赵艳利, 魏晓梦, 吴传发, 邓扬悟, 廖健利, 黄丹枫, 吴金水, 葛体达. 不同年限有机栽培对土壤生物固氮活性的影响[J]. 土壤通报, 2021, 52(3): 602 − 610. DOI: 10.19336/j.cnki.trtb.2020091801
引用本文: 赵艳利, 魏晓梦, 吴传发, 邓扬悟, 廖健利, 黄丹枫, 吴金水, 葛体达. 不同年限有机栽培对土壤生物固氮活性的影响[J]. 土壤通报, 2021, 52(3): 602 − 610. DOI: 10.19336/j.cnki.trtb.2020091801
ZHAO Yan-li, WEI Xiao-meng, WU Chuan-fa, DENG Yang-wu, LIAO Jian-li, HUANG Dan-feng, WU Jin-shui, GE Ti-da. Soil Biological Nitrogen Fixation under Organic Management in Different Years[J]. Chinese Journal of Soil Science, 2021, 52(3): 602 − 610. DOI: 10.19336/j.cnki.trtb.2020091801
Citation: ZHAO Yan-li, WEI Xiao-meng, WU Chuan-fa, DENG Yang-wu, LIAO Jian-li, HUANG Dan-feng, WU Jin-shui, GE Ti-da. Soil Biological Nitrogen Fixation under Organic Management in Different Years[J]. Chinese Journal of Soil Science, 2021, 52(3): 602 − 610. DOI: 10.19336/j.cnki.trtb.2020091801

不同年限有机栽培对土壤生物固氮活性的影响

Soil Biological Nitrogen Fixation under Organic Management in Different Years

  • 摘要: 氮是对作物生长和产量维持最重要的元素。有机农业无化学肥料投入,生物固氮是氮素最重要的来源之一。然而到目前为止,有机栽培对农田土壤微生物固氮活性的影响尚不清楚。本文以20年常规栽培花椰菜农田土壤为对照,比较经10年、14年、20年有机栽培后土壤微生物固氮活性的变化,并通过多元统计分析探究了影响土壤生物固氮活性的因素。研究结果表明,在7天的测定周期中,与常规栽培相比,10年和14年有机栽培降低了前期土壤生物固氮速率,但整个周期累积固氮在量各处理间无显著差异。不同年限有机栽培对土壤生物固氮速率和累积固氮量影响显著,整体而言14年有机栽培的最低,10年和20年有机栽培间的差异因培养时间而异。培养结束时,常规栽培土壤固氮速率接近于0,有机栽培的花椰菜土壤则仍保持较高活性。皮尔森相关分析和冗余分析(RDA)表明,NH4+、NO3及Olsen P含量是影响有机栽培土壤生物固氮活性的关键因素;其中,NO3对固氮有抑制作用,Olsen P则促进了土壤生物固氮活性的增加。

     

    Abstract: Nitrogen (N) is the most important element for the growth and yield of crops. Biological N fixation plays an essential role in N supply in organic agriculture without chemical fertilizer input. However, the effect of organic management years on biological N fixation activity is still unclear. This study compared the dynamics of N fixation rate and cumulative N fixation in soils under the organic management of cauliflower for 10 years, 14 years, 20 years and its conventional management for 20 years. And the factors influencing N fixation were explored using multivariate statistical analysis. The results showed that during the 7-day incubation, 10-year and 14-year organic managements reduced the N fixation rate compared with conventional management. However, the accumulative N fixation over the incubation showed no significant difference among all treatments. The N fixation rate and cumulative N fixation amount were significantly affected by organic management years and were the lowest in 14-year organic management. At the end of incubation, the soil N fixation rate under conventional management was near zero, whereas N fixation activity remained high under organic managements. Pearson correlation and redundancy analysis showed that the N fixation activity was primarily affected by the contents of NH4+, NO3 and Olsen P. NO3 suppressed the N fixation, while Olsen P increased the N fixation activity.

     

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