College of Agronomy, Anhui Agricultural University, Hefei, 230036, China.
College of Agronomy, Anhui Agricultural University, Hefei, 230036, China.
J Environ Manage. 2020 Jun 1;263:110384. doi: 10.1016/j.jenvman.2020.110384. Epub 2020 Mar 14.
Soil NO emissions depend on the status of stoichiometric balance between organic C and inorganic N. As a beneficial management practice to sustain soil fertility and crop productivity, partial substitution of organic fertilizers (OFs) for synthetic fertilizers (SFs) can directly affect this balance status and regulate NO emissions. However, no multi-year field studies of NO emissions under different ratios of OF to SFs have been performed. We conducted a 4-year experiment to measure NO emissions in a maize-wheat rotation in central China. Six treatments were included: total SF (TS), total OF, no N fertilizer, and ratios of to SF with 1: 2 (LO), 1: 1 (MO), and 2: 1 (HO), based on N content. Two incubation experiments were performed to further interpret the field data. In the first year, cumulative NO emissions (kg N ha) in LO, MO, and HO were 4.59, 4.68, and 3.59, respectively, significantly lower than in TS (6.67). However, from the second year onwards, organic substitution did not reduce NO emissions and even significantly enhanced them in the fourth year relative to TS. Soil respiration under OF-amended soils increased over the course of the experiment. From the second year onwards, there was no marked difference in mineral N concentrations between OF- and SF-amended soils. OF caused a drop in soil pH. Cumulative NO was negatively correlated with pH. Long-term organic substitution enhanced NO emissions produced via denitrification rather than nitrification and resulted in higher temperature sensitivity of NO emissions than TS. The enhanced NO emissions from the OF-treated soils were mainly attributable to accelerated OF decomposition, increased denitrification-NO emissions, and lessened NO reduction due to lower pH and greater NO. These results indicate that OF substitution can reduce NO emissions in the first year, but in the long-term it can increase emissions, especially as soils warm.
土壤氮氧化物排放取决于有机碳和无机氮之间化学计量平衡的状态。作为维持土壤肥力和作物生产力的有益管理实践,有机肥(OFs)部分替代化肥(SFs)可以直接影响这种平衡状态,并调节氮氧化物排放。然而,目前还没有进行不同有机肥与化肥比例下氮氧化物排放的多年田间研究。我们在中国中部的玉米-小麦轮作中进行了一项为期 4 年的实验,以测量氮氧化物排放。该实验共设置了 6 个处理,包括:总 SF(TS)、总 OF、不施氮肥,以及基于氮含量的 SF 与 OF 比例为 1:2(LO)、1:1(MO)和 2:1(HO)。进行了两项培养实验以进一步解释田间数据。在第一年,LO、MO 和 HO 处理的累积氮氧化物排放量(kg N ha)分别为 4.59、4.68 和 3.59,显著低于 TS(6.67)。然而,从第二年开始,有机替代并没有减少氮氧化物排放,甚至在第四年相对于 TS 显著增加。在整个实验过程中,施有机肥土壤的土壤呼吸增加。从第二年开始,OF 和 SF 施肥土壤之间的矿质氮浓度没有明显差异。OF 降低了土壤 pH 值。累积氮氧化物与 pH 值呈负相关。长期有机替代增强了反硝化产生的氮氧化物排放,而不是硝化产生的氮氧化物排放,导致氮氧化物排放的温度敏感性高于 TS。OF 处理土壤中增强的氮氧化物排放主要归因于 OF 分解加速、反硝化-氮氧化物排放增加,以及由于 pH 值降低和氮氧化物增加导致的氮氧化物还原减少。这些结果表明,OF 替代可以在第一年减少氮氧化物排放,但从长期来看,它会增加排放,尤其是在土壤变暖的情况下。