淮南潘一矿区煤矸石山复垦区不同重构层次基质大孔隙特征

    Characteristics of macropores in different reconstructed matrix layers in the coal gangue reclamation area of Panyi Mine, Huainan

    • 摘要: 煤矿复垦区在施工过程中受机械碾压和扰动影响,土壤原有结构和剖面层次遭到破坏,重构土壤生产力难以恢复至原状土壤水平,常出现植被恢复初期良好而后期退化的问题。大孔隙是土壤水分和空气流通的重要通道,对土壤的物理、化学和生物过程具有显著影响。通过定性与定量相结合的方法分析复垦区不同重构层次基质大孔隙特征,有助于识别重构土壤关键层,优化复垦工艺设计。本研究采用工业CT扫描技术,对潘一矿不同重构层次土壤样品进行三维成像,以原状土壤为对照,结合VG Studio Max软件开展数字图像定量分析。研究结果表明:不同重构层中大孔隙的主要分布范围较为一致,但在Ø>10 mm的孔径范围内,覆土和煤矸石层的孔隙贡献率分别达90.83%和97.80%,显著高于原状土和泥矸混合土。覆土层在植被根系和外界环境作用下形成孔隙-裂隙网络,入渗条件改善,但比表面积降低使得持水与固土效应受限。泥矸混合土层孔隙结构分布均匀、比表面积适中,具备良好的蓄水能力,是复垦剖面中的典型蓄水功能层;煤矸石层因含有大量碎块物质,孔隙集中分布,连通性强但比表面积较小,整体蓄水性能较差。建议煤矸石充填前应充分破碎,提高孔隙结构均匀性;在表层优先种植浅根型草本植物增强稳固性,并避开汛期开展种植作业,降低水蚀风险。研究成果可为煤矸石复垦区土壤结构优化与施工工艺改进提供技术支撑。

       

      Abstract: The coal mine reclamation area is affected by mechanical compaction and disturbance during the construction process, the original structure and sectional hierarchy of the soil have been destroyed, reconstructing soil productivity is difficult to restore to the original soil level, and there is often a problem of good vegetation restoration in the early stage but degradation in the later stage. Macropores are important channels for soil moisture and air circulation, and have a significant impact on the physical, chemical, and biological processes of soil. By combining qualitative and quantitative methods to analyze the characteristics of macropores at different reconstruction matrix levels in reclamation areas, it is helpful to identify key layers of reconstructed soil and optimize the design of reclamation processes. This study uses industrial computed tomography (CT) scanning to create three-dimensional images of soil samples from various reconstructed layers in the Panyi Mine. The original soil is used as a control and digital image quantitative analysis is carried out using VG Studio Max software. The research results show the main distribution range of macropores in different reconstruction layers is relatively consistent, but within the bore range of Ø>10 mm, the pore contribution rates of the overlying soil and coal gangue layer reach 90.83% and 97.80%, respectively, which are significantly higher than those of the original soil and the mixed soil of mud and gangue. The topsoil layer develops a pore–fissure network driven by plant roots and environmental factors. This network enhances infiltration but reduces specific surface area, which in turn constrains the soil’s water-retention and stabilization capacity. The pore structure of the mixed soil layer of mud and gangue is evenly distributed, with a moderate specific surface area and good water storage capacity, making it a typical water storage functional layer in the reclamation profile. The coal gangue layer contains a large amount of fragmented material, with concentrated pores and strong connectivity, but with a small specific surface area, resulting in poor overall water storage performance. It is recommends that coal gangue be fully crushed before filling to improve the uniformity of pore structure; prioritize planting shallow rooted herbaceous plants on the surface to enhance stability, and avoid planting operations during flood season to reduce the risk of water erosion. The research results can provide technical support for optimizing soil structure and improving construction technology in coal gangue reclamation areas.

       

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