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小兴安岭林下植被及幼树碳储量分布及模型构建

Distribution and Modelling of Carbon Stocks in Understorey Vegetation and Young Trees in the Xiaoxing'an Mountains Forests

  • 摘要: 根据嘉荫县2021年调查的林下植被调查数据,计算林下植被生物量,实测各物种含碳率,计算各样地的碳储量和碳密度,分析林下植被层碳储量分配情况。运用反距离插值和重分类工具,制作嘉荫县林下植被碳储量和碳密度的空间分布格局图。对研究区草本层碳储量和主要林分类型的灌木及幼树层碳储量与各因子进行逐步回归分析,构建嘉荫县灌木及幼树层、草本层碳储量模型。结果表明:嘉荫县林下植被层碳储量为282245.023 t,平均碳密度为0.437 t/hm2,其中灌木及幼树层碳储量占 91.65%,草本层碳储量占8.35%。林下植被层碳储量主要受灌木及幼树层影响,受草本影响较小。在空间分布上,灌木及幼树层高碳密度分布区域的海拔均高于300 m;草本层碳储量高密度区域集中分布在海拔153~474 m;林下植被层碳储量与灌木及幼树层分布一致。林下植被层碳储量和碳密度随海拔升高先增加后减少,碳密度在海拔500~600 m时达到最高0.8956 t/hm2。不同海拔林下植被碳储量大小顺序:丘陵区>低山区>平原区;碳密度的大小顺序:低山区>丘陵区>平原区。得到最优草本层碳储量模型拟合R2为 0.400,因子间不存在共线性;6种主要林分类型最优灌木及幼树碳储量模型,模型拟合R2最低为0.534,最高为0.929,各因子间均不存在共线性。

     

    Abstract: According to the understory vegetation data surveyed in Jiayin County in 2021, the understory vegetation biomass was calculated, the carbon content of each species was measured, the carbon reserves and carbon density of various places were calculated, and the allocation of carbon reserves in the understory vegetation layer was analyzed. The reverse distance interpolation and reclassification tools were used to make the spatial distribution pattern map of the carbon reserves and carbon density of the understory vegetation in Jiayin County. The progressive regression analysis of the carbon reserves and the carbon reserves of shrubs and young layers in Jiayin County: The carbon reserves of understvegetation layer in Jiayin County is 282245.023 t, and the average carbon density is 0.437 t/hm2, among which the carbon reserves of shrub and young layer account for 91.65%, and the carbon reserves of herbaceous layer account for 8.35%. The carbon reserve of understory vegetation layer is mainly affected by shrubs and young trees, but less affected by herbs. In terms of spatial distribution, the altitude of high carbon density in shrub and young layer is above 300 m; the area of high carbon density in herbaceous layer is concentrated at 153-474 m; the carbon reserve in understory vegetation layer is consistent with that of shrubs and young layer. The carbon reserves and carbon density in the understory vegetation layer first increased and then decreased with the altitude, and the carbon density reached 0.8956 t / hm 2 at the altitude of 500-600 m. Order of carbon reserves under different altitude forests: hilly area> low mountainous area> plain area; order of carbon density: low mountainous area> hilly area> plain area. If the optimal herb layer carbon storage model was 0.400, there is no collinearity among factors; for the carbon storage model of optimal shrubs and saplings of 6 main forest types, the lowest model fitting R2 was 0.534 and the highest was 0.929, and there is no collinearity among all factors.

     

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