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Modification of a natural zeolite with Fe(III) for simultaneous phosphate and ammonium removal from aqueous solutions

机译:用Fe(III)改性天然沸石,同时从水溶液中除去磷酸和铵

摘要

BACKGROUND: The incorporation of Fe(III) was performed in a natural clinoptilolite (Z-N) for simultaneous phosphate and ammonium removal. RESULTS: The existence of hydroxyl groups (congruent to Fe-OH) in the iron zeolite (Z-Fe) enhances the phosphate uptake from 0.6 +/- 0.1 mg-P g(-1) in Z-N to 3.4 +/- 0.2 mg-P g(-1) in Z-Fe. However, the ammonium sorption capacity slightly decreases from 33 +/- 2 mg-N g(-1) in Z-N to 27 +/- 2 mg-N g(-1) in Z-Fe. The equilibrium and kinetics sorption were well explained by the Langmuir isotherm and the intraparticle diffusion model, respectively. CONCLUSIONS: Both the phosphate and ammonium uptake were slightly affected by the coexistence of competing ions. The phosphate sorption capacity of iron zeolite was decreased in the regeneration cycles. Desorption using a 1 mol L-1 NaOH solution under dynamic conditions provided higher enrichment factors for ammonium than phosphate
机译:背景:Fe(III)的掺入是在天然斜发沸石(Z-N)中进行的,以同时去除磷酸盐和铵盐。结果:铁沸石(Z-Fe)中存在羟基(与Fe-OH一致)可将磷酸盐从ZN中的0.6 +/- 0.1 mg-P g(-1)吸收增加到3.4 +/- 0.2 mg Z-Fe中的-P g(-1)。但是,铵的吸附容量从Z-N中的33 +/- 2 mg-N g(-1)略微降低到Z-Fe中的27 +/- 2 mg-N g(-1)。朗格缪尔等温线和颗粒内扩散模型分别很好地解释了平衡和动力学吸附。结论:竞争性离子的共存对磷酸盐和铵的吸收都有轻微的影响。铁沸石的磷酸盐吸附能力在再生循环中降低。在动态条件下使用1 mol L-1 NaOH溶液解吸可提供比磷酸盐更高的铵富集因子

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