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几种吸附剂吸附亚砷酸根离子过程中pH值的动态变化
引用本文:叶瑛,季珊珊,邬黛黛,张维睿.几种吸附剂吸附亚砷酸根离子过程中pH值的动态变化[J].高校地质学报,2006,12(2):228-233.
作者姓名:叶瑛  季珊珊  邬黛黛  张维睿
作者单位:浙江大学地球科学系,杭州 310027
基金项目:国际科学基金(IFS)
摘    要:观察了三种吸附剂吸附亚砷酸根离子过程中溶液pH值随时间的变化。氢氧化铁在吸附过程中的pH值变化大致可分为三个阶段,0~6分钟为第一阶段,体系的pH值快速上升,指示亚砷酸根置换了固相中的氢氧根;7~40分钟为第二阶段,pH值变化不大,指示Fe(OH)3凝胶对亚砷酸根离子的吸附达到动态平衡;40分钟后为第三阶段,溶液的pH值呈单边下降趋势,这一阶段吸附剂与被吸附的阴离子之间发生了缩合反应,并释放出H+。Mg-Al-LDO在吸附亚砷酸根的反应过程中pH值持续上升,它具有从水溶液中获取阴离子以恢复其前驱体结构的能力,这一反应中有氢氧根生成;Mg-Fe-LDO兼有前两者的吸附机理,吸附反应过程pH值的变化趋势此介于二者之间。氢氧化铁在加热前后吸附容量变化不大,25?C和90?C时分别为69.7mg/g和73.7mg/g,而Mg-Al-LDO和Mg-Fe-LDO的吸附容量在25?C时分别为62.4mg/g和82.5mg/g,在90?C时分别增加到114.9 mg/g和199.0 mg/g。Mg-Al-LDO和Mg-Fe-LDO在90?C条件下吸附容量的大幅增加,可能和溶解CO2的干扰被抑制有关。

关 键 词:亚砷酸根  吸附反应  pH变化  氢氧化铁  双金属氧化物
文章编号:1006-7493(2006)02-0228-06
收稿时间:2005-10-21
修稿时间:2005-12-09

pH Variation as Indicator for the Reaction between Arsenite and Absorbents
YE Ying,JI Shan-shan,WU Dai-dai,ZHANG Wei-rui.pH Variation as Indicator for the Reaction between Arsenite and Absorbents[J].Geological Journal of China Universities,2006,12(2):228-233.
Authors:YE Ying  JI Shan-shan  WU Dai-dai  ZHANG Wei-rui
Institution:Department of Earth Science, Zhejiang University, Hangzhou 310027, China
Abstract:Three types of absorbents, ferric hydroxide, Mg-Al layered double oxide (Mg-Al-LDO) and Mg-Fe layered double oxide (Mg-Fe-LDO) were studied for their absorption on arsenite. Initial pH value of NaAsO2 solution is 9.71. After ferric hydroxide being added, the pH variation with time can be divided into 3 stages: in the first 6 minutes, pH increased from 9.71 to 10.36, which indicated that OH- from the solid phase was released into the solution; during the 7 to 40 minutes, pH changed only a little between 10.36-10.34, which indicated that the absorption of ferric hydroxide on AsO2- reached dynamic equilibrium; after 40 minutes, pH value decreased continuously to 9.72 at the 360th minute, which was caused by the condensation reaction between arsenite and the absorbent, H+ was released as a result. During the absorption of Mg-Al-LDO on arsenite, pH values increased with time continuously, this is because that Mg-Al-LDO takes anions from the solution to recover the crystal structure of its precursor, in this reaction hydroxyl is formed. It is found that Mg-Fe-LDO has double absorption effects on arsenite as shown by ferric hydroxide and Mg-Al-LDO, for that its pH-time curve is between the two absorbents. The absorption capacity of ferric hydroxide on arsenite changed a little with temperature, from 69.7mg/g at 25℃ to 73.7mg/g at 90℃. Absorption capacity of Mg-Al-LDO and Mg-Fe-LDO increased apparently when the medium was heated, from 62.4mg/g and 82.5mg/g at 25℃, to 114.9mg/g and 199.0mg/g at 90℃ respectively. Ascending absorption capacity of Mg-Al-LDO and Mg-Fe-LDO on arsenite at 90℃ is quite possibly because that the competition from carbonic anion on arsenite is suppressed by heating, which expelled dissolved CO2 from the solution.
Keywords:Arsenite  absorption  pH variation  ferric hydroxide  LDO
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