氢氧化钠处理稻壳吸附去除铁(II):吸附平衡和动力学

Sunita Shrestha, A. K. Dhami, A. Rajbhandari Nyachhyon
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Results revealed that the maximum efficiency was achieved at pH 3 for Fe(II). The adsorption process was found to be best fitted to Langmuir adsorption isotherm model controlled by pseudo-second–order kinetics with the rate constant value i.e. 0.0218 and 0.0235 g/(mg·min) for RRH and NRH respectively. The χ2 values of pseudo second order was found to be lower which confirmed chemisorption, involving ion exchange and valence forces through sharing or exchange of electrons between adsorbent and adsorbate. The maximum adsorption capacity for Fe(II) on RRH and NRH was found to be 2.9 mg/g and 5.6 mg/g respectively. The positive ∆G value represents the randomness of the system during adsorption process. The slope of the linear plot of Qt vs t0.5 was linear but not passed through the origin, which indicates that, the intraparticle diffusion was not only rate controlling step. Temkin value showed the maximum binding energy (KT) for NRH was 16.4 L/g and for RRH it was 12.2 L/g. Key word: Rice husk; Iron; Langmuir adsorption. INTRODUCTION Metals of having relatively high densities (> 5 g/cm3) and high atomic weights simply means heavy metals1. Copper, aluminium, iron, zinc, platinum, arsenic, chromium, etc are some of the examples. Heavy metals are either essential nutrients like iron, cobalt and zinc or relatively harmless such as ruthenium, silver and indium while other are highly poisonous such as arsenic, cadmium, mercury and lead1. Among the wide variety of heavy metals, iron i s one of the most common heavy metals that is found in nature. The magnetite [Fe3O4, 72.4 % Fe], hematite [Fe2O3, 69.9% Fe], goethite [FeO(OH), 62.9% Fe], limonite [FeO(OH).n(H2O)] or siderite [FeCO3, 48.2% Fe] are the most common ore of iron that is found in earth’s crust. Among them, hematite and magnetite are found in the form of rocks2 which during demineralization introduced in ground water by leaching and percolation. It also introduced from anthropogenic sources specially from industrial sector3. Heavy metals have become one of the major causes of concern for water pollution1. In ground water, iron exists in ferrous state and remains dissolved in water. Nonetheless when it is exposed to atmosphere, it gets oxidised to ferric ion. The iron in ferric state does not dissolved in water and forming reddish brown colour2. The relatively high content of iron levels in water can cause stains in plumbing, laundry and cooking utensils that can impart objectionable tastes and colours to foods3. Additionally, excessive Author for Correspondence: Armila Rajbhandari (Nyachhyon), Central Department of Chemistry, Tribhuvan University, Kirtipur, Nepal. E-mail: armila3@yahoo.com Received: 30 May 2020; First Review: 22 Sep 2020; Second Review: 23 Sep 2020; Accepted: 27 Sep 2020. 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引用次数: 2

摘要

以生稻壳(RRH)和氢氧化钠处理稻壳(NRH)为原料制备了低成本的吸附剂。然后用XRD、FTIR对制备的材料进行表征,用亚甲基蓝吸附法测定稻壳吸附剂的比表面积。XRD显示材料为非晶态,结晶度较低。红外光谱分析表明,材料表面存在酯、酚、羰基和二氧化硅等含氧官能团。RRH和NRH的表面积分别为387和417 m2/g。因此,制备的吸附剂用于去除水溶液中的铁(II)离子。考察了pH、吸附剂用量、接触时间等参数对稻壳吸附剂吸附铁(II)效果的影响。结果表明,在pH为3时,Fe(II)的效率最高。RRH和NRH的吸附速率常数分别为0.0218和0.0235 g/(mg·min),符合拟二级动力学控制的Langmuir吸附等温线模型。拟二级χ2值较低,证实了化学吸附作用,即通过吸附剂和吸附物之间的共享或交换电子进行离子交换和价电子力。RRH和NRH对Fe(II)的最大吸附量分别为2.9 mg/g和5.6 mg/g。正∆G值表示吸附过程中体系的随机性。Qt vs t0.5线性曲线的斜率呈线性,但没有通过原点,说明颗粒内扩散不仅仅是速率控制步骤。Temkin值显示NRH的最大结合能KT为16.4 L/g, RRH的最大结合能KT为12.2 L/g。关键词:稻壳;铁;朗缪尔吸附。具有相对较高密度(> 5 g/cm3)和高原子量的金属仅指重金属1。铜、铝、铁、锌、铂、砷、铬等就是其中的一些例子。重金属要么是必需的营养物质,如铁、钴和锌,要么是相对无害的,如钌、银和铟,而其他重金属则是剧毒的,如砷、镉、汞和铅。在种类繁多的重金属中,铁是自然界中最常见的重金属之一。磁铁矿[Fe3O4, 72.4% Fe]、赤铁矿[Fe2O3, 69.9% Fe]、针铁矿[FeO(OH), 62.9% Fe]、褐铁矿[FeO(OH).n(H2O)]和菱铁矿[FeCO3, 48.2% Fe]是地壳中最常见的铁矿石。其中赤铁矿和磁铁矿以岩石的形式存在,在脱矿过程中通过淋滤和渗滤引入地下水。它还从人为来源,特别是从工业部门引进。重金属已经成为水污染的主要原因之一。在地下水中,铁以亚铁态存在,并溶解于水中。然而,当它暴露在大气中时,它被氧化成铁离子。铁态的铁不溶于水而形成红棕色。水中相对较高的铁含量会在管道、洗衣和烹饪器具上造成污渍,从而给食物带来令人讨厌的味道和颜色。此外,过度作者通信:Armila Rajbhandari (Nyachhyon),中央化学系,Tribhuvan大学,Kirtipur,尼泊尔。收稿日期:2020年5月30日;初审:2020年9月22日;复核:2020年9月23日;录用日期:2020年9月27日。Doi: https://doi.org/10.3126/sw.v14i14.34991
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Adsorptive Removal of Fe (II) By NaOH Treated Rice Husk: Adsorption Equilibrium And Kinetics
The low cost adsorbents were prepared from raw rice husk (RRH) and NaOH treated rice husk (NRH). Then prepared materials were characterized by XRD, FTIR and surface area of rice husk adsorbent were determined by methylene blue adsorption method. XRD showed amorphous nature with low crystallinity of the material. The FTIR spectra showed the presence of oxygenated functional groups such as ester, phenol, carbonyl and silica on the material. The surface area of RRH and NRH were found to be 387 and 417 m2/g respectively. Thus, prepared adsorbents were used for the removal of Fe(II) ion from aqueous solution. The influence of various parameters like pH, adsorbent doge, and contact time were studied for the better adsorption of Fe(II) on rice husk adsorbents. Results revealed that the maximum efficiency was achieved at pH 3 for Fe(II). The adsorption process was found to be best fitted to Langmuir adsorption isotherm model controlled by pseudo-second–order kinetics with the rate constant value i.e. 0.0218 and 0.0235 g/(mg·min) for RRH and NRH respectively. The χ2 values of pseudo second order was found to be lower which confirmed chemisorption, involving ion exchange and valence forces through sharing or exchange of electrons between adsorbent and adsorbate. The maximum adsorption capacity for Fe(II) on RRH and NRH was found to be 2.9 mg/g and 5.6 mg/g respectively. The positive ∆G value represents the randomness of the system during adsorption process. The slope of the linear plot of Qt vs t0.5 was linear but not passed through the origin, which indicates that, the intraparticle diffusion was not only rate controlling step. Temkin value showed the maximum binding energy (KT) for NRH was 16.4 L/g and for RRH it was 12.2 L/g. Key word: Rice husk; Iron; Langmuir adsorption. INTRODUCTION Metals of having relatively high densities (> 5 g/cm3) and high atomic weights simply means heavy metals1. Copper, aluminium, iron, zinc, platinum, arsenic, chromium, etc are some of the examples. Heavy metals are either essential nutrients like iron, cobalt and zinc or relatively harmless such as ruthenium, silver and indium while other are highly poisonous such as arsenic, cadmium, mercury and lead1. Among the wide variety of heavy metals, iron i s one of the most common heavy metals that is found in nature. The magnetite [Fe3O4, 72.4 % Fe], hematite [Fe2O3, 69.9% Fe], goethite [FeO(OH), 62.9% Fe], limonite [FeO(OH).n(H2O)] or siderite [FeCO3, 48.2% Fe] are the most common ore of iron that is found in earth’s crust. Among them, hematite and magnetite are found in the form of rocks2 which during demineralization introduced in ground water by leaching and percolation. It also introduced from anthropogenic sources specially from industrial sector3. Heavy metals have become one of the major causes of concern for water pollution1. In ground water, iron exists in ferrous state and remains dissolved in water. Nonetheless when it is exposed to atmosphere, it gets oxidised to ferric ion. The iron in ferric state does not dissolved in water and forming reddish brown colour2. The relatively high content of iron levels in water can cause stains in plumbing, laundry and cooking utensils that can impart objectionable tastes and colours to foods3. Additionally, excessive Author for Correspondence: Armila Rajbhandari (Nyachhyon), Central Department of Chemistry, Tribhuvan University, Kirtipur, Nepal. E-mail: armila3@yahoo.com Received: 30 May 2020; First Review: 22 Sep 2020; Second Review: 23 Sep 2020; Accepted: 27 Sep 2020. Doi: https://doi.org/10.3126/sw.v14i14.34991
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