土壤中全氟烷基和多氟烷基物质的固存和降解:机遇和挑战

Zhenyu Cao , Fugen Dou , Youjun Deng , Xingmao Ma
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引用次数: 0

摘要

在土壤中检测到的全氟烷基和多氟烷基物质(PFAS)越来越多,它们通过在粮食作物中的积累对人类健康构成潜在风险。不幸的是,有效修复pfas污染土壤的选择是有限的。本文综述了土壤修复技术的最新进展,旨在通过集中于固存或原位降解来降低PFAS的生物利用度。具体来说,高效的土壤改良剂如粘土矿物和活性炭通常用于PFAS固定。然而,尽管它们具有最初的有效性,但由于吸附剂老化和土壤条件的变化,所吸附的PFAS的长期稳定性可能会受到损害,从而导致所吸附的PFAS的潜在再活化。包括高级氧化和高级还原工艺在内的原位化学降解可以实现PFAS的长期去除,特别是与其他下游处理技术相结合。然而,目前还缺乏详细的研究。这篇综述强调了推进土壤中PFAS修复的几个迫切的研究需求,并提出了新的方法,如将封存与化学降解相结合的综合方法,以实现更可持续的长期稳定和从污染土壤中去除PFAS。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Sequestration and degradation of per- and polyfluoroalkyl substances in soil: Opportunities and challenges

Sequestration and degradation of per- and polyfluoroalkyl substances in soil: Opportunities and challenges
Per- and polyfluoroalkyl substances (PFAS) are increasingly detected in soils, posing potential risks to human health via their accumulation in food crops. Unfortunately, options for effective remediation of PFAS-contaminated soils are limited. This review provides a comprehensive analysis of recent advancements in soil remediation technologies aiming to lower PFAS bioavailability by focusing on either sequestration or in situ degradation. Specifically, highly effective soil amendments such as clay minerals and activated carbon are often used for PFAS immobilization. However, despite their initial effectiveness, the long-term stability of sequestered PFAS may be compromised as a result of sorbent aging and soil condition changes, leading to the potential remobilization of the sorbed PFAS. In situ chemical degradation including advanced oxidation and advanced reduction processes can achieve long-term PFAS removal, especially by combining with other downstream treatment technologies. However, detailed studies are still lacking. This review highlighted several urgent research needs to advance PFAS remediation in soil and proposed new approaches such as an integrated approach that combines sequestration with chemical degradation to achieve more sustainable long-term stabilization and removal of PFAS from contaminated soils.
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