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矿渣-粉煤灰重构土壤中添加污泥和丛枝菌根真菌后 6 年的有机碳、团聚体和酶活性变化。

Variations in organic carbon, aggregation, and enzyme activities of gangue-fly ash-reconstructed soils with sludge and arbuscular mycorrhizal fungi during 6-year reclamation.

机构信息

School of Environment and Spatial Informatics, China University of Mining & Technology, No. 1, Daxue Road, Xuzhou, Jiangsu, 221116, China.

Department of Civil and Environmental Engineering, The Hong Kong University of Science and Technology, New Territories, Hong Kong.

出版信息

Environ Sci Pollut Res Int. 2016 Sep;23(17):17840-9. doi: 10.1007/s11356-016-6941-5. Epub 2016 Jun 1.

Abstract

Mining activities can cause drastic disturbances in soil properties, which adversely affect the nutrient cycling and soil environment. As a result, many efforts have been made to explore suitable reclamation strategies that can be applied to accelerate ecology restoration. In this study, we reconstructed mine soils with fly ash, gangue, sludge, planted ryegrass, and inoculated arbuscular mycorrhizal fungi (AMF) in Pangzhuang mine of Xuzhou during 2009 to 2015. The soil aggregation process, enzyme activities (i.e., invertase, urease and acid phosphatase activities), soil organic carbon (SOC) as well as other soil nutrients such as nitrogen, phosphorus, and potassium contents of the reconstructed mine soils were monitored during 6-year reclamation. The integrated application of sludge and AMF led to a promising reclamation performance of mining areas, in which soil aggregate stability, enzyme activities, SOC, and ryegrass biomass were effectively enhanced. The micro-aggregates (< 0.25 mm) decreased with the increase of macro-aggregates (> 0.25 mm) during the reclamation, indicating that macro-aggregates were gradually formed from micro-aggregates during the pedogenesis of reconstructed mine soils. The correlation analysis shows that SOC contents in aggregate fraction of 0.25∼0.5 mm were correlated with aggregate distribution and enzyme activities. Enzyme activities, however, were not significantly correlated with aggregate distribution. The outcomes from the present study could enrich our understanding on soil property changes in pedogenesis process of reconstructed mine soils, and meanwhile, the employment of sludge combined with AMF is suggested to be an effective alternative for the mine soil reclamation.

摘要

采矿活动会对土壤性质造成剧烈干扰,从而对养分循环和土壤环境产生不利影响。因此,人们已经做了很多努力来探索合适的复垦策略,以加速生态恢复。在本研究中,我们在 2009 年至 2015 年期间,采用粉煤灰、煤矸石、污泥、黑麦草种植和接种丛枝菌根真菌(AMF)对徐州庞庄矿的废弃土壤进行了重构。在 6 年的复垦过程中,监测了重构废弃土壤的土壤团聚体过程、酶活性(即转化酶、脲酶和酸性磷酸酶活性)、土壤有机碳(SOC)以及氮、磷、钾等其他土壤养分含量。污泥和 AMF 的综合应用为矿区的复垦提供了有希望的效果,有效提高了土壤团聚体稳定性、酶活性、SOC 和黑麦草生物量。在复垦过程中,随着大团聚体(>0.25mm)的增加,微团聚体(<0.25mm)减少,表明在重构废弃土壤的成土过程中,大团聚体逐渐从小团聚体形成。相关分析表明,0.25∼0.5mm 团聚体中 SOC 含量与团聚体分布和酶活性相关。然而,酶活性与团聚体分布没有显著相关性。本研究的结果可以丰富我们对重构废弃土壤成土过程中土壤性质变化的认识,同时建议采用污泥与 AMF 结合的方法作为废弃土壤复垦的有效替代方法。

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