Vegetation and soil restoration in refuse dumps from open pit coal mines

被引:129
作者
Huang Lei [1 ,2 ]
Zhang Peng [1 ,2 ]
Hu Yigang [1 ,2 ]
Zhao Yang [1 ,2 ]
机构
[1] Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Shapotou Desert Res & Expt Stn, Lanzhou 730000, Peoples R China
[2] Key Lab Stress Physiol & Ecol Cold & Arid Reg, Lanzhou 730000, Gansu, Peoples R China
关键词
Refuse dumps; Open pit coal mine; Chronosequence; Recovery rate; Ecological restoration; ECOLOGICAL RESTORATION; TENGGER DESERT; MINING AREAS; PHYSICOCHEMICAL PROPERTIES; SHANXI PROVINCE; ECOSYSTEM; SUCCESSION; RECLAMATION; ENVIRONMENT; ENVELOPE;
D O I
10.1016/j.ecoleng.2016.06.108
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Because the exploitation of mineral resources has resulted in the destruction of vast amounts of land and caused serious environmental problems, ecological restoration and mine reclamation have become important components of the sustainable development strategies of many countries. In this study, the changes in plant species diversity and succession of soil physicochemical properties were studied in revegetated refuse dumps of varying ages (1995, 1998, 2003, 2005 and 2014) and an undisturbed reference site of the Heidaigou opencast coal mine, which is located in the Inner Mongolia Autonomous Region, China. In addition, based on the space-for-time substitution approach, the rate and extent of recovery of the vegetation and soil characteristics in the above long-term chronosequence were estimated. The results showed that opencast mining revegetation have a positive effect on environmental restoration. The total species number and the richness, coverage and biomass of herbaceous species increased significantly with increasing site age. However, for shrub species, an initial increase was observed over a period of 10 years and then followed by a subsequent decrease. The mean soil water content in the oldest vegetated areas (1995 site, 2.3-5.9%) was significantly greater than in the younger vegetated areas (e.g., 2014 site, 1.1-2.5%) in the shallow layer (0-60 cm); however, in the deeper layers (60-200 cm), the mean soil water content in the oldest vegetated areas (4.2-8.1%) was significantly lower than in the younger vegetated areas (5.1-12.5%). The proportions of silt and clay, depth of topsoil and biological soil crusts, and concentrations of soil organic C, K, total N, and total P increased with the years since revegetation. The estimated time required for plant traits and soil properties in the revegetated site to reach the same levels as in the reference site was between 23 and 25 years. These results suggest that soil recovery and vegetation recovery are equally important in eco-restoration activities in semiarid areas, and the conservation of soil and vegetation habitat is therefore a crucial issue for land managers. (C) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:638 / 646
页数:9
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