Wang Xin, Liu Yunguo, Zeng Guangming, Chai Liyuan, Xiao Xin, Song Xiaochen, Min Zongyi
College of Environmental Science and Engineering, Hunan University, Changsha, China.
Chemosphere. 2008 Jul;72(9):1260-6. doi: 10.1016/j.chemosphere.2008.05.001. Epub 2008 Jun 16.
In southern China revegetation and ecological restoration of many abandoned Mn tailings has become a major concern. To determine the major constraints for plant establishment and evaluate the feasibility of remediation, a comparative study was conducted on Mn tailings and rhizosphere soils at the boundary of the tailings pond. Both tailings and rhizosphere soils had neutral to slightly alkaline pH and normal electrical conductivity. They were both enriched with organic matter (6.8-9.2%), total N (1.77-5.94 g kg(-1)), available P (41.78-73.83 mg kg(-1)) and K (146.7-906.9 mg kg(-1)), suggesting the tailings were a nutrient rich substrate for revegetation. Mn tailings were clay textured, while rhizosphere soils were silty loam or clay loam. The compaction and anoxic nature of Mn tailings were considered to be the major constraints for plant establishment. Total Mn (31903 mg kg(-1)), Cd (119 mg kg(-1)), Cu (126 mg kg(-1)) and Zn (2490 mg kg(-1)) in tailings were all at phytotoxic levels, but did not differ significantly from those in rhizosphere soils. In both tailings and rhizosphere soils, percentages of water- and DTPA-extractable metals were less than 1% and 2% of the total metal pools, respectively. Sequential extraction revealed that the majority of Mn, Cu and Zn were associated with the residual fraction, while the majority of Cd occurred as Fe-Mn oxides. The natural succession of plants around Mn tailings formed a distinctive metal-tolerant plant community, mainly comprising nine species such as Cynodon dactylon and Humulus scandens and so on. All species studied could be good candidates for revegetation of Mn tailings.
在中国南方,许多废弃锰尾矿的植被恢复和生态修复已成为一个主要问题。为了确定植物定植的主要限制因素并评估修复的可行性,对尾矿库边界处的锰尾矿和根际土壤进行了一项对比研究。尾矿和根际土壤的pH值均为中性至微碱性,电导率正常。它们都富含有机质(6.8 - 9.2%)、全氮(1.77 - 5.94 g kg⁻¹)、有效磷(41.78 - 73.83 mg kg⁻¹)和钾(146.7 - 906.9 mg kg⁻¹),这表明尾矿是植被恢复的富营养基质。锰尾矿质地为黏土,而根际土壤为粉质壤土或黏壤土。锰尾矿的紧实度和缺氧性质被认为是植物定植的主要限制因素。尾矿中的总锰(31903 mg kg⁻¹)、镉(119 mg kg⁻¹)、铜(126 mg kg⁻¹)和锌(2490 mg kg⁻¹)均处于植物毒性水平,但与根际土壤中的含量无显著差异。在尾矿和根际土壤中,水溶态和DTPA提取态金属的百分比分别占总金属库的不到1%和2%。连续提取表明,大部分锰、铜和锌与残渣态相关,而大部分镉以铁锰氧化物形态存在。锰尾矿周围植物的自然演替形成了一个独特的耐金属植物群落,主要包括狗牙根、葎草等9个物种。所有研究的物种都可能是锰尾矿植被恢复的良好候选物种。