镁铁锰锆四元类水滑石钝化修复锑污染黄壤研究
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X53;P579

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国家自然科学基金项目(42267009); 贵州省地质矿产勘查开发局地质科研项目(〔2023〕10 号)


Passivation remediation of antimony-contaminated yellow soil by magnesium- iron-manganese-zirconium quaternary hydrotalcites
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    摘要:

    为研究镁铁锰锆四元类水滑石(MgFeMnZr-LDH)对锑(Sb)污染土壤的钝化修复效果,将MgFeMnZr-LDH添加到Sb含量为1 450 mg/kg的黄壤中进行45 d淹水培育,采用NaH2PO4、Na2HPO4和乙二胺四乙酸(EDTA)提取土壤有效态Sb(Ⅲ)和Sb(Ⅴ),采用Wenzel连续提取法提取土壤中不同形态Sb(Ⅲ)和Sb(Ⅴ),讨论了MgFeMnZr-LDH添加量、土壤有效态Sb和各形态Sb的相关性,探究了MgFeMnZr-LDH对土壤Sb的钝化机理。结果显示,随着MgFeMnZr-LDH添加量的逐渐增加,Na2HPO4、NaH2PO4和EDTA提取的有效态总Sb含量均逐渐下降,最大下降率分别为26.5%、25.2%和35.5%,而且有效态Sb(Ⅲ)占比也逐渐降低;土壤中Sb(Ⅲ)和Sb(Ⅴ)的非专性吸附态(F1)、专性吸附态(F2)、无定形铁铝氧化物结合态(F3)含量均大幅下降,晶形铁铝氧化物结合态(F4)含量大幅增加,F3和F4占比变化幅度最大;材料添加量与土壤中Sb(Ⅲ)和Sb(Ⅴ)的F1、F2、F3呈极显著负相关,与F4呈极显著正相关,与残渣态Sb(Ⅲ)(F5)呈显著正相关。研究结果显示,MgFeMnZr-LDH通过静电、离子交换、配位、沉淀和氧化作用将土壤中Sb的F1、F2、F3逐渐转化为F4、F5,降低了Sb的生物有效性,实现了Sb污染土壤的钝化修复。

    Abstract:

    In order to study the effect of magnesium-iron-manganese-zirconium quaternary hydrotalcite (MgFeMnZr-LDH) on the passivation remediation of antimony (Sb)-contaminated soils, MgFeMnZr-LDH was added to the yellow soil with a Sb content of 1 450 mg/kg and for 45 d of flooding, and NaH2PO4, Na2HPO4 and ethylenediaminetetraacetic acid (EDTA) were used to extract soil available Sb(Ⅲ) and Sb(Ⅴ); different forms of Sb(Ⅲ) and Sb(Ⅴ) in soil were extracted by Wenzel sequential extraction procedure; the correlation between the addition of MgFeMnZr-LDH, soil available Sb and different forms of Sb were discussed, and the passivation mechanism of MgFeMnZr-LDH on soil Sb was explored. The results showed that with the increase of MgFeMnZr-LDH addition, the total content of available Sb extracted by Na2HPO4, NaH2PO4 and EDTA gradually decreased, with maximum reduction rates of 26.5%, 25.2%, and 35.5%, respectively, in which the percentage of available Sb(Ⅲ) also decreased gradually; soil content of Sb (Ⅲ) and Sb(Ⅴ) decreased significantly in the non-specifically adsorption state(F1), the specifically adsorption state(F2), and the amorphous iron and aluminium oxide-bound state(F3), and increased significantly in the crystallized iron and aluminium oxide-bound state(F4); F3 and F4 had the largest variation in percentage. The material additions showed highly significant negative correlation with F1, F2, F3 of Sb(Ⅲ) and Sb(Ⅴ), highly significant positive correlation with F4 of Sb(Ⅲ) and Sb(Ⅴ), and significant positive correlation with the residual phases Sb(Ⅲ)(F5)in the soils. MgFeMnZr-LDH gradually transformed F1, F2 and F3 of Sb in soils into F4 and F5 through electrostatic, ion exchange, coordination, precipitation and oxidation, which reduced the bioeffectiveness of Sb and realized the passivation remediation of Sb-contaminated soil.

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钟佳祺,朱霞萍,任维,等, 2025. 镁铁锰锆四元类水滑石钝化修复锑污染黄壤研究[J]. 岩石矿物学杂志, 44(5):1246~1256.
ZHONG Jia-qi, ZHU Xia-ping, REN Wei, et al, 2025. Passivation remediation of antimony-contaminated yellow soil by magnesium- iron-manganese-zirconium quaternary hydrotalcites[J]. Acta Petrologica et Mineralogica, 44(5): 1246~1256.

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  • 收稿日期:2024-11-02
  • 最后修改日期:2025-06-03
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  • 在线发布日期: 2025-09-25
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