不同秸秆还田量对土壤氨基糖态氮及总氮动态的影响

Effects of Different Straw Return Rates on Soil Amino Sugar Nitrogen and Total Nitrogen Dynamics

  • 摘要:
    目的 本研究旨在阐明不同秸秆还田量对农田土壤氨基糖态氮积累特征及其组成变化的影响,对于理解微生物在土壤氮素保持与循环中的作用具有重要意义。
    方法 基于东北地区连续9年的玉米秸秆还田长期定位试验,设置单施化肥(T0)、化肥 + 50%秸秆(T1)和化肥 + 100%秸秆(T2)三个处理,测定土壤总氮和三种氨基糖(氨基葡萄糖、氨基半乳糖、胞壁酸)态氮含量及其比例的动态变化。
    结果 T1和T2处理显著增加了土壤总氮和总氨基糖态氮含量,并且总氨基糖态氮积累幅度超过土壤总氮。第9年时,T2处理土壤总氨基糖态氮较第1年增加67.1%,占土壤总氮比例达7.31%。秸秆还田对真菌来源的氨基葡萄糖态氮具有明显的提升作用,且高量秸秆作用更为明显。而细菌来源的胞壁酸态氮则是在低量秸秆处理下增加比例更多。氨基半乳糖态氮含量随秸秆还田量增加和时间增长而提升。
    结论 本研究表明,长期秸秆还田促进氮同化过程,显著促进土壤氮素积累。高量秸秆还田加速微生物残体特别是真菌残体的积累,增加了土壤氮库库容及其稳定性,为提升土壤氮利用效率和土壤可持续管理提供了科学依据。

     

    Abstract:
    Objective Amino sugar nitrogen (ASN), a key component of microbial residues, is an important indicator of microbial involvement in soil nitrogen (N) cycling. This study aimed to clarify the accumulation patterns and compositional changes of ASN under different maize straw return rates, providing insights into the microbial role in soil N retention and turnover.
    Method A 9-year long-term field experiment was conducted in Northeast China with three treatments: chemical fertilizer alone (T0), chemical fertilizer with 50% straw return (T1), and chemical fertilizer with 100% straw return (T2). Soil total N (TN) and the concentrations of three kings of ASN—glucosamine N (N-GluN), galactosamine N (N-GalN), and muramic acid N (N-MurN)-were measured to assess ASN accumulation and its composition over time.
    Result Both T1 and T2 treatments significantly increased TN and total ASN contents, with the accumulation of ASN exceeding that of TN. By the 9th year, the total ASN content in T2 increased by 67.1% compared to the 1st year, accounting for 7.31% of TN. Straw return significantly enhanced the accumulation of fungal-derived N-GluN, particularly under the high straw input. In contrast, bacterial-derived N-MurN increased more under the lower straw input treatment. N-GalN content increased progressively with both straw return rate and duration.
    Conclusion Long-term straw return promoted N assimilation and significantly enhanced soil N accumulation. High-rate straw return accelerated the accumulation of microbial residues, particularly fungal residues, thereby increasing the size and stability of the soil N pool. These findings provide scientific evidence for improving N use efficiency and guiding sustainable soil management in agroecosystems.

     

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