2 = 0.34–0.43. The increase in the yield of fodder units is accompanied with the 1.32- fold decrease in the nitrogen balance capacity regarding the intense system of fertilization. Conclusions. It was established that in case of organic system of fertilization the ratio of organic carbon and N in the agrocenosis of a short crop rotation is the most optimal and approximates 30:1, which is the most profi table for humifi cation of by-products and decrease in the intensity of humus mineralization. Balance capacity is a restrictive factor in the circulation of organic carbon and N at the organic fertilization system, as it may considerably concede the balance capacity of organic carbon and N at the intense fertilization system, which had a negative impact on the performance of crop rotation.
不同施肥制度下农田土壤的氮碳循环
的目标。比较乌克兰中部森林草原灰化土高退化低腐殖土短轮作粮作间作的黑钙土上有机肥和强施肥系统的氮碳循环。方法。总结了长期田间试验的研究结果、统计方法、离散方法、性能参数、生物量结构、碳氮平衡质与量项目的相关分析。结果。在有机施肥系统中,氮素的去除量增加到每容量单位氮平衡的0.25个单位,增加了1.47倍;氮素的总损失量增加了1.1倍(每容量单位氮平衡的0.31个单位),但土壤中氮素的平衡项值较低。饲料单位产量与总生物量结构组分中有机碳含量呈显著正相关,主要产物有机碳含量与根系质量呈显著正相关,R = 0.86 ~ 0.88±0.02;R^2 = 0.74 ~ 0.77,副产物有机碳含量和非商品总生物量与饲料单位产量呈直接平均相关,R = 0.58 ~ 0.65±0.02;R^2 = 0.34-0.43。在高施肥系统下,饲料单位产量增加的同时,氮素平衡能力降低了1.32倍。结论。结果表明,在有机系统施肥条件下,短轮作土壤中有机碳氮比最优,约为30:1,最有利于副产物的腐殖化和腐殖质矿化强度的降低。平衡能力是有机施肥系统中有机碳和氮循环的制约因素,因为它可能在很大程度上削弱了密集施肥系统中有机碳和氮的平衡能力,从而对作物轮作性能产生负面影响。
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来源期刊
Agricultural Science and Practice
Agricultural Science and Practice AGRICULTURE, MULTIDISCIPLINARY-
自引率
25.00%
发文量
6
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