Accumulation of Atmospheric Carbon by Crops in Rotation and the Effect of Fertilization Systems on the Accumulation of Organic Carbon by Cultivated Sod-Podzol Soil

N. E. Zavyalova, M. T. Vasbieva, V. R. Yamaltdinova, I. V. Kazakova
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Abstract

The study reports experimental data on the accumulation and loss of organic carbon in sod-podzol soil over six rotations of a long-term station experiment. It was found that, during photosynthesis, spring barley plants bound to organic compounds 2.84–3.25 t C/ha from the atmosphere (10.3–11.6 t CO2/ha) and meadow clover of the second year of rotation bound 4.23–5.19 t C/ha (15.1–18.6 t CO2/ha) over the growing season, depending on experimental variant. Cultivated crops sequestered from the atmosphere 82.28–99.31 t of CO2/ha or 22.4–27.1 t C/ha over a rotation of the eight-field crop rotation, depending on the soil fertilization system. Long-term use of cultivated land without fertilizers led to a decrease in carbon content in the soil by 13.5% in relation to the initial level. The soil of the station experiment was characterized by the maximum content and stock of organic carbon under saturation of tilled land with manure at a dose of 20 t/ha and an equivalent amount of NPK. Over six rotations, carbon content increased by 15% of the initial content in the 0–20 cm layer, while the carbon stock increased by 5 t/ha in this layer and by 32 t/ha in the 0–100 cm layer. Mean value of the carbon-protective capacity of the studied soil varied between 29 and 31 g/kg in the 0–20 cm layer regardless of the applied fertilization systems. The quantity and qualitative composition of biomass, entering the soil under different systems of fertilization, had a significant effect on the accumulation of organic carbon.

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轮作作物对大气碳的积累以及施肥系统对种植草皮的土壤对有机碳积累的影响
摘要 该研究报告了在一个长期试验站进行的六轮试验中,草皮-稻瘟病土壤中有机碳积累和损失的试验数据。研究发现,在光合作用过程中,春大麦植株在生长季节从大气中吸收了 2.84-3.25 吨二氧化碳/公顷(10.3-11.6 吨二氧化碳/公顷),第二年轮作的草甸三叶草吸收了 4.23-5.19 吨二氧化碳/公顷(15.1-18.6 吨二氧化碳/公顷),这取决于实验变量。根据土壤施肥系统的不同,在八田轮作过程中,耕地从大气中螯合了 82.28-99.31 吨二氧化碳/公顷或 22.4-27.1 吨二氧化碳/公顷。长期不施肥的耕地导致土壤中的碳含量比初始水平减少了 13.5%。试验站土壤的特点是,在耕地中施用 20 吨/公顷的肥料和等量的氮磷钾(NPK),土壤中的有机碳含量和存量达到最高。在六次轮作中,0-20 厘米土层的碳含量比初始含量增加了 15%,该土层的碳储量增加了 5 吨/公顷,0-100 厘米土层的碳储量增加了 32 吨/公顷。所研究土壤的碳保护能力平均值在 0-20 厘米土层介于 29 至 31 克/千克之间,与施肥系统无关。在不同施肥系统下,进入土壤的生物质的数量和质量组成对有机碳的积累有显著影响。
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