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    兴安落叶松火烧迹地林褥层碳氮化学计量特征

    Stoichiometric characteristics of C and N of post-fire forest floor of Larix gmelinii

    • 摘要:
        目的  林褥层是主要的森林地被可燃物,是林火干扰北方森林生态系统进程的物质基础。养分循环和能量流动属于森林火烧迹地生态恢复的核心内容,探寻火烧迹地林褥层碳、氮化学计量特征与时间、空间因子间的关系,能够为研究火干扰对森林生态系统碳氮循环的影响提供理论依据。
        方法  以不同过火年份兴安落叶松火烧迹地和未过火兴安落叶松林样地的林褥层(未分解凋落物层、半分解凋落物层)作为研究对象,测定样品全碳、全氮、铵态氮、硝态氮、可溶性有机碳含量。采用单因素方差分析(ANOVA)比较林褥层碳、氮化学计量特征在不同恢复时长、不同空间特征上的显著差异性;用皮尔森相关性表明林褥层碳含量、氮含量和碳氮比与各因子之间的相关程度;用因子分析法综合分析不同因子对林褥层碳氮化学计量比的影响程度。
        结果  随恢复时长增加,未分解层碳、氮含量和C/N呈先升高再降低的趋势,半分解层与之相反。随着海拔升高,未分解层碳含量和C/N、半分解层碳含量呈现上升趋势,半分解层C/N呈先降低再升高的趋势。未分解层碳含量和C/N平坡显著高于缓坡(P < 0.05),氮含量平坡略低于缓坡(P > 0.05)。半分解层碳含量和氮含量缓坡略高于平坡,C/N平坡略高于缓坡。环境因子对未分解层碳氮比影响大小顺序为经度 > 纬度 > 铵态氮含量 > 氮含量 > 碳含量 > 坡度 > 坡向 > pH,对半分解层碳氮比影响大小顺序为经度 > 碳含量 > 坡向 > 海拔 > 氮含量 > pH > 硝态氮含量。
        结论  恢复时长和空间因子均是兴安落叶松火烧迹地林褥层碳含量、氮含量和碳氮化学计量比的影响因子。部分空间因子如坡度、坡向对兴安落叶松火烧迹地林褥层碳含量、氮含量和碳氮化学计量比具有显著影响。时间因子和空间因子可通过改变兴安落叶松火烧迹地林褥层的分解速率进而对其所在的火顶极森林生态系统的碳、氮循环过程产生一定影响。

       

      Abstract:
        Objective  Forest floor is the main fuel of forest soil surface, and it is also the fundamental substance for wildfire to disturb the ecological process of boreal forest. Nutrient cycling and energy flow are the core contents for the ecological restoration of post-fire stands. In order to better understand the effects of fire disturbance on the forest floor carbon (C) and nitrogen (N) cycles of boreal forest ecosystem, this study explored the relationship between C, N or C/N ratio and spatial or temporal factors in post-fire forest floor.
        Method  In the forest floors (Oi horizon and Oe horizon) of different burned and unburned Larix gmelinii stands, the total organic C, N, ammonium N, nitrate N and soluble organic C contents were measured. We used one-way analysis of variance (ANOVA) to compare differences in the stoichiometric characteristics of forest floor C and N in post-fire forests, which were characteristics of different environments and time since fire. Pearson correlation was used to show the correlation between carbon content, nitrogen content, carbon nitrogen ratio and various factors; the influence of different factors on the stoichiometric ratio of carbon and nitrogen in forest floor was analyzed by factor analysis. ower than that in gentle slope (P > 0.05). In Oe horizon, the C and N contents of samples collected from gentle slope were slightly higher than that from flat slope, but the C/N ratio in flat slope was slightly higher than that in gentle slope. The sequential order of environmental factors affecting the C/N ratio in Oi horizon was longitude > latitude > ammonium N content > N content > C content > slope gradient > slope aspect > pH; whereas, in Oe horizon, the sequential order was longitude > C content > slope aspect > altitude > N content > pH > nitrate N content.
        Conclusion  Time since fire and environmental factors could influence C, N and C/N ratio in post-fire Larix gmelinii forest floor. Some environmental factors, such as slope gradient and slope aspect, could significantly affect the C, N and C/N ratio of post-fire Larix gmelinii forest floor. Time factor and environmental factors could affect the C and N cycles in post-fire boreal forest ecosystem by changing the decomposition rate of the forest floor.

       

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