铁活化天然斜发沸石吸附水中氟的研究  被引量:12

Adsorption of Fluoride from Drinking Water by Iron-activated Clinoptilolites

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作  者:苗茵[1] 刘晓飞[1] 李曼尼[1] 

机构地区:[1]内蒙古大学化学化工学院,呼和浩特010021

出  处:《内蒙古大学学报(自然科学版)》2005年第6期647-652,共6页Journal of Inner Mongolia University:Natural Science Edition

摘  要:用2%N aOH预处理,再经5%F eC l3静态热浸渍和动态热浸渍的铁活化斜发沸石矿样(3#和4#),对水中氟离子的吸附能力有了明显提高,饱和吸附量分别达到664、788 m g/kg,其吸附行为分别属指数型和S型等温线.用D-R方程线性拟合发现3#矿样化学吸附为主,4#矿样化学吸附和物理吸附兼有.吸附机理的差异主要来自铁活化引起的矿样比表面积、孔分布以及表面极性的不同.Two iron activated clinoptilolites (3^# and 4^#) were studied to determine their adsorption capacities of fluoride from drinking water. The clinoptilolites were prepared by the static and dynamic thermal impregnation method with 2% NaOH and 5% FeCl3 solutions, respectively. The results showed that their adsorption capacities were enhanced obviously, their saturated adsorption capacities were 664 and 788 mg/kg, respectively and their adsorption isotherms belonged to the exponential type and S-type respectively. The linear fitting of D-R isotherm equation showed that the adsorption behavior was the chemical adsorption mainly in sample 3^# and both chemical and physical adsorption in samples 4^#. The difference of adsorption behaviour was from the difference of specific area, pore distribution and surface polarization of two samples.

关 键 词:斜发沸石 铁活化 水中氟 吸附机理 

分 类 号:P578.974[天文地球—矿物学]

 

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