Intensity of CO2 emissions of sod-podzolic soil depending on fertilization and lime application

V. Polovyi, G. Rovna, L. Yashchenko, B. Huk
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Abstract

Topicality. With climate change, agricultural production accounts for about 15 % of green-house gas emissions. Disbalance of organic carbon decreases the environmental sustainability and productivity of agroecosystems and soil fertility. With soil management, the intensity of carbon monoxide emission from the soil can reduce to optimize its organic matter. Issues. There is a crucial need to study and analyze comprehensively the effects of different rates of chemical meliorants and mineral fertilizers for crops in the Western Polissia crop rotation on the volume of CO2 emissions from sod-podzolic soil. Aim. To study the characteristic features of carbon dioxide emissions from sod-podzolic soil during winter wheat and spring barley cultivation with different rates of meliorants and fertilizers. Materials and Methods. Field experiment, agrochemical and statistical methods. Results. On the background of mineral fertilization, land reclamation with limestone materials at 0.5 and 1.0 rates determined by the hydrolytic acidity of the soil generally decreases CO2 emissions into the air. During the growing season, depending on the development stage of spring barley, the level of carbon dioxide emission in the variant with N90P90K90 was 89.8–68.3–63.5 mg CO2/kg soil, and in combination with 1.0 rate of dolomite powder – 83.1–59.8–63.6 mg CO2/kg soil. It is noted that the intensity of CO2 accumulation in the surface layer depended on rates of ameliorant, soil moisture and temperature. Thus, the carbon dioxide emission in a winter wheat field was the highest when 1.5 rates of dolomite powder were applied on the background of N120P60K90 , and in the stem elongation stage at air temperature 13.2 ℃ was 77.7 mg CO2/kg of soil. When air temperature increased to 22.0 ℃ in the heading stage, this indicator increased by 1.2 times and at air temperature of 20.4 ℃ in the full maturity stage, it decreased by 1.3 times. When 1.0 rate of dolomite powder was applied, CO2 emission decreased to 18.2 mg CO2/kg of soil compared with 1.5 rates in the full maturity stage of wheat due to the intensity of redox processes in the soil when different rates of limestone materials was applied. Conclusions. In the short-term crop rotation, lime application had a positive effect on the for-mation of deficit-free balance of organic carbon in sod-podzolic soil with intensive application of mineral fertilizers for crops. When we applied 1.0 and 1.5 rates of dolomite powder on the background of N120P60K90 in winter wheat crops, the organic carbon balance was 0.35–0.28 t/ha, in spring barley crops on the background of N90P90K90 – 0.10–0.16 t/ha. Key words: winter wheat, spring barley, land reclamation, fertilizers, carbon dioxide, balance.
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不同施肥和石灰施用量的灰化土CO2排放强度
时事性。随着气候变化,农业生产占温室气体排放量的15%左右。有机碳失衡降低了农业生态系统的环境可持续性、生产力和土壤肥力。通过土壤管理,可以降低土壤一氧化碳排放强度,优化土壤有机质。问题。目前迫切需要综合研究和分析波兰西部轮作中不同比例的化学改良剂和矿物肥料对草灰土壤CO2排放量的影响。的目标。研究冬小麦和春大麦栽培过程中不同施肥量和良品肥量下灰化土二氧化碳排放的特征特征。材料与方法。田间试验、农化和统计方法。结果。在矿物施肥的背景下,由土壤水解酸度决定的0.5和1.0比例的石灰石材料复垦总体上减少了向大气中排放的CO2。在生长季节,根据春大麦发育阶段的不同,N90P90K90变异株的二氧化碳排放水平为89.8 ~ 68.3 ~ 63.5 mg CO2/kg土壤,与1.0浓度的白云石粉组合为83.1 ~ 59.8 ~ 63.6 mg CO2/kg土壤。结果表明,土壤表层CO2积累强度与改良剂、土壤湿度和温度有关。由此可见,在N120P60K90背景下,1.5倍白云石粉处理的冬小麦土壤二氧化碳排放量最高,在茎伸长期,气温13.2℃时,土壤二氧化碳排放量为77.7 mg /kg。抽穗期气温升高至22.0℃时,该指标升高1.2倍,成熟期气温升高至20.4℃时,该指标下降1.3倍。在小麦成熟期,当白云石粉施用量为1.0时,土壤中氧化还原过程的强度比施用量为1.5时降低至18.2 mg CO2/kg。结论。在短期轮作中,石灰对土壤有机碳无亏平衡的形成有积极的影响。以N120P60K90为背景施用1.0和1.5浓度白云石粉时,冬小麦作物有机碳平衡为0.35 ~ 0.28 t/ha,春大麦作物有机碳平衡为0.10 ~ 0.16 t/ha。关键词:冬小麦,春大麦,土地复垦,肥料,二氧化碳,平衡。
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