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Arsenic Speciation: Involvement in Evaluation of Environmental Impact Caused by Mine Wastes
Author(s) -
Roussel Christophe,
Bril Hubert,
Fernandez Angel
Publication year - 2000
Publication title -
journal of environmental quality
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.888
H-Index - 171
eISSN - 1537-2537
pISSN - 0047-2425
DOI - 10.2134/jeq2000.00472425002900010023x
Subject(s) - arsenic , arsenite , genetic algorithm , environmental chemistry , particulates , arsenate , lepidocrocite , pollutant , extraction (chemistry) , tailings , metalloid , groundwater , chemistry , environmental science , environmental engineering , goethite , metal , geology , adsorption , geotechnical engineering , organic chemistry , chromatography , evolutionary biology , biology
Since large areas have been contaminated by arsenic‐rich industrial and mining by‐products in several countries, knowledge of arsenic (As) behavior in soils and water is of major concern for reclamation of polluted sites and evaluation of environmental risk. Cheni's tailings (France) contains average concentrations up to 7000 mg kg −1 As and was listed by the authority as an important potentially pollutant site. Because As speciation determines its mobility, it was investigated in surface and ground waters of the site and a study of the solid As‐bearing phase was performed on suspended particulate material (SPM). Results of sequential extraction, carried out on the SPM collected in drainage waters, show that most of total extracted As (78%) and Fe (77%) is bound to an iron hydrous oxide phase, which was determined to be lepidocrocite (γ‐FeOOH) by x‐ray diffraction and infrared spectrometry. Particulate material was >220 times more concentrated than dissolved As. Conditions for the stability of dissolved (<0.45 µm) arsenite [As(III)] and arsenate [As(V)] are discussed on the basis of thermodynamical data and field measurements of pH and redox potentials. The theoretical stability of As(V) corresponds to a large association between As and particulate material, and large amounts of the metalloid are released in solution when As‐rich particles come from oxidized ground waters to moderately reduced conditions. These results are important for evaluating, modeling, and rehabilitating As‐polluted sites.