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Combined application of strong alkaline materials and specific organic fertilizer accelerates nitrification process of a rare earth mining soil
Science of the Total Environment ( IF 8.2 ) Pub Date : 2023-03-23 , DOI: 10.1016/j.scitotenv.2023.163042
Min Wang 1 , Song Wu 1 , Yilin Lu 1 , Haotian Wu 1 , Dunfeng Si 1 , Dongmei Zhou 1
Affiliation  

The extensive usage of ammonium sulfate as the leaching agent to extract rare earth elements led to widespread ammonia nitrogen (NH4+-N) pollution in the tailing soils of ion-adsorbed rare earth deposits in southern China. However, the cost-effective technologies to tackle with the long-term retention of NH4+-N in the rare earth mining soil have been largely unresolved. In this study, we developed a cost-effective approach to activate soil nitrification by the co-application of alkaline materials and organic fertilizer. The co-application of 0.3 % of organic fertilizer and 0.1 % ∼ 0.2 % of CaO or MgO or Mg(OH)2 stimulated a soil NH4+-N decrease rate of 2.01–7.58 mg kg−1 d−1 and a soil NO3-N accumulation rate of 1.56–7.09 mg kg−1 d−1. Noting that only if the soil pH was elevated to 7.81–9.00, the NH4+-N decrease rate and NO3-N accumulation rate were dependent on the proton consumption capacity of the alkaline materials. The application of CaCO3 could not stimulate soil nitrification possibly due to the soil pH was uncapable to be elevated to above 7.68. The qPCR, amplicon sequencing, and nitrification inhibitor batch incubation results demonstrated that organic fertilizer supplied active ammonia-oxidizing bacteria Nitrosomonas europaea. The proliferation of Nitrosomonas europaea in the alkaline materials and organic fertilizer co-applied soil was responsible for the soil nitrification. Furthermore, the application of commercial denitrifying bacteria inoculum promoted the removal of accumulated NO3-N. The findings of this study provide a lost-cost technology to remove NH4+-N from the rare earth mining soil.



中文翻译:

强碱性物质与专用有机肥配施加速稀土矿区土壤硝化作用

大量使用硫酸铵作为浸出剂提取稀土元素,导致我国南方离子吸附型稀土矿床尾矿土壤普遍存在氨氮(NH 4 + -N)污染。然而,解决 NH 4 + -N 在稀土采矿土壤中长期滞留的成本效益技术在很大程度上尚未得到解决。在这项研究中,我们开发了一种经济高效的方法,通过共同施用碱性物质和有机肥来激活土壤硝化作用。0.3%的有机肥和0.1%~0.2%的CaO或MgO或Mg(OH) 2 的共同施用刺激土壤NH 4 + -N的减少率为2.01–7.58 mg kg −1d −1和土壤 NO 3 -N 积累率为 1.56–7.09 mg kg −1 d −1。注意到只有当土壤 pH 值升高到 7.81–9.00 时,NH 4 + -N 减少率和 NO 3 - -N 积累率才取决于碱性物质的质子消耗能力。施用CaCO 3不能刺激土壤硝化作用可能是由于土壤pH值不能升高到7.68以上。qPCR、扩增子测序和硝化抑制剂批次孵育结果表明,有机肥料提供了活性氨氧化细菌Nitrosomonas europaea. Nitrosomonas europaea在碱性物质和有机肥共施土壤中的增殖是土壤硝化作用的原因。此外,商业反硝化细菌接种物的应用促进了累积的NO 3 - -N的去除。本研究结果提供了一种从稀土矿区土壤中去除NH 4 + -N的成本损失技术。

更新日期:2023-03-26
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