Chromium Immobilization as Cr-Spinel by Regulation of Fe(II) and Fe(III) Concentrations

被引:0
作者
Hua, Tianci [1 ,2 ]
Li, Yanzhang [1 ,2 ]
Hou, Bingxu [1 ,2 ]
Du, Yimei [1 ,2 ]
Lu, Anhuai [1 ,2 ]
Li, Yan [1 ,2 ]
机构
[1] Peking Univ, Sch Earth & Space Sci, Key Lab Orogen Belts & Crustal Evolut, Beijing 100871, Peoples R China
[2] Peking Univ, Sch Earth & Space Sci, Beijing Key Lab Mineral Environm Funct, Beijing 100871, Peoples R China
基金
中国国家自然科学基金;
关键词
chromium pollution; Cr-spinel; stoichiometric ratio; mineralization; PHOTOCATALYTIC REDUCTION; HEXAVALENT CHROMIUM; AQUEOUS-SOLUTION; OXIDATION; CR(VI); SOLUBILITY; SORPTION; CR(III); REMOVAL; BIOTITE;
D O I
10.3390/min14101024
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 complex environmental conditions at Cr-contaminated sites, characterized by uneven ion distribution, oxidants competition, and limited solid-phase mobility, lead to inadequate mixing of Fe-based reducing agents with Cr, posing significant challenges to the effectiveness of Cr remediation through Cr-spinel precipitation. This study investigates the distinct roles of Fe(II), Fe(III), and Cr(III) in Cr-spinel crystallization under ambient temperature and pressure. X-ray diffraction, scanning electron microscopy, transmission electron microscopy, X-ray absorption near-edge structure spectroscopy, and M & ouml;ssbauer spectroscopy were employed to elucidate the phase composition, microstructure, and ion coordination within the precipitates. Our findings indicate that Fe(II) acts as a catalyst in the formation of the spinel phase, occupying octahedral sites within the spinel structure. Under the catalytic influence of Fe(II), Fe(III) transitions into the spinel phase, occupying both the tetrahedral and the remaining octahedral sites. Meanwhile, Cr(III), due to its high octahedral site preference energy, preferentially occupies the octahedral sites. When Fe(II) or Fe(III) is present but does not meet the ideal stoichiometric ratio, a deficiency in Fe(II) leads to low yield and poor crystallinity of Cr-spinel, whereas a deficiency in Fe(III) can completely inhibit its formation. Conversely, when either Fe(II) or Fe(III) is in excess, the formation of Cr-spinel remains feasible. Furthermore, metastable Cr phases can be transformed into stable Cr-spinel by adjusting the Fe(II)/Fe(III)/Cr(III) ratio. These results highlight the broad range of conditions under which Cr-spinel mineralization can occur in environmental settings, enhancing our understanding of the mechanisms driving Cr-spinel formation in Cr-contaminated sites treated with Fe-based reducing agents. This research provides critical insights for optimizing Cr remediation strategies.
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页数:12
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