TY - JOUR
T1 - Leaching kinetics of ionic rare-earth in ammonia-nitrogen wastewater system added with impurity inhibitors
AU - Qiu, Tingsheng
AU - Zhu, Dongmei
AU - Fang, Xihui
AU - Zeng, Qinghua
AU - Gao, Guangkuo
AU - Zhu, Hualei
PY - 2014
Y1 - 2014
N2 - Ammonia-nitrogen wastewater is produced during the dressing and smelting process of rare-earth ores. Such wastewater includes a very high concentration of NH4 +, as well as other ions (e.g., NH4 +, RE3+, Al3+, Fe3+, Ca2+, Cl-, and SiO3 2-) with a pH of 5.4-5.6. Its direct discharge will pollute, yet it can be recycled and used as a leaching reagent for ionic rare-earth ores. In this study, leaching kinetics studies of both rare earth ions and impurity ion Al3+ were conducted in the ammonia-nitrogen wastewater system with the aid of impurity inhibitors. Results showed that the leaching process of rare-earth followed the internal diffusion kinetic model. When the temperature was 298 K and the concentration of NH4 + was 0.3 mol/L, the leaching reaction rate constant of ionic rare-earth was 1.72 and the apparent activation energy was 9.619 kJ/mol. The leaching rate was higher than that of conventional leaching system with ammonium sulfate, which indicated that ammonia-nitrogen wastewater system and the addition of impurity inhibitors could promote ionic rare-earth leaching. The leaching kinetic process of impurity Al3+ did not follow either internal diffusion kinetic model or chemical reaction control, but the hybrid control model which was affected by a number of process factors. Thus, during the industrial production the leaching of impurity ions could be reduced by increasing the concentration of impurity inhibitors, reducing the leaching temperature to a proper range, accelerating the seepage velocity of leaching solution, or increasing the leaching rate of rare earths.
AB - Ammonia-nitrogen wastewater is produced during the dressing and smelting process of rare-earth ores. Such wastewater includes a very high concentration of NH4 +, as well as other ions (e.g., NH4 +, RE3+, Al3+, Fe3+, Ca2+, Cl-, and SiO3 2-) with a pH of 5.4-5.6. Its direct discharge will pollute, yet it can be recycled and used as a leaching reagent for ionic rare-earth ores. In this study, leaching kinetics studies of both rare earth ions and impurity ion Al3+ were conducted in the ammonia-nitrogen wastewater system with the aid of impurity inhibitors. Results showed that the leaching process of rare-earth followed the internal diffusion kinetic model. When the temperature was 298 K and the concentration of NH4 + was 0.3 mol/L, the leaching reaction rate constant of ionic rare-earth was 1.72 and the apparent activation energy was 9.619 kJ/mol. The leaching rate was higher than that of conventional leaching system with ammonium sulfate, which indicated that ammonia-nitrogen wastewater system and the addition of impurity inhibitors could promote ionic rare-earth leaching. The leaching kinetic process of impurity Al3+ did not follow either internal diffusion kinetic model or chemical reaction control, but the hybrid control model which was affected by a number of process factors. Thus, during the industrial production the leaching of impurity ions could be reduced by increasing the concentration of impurity inhibitors, reducing the leaching temperature to a proper range, accelerating the seepage velocity of leaching solution, or increasing the leaching rate of rare earths.
UR - http://handle.uws.edu.au:8081/1959.7/564417
U2 - 10.1016/S1002-0721(14)60200-3
DO - 10.1016/S1002-0721(14)60200-3
M3 - Article
SN - 1000-4343
VL - 32
SP - 1175
EP - 1183
JO - Journal of Rare Earths
JF - Journal of Rare Earths
IS - 12
ER -