摘要
离子型稀土开采以硫酸铵为浸矿剂进行原地浸矿,大量的浸矿剂通过离子交换作用置换出稀土元素离子后,高浓度的氨氮则留存于稀土矿层土壤中。以广东某稀土矿区为研究对象,采用土柱模拟试验,对浸矿后的土柱体进行清水淋洗,研究了不同pH值浸矿剂、不同清水淋洗工艺特征下氨氮的解析规律。结果表明,以出水氨氮浓度达到《稀土工业污染物排放标准》(GB26451—2011)且变化平稳为淋洗终点,所用淋洗水量与矿样体积比在2.1~2.3倍,氨氮淋出率大于62%,硫酸盐淋出率大于58%,淋洗初期淋洗液氨氮浓度大幅下降,而后随着淋洗水量增加缓慢下降。研究结论为离子型稀土矿区土壤氨氮污染控制奠定一定理论基础。
In the ionic rare earth mining,ammonium sulfate is used as a leaching agent for in-situ leaching.After a large amount of leaching agent replaces the rare earth element ions through ion exchange,the ammonia nitrogen of high concentration remains in the rare earth mineral layer soil.In this paper,taking a rare earth mining area in Guangdong as the research object,after leaching with water on the soil column that completely leached,in condition of using different leaching agents of pH values and different water leaching process characteristics,the desorption rules of ammonia nitrogen was studied.The results showed that,taking the time when the concentration of ammonia nitrogen stable compliance with the"Rare Earth Industry Pollutant Discharge Standard"(GB26451—2011)as the leaching end point,The ratio of the leaching water volume to the volume of the rare earth ore was between 2.1 and 2.3 times,and the leaching removal rate of ammonia nitrogen was larger than 62%,the leaching removal rate of sulfate was larger than 58%,the ammonia nitrogen concentration of the leaching liquid at the initial stage of leaching dropped significantly,and then slowly decreased as the amount of leaching water increases.The research conclusions can lay a theoretical foundation for soil ammonia nitrogen pollution control in ion-type rare earth mining areas.
作者
徐星
陈斌
霍汉鑫
祝怡斌
XU Xing;CHEN Bin;HUO Hanxin;ZHU Yibin(Guangsheng Nonferrous Metals Co.,LTD.,Shaoguan Guangdong 512000,China;BGRIMM Technology Group,Beijing 100160,China)
出处
《有色金属(矿山部分)》
2021年第5期128-131,共4页
NONFERROUS METALS(Mining Section)
基金
国家自然科学基金资助项目:多金属矿山尾矿渗滤液复杂污染物的原位修复及机理研究(0102-1901)。
关键词
离子型稀土矿
土壤
淋洗
氨氮
ionic type rare-earth ore
soil
leaching
ammonium nitrogen