不同植被恢复模式下煤矸石充填复垦土壤物理性质与有机无机复合体的关系

目的]揭示复垦土壤物理性质与有机无机复合体的关系,为改善复垦土壤的物理特性提供依据。方法]选择淮南大通煤矸石充填复垦区三种典型植被恢复模式下人工恢复7a的土壤,定量分析其物理性质及有机无机复合体,并运用多元统计分析两者的关系。结果]研究区土壤的有机无机复合状况及结合态腐殖质在不同植被恢复下发生了不同程度的变化。结合态腐殖质以稳结态为主,所占比例为41%~67%。植被恢复降低了复垦土壤的容重而增加了其总孔隙度,而且臭椿+草本恢复模式效果最佳。土壤非毛管孔隙度与有机无机复合量及紧结态/重组碳呈显著正相关,而与稳结态/重组碳呈显著负相关。毛管孔隙度与有机无机复合量及紧结态/重组碳呈显著负相关,而与稳结态/重组碳呈显著正相关。土壤总孔隙度及容重与结合态腐殖质各组分的绝对含量分别呈显著正相关和负相关关系。结论]复垦土壤物理性质与有机无机复合体具有密切关系。

Relationship Between Physical Properties and Organic-mineral Complexes of Reclaimed Soil Back-filled with Coal Gangue Under Various Vegetation Restoration Models

Objective] Clarifying the relationship between physical properties and organic-mineral complexes of reclaimed soil was supposed to provide a support for ameliorating the reclaimed soil physical condition.Methods] This study chose the soil under three patterns of typical artificial vegetation restoration for seven years in Datong Reclamation District of Huainan City, which had been back-filled with coal gangue. Soil physical indictors and formations of organic-mineral complexes were quantified using standard procedures, and their relationship was determined by multivariate statistical analysis.Results] Soil organic-mineral status and the combined humus varied with different vegetation restoration patterns in the survey region. The stably-combined humus dominated, and it accounted for 41%~67% of combined humus. Vegetation restoration lowered oil bulk density and increased total porosity significantly in contrast with that of natural soil. These effects were more obvious in the mixed plantation pattern of Ailanthus altissima and grass. Soil non-capillary porosity had significantly positive correlations with the amount of organic-mineral complexes and the ratio of tightly-combined humus to combined humus; however, a negative correlation was found of it with the ratio of stably-combined humus to combined humus. Soil capillary porosity was negatively and significantly correlated with the amount of organic-mineral complexes and the ratio of tightly-combined humus to combined humus; and was positive and significantly correlated with the ratio of stably-combined humus to combined humus. Positive association existed between contents of three fractions of soil combined humus, and total porosity and negative correlation it was between the combined contents and low bulk density.Conclusion] The physical condition showed strong correlations with organic-mineral complexes in reclaimed soils.