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河北平泉油松林火烧迹地土壤氮变化特征

李炳怠/a>,刘冠宎/a>,顾泽,李伟兊/a>,田野,王博,刘晓丛/a>,舒立禎/a>

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李炳? 刘冠? 顾泽, 李伟? 田野, 王博, 刘晓? 舒立? 河北平泉油松林火烧迹地土壤氮变化特征[J]. 北京林业大学学报, 2023, 45(3): 1-10. doi: 10.12171/j.1000-1522.20220007
引用本文: 李炳? 刘冠? 顾泽, 李伟? 田野, 王博, 刘晓? 舒立? 河北平泉油松林火烧迹地土壤氮变化特征[J]. 北京林业大学学报, 2023, 45(3): 1-10.doi:10.12171/j.1000-1522.20220007
Li Bingyi, Liu Guanhong, Gu Ze, Li Weike, Tian Ye, Wang Bo, Liu Xiaodong, Shu Lifu. Characteristics of soil nitrogen change in the burned area of Pinus tabuliformis forest in Pingquan County, Hebei Province of northern China[J]. Journal of Beijing Forestry University, 2023, 45(3): 1-10. doi: 10.12171/j.1000-1522.20220007
Citation: Li Bingyi, Liu Guanhong, Gu Ze, Li Weike, Tian Ye, Wang Bo, Liu Xiaodong, Shu Lifu. Characteristics of soil nitrogen change in the burned area ofPinus tabuliformisforest in Pingquan County, Hebei Province of northern China[J].Journal of Beijing Forestry University, 2023, 45(3): 1-10.doi:10.12171/j.1000-1522.20220007
doi:10.12171/j.1000-1522.20220007
基金项目:国家重点研发计划重点专项的子课题?020YFC1511601(/div>
详细信息
    作者简今

    李炳怡,博士生。主要研究方向:森林防火、火烧迹地恢复。Email9a href="//www.inggristalk.com/j/article/doi/10.12171/mailto:494388689@qq.com">494388689@qq.com 地址?00091 北京市海淀区香山路东小? 中国林业科学研究陡/p>

    责任作耄

    舒立福,研究员。主要研究方向:森林防火。Email9a href="//www.inggristalk.com/j/article/doi/10.12171/mailto:slfhxk@126.com">slfhxk@126.com 地址:同三/span>

  • 中图分类叶S791.254

Characteristics of soil nitrogen change in the burned area ofPinus tabuliformisforest in Pingquan County, Hebei Province of northern China

  • 摘要: 目的分析河北省平泉县火烧迹地油松天然次生林的土壤氮在火后不同年份的变化特征,结合林分因子、立地因子和可燃物因子,研究土壤氮变化的影响因素,为火烧迹地养分循环研究及恢复提供科学依据、/sec> 方法选取河北平泉县柳溪镇油松林火烧迹地为研究对象,分别于2015年(火后当年)?016年(火后1年)?021年(火后6年)采集土壤样品,测定土壤全氮(TN)、碱解氮(AN)、铵态氮(NH 4 +-N)和硝态氮(NO 3 ∑/sup>-N)含量,比较和分析上?种氮含量在不同火强度(轻度火烧、中度火烧、重度火烧、对照样地)、不同土层深度(0 ~ 10 cm?0 ~ 20 cm)在不同年份?015?016?021年)的变化趋势。使用相关性分析和冗余分析探究林分因子(树高、胸径、郁闭度)、立地因子(坡度、坡向)和可燃物因子??0?00 时滞可燃物载量??0?00 时滞可燃物含水率)对土壤氮元素的影响、/sec> 结果?)整体而言,火强度、土层深度、年份对4种土壤氮含量具有显著影响'i>P< 0.05),火强度和土层深度?015年的4种土壤氮含量存在交互作用'i>P< 0.05),火强度和年份?种土壤氮含量存在交互作用'i>P< 0.05),火强度、土层深度和年份对土壤氮含量不具有三因素交互影响'i>P> 0.05);?)火?年(2016)土壤全氮、铵态氮、硝态氮含量回升,以重度火烧样地最为明显,增幅分别?64.67%?97.97%?85.63%,碱解氮含量降低,中度样地降幅为52.48%。火? 年(2021)土壤全氮、铵态氮、碱解氮含量在中度样地回升明显,增幅分别?68.78%?09.00%?27.51%,硝态氮含量在中、低强度下降,降幅为14.31%?4.34%;(3)RDA结果表明,可燃物含水率对土壤氮含量的变化贡献最多解释度?时滞可燃物含水率影响碱解氮含量,并与其成正比关系?00时滞可燃物含水率影响硝态氮含量,并与其呈正比关系。林分因子和立地因子对土壤氮含量变化解释度较小,主要是间接作用、/sec> 结论火后6年内土壤氮含量的变化先降低再回升,这是火强度、土壤和年份共同作用的结果。火烧初期(火后当年?年),火强度对土壤氮含量的影响起主导作用,但是随着年限增加?年),火强度对土壤氮含量的直接影响降低,火强度与土壤的介导作用,通过土壤含水率、温度、pH等指标继续影响土壤氮含量的变化。火烧迹地植物的更新与发育同样受到介导作用影响,不同生长阶段的养分利用策略差异,以及植被凋落物的累积也是土壤氮含量在火后1年和6年发生明显变化的重要原因、/sec>

  • ?nbsp; 1不同年份土壤氮含量变匕/p>

    CK代表对照样地,L代表轻度火烧样地,M代表中度火烧样地,H代表重度火烧样地,不同颜色柱形代表不同年份。在同一年份下,相同字母表示不同火强度土壤氮含量差异性不显著,不同字母代表差异性显著。下同。CK means controlled sample plots, L means light burned sample plots, M means moderate sample plots, H means heavy/severe sample plots, and different color columns represent different years. In the same year, the same letter means that the difference of soil nitrogen content with different fire intensities is not significant, different letters mean the difference is significant. The same below.

    Figure 1.Changes of soil nitrogen content in different years

    ?nbsp; 2土壤氮元素和林分因子、立地因子、可燃物因子的相关性矩阴/p>

    TN.全氮;NH4+-N.铵态氮;NO3∑/sup>-N.硝态氮;AN.碱解氮;TH.树高;Ccover.郁闭度;Slope.坡度;Position.坡位;m1h、m10h、m100h??0?00时滞可燃物含水率;l1h、l10h、l100h??0?00时滞可燃物载量,下同。TN, total nitrogen; NH4+-N, ammonium nitrogen; NO3∑/sup>-N, nitrate nitrogen; AN, alkali-hydrolysable nitrogen; TH, tree height; Ccover, canopy coverage; Slope, slope gradient; Position, slope position; m1h, m10h, m100h: the fuel moisture content of 1, 10 and 100 h; l1h, l10h, l100h: the fuel loads of 1, 10, 100 h. The same below.

    Figure 2.Correlation matrix of soil nitrogen element with stand factor, site factor and fuel factor

    ?nbsp; 3土壤氮冗余分枏/p>

    Figure 3.Soil nitrogen redundancy analysis

    ?nbsp; 2方差分析结果

    Table 2.Analysis of variance results

    指标
    Index
    全氮 TN 铵态氮 NH4+-N 硝态氮 NO3∑/sup>-N 碱解 AN
    2015 2016 2021 2015 2016 2021 2015 2016 2021 2015 2016 2021
    火强 Fire intensity (I) 0.000* 0.006* 0.202 0.000* 0.108 0.070 0.003* 0.000* 0.053 0.000* 0.197 0.066
    土层深度 Soil layer depth (La) 0.000* 0.003* 0.013* 0.000* 0.012* 0.252 0.005* 0.004* 0.284 0.000* 0.405 0.009*
    I× La 0.000* 0.629 0.980 0.000* 1.000 0.870 0.022* 0.034* 0.573 0.000* 0.513 0.934
    年份 Year (Y) 0.000* 0.000* 0.167 0.000*
    I×Y 0.007* 0.001* 0.000* 0.004*
    La ×Y 0.209 0.000* 0.055 0.003*
    I× La ×Y 0.787 0.957 0.119 0.962
    注:*表示显著影响+i>P< 0.05,加粗字体表示双因素/三因素方差分析结果显著。Notes: * means significant impact,P< 0.05. Bold font indicates significant results of two-factor/three-factor ANOVA.
    下载: 导出CSV
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    • 收稿日期:2022-01-13
    • 修回日期:2022-02-20
    • 网络出版日期:2023-02-27
    • 刊出日期:2023-03-25

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