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Multiple Isotopes (Fe, S and C) to Reveal the Co-oxidation Mechanism of Fe(Ⅱ)-Sb(Ⅲ) in High Antimony Groundwater
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Jun-mei ZHAO1, Ya-ping LIU1, Wei-jiao LI1, Zi-yao LI1, Tao-li MU1, Chun-ming HAO2, Hui-jun DONG1, *
Science Technology and Engineering | 2025, 25(17) : 7430 - 7438
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Science Technology and Engineering | 2025, 25(17): 7430-7438
Papers-Environmental and Safe Science
Multiple Isotopes (Fe, S and C) to Reveal the Co-oxidation Mechanism of Fe(Ⅱ)-Sb(Ⅲ) in High Antimony Groundwater
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Jun-mei ZHAO1, Ya-ping LIU1, Wei-jiao LI1, Zi-yao LI1, Tao-li MU1, Chun-ming HAO2, Hui-jun DONG1, *
Affiliations
  • 1 Hebei Key Laboratory of Geological Resources and Environment Monitoring and Protection, Hebei Geological Environment Monitoring, Shijiazhuang 050021, China
  • 2 School of Mines Safety, North China Institute of Science and Technology, Sanhe 065201, China
Published: 2025-06-18 doi: 10.12404/j.issn.1671-1815.2406106
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The oxidation of Sb(III) occurred rapidly in aerobic and dark groundwater environments, with previous studies suggesting that co-oxidation of Fe(II) and Sb(III) may be the predominant driving mechanism. However, there is a lack of field evidence confirming environmental isotope fractionation. Therefore, 20 groups of Magunao aquifer (${\mathrm{Dx}}_{3}^{4}$ water) samples were collected from the North mine of Xikuangshan antimony mining area in Hunan Province to compare the differences in environmental isotopes (δ56Fe, δ13C, and δ34S) between high- and low-Sb groundwater and investigate the fractionation process of these isotopes. The results reveal that total Sb(TSb) concentrations ranged from 5.30 μg/L to 20 700 μg/L, with a mean concentration of 3 660.61 μg/L. Additionally, Sb(V) is found to be the most dominant valence state for Sb in ${\mathrm{Dx}}_{3}^{4}$ water. The neutral-alkaline and oxygen-enriched conditions in ${\mathrm{Dx}}_{3}^{4}$ water facilitate the co-oxidation of FeS2 and Sb2S3, as well as induce fractionation of δ18${\mathrm{O}}_{\mathrm{S}{\mathrm{O}}_{4}}$, δ34${\mathrm{S}}_{\mathrm{S}{\mathrm{O}}_{4}}$and δ56Fe between sediments and groundwater, resulting in the increase of $\mathrm{S}{\mathrm{O}}_{4}^{2-}$,total Fe (TFe) and Sb(Ⅴ) contents in high Sb groundwater. Furthermore, microbial activities promote the oxidative decomposition of organic carbon, thereby enhancing the co-oxidation rate of Fe(Ⅱ) and Sb(Ⅲ). This conclusion unveils a novel mechanism for aerobic oxidation of Sb(III) in dark groundwater environments while providing a scientific foundation for advancing our understanding of the Sb geochemical cycle and preventing environmental pollution from high Sb groundwater.

multiple isotopes  /  co-oxidation of Fe(II) and Sb(III)  /  oxidative decomposition of organic carbon  /  Sb(Ⅴ)  /  high-Sb groundwater
Jun-mei ZHAO, Ya-ping LIU, Wei-jiao LI, Zi-yao LI, Tao-li MU, Chun-ming HAO, Hui-jun DONG. Multiple Isotopes (Fe, S and C) to Reveal the Co-oxidation Mechanism of Fe(Ⅱ)-Sb(Ⅲ) in High Antimony Groundwater[J]. Science Technology and Engineering, 2025 , 25 (17) : 7430 -7438 . DOI: 10.12404/j.issn.1671-1815.2406106
Year 2025 volume 25 Issue 17
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doi: 10.12404/j.issn.1671-1815.2406106
  • Receive Date:2024-08-15
  • Online Date:2025-12-15
  • Published:2025-06-18
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  • Received:2024-08-15
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    1 Hebei Key Laboratory of Geological Resources and Environment Monitoring and Protection, Hebei Geological Environment Monitoring, Shijiazhuang 050021, China
    2 School of Mines Safety, North China Institute of Science and Technology, Sanhe 065201, China
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表12种不同金属材料的力学参数

Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)

Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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