Ameer Muhammad Jamal, Liu Yushan, Yan Siyu, Qu Tongbao
College of Forestry and Grassland, Jilin Agricultural University, Changchun 130118, China.
Life (Basel). 2025 Sep 4;15(9):1403. doi: 10.3390/life15091403.
Climate change and injudicious nitrogen addition alter the soil physico-chemical properties and microbial activity in oligotrophic forest soil, which disrupts the nitrogen cycle balance. Nevertheless, recommended fertilizer forms and levels are considered to be crucial for stable nitrogen application. We established a short-term field trial for the first time using a randomized complete block design under the yellow larch forest, with six treatments applied, including urea CO(NH), ammonium chloride NHCl, and sodium nitrate NaNO at concentrations of 10 and 20 kg N hm yr, each extended by three replicates. The gene abundances were measured using quantitative PCR (qPCR), in which the abundance levels of AOA () and were higher under high CO(NH) 2.87 × 10 copies g dry soil and low NO 8.82 × 10 copies g dry soil, compared to CK, representing 2.8-fold and 1.5-fold increases, respectively. We found niche partitioning as revealed despite AOA () increasing in number, AOB () contributing more to ammonia oxidation while proved opportunistic under stress conditions. This was supported by distinct significant correlations among factors, in which soil urease enzymatic activity (S-UE) was associated with AOA () and , while AOB () and positively correlated with NH content and soil potential of hydrogen (pH), respectively. Among the applied treatments, high-level NO increased total nitrogen content and had a significant effect on soil N-acetyl-β-d-glucosaminidase (S-NAG) and soil acid protease (S-ACPT) activity. In summary, we observed an increase in growth with high nitrogen retention.
气候变化和不合理的氮添加会改变贫营养森林土壤的物理化学性质和微生物活性,从而破坏氮循环平衡。然而,推荐的肥料形式和施用量被认为对稳定施氮至关重要。我们首次在落叶松林下采用随机完全区组设计进行了短期田间试验,设置了六种处理,包括浓度为10和20 kg N hm² yr⁻¹的尿素CO(NH₂)₂、氯化铵NH₄Cl和硝酸钠NaNO₃,每种处理重复三次。使用定量PCR(qPCR)测量基因丰度,其中在高浓度CO(NH₂)₂(2.87×10⁹拷贝 g干土)和低浓度NO₃⁻(8.82×10⁸拷贝 g干土)条件下,氨氧化古菌(AOA)和氨氧化细菌(AOB)的丰度水平高于对照(CK),分别增加了2.8倍和1.5倍。我们发现尽管AOA数量增加,但仍存在生态位划分,AOB对氨氧化的贡献更大,而在胁迫条件下证明具有机会主义性。这得到了各因素之间明显显著相关性的支持,其中土壤脲酶活性(S-UE)与AOA和AOB相关,而AOB和分别与NH₄⁺含量和土壤酸碱度(pH)呈正相关。在所应用的处理中,高浓度NO₃⁻增加了总氮含量,并对土壤N-乙酰-β-D-氨基葡萄糖苷酶(S-NAG)和土壤酸性蛋白酶(S-ACPT)活性有显著影响。总之,我们观察到高氮保留条件下的生长增加。