为探究尾矿残留NH4+的缓释性,以江西信丰离子型稀土矿为研究对象,柱浸制备浸出尾矿,去离子水淋洗尾矿.按照淋洗→封存→再淋洗的步骤,考察了淋洗尾矿不同含水率(1.3%,15%,35%,250%),不同封存时间(15,30,60,120,180,195,210,240d)和不同传质机制(对流、扩散)下NH4+的淋出量.结果表明:尾矿再淋洗仍能淋出NH4+,NH4+淋出量受含水率、封存时间和传质方式影响;含水率≥15%时,NH4+淋出量整体随时间推移而递增;同时间下,NH4+淋出量整体随含水率增大而增大;其他条件相同时,对流传质下NH4+淋出量大于扩散.尾矿再次淋出的NH4+是可交换态NH4+向水溶态NH4+转化的结果.
Abstract
In order to explore the slow-release of residual NH4+, ion-absorbed type rare earth ore from Xinfeng (Jiangxi Province) was taken as the research object. The leached tailings were prepared by column leaching, and then drip washing with deionized water. Follow the steps of drip washing → sealing and storing → re drip washing, NH4+ amount in drip washed tailings with different water content (1.3%, 15%, 35%, 250%), under different time (15, 30, 60, 120, 180, 195, 210, 240d), different mass transfer mechanisms (convection, diffusion) were investigated. The results show that NH4+ can still be washed out from the drip washed tailings after being sealed and preserved for a long time. NH4+ washing amount is affected by water content, time and mass transfer mechanism. NH4+ washing amount, as a whole, increase with time proceeding, when the water content is ≥15%, and increase with the increase of water content, in the same preserved time. When other conditions are the same, NH4+ washing amount under convective is greater than diffusion. NH4+ re-washed out from the tailings is the result of transformation of NH4+ from exchangeable to water-soluble.
关键词
铵 /
缓释 /
可交换态 /
扩散双电层 /
离子型稀土 /
水溶态 /
尾矿
Key words
ammonium /
diffusion double layer /
exchangeable /
ion-absorbed type rare earth /
slow-release /
tailings /
water-soluble
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基金
国家自然科学基金资助项目(51874147);国家重点研发计划资助项目(2019YFC0605001);江西省高等学校井冈学者特聘教授岗位资助项目