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电感耦合等离子体质谱仪测定可可西里冰芯样品中超痕量Cd和Pb
引用本文:李月芳,王宁练,姚檀栋. 电感耦合等离子体质谱仪测定可可西里冰芯样品中超痕量Cd和Pb[J]. 冰川冻土, 2002, 24(1): 93-97. DOI: 10.3969/j.issn.1000-0240.2002.01.016
作者姓名:李月芳  王宁练  姚檀栋
作者单位:中国科学院, 寒区旱区环境与工程研究所冰芯与寒区环境重点实验室, 甘肃, 兰州, 730000
基金项目:国家自然科学基金;49801004;
摘    要:介绍了利用电感耦合等离子体质谱仪(ICPMS)直接测定冰芯样品中超痕量重金属Cd和Pb的实验和分析方法,用国家一级标准溶液进行分析过程中的质量控制.仪器对测定浓度在20~100ng·L-1之间Pb的分析精度<10%,对浓度在5~100ng·L-1Cd的分析精度<10%,标准加入回收率在85%~107%之间.Cd和Pb的检测下限分别为0.62ng·L-1和0.15ng·L-1.初步探索了冰芯外部被污染部分的去除方法,给出了实验结果,并利用此方法对青藏高原马兰冰川的一根22m深冰芯进行了处理,分析了其中的Cd和Pb的浓度。

关 键 词:电感耦合等离子体质谱法  痕量元素Cd和Pb  冰芯样品  
文章编号:1000-0240(2002)01-0093-05
收稿时间:2001-03-04
修稿时间:2001-03-04

Directly Determining Cd and Pb in Ice Core of Hoh Xil Region by Inductively Coupled Plasma Mass Spectrometry
LI Yue-fang,WANG Ning-lian,YAO Tan-dong. Directly Determining Cd and Pb in Ice Core of Hoh Xil Region by Inductively Coupled Plasma Mass Spectrometry[J]. Journal of Glaciology and Geocryology, 2002, 24(1): 93-97. DOI: 10.3969/j.issn.1000-0240.2002.01.016
Authors:LI Yue-fang  WANG Ning-lian  YAO Tan-dong
Affiliation:Key Laboratory of Ice cCore and Cold Regions Environment, CAREERI, CAS, Lanzhou Gansu 730000, China
Abstract:A new directly determining Cd and Pb in ice core with ng·L-1 level by Inductively Coupled Plasma Mass Spectrometry (ICP-MS) is presented in this paper. The procedures of labware cleaning and the preparing standard solution are described. The blank values are also showed in order to illustrate the reliability of labware cleaning. The determined concentration is in the range of 5 to 200 ng·L-1. Solutions with national standard certificate are used to insure the reliability of the determining. The blank value of Cd is less than 2 ng·L-1 and that of Pb is less than 10 ng·L-1, respectively. For individual determining, the precision for both Cd and Pb is less 10%. The precision among several determined values for a individual concentration value is less 5% for Cd and <10% for Pb, respectively. The recovery determined from standard solutions is in the range of 85%~107%. The limit of detection is 0.15 ng·L-1 for Cd and 0.62 ng·L-1 for Pb, respectively, based on ten repeatedly determined blank values. The decontamination method is described, and the concentration of Cd and Pb decreases from the outside to the inner of a core, showing proficiency in the decontamination.;Concentrations of Cd and Pb changing with depth of Malan Ice Core drilled in Hoh Xil of Qinghai Province are also presented. The concentration of Cd is in the range of 0.399~14.735 ng·L-1 with a mean value of 4.6 ng·L-1; the concentration of Pb is in the range of 9~51 ng·L-1 with a mean value of 20 ng·L-1. No obvious change trend of concentrations with depth is found.
Keywords:trace Cd and Pb  ice core samples  directly determining by ICP
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