Department of Soil and Water Science, College of Land Science and Technology, China Agricultural University, No. 2 West Road of Yuanmingyuan, Haidian, Beijing 100193, PR China.
Department of Soil and Water Science, College of Land Science and Technology, China Agricultural University, No. 2 West Road of Yuanmingyuan, Haidian, Beijing 100193, PR China; Beijing Soil & Fertilizer Extension Service Center, No. 6 Yumin Zhong Road, Xicheng, Beijing 100029, PR China.
Sci Total Environ. 2020 Dec 1;746:141235. doi: 10.1016/j.scitotenv.2020.141235. Epub 2020 Jul 31.
Combined application of organic fertilizer (OF) and chemical nitrogen (N) fertilizer (CF) is a common fertilization practice, providing better N supply pattern for crop growth. However, few studies focused on the effect of granulation method of these two fertilizers on N supply to soil. To validate this effect, we mixed the CF (N-(NH)SO) into cow manure powders with maize straw powder at rate of 2% or 8% (dry weight), respectively, in two forms, homogeneous granulation (HG) and spatial heterogeneous granulation (SG), and applied them to soil to investigate their difference in N transformations during an 80-day incubation. Results showed that there were more NH, NO and microbial biomass N (MBN) in the SG granules and the surrounding soil, while more dissolved organic N (DON) in the HG granules and the corresponding soil after day 30. At day 80, compared to HG, SG released less CF-N into the surrounding soil, but primed more organic N into mineral N. Structural equation model (SEM) revealed that DON was the main form of N transported from fertilizer granules to the surrounding soil, and then drove the changes of soil microbial activity, which determined the amount and dynamic of mineral N in the surrounding soil. These results indicated that, in heterogeneous granulation, the spatial separation between OF and CF slow down, but more importantly enhanced up, the microbial transformation of CF in the granules. This demonstrated that the spatial heterogeneous granulation of OF and CF could change the pattern of N release from fertilizer to soil and offer a potential way to optimize N fertilizer management strategies in the future.
有机肥(OF)和化学氮肥(CF)的联合应用是一种常见的施肥方式,可为作物生长提供更好的氮供应模式。然而,很少有研究关注这两种肥料的造粒方法对土壤氮供应的影响。为了验证这一效果,我们将 CF(N-(NH )SO )以 2%或 8%(干重)的比例分别混入牛粪粉和玉米秸秆粉中,采用均相造粒(HG)和空间异质造粒(SG)两种形式,并将其应用于土壤中,以研究它们在 80 天培养过程中氮转化的差异。结果表明,SG 颗粒及其周围土壤中含有更多的 NH 、NO 和微生物生物量氮(MBN),而 HG 颗粒及其相应土壤中在第 30 天后含有更多的溶解有机氮(DON)。在第 80 天,与 HG 相比,SG 向周围土壤释放的 CF-N 较少,但向矿质氮激发的有机氮较多。结构方程模型(SEM)显示,DON 是从肥料颗粒向周围土壤运输氮的主要形式,然后驱动土壤微生物活性的变化,从而决定了周围土壤中矿质氮的数量和动态。这些结果表明,在异质造粒中,OF 和 CF 之间的空间分离虽然减缓了,但更重要的是增强了 CF 在颗粒中的微生物转化。这表明 OF 和 CF 的空间异质造粒可以改变肥料向土壤中释放氮的模式,并为未来优化氮肥管理策略提供了一种潜在途径。