Mineral Nitrogen Release Patterns in Various Soil and Texture Types and the Impact of Urea and Coated Urea Potassium Humate on Barley Biomass

IF 2.9 Q2 SOIL SCIENCE
Samar Swify, Romas Mažeika, Jonas Volungevičius
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Abstract

Controlled-release urea fertilization is an innovative approach and effective means to reduce the loss of nitrogen and enhance fertilizer use efficiency to optimize crop yield while minimizing the environmental impact. The objective of this study was to investigate the dynamic process of mineral nitrogen (Nmin) release in Luvisols, Cambisols, Retisols, and Arenosols to understand the interaction between soil characteristics and mineral nitrogen release and evaluate the impact of conventional urea compared to coated urea potassium humate on barley biomass production. A pot experiment was conducted under glasshouse conditions (20 ± 2 °C and 60% Humidity). Five treatments including no fertilization as a control (C), 100 kg·N·ha−1 of urea (U100), 200 kg·N·ha−1 of urea (U200), 100 kg·N·ha−1 of coated urea potassium humate (UPH100), and 200 kg·N·ha−1 of coated urea potassium humate (UPH200) were applied to four soil and texture types. Our findings indicate that there are different patterns of mineral nitrogen release across the different soil and texture types. Ammonium levels reached their peak point in all soils within 2–7 days after application. On the other hand, the concentration of nitrate NO3−–N showed a linear increase over 45 days during the experiment. The Retisol, which had a sandy clay texture, obtained the highest concentration of mineral nitrogen in both forms (NH4 and NO3), while the sandy texture of Arenosol showed the lowest accumulation of mineral nitrogen and its forms. The application of potassium humate caused a delay of 1–4 days in the peak of soil ammonium, which at peak accounted for approximately 25–44% of the mineral nitrogen in the soil. Furthermore, the application of urea and coated urea potassium humate exhibited significant effects on barley biomass with an increase of approximately 14–91% compared to the unfertilized treatment (control). This research contributes to our understanding of nutrient dynamics in diverse soil environments and provides insights into optimizing sustainable fertilization strategies such as controlled-release fertilizer application. The implications of these findings highlight the significance of tailored nutrient management practices based on soil texture type, which can lead to improved agricultural productivity and environmental impact.
不同土壤和质地类型下矿质氮释放模式及尿素和包膜尿素腐植酸钾对大麦生物量的影响
控释尿素施肥是减少氮素流失,提高肥料利用效率,优化作物产量,同时最大限度减少对环境影响的创新途径和有效手段。本研究的目的是研究草甘醇(luvisol)、甘露醇(cambisol)、雷红壤(reicsols)和香薄荷醇(Arenosols)中矿物氮(Nmin)释放的动态过程,了解土壤特征与矿物氮释放之间的相互作用,并评估常规尿素与包膜尿素腐植酸钾对大麦生物量产量的影响。盆栽试验在温室条件下(20±2℃,60%湿度)进行。对4种土壤和质地类型分别施用不施肥(C)、100 kg·N·ha−1尿素(U100)、200 kg·N·ha−1尿素(U200)、100 kg·N·ha−1包膜尿素腐植酸钾(UPH100)和200 kg·N·ha−1包膜尿素腐植酸钾(UPH200) 5个处理。我们的研究结果表明,在不同的土壤和质地类型中存在不同的矿物氮释放模式。施用后2 ~ 7 d内铵含量均达到峰值。硝态氮(NO3−-N)浓度在45 d内呈线性上升趋势。砂质粘土结构的壤壤中矿质氮(NH4和NO3)浓度最高,砂质结构的砂壤中矿质氮及其形态积累最低。施用腐植酸钾导致土壤铵态氮峰值延迟1 ~ 4 d,铵态氮峰值约占土壤矿质氮的25 ~ 44%。此外,施用尿素和包膜尿素腐植酸钾对大麦生物量有显著影响,与未施肥处理(对照)相比,增加了约14-91%。该研究有助于我们了解不同土壤环境下的养分动态,并为优化控释施肥等可持续施肥策略提供见解。这些发现的意义突出了基于土壤质地类型的量身定制的养分管理实践的重要性,这可以提高农业生产力和环境影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Soil Systems
Soil Systems Earth and Planetary Sciences-Earth-Surface Processes
CiteScore
5.30
自引率
5.70%
发文量
80
审稿时长
11 weeks
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