The effect of metal oxide coating of urea on mineralization in two contrasting soils

Viran Kathri Arachchige, Therese M. McBeath, Ronald J. Smernik, Ganga M. Hettiarachchi, Roya Khalil
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Abstract

Urease inhibitors are used to delay the conversion of N supplied to soil as urea to better match the mineral N supply to crop demand. Using soil in petri dishes, we compared the spatial and temporal mineral N dynamics close to the site of urea addition for two soils of contrasting texture—sandy soil (2% clay) and clay soil (51% clay)—treated with N fertilizer products that had the potential to inhibit urease. The treatments included trace metal oxide coatings (ZnO, NiO, and CuO) of granular urea fertilizer, N-(n-butyl)thiophosphoric triamide (NBPT; a commercial urease inhibitor) coated urea and uncoated urea. In the sandy soil, NBPT inhibited urea hydrolysis, whereas the metal oxide–coated urea had little effect. Unlike in the sandy soil, the most striking result for the clay soil was the “disappearance” of mineral N in the latter part of the incubation. However, a delay in the disappearance of mineral N, hence a higher recovery, for the NBPT-urea and CuO-urea was observed at day 14 in the clay soil presumably due to the slower hydrolysis of urea compared to other treatments. Overall, the study of both spatial and temporal mineral N dynamics in soils supplied with urea fertilizers suggests that CuO-coated urea could have properties that delay the hydrolysis of urea in certain soils. Given the strongly contrasting outcomes for the two soils, further experiments with soils that span the range of texture between these two extremes are warranted.

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尿素金属氧化物包膜对两种对比土壤矿化的影响
脲酶抑制剂用于延缓供给土壤的氮转化为尿素,以更好地匹配矿物氮供应与作物需求。在培养皿中,我们比较了两种不同质地的土壤——砂质土(2%粘土)和粘土土(51%粘土)——在尿素添加位点附近的时空矿物氮动态。处理包括颗粒尿素肥料的微量金属氧化物涂层(ZnO、NiO和CuO)、N-(正丁基)硫代磷三酰胺(NBPT);(一种商用脲酶抑制剂)包被尿素和未包被尿素。在砂质土壤中,NBPT对尿素水解有抑制作用,而金属氧化物包覆尿素对尿素水解作用不大。与砂质土不同,粘土最显著的结果是在孵育后期矿物氮的“消失”。然而,在粘土土壤中,nbpt -尿素和cuo -尿素的矿物氮消失延迟,因此回收率更高,这可能是由于与其他处理相比,尿素水解速度较慢。综上所述,对尿素施用土壤矿质氮时空动态的研究表明,cuo包覆尿素可能具有延缓某些土壤尿素水解的特性。考虑到两种土壤的强烈对比结果,进一步的土壤实验跨越这两个极端之间的纹理范围是有必要的。
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