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    采煤塌陷对神东矿区樟子松根系生物量及土壤水碳的影响

    Effects of coal mining subsidence on root biomass and soil water-carbon of Pinus sylvestris var. mongolica in Shendong mining area

    • 摘要:
      目的 采煤塌陷会显著改变人工林的水土环境,进而可能会引发植被退化与土壤碳库的扰动。对此进行研究,旨为揭示采煤塌陷对干旱矿区樟子松(Pinus sylvestris var. mongolica)人工林根系生物量及土壤水碳的影响。
      方法 以神东矿区典型采煤塌陷区与非塌陷区樟子松林地为研究对象,通过0 ~3 m剖面分层采样,通过对比分析的方法分析土壤水分、根系生物量与有机碳的垂直分布特征,并基于水−碳耦合协调度模型进行综合评价。
      结果 1)采煤塌陷区土壤剖面含水率为2.5%~6.5%,非塌陷区土壤剖面含水率为1.5%~5.6%,采煤塌陷显著提升0.6~1.8 m土壤含水率。2)塌陷扰动诱导樟子松根系向深层增殖,根系生物量密度较非塌陷区显著增加,驱动深层土壤有机碳质量分数提升,但浅层土壤因结构破坏导致有机碳损失。3)耦合协调度(D)模型显示,采煤塌陷使得0.8 ~ 2.6 m土层的水−碳耦合协调度由失调衰败状态(D < 0.4)提升至过度发展阶段(0.4≤ D < 0.6),整体系统协调度从0.40增至0.47,有利于土壤水−碳耦合协调发展。
      结论 研究表明,采煤塌陷具有“深层增储增效”的生态正效应,可为干旱矿区人工林可持续管理与生态修复提供依据。

       

      Abstract:
      Objective Coal mining subsidence can significantly alter the hydrological and soil environment of artificial forests, which may in turn trigger vegetation degradation and disturbance of the soil carbon pool.
      Methods To reveal the impact of coal mining subsidence on the root biomass and soil water-carbon in the artificial forest of Pinus sylvestris var. mongolica in arid mining areas, this study took the P. sylvestris var. mongolica plantations in the typical coal mining subsidence area and the non-subsidence area of the Shendong mining area as the research objects. Through stratified sampling of the 0–3 m soil profile, the vertical distribution characteristics of soil moisture, root biomass, and organic carbon were analyzed, and a comprehensive evaluation was carried out based on the water-carbon coupling coordination degree model.
      Results 1) The soil profile water content in the coal mining subsidence area was 2.5%−6.5%, and that in the non-subsidence area was 1.5%−5.6%. Coal mining subsidence significantly increased the water content at depths of 0.6−1.8 m. 2) The subsidence disturbance induced the proliferation of P. sylvestris var. mongolica roots into deep layers, and the root biomass density increased significantly compared with that in the non-subsidence area, which drove the increase of the mass fraction of organic carbon in the deep soil. However, the organic carbon in the shallow soil was lost due to the structural damage. 3) The coupling coordination degree model showed that coal mining subsidence increased the water-carbon coupling coordination degree of the 0.8−2.6 m soil layers from the disorderly decline state (D < 0.4) to the excessive development stage (0.4 ≤ D < 0.6), and the overall system coordination degree increased from 0.40 to 0.47, which was beneficial to the coordinated development of soil water-carbon coupling.
      Conclusions This study shows that coal mining subsidence has a positive ecological effect of "increasing storage and efficiency in the deep layer", providing a scientific basis for the sustainable management of artificial forests and ecological restoration in arid mining areas.

       

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