Effective cadmium immobilization in paddy soil by the interaction of sulfate reducing bacteria and manganese fertilizer.

IF 8 2区 环境科学与生态学 Q1 ENVIRONMENTAL SCIENCES
Peng Yang, Bin Wu, Shuai Zheng, Yuxian Shangguan, Lujie Liang, Qingjuan Zheng, Junqi Hu
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Abstract

Manganese fertilizer (MnSO4) was widely applied to control the Cadmium (Cd) uptake by rice, but the overall process of microbial activities controlling Cd mobilization in paddy soil is poorly understood. This study investigated the stimulation effect of sulfate reducing bacteria (SRB) on Cd bioavailability with the input of different doses MnSO4 (0.5, 1.0, 2.0 g/kg) under the anaerobic paddy soil. The results show that the input of MnSO4 generated soil H+ release. However, the stimulation of SRB remarkedly increased soil pH and reduced the redox potential (Eh) by inhibiting the exchange of Mn2+ and H+, resulting in the available Cd decreased and the amorphous Fe/Mn Oxide-Cd increased significantly. In the co-existed SRB and 1.0 g/kg MnSO4, the available Cd decreased remarkedly by 40.18%, which was transformed to reducible Cd. Meanwhile, the addition of MnSO4 and SRB enhanced the abundance of Cd immobilization related bacteria, including Desulfobacterota, Chloroflexi, Bacteroidota, and Myxococcota. KEGG results showed that MnSO4 and SRB treatment enhanced the ability of microbial sulfur and secondary metabolites. Furthermore, the sulfate reduction related genes (i.e. aprA, sat) obviously enriched in soils. Structural equation modeling showed that Mn, Fe, DOC, Eh, and pH are the key factors affecting available Cd. These findings add to the current knowledge of how MnSO4 and microorganisms affect the mobilization and availability of Cd under paddy soil media, providing new ideas and a theoretical basis for reducing the environmental risk of Cd.

通过硫酸盐还原菌和锰肥的相互作用有效固定稻田土壤中的镉。
锰肥(MnSO4)被广泛用于控制水稻对镉(Cd)的吸收,但人们对控制水稻土壤中镉迁移的微生物活动的整个过程知之甚少。本研究探讨了在厌氧稻田土壤中投入不同剂量的 MnSO4(0.5、1.0、2.0 g/kg)后,硫酸盐还原菌(SRB)对镉生物利用率的促进作用。结果表明,加入 MnSO4 会释放土壤中的 H+。然而,SRB 的刺激通过抑制 Mn2+ 和 H+ 的交换,显著提高了土壤的 pH 值,降低了氧化还原电位(Eh),导致可利用的镉减少,无定形的铁/氧化锰-镉显著增加。在 SRB 和 1.0 g/kg MnSO4 共存的情况下,可利用镉明显减少了 40.18%,并转化为可还原镉。同时,添加 MnSO4 和 SRB 还提高了镉固定化相关细菌的丰度,包括脱硫菌群(Desulfobacterota)、绿藻菌群(Chloroflexi)、类杆菌群(Bacteroidota)和肌球菌群(Myxococcota)。KEGG 结果显示,MnSO4 和 SRB 处理提高了微生物硫和次级代谢产物的能力。此外,土壤中与硫酸盐还原相关的基因(如 aprA、sat)明显富集。结构方程模型显示,锰、铁、DOC、Eh 和 pH 是影响可利用镉的关键因素。这些发现丰富了目前关于硫酸锰和微生物如何影响水稻土壤介质中镉的动员和可得性的知识,为降低镉的环境风险提供了新的思路和理论依据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Journal of Environmental Management
Journal of Environmental Management 环境科学-环境科学
CiteScore
13.70
自引率
5.70%
发文量
2477
审稿时长
84 days
期刊介绍: The Journal of Environmental Management is a journal for the publication of peer reviewed, original research for all aspects of management and the managed use of the environment, both natural and man-made.Critical review articles are also welcome; submission of these is strongly encouraged.
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