Chinese Research Academy of Environmental Sciences, Beijing, China.
College of Water and Architectural Engineering, Shihezi University, Shihezi, China; Institute of Geographic Sciences and Natural Resources Research, Beijing, China; Xinjiang Production and Construction Group Key Laboratory of Modern Water-Saving Irrigation, Shihezi, China.
Environ Pollut. 2020 Dec;267:115449. doi: 10.1016/j.envpol.2020.115449. Epub 2020 Sep 2.
The ammonium sulphate ((NH)SO) in-situ leaching process is the most widely used extraction technology for weathered crust elution-deposited rare earth ores (WCED-REOs). Highly concentrated (NH)SO, a representative leaching agent, is often used in the leaching process of WCED-REOs. However, this in-situ leaching process causes nitrogen pollution in the soil, surrounding surface and ground water due to the high concentrations of (NH)SO solutions used as a long term leaching agent. To date, the mechanism behind the variations in ammonia nitrogen (AN) in deep soil profiles is unclear. We conducted vertical and lateral soil sampling and analyzed the collected samples for soil moisture, pH, ammonia forms, and AN contents in soil profiles deeper than 500 cm in an in-situ leaching mining area of Ganzhou, Jiangxi Province, southern China. The results show that primary chemical pollutants in the soil are derived from residual leaching agents with high acidities and concentrations of AN. Twelve years after the mining process was completed, the mean pH values of the tailings in the mining area were 3.90 and 4.87 in its lower reaches. Due to the presence of chemical residues, the AN concentration was 12-40 times higher than that of the raw ore soil before it was mined. The percentages of different ammonium forms in the rare earth tailing soil were 65%, 30%, and 5% for the water-soluble, exchangeable, and fixed ammonium forms, respectively. The results of this study support effective prevention and remediation treatment of environmental problems caused by AN pollution of the soil in WCED-REOs.
硫酸铵((NH4)2SO4)原位浸出工艺是风化壳淋积型稀土矿(WCED-REO)最广泛使用的提取技术。高浓度的(NH4)2SO4,一种代表性的浸出剂,通常用于 WCED-REO 的浸出过程。然而,由于长期使用高浓度的(NH4)2SO4 作为浸出剂,这种原地浸出过程会导致土壤、周围地表水和地下水的氮污染。迄今为止,深层土壤剖面中氨氮(AN)变化的机制尚不清楚。我们在中国南方江西省赣州市的一个原地浸矿开采区进行了垂直和横向土壤采样,并分析了采集的土壤样本,以了解土壤剖面中超过 500cm 深的土壤水分、pH 值、氨形态和 AN 含量。结果表明,土壤中的主要化学污染物来自残留的浸出剂,这些浸出剂具有高酸度和高 AN 浓度。采矿过程完成 12 年后,矿区下游尾矿的平均 pH 值分别为 3.90 和 4.87。由于存在化学残留物,AN 浓度比开采前原矿土壤高 12-40 倍。稀土尾矿土壤中不同铵形态的比例分别为水溶性铵、可交换铵和固定铵的 65%、30%和 5%。本研究结果为 WCED-REO 中 AN 污染土壤的环境问题提供了有效的预防和修复处理措施。