K. H. Shah, M. Fahad, Z. Ghazi, Sajjad Ali, Asim Shahzad, Salah ud Din
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引用次数: 1
Abstract
The potential of natural (N) and magnetized (M) forms of different rocks (calcite and dolomite) and clays (bentonite, kaolinite, and hematite) were evaluated for the removal of As(III) from aqueous solutions, in order to optimize and scrutinize the most suitable adsorbent. The order observed for efficiency of As(III) removal was N-calcite > N-dolomite > M-calcite > M-dolomite > N-bentonite > M-bentonite > M-kaolinite > N-kaolinite > M-hematite > N-hematite. On the basis of this analysis, natural calcite was further selected for in-depth analysis of various adsorption parameters such as time, pH, temperature, dosage, and concentration of As(III) ions. An excellent adsorption capacity of 19.05 mg‧g−1 was displayed by calcite for As(III), which was significantly higher than that previously reported for other studies. The characterization of adsorbent calcite was performed by various analytical techniques:XRD, XRF, FTIR, SEM-EDS, TG/DTA and PZC. The kinetic investigation revealed that the adsorbent successfully removed over 98% of As(III) from aqueous solution after 160 minutes of equilibration time. The adsorption data was well fitted to the Freundlich isotherm model and fairly described by the pseudo-second-order mechanism. The mean energy of adsorption (E) determined from the Dubinin-Radushkevich (D-R) model was less than 8 kJ‧mol-1 , which indicates a physical adsorption process. The calculated thermodynamic parameters revealed that the adsorption of As(III) by calcite is endothermic, favourable and spontaneous.
评估了不同岩石(方解石和白云石)和粘土(膨润土、高岭石和赤铁矿)的天然(N)和磁化(M)形式对水溶液中As(III)的去除潜力,以优化和审查最合适的吸附剂。As(III)的去除率顺序为n -方解石> n -白云石> m -方解石> m -白云石> n -膨润土> m -膨润土> m -高岭石> n -高岭石> m -赤铁矿> n -赤铁矿。在此基础上,进一步选择天然方解石,深入分析时间、pH、温度、用量、浓度等对as (III)离子的各种吸附参数。方解石对As(III)的吸附量为19.05 mg·g−1,明显高于其他研究报道。采用XRD、XRF、FTIR、SEM-EDS、TG/DTA、PZC等分析技术对吸附方解石进行了表征。动力学研究表明,经过160分钟的平衡时间,吸附剂成功地从水溶液中去除了98%以上的As(III)。吸附数据与Freundlich等温线模型拟合较好,用拟二级机理描述较好。Dubinin-Radushkevich (D-R)模型的平均吸附能(E)小于8 kJ·mol-1,表明吸附过程为物理吸附过程。计算的热力学参数表明,方解石对As(III)的吸附是吸热的、有利的和自发的。
期刊介绍:
WaterSA publishes refereed, original work in all branches of water science, technology and engineering. This includes water resources development; the hydrological cycle; surface hydrology; geohydrology and hydrometeorology; limnology; salinisation; treatment and management of municipal and industrial water and wastewater; treatment and disposal of sewage sludge; environmental pollution control; water quality and treatment; aquaculture in terms of its impact on the water resource; agricultural water science; etc.
Water SA is the WRC’s accredited scientific journal which contains original research articles and review articles on all aspects of water science, technology, engineering and policy. Water SA has been in publication since 1975 and includes articles from both local and international authors. The journal is issued quarterly (4 editions per year).