4.5 Article

Effect of hydroquinone-induced iron reduction on the stability of Fe(III)-As(V) Co-precipitate and arsenic mobilization

期刊

APPLIED GEOCHEMISTRY
卷 97, 期 -, 页码 1-10

出版社

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.apgeochem.2018.07.017

关键词

Fe(III)-As(V) co-precipitate; Iron reduction; Arsenic mobilization; Stability

资金

  1. National Natural Science Foundation of China [41530643, 41673130, 41703133, 41473111]
  2. Chinese Academy of Sciences [QYZDJ-SSW-DQC038]

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Long-term storage of Fe(III)-As(V) co-precipitate wastes derived from the industrial As removal process poses the risk of secondary arsenic pollution to the local environment. However, its stability in only iron-reducing environment remains unclear. The effect of iron reduction by hydroquinone (QH(2)) on the stability of co-precipitate at Fe/As molar ratio of 5 was investigated in this study. The results showed that 16.5-93% of Fe(III) reduction in NaOH-neutralized co-precipitate caused 0.1-11% (0.1-8.5 mg L-1) As release and 0.9-46% (2.6-130 mg L-1) Fe (II) release at pH 4 and 6. Most of the As(V) and more than half of the Fe(II) generated by the reductive decomposition of Fe(III)-As(V) co-precipitate were retained in solid phases. Solid characterization and thermodynamic calculation indicated that amorphous Fe-3(AsO4)(2) was probably the major secondary mineral for As immobilization. At pH 8, 11-39% As and less than 4% Fe(II) were released into solution after 3.6-87% Fe(III) was reduced to Fe(II). Both amorphous Fe-3(AsO4)(2) and Fe(II, III) (hydr) oxides were responsible for As retention. The solubility of NaOH-neutralized co-precipitates in terms of dissolved As concentration upon Fe(III) reduction at pH 4, 6 and 8 with QH(2)/Fe(III) mol of 1 was lower than that in oxic environment. It was also lower than the solubility of Ca(OH)(2)-neutralized co-precipitate after Fe(III) reduction at pH 4 and 6.

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