干旱模拟实验对土壤氮矿化过程及其驱动机制的影响

Effects of Drought Simulations on Soil Nitrogen Mineralization and Its Driving Mechanisms

  • 摘要:
    目的 实验室模拟干旱和原位干旱控制是研究土壤生态过程响应气候干旱的两种常用方法。然而,由于实验室简化环境因子,而原位存在较大环境扰动,常导致结果出现较大差异。
    方法 研究以江苏省东台林场美洲黑杨(Populus deltoides)人工林为对象,比较了室内(培养瓶、PVC管)和原位(PVC管)培养条件的三种干旱梯度(自然、减少30%穿透雨、减少50%穿透雨)下土壤氮矿化过程及其驱动因素的差异。
    结果 室内培养实验相较于原位模拟实验在评估土壤pH、无机氮和净氨化速率时存在显著差异,但对微生物生物量和净硝化速率的干旱效应评估结果一致。PLS-SEM分析表明,室内培养实验难以捕捉原位环境下土壤氮矿化的复杂生态联系,可能因此低估或误判干旱对生物地球化学交互作用的影响。然而,室内实验在减少环境扰动下分析土壤含水量与微生物关系方面仍有价值。此外,室内培养瓶中土壤物理结构改变可能低估干旱处理对氮矿化的效应。
    结论 研究强调室内研究虽有价值,但不能完全替代原位实验,未来应基于原位研究,并结合更合理的室内培养结果,以期更准确地理解干旱对土壤生态过程的影响机制。

     

    Abstract:
    Objective Laboratory drought simulation and in-situ drought manipulation are two common methods for studying soil ecological processes in response to climate drought. However, the results often differ significantly because laboratory settings simplify environmental factors, whereas in-situ conditions are subject to complex disturbances.
    Method The study compared the soil nitrogen mineralization and its driving factors under three drought gradients (ambient, 30% reduction in throughfall, and 50% reduction in throughfall) using laboratory (incubation bottles and PVC tubes) and in-situ (PVC tubes) culture conditions. The study was conducted in a poplar (Populus deltoides) plantation at Dongtai Forest Farm, Jiangsu Province.
    Result The results suggested that laboratory incubation experiments exhibited significant differences compared to in-situ simulations experiments when assessing soil pH, inorganic nitrogen, and net ammonification rate. However, the results for the drought effects on microbial biomass and net nitrification rate were consistent between the two conditions. PLS-SEM analysis showed that laboratory incubation experiments could not fully reflect the complex ecological correlations of soil nitrogen mineralization in an in-situ environment, potentially leading to an underestimation or misjudgment of drought's effect on biogeochemical interactions. However, laboratory experiments remained valuable for analyzing the correlation between soil water content and microbes under reduced environmental disturbance. Furthermore, the altered soil physical structure in incubation bottles could underestimate the effect of drought on nitrogen mineralization.
    Conclusion In conclusion, the study emphasizes that while laboratory experiments are valuable, they cannot fully replace in-situ experiments. Future research should build upon in-situ findings and integrate results from more judiciously designed laboratory cultures to achieve more accurate understandings of the mechanisms by drought impacts on soil ecological processes.

     

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