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铁氧化菌结合有机肥修复砷污染石灰性农田土壤。

Remediation of arsenic-contaminated calcareous agricultural soils by iron-oxidizing bacteria combined with organic fertilizer.

机构信息

College of Earth and Environmental Sciences, Lanzhou University, 222 Tianshui South Road, Lanzhou, 730000, China.

出版信息

Environ Sci Pollut Res Int. 2023 Jun;30(26):68258-68270. doi: 10.1007/s11356-023-27217-5. Epub 2023 Apr 29.

Abstract

In arid soil with low-iron and high-calcium carbonate contents, the fate of arsenic (As) is mainly controlled by the contents of calcium and organic matter in the soil. However, there is still a lack of knowledge about their interaction and that effect on their absorption by maize. The purpose of this study was to explore the long-term immobilization and repair mechanism of in situ As-contaminated farmland. We designed three treatments: iron-oxidizing bacteria (FeOB), organic fertilizer, FeOB and organic fertilizer added in combination. After 140-day field farmland remediation trial, the results showed that the FeOB can effectively immobilize the water-soluble As (F) in soil, and the organic fertilizer promoted the remediation of FeOB. In addition, the content of As in maize grains was reduced after treatment by FeOB and organic fertilizer. The XRD and XPS analysis of the topsoil showed that the combined treatment of FeOB and organic fertilizer promoted the formation of calcium arsenate mineral with low solubility and high stability; As(III) would gradually transform into As(V). The biological iron (hydr)oxide can increase the contents of Fe and As in the rhizosphere and form iron plaques on the surface of the roots by SEM-EDS analysis of maize root. Collectively, these results clarify the main biogeochemical ways to control the fate of As in calcareous soils with low-iron and low-organic matter contents and provide a basis for in situ remediation of As.

摘要

在铁含量低、碳酸钙含量高的干旱土壤中,砷(As)的命运主要受土壤中钙和有机质的含量控制。然而,我们对它们之间的相互作用及其对玉米吸收的影响仍然缺乏了解。本研究旨在探讨原位砷污染农田的长期固定和修复机制。我们设计了三种处理方法:氧化铁细菌(FeOB)、有机肥、FeOB 和有机肥联合添加。经过 140 天的田间农田修复试验,结果表明,FeOB 可有效固定土壤中的水溶性 As(F),有机肥促进了 FeOB 的修复。此外,FeOB 和有机肥处理后玉米籽粒中的砷含量降低。表层土壤的 XRD 和 XPS 分析表明,FeOB 和有机肥的联合处理促进了低溶解度和高稳定性的钙砷酸盐矿物的形成;As(III)会逐渐转化为 As(V)。通过对玉米根进行扫描电镜-能谱分析(SEM-EDS),生物铁(氢)氧化物可以增加根际铁和砷的含量,并在根表面形成铁斑。总的来说,这些结果阐明了控制低铁低有机质含量石灰性土壤中砷命运的主要生物地球化学途径,为砷的原位修复提供了依据。

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