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合理应用磷肥修复碱性土壤中铀污染的效果及机制。

Remediation of uranium-contaminated alkaline soil by rational application of phosphorus fertilizers: Effect and mechanism.

机构信息

Key Laboratory of Microbial Technology for Industrial Pollution Control of Zhejiang Province, College of Environment, Zhejiang University of Technology, Hangzhou, China.

Key Laboratory of Microbial Technology for Industrial Pollution Control of Zhejiang Province, College of Environment, Zhejiang University of Technology, Hangzhou, China.

出版信息

Environ Res. 2023 Mar 1;220:115172. doi: 10.1016/j.envres.2022.115172. Epub 2022 Dec 27.

Abstract

In alkaline soil, abundant carbonates will mobilize uranium (U) and increase its ecotoxicity, which is a serious threat to crop growth. However, the knowledge of U remediation in alkaline soils remains very limited. In this study, U-contaminated alkaline soil (tillage layer) was collected from the Ili mining area of Xinjiang, the soil remediation was carried out by using phosphorus (P) fertilizers of different solubility (including KHPO, Ca(HPO), CaHPO, and Ca(PO)), and the pathways and mechanisms of U passivation in the alkaline soil were revealed. The results showed that water-soluble P fertilizers, KHPO and Ca(HPO), were highly effective at immobilizing U, and significantly reduced the bioavailability of soil U. The exchangeable U was reduced by 70.5 ± 0.1% (KHPO) and 68.2 ± 1.9% (Ca(HPO)), which was converted into the Fe-Mn oxide-bound and residual phases. Pot experiments showed that soil remediation by KHPO significantly promoted crop growth, especially for roots, and reduced U uptake in crops by 94.5 ± 1.0%. The immobilization of U by KHPO could be attributed to the release of phosphate anions, which react with the uranyl ion (UO) forming a stable mineral of meta-ankoleite and enhancing the binding of UO to the soil Fe-Mn oxides. In addition, KHPO dissolution produces acidity and P fertilizer, which can reduce soil alkalinity and improve crop growth. The findings in this work demonstrate that a rational application of P fertilizer can effectively, conveniently, and cheaply remediate U contamination and improve crop yield and safety on alkaline farmland.

摘要

在碱性土壤中,丰富的碳酸盐会使铀(U)活化并增加其生态毒性,这对作物生长构成了严重威胁。然而,关于碱性土壤中铀的修复知识仍然非常有限。本研究从新疆伊犁矿区采集了受铀污染的碱性土壤(耕作层),利用不同溶解性的磷(P)肥料(包括 KHPO、Ca(HPO)、CaHPO 和 Ca(PO))进行土壤修复,并揭示了 U 在碱性土壤中钝化的途径和机制。结果表明,水溶性 P 肥料 KHPO 和 Ca(HPO) 对 U 具有高效的固定作用,显著降低了土壤 U 的生物有效性。交换态 U 减少了 70.5 ± 0.1%(KHPO)和 68.2 ± 1.9%(Ca(HPO)),这部分 U 被转化为铁锰氧化物结合态和残留态。盆栽实验表明,KHPO 土壤修复显著促进了作物的生长,尤其是根系的生长,并降低了作物对 U 的吸收 94.5 ± 1.0%。KHPO 对 U 的固定作用归因于磷酸根阴离子的释放,它与铀酰离子(UO)反应形成稳定的钙铀云母矿物,并增强了 UO 与土壤铁锰氧化物的结合。此外,KHPO 的溶解会产生酸度和 P 肥料,这可以降低土壤碱性并改善作物生长。本研究结果表明,合理施用 P 肥料可以有效地、方便地、廉价地修复碱性农田中的 U 污染,并提高作物产量和安全性。

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