Mobilisation of arsenic from bauxite residue (red mud) affected soils: Effect of pH and redox conditions

被引:51
|
作者
Lockwood, Cindy L. [1 ]
Mortimer, Robert J. G. [1 ]
Stewart, Douglas I. [2 ]
Mayes, William M. [3 ]
Peacock, Caroline L. [1 ]
Polya, David A. [4 ,5 ]
Lythgoe, Paul R. [4 ,5 ]
Lehoux, Alizee P. [1 ]
Gruiz, Katalin [6 ]
Burke, Ian T. [1 ]
机构
[1] Univ Leeds, Sch Earth & Environm, Leeds LS2 9JT, W Yorkshire, England
[2] Univ Leeds, Sch Civil Engn, Leeds LS2 9JT, W Yorkshire, England
[3] Univ Hull, Ctr Environm & Marine Sci, Scarborough YO11 3AZ, N Yorkshire, England
[4] Univ Manchester, Sch Earth Atmospher & Environm Sci, Manchester, Lancs, England
[5] Univ Manchester, Williamson Res Ctr Mol Environm Sci, Manchester, Lancs, England
[6] Budapest Univ Technol & Econ, Dept Appl Biotechnol & Food Sci, H-1111 Budapest, Hungary
基金
英国自然环境研究理事会;
关键词
DISSIMILATORY REDUCTION; REDUCING BACTERIUM; AQUEOUS-SOLUTIONS; BAYER PROCESS; SODA LAKES; SEDIMENTS; HUNGARY; METALS; WASTE; WATER;
D O I
10.1016/j.apgeochem.2014.10.009
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The tailings dam breach at the Ajka alumina plant, western Hungary in 2010 introduced similar to 1 million m(3) of red mud suspension into the surrounding area. Red mud (fine fraction bauxite residue) has a characteristically alkaline pH and contains several potentially toxic elements, including arsenic. Aerobic and anaerobic batch experiments were prepared using soils from near Ajka in order to investigate the effects of red mud addition on soil biogeochemistry and arsenic mobility in soil-water experiments representative of land affected by the red mud spill. XAS analysis showed that As was present in the red mud as As(V) in the form of arsenate. The remobilisation of red mud associated arsenate was highly pH dependent and the addition of phosphate to red mud suspensions greatly enhanced As release to solution. In aerobic batch experiments, where red mud was mixed with soils, As release to solution was highly dependent on pH. Carbonation of these alkaline solutions by dissolution of atmospheric CO2 reduced pH, which resulted in a decrease of aqueous As concentrations over time. However, this did not result in complete removal of aqueous As in any of the experiments. Carbonation did not occur in anaerobic experiments and pH remained high. Aqueous As concentrations initially increased in all the anaerobic red mud amended experiments, and then remained relatively constant as the systems became more reducing, both XANES and HPLC-ICP-MS showed that no As reduction processes occurred and that only As(V) species were present. These experiments show that there is the potential for increased As mobility in soil-water systems affected by red mud addition under both aerobic and anaerobic conditions. (C) 2014 The Authors. Published by Elsevier Ltd.
引用
收藏
页码:268 / 277
页数:10
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