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采用创新性白云母基钠沸石,通过批次和固定床柱实验研究,实现地下水的钙镁硬度有效去除;动力学和平衡研究。

Effective decontamination of Ca and Mg hardness from groundwater using innovative muscovite based sodalite in batch and fixed-bed column studies; dynamic and equilibrium studies.

机构信息

Chemistry Department, Faculty of Science, King Abdulaziz University, P.O Box 80200, Jeddah 21589, Saudi Arabia.

Geology Department, Faculty of Science, Beni-Suef University, Beni-Suef 65211, Egypt; Materials Technologies and their Applications Lab, Geology Department, Faculty of Science, Beni-Suef University, Beni-Suef, Egypt.

出版信息

J Contam Hydrol. 2021 Aug;241:103817. doi: 10.1016/j.jconhyd.2021.103817. Epub 2021 May 3.

Abstract

A novel form of sodalite was synthesized from muscovite (M.SD) as low-cost softening material for both Ca and Mg ions from real groundwater in batch and column studies. The sodalite sample showed significant surface area (105 m/g) and ion exchange capacity (87.3 meq/100 g) which qualifies it strong for softening applications. The incorporation of the M.SD as a fixed bed in column system at a fixed thickness of 4 cm and flow rates of 5 mL/min resulted in removal percentages of 90.5% and 92.2% for Ca and Mg, respectively at pH 7.6. Considering the real concentrations of the ions (Ca (233 mg/L) and Mg (114 mg/L)), the M.SD bed has the ability to reduce their concentrations according to the recommended limits (75 mg/L for Ca and 50 mg/L for Mg). These conditions resulted in purification of about 8.1 L and 8.7 L with breakthrough intervals of 1380 min and 1440 min; and saturation interval more than 1620 min for Ca and Mg, respectively. The M.SD columns' performances were described considering the assumption of the Thomas model, Adams-Bohart model, and Yoon-Nelson model. The batch studies demonstrate the uptake of both Ca and Mg ions according to the Pseudo-First order kinetics and Langmuir equilibrium behaviour. Considering the values of Gaussian energies (0.77 KJ/mol (Ca) and 1.36 KJ/mol (Mg)), the uptake of these ions occurred by homogenous reactions of monolayer form and physical nature. The thermodynamic studies declared the spontaneous properties of the reactions and their exothermic properties.

摘要

从白云母(M.SD)合成了一种新型方钠石,作为从实际地下水中批量和柱研究中去除 Ca 和 Mg 离子的低成本软化材料。方钠石样品具有显著的表面积(105 m/g)和离子交换容量(87.3 meq/100 g),非常适合用于软化应用。将 M.SD 作为固定床加入柱系统,固定厚度为 4 cm,流速为 5 mL/min,在 pH 7.6 时,Ca 和 Mg 的去除率分别为 90.5%和 92.2%。考虑到离子的实际浓度(Ca(233 mg/L)和 Mg(114 mg/L)),M.SD 床具有根据建议的限值降低其浓度的能力(Ca 为 75 mg/L,Mg 为 50 mg/L)。这些条件导致 Ca 和 Mg 的穿透间隔分别为 1380 min 和 1440 min,分别净化了约 8.1 L 和 8.7 L;Ca 和 Mg 的饱和度间隔分别超过 1620 min。M.SD 柱的性能是根据托马斯模型、亚当斯-博哈特模型和 Yoon-Nelson 模型的假设来描述的。批量研究表明,根据准一级动力学和朗缪尔平衡行为,Ca 和 Mg 离子的吸收符合假一级动力学和朗缪尔平衡行为。考虑到高斯能量值(Ca 为 0.77 KJ/mol,Mg 为 1.36 KJ/mol),这些离子的吸收是通过均相反应的单层形式和物理性质发生的。热力学研究表明了反应的自发性质及其放热性质。

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