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离子色谱-柱切换法测定土壤浸出液中的氟离子
引用本文:姜新华,倪承珠,朱彬和,赵训燕,陈素清,吕伟德,张嘉捷,张培敏,李刚,朱岩.离子色谱-柱切换法测定土壤浸出液中的氟离子[J].色谱,2016,34(4):442-446.
作者姓名:姜新华  倪承珠  朱彬和  赵训燕  陈素清  吕伟德  张嘉捷  张培敏  李刚  朱岩
作者单位:1. 浙江衢化医院, 浙江衢州 324004; 2. 浙江大学化学系, 浙江杭州 310028; 3. 台州学院医药化工学院, 浙江台州 317000; 4. 杭州职业技术学院临江学院, 浙江杭州 310018; 5. 绍兴市环境监测中心站, 浙江绍兴 312000
基金项目:国家重大科学仪器设备开发专项(2012YQ09022903);浙江省微量有毒化学物健康风险评估技术研究重点实验室项目(2014006,2014007);浙江省自然科学基金项目(LZ16B050001,LY15B050001,LY12B05003,LQ13B050001,LY13B020001);浙江省公益性技术应用研究(分析测试)项目(2015C37022).
摘    要:建立了离子色谱-柱切换测定土壤浸出液中氟离子的方法。使用柱切换技术,将样品通过高聚物反相色谱柱进行在线预处理,分离氟离子和小分子有机酸,同时除去水溶性有机杂质,采用收集环收集氟离子并进入分析系统分析,消除了测定氟离子时普遍存在的干扰问题。分析系统的淋洗液为KOH溶液,流速为1.0 mL/min,采用抑制性电导检测,外标法定量。氟离子的线性范围为0.05~10.0 mg/L,相关系数为0.9999,加标回收率为103.4%~105.3%,相对标准偏差为2.0%~2.1%,检出限 (S/N=3)为5.50 μg/L。该方法适用于测定复杂基体样品中的氟离子。

关 键 词:氟离子  浸出液  离子色谱  土壤  柱切换  
收稿时间:2015-12-22

Determination of fluoride in soil water extract by ion chromatography with column-switching technique
JIANG Xinhua,NI Chengzhu,ZHU Binhe,ZHAO Xunyan,CHEN Suqing,LV Weide,ZHANG Jiajie,ZHANG Peimin,LI Gang,ZHU Yan.Determination of fluoride in soil water extract by ion chromatography with column-switching technique[J].Chinese Journal of Chromatography,2016,34(4):442-446.
Authors:JIANG Xinhua  NI Chengzhu  ZHU Binhe  ZHAO Xunyan  CHEN Suqing  LV Weide  ZHANG Jiajie  ZHANG Peimin  LI Gang  ZHU Yan
Institution:1. Zhejiang Quhua Hospital, Quzhou 324004, China; 2. Department of Chemistry, Zhejiang University, Hangzhou 310028, China; 3. School of Pharmaceutical and Chemical Engineering, Taizhou University, Taizhou 317000, China; 4. School of Linjiang, Hangzhou Vocational & Technical College, Hangzhou 310018, China; 5. Shaoxing Environmental Monitoring Central Station, Shaoxing 312000, China
Abstract:A new method was proposed for the determination of fluoride in soil water extract by ion chromatography with column-switching technique. A reversed-phase column was used as a pretreatment column on-line to separate fluoride and organic acids as well as to eliminate organics. Fluoride was collected by a collection loop and delivered to the analytical system. Under the optimum conditions, the linear range of the method for fluoride was 0.05-10.0 mg/L (r=0.9999), and the limit of detection (S/N=3) was 5.50 μg/L. The recovery was in the range of 103.4%-105.3% with the relative standard deviation of 2.0%-2.1%. The method could be applied to determine fluoride in complicated samples.
Keywords:column-switching  fluoride  ion chromatography (IC)  soil  water extract  
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