Dual role of microbe-FexSy interaction to drive perfluorooctanoic acid multi-path chain reaction decay cycles and secondary minerals-ions (Fe2+/Fe3+) transformation cycles
ID:2470 View Protection:ATTENDEE Updated Time:2024-04-12 13:16:43 Hits:1871 Oral Presentation

Start Time:2024-05-19 14:30(Asia/Shanghai)

Duration:10min

Session:S2 主题2、地球化学 » S2-3主题2、地球化学 专题2.8、专题2.4(19日下午,4F观海厅1)

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Abstract
The coexistence of iron-sulfur minerals (FexSy) and microorganisms is a common phenomenon, often leading to intricate and multifaceted interactions. Perfluorooctanoic acid (PFOA) presents extensive transport and spatial-temporal attenuation characteristics. However, the transport and attenuation mechanism governing PFOA in diverse PFOA-ions occurrence environments, specifically in conjunction with microbe-mineral interaction, remains unclear. In this study, the effects difference between microbe/FexSy (pyrite (FeS2) and pyrrhotite (Fe1−nS)) and microbe-FexSy interaction media on PFOA, and specific effects of four PFOA-ions occurrence environments on PFOA considering microbe-FexSy interaction were investigated. A microbe-FexSy interaction-induced multi-process reaction model was constructed to quantitatively describe influential effects. Results showed a remarkable 277% increase in PFOA attenuation rate (λ) in microbe-FexSy interaction media (0.343 h-1) than in alone FexSy (0.091 h-1). The ions inhibiting effect on PFOA attenuation was demonstrated (λ from 0.343 to 0.159 h-1), with the maximum effect in HCO3-. It can be attributed to the occupation of sites by HCO3- which led to a greater repulsion. More PFOA was dispersed into distant regions (low reaction zone with poor Fe2+/microorganism) compared to other ion environments. Moreover, SO42- or NO3- with microbe-FexSy interaction exhibited pronounced retardation effects (Kd from 0.292 to 0.447 cm3·g-1) on PFOA. Notably, enhanced formations of β-Fe2O3·H2O and α-Fe2O3·H2O regulated PFOA transport behavior in PFOA-SO42- and PFOA-NO3- environments. The common attenuation pathway of PFOA was proposed as Deprotonation (A) with the cycle of Activation (B), decarboxylation (C), hydroxylation (D), HF elimination (E), hydrolysis (F), and HF elimination (E). Pseudomonas reduced Fe3+ to Fe2+, and Rhizobiales contributed to producing 3 Fe2+ after consuming 2 Fe2+. Fe2+ and Pseudomonas combined to drive PFOA multi-path chain reaction decay cycles. This study provided the theoretical basis for understanding PFOA cross-media transport and fate in microbe-mineral-ions interaction environments.
Keywords
PFOA,iron sulfur mineral,microorganisms,transport and fate,interaction
Speaker
王文兵
副研究员 上海大学

Submission Author
张梦 上海大学
王文兵 上海大学
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    May 17

    2024

    to

    May 20

    2024

  • Mar 31 2024

    Draft paper submission deadline

  • Mar 31 2024

    Contribution Submission Deadline

  • May 20 2024

    Registration deadline

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青年地学论坛理事会
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厦门大学近海海洋环境科学国家重点实验室
中国科学院城市环境研究所
自然资源部第三海洋研究所
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