三种施肥制度下土壤孔隙结构对土壤有机质中硝酸盐释放及施肥量的影响

Renjie Ruan, Zhongbin Zhang, Ting Lan, Yaosheng Wang, Wei Li, Huan Chen, Xinhua Peng
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摘要

土壤孔隙结构随土壤管理方式的不同而变化很大,在土壤养分有效性中起着重要作用。然而,土壤孔隙特征(孔隙连通性和孔径分布)与土壤有机质或施用肥料中硝酸盐释放的关系尚不清楚。本研究旨在确定三种施肥方式下土壤孔隙结构对硝酸盐释放的影响:Control(不施肥)、NPK(无机氮磷钾施肥)和OF(有机施肥)。土壤样品在每次施肥处理中受到三种物理干扰(完整、重新包装和压实),以改变土壤孔隙结构特征,并使用计算机断层扫描(CT)进行量化。土壤有机质(Ndfs)和施用肥料(Ndff)释放的硝酸盐与15N标记的尿素进行了区分,并在培养过程中进行了浸出。结果表明,与对照相比,氮磷钾和有机肥处理的累积Ndfs有所降低,而有机肥处理的累积Ndfs有所增加。与完整处理相比,重新包装处理的累积Ndff较高,而压实处理的累积Ndff较低。相关分析表明,累积Ndfs受土壤有机碳含量(SOC)和氨氧化菌丰度的正影响,而累积Ndff受土壤有机碳含量(SOC)的负影响。此外,累积ndf与土壤孔隙特征无关;累积Ndff与大孔隙度、大孔隙连通性以及孔径在100 ~ 500 μm和500 ~ 1000 μm之间的孔隙度呈正相关。通径分析表明,100 ~ 500 μm孔隙通过调节持水性和透气性间接影响Ndff的势和速率。我们的研究结果提供了一个新的视角,表明土壤孔隙结构特征显著影响肥料中硝酸盐的释放,而不是土壤有机质中硝酸盐的释放,其中100-500 μm孔隙度对肥料中硝酸盐的释放影响特别有效。
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The role of soil pore structure on nitrate release from soil organic matter and applied fertilizer under three fertilization regimes
Soil pore structure is highly variable with soil management practices, and plays an important role in nutrient availability. However, the relationships between soil pore characteristics (pore connectivity and pore size distribution) and nitrate release from soil organic matter or applied fertilizer are still unclear. This study aimed to identify how soil pore structure affects nitrate release under three fertilization regimes: Control (no fertilization), NPK (mineral NPK fertilization), and OF (organic fertilization). Soil samples were subjected to three physical disturbances (Intact, Repacked, and Compacted) for each fertilization treatment to alter soil pore structure characteristics which were quantified using computed tomography (CT). Nitrate release derived from soil organic matter (Ndfs) and applied fertilizer (Ndff) was distinguished with 15N labelled urea and leached during an incubation. The results showed a decrease in cumulative Ndff in the NPK and OF treatments, compared to the Control, while an increase in cumulative Ndfs in the OF treatment, compared to the Control. Cumulative Ndff was higher in the Repacked treatment, but lower in the Compacted treatment, than in the Intact treatment. Correlation analysis showed that cumulative Ndfs was positively influenced by soil organic carbon content (SOC) and ammonia-oxidizing bacteria abundance, while cumulative Ndff was negatively influenced by SOC. Furthermore, cumulative Ndfs was not associated with soil pore characteristics; however, cumulative Ndff was positively associated with macroporosity, macropore connectivity, and the porosities of pores with diameters in the ranges of 100–500 μm and 500–1000 μm. Path analysis indicated that 100–500 μm pores indirectly influenced the potential and rate of Ndff by modulating water holding capacity and air permeability. Our findings provide a novel perspective, indicating that soil pore structure characteristics significantly influence nitrate release from applied fertilizer rather than that from soil organic matter, with porosity of 100–500 μm being particularly effective in influencing nitrate release from applied fertilizer.
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