The determination of 52 elements in marine geological samples by an inductively coupled plasma optical emission spectrometry and an inductively coupled plasma mass spectrometry with a high-pressure closed digestion method
Gao Jingjing1,2,3; Liu Jihua2,3; Li Xianguo1; Yan Quanshu2,3; Wang Xiaojing2,3; Wang Hongmin2,3
刊名ACTA OCEANOLOGICA SINICA
2017-01
卷号36期号:1页码:109-117
关键词marine geological sample high-pressure closed digestion method inductively coupled plasma optical emission spectrometry inductively coupled plasma mass spectrometry major element minor element trace element
ISSN号0253-505X
DOI10.1007/s13131-017-0991-5
英文摘要An improved analytical method to determine the content of 52 major, minor and trace elements in marine geological samples, using a HF-HCl-HNO3 acid system with a high-pressure closed digestion method (HPCD), is studied by an inductively coupled plasma optical emission spectrometry (ICP-OES) and an inductively coupled plasma mass spectrometry (ICP-MS). The operating parameters of the instruments are optimized, and the optimal analytical parameters are determined. The influences of optical spectrum and mass spectrum interferences, digestion methods and acid systems on the analytical results are investigated. The optimal spectral lines and isotopes are chosen, and internal standard element of rhodium is selected to compensate for matrix effects and analytical signals drifting. Compared with the methods of an electric heating plate digestion and a microwave digestion, a high-pressure closed digestion method is optimized with less acid, complete digestion, less damage for digestion process. The marine geological samples are dissolved completely by a HF-HCl-HNO3 system, the relative error (RE) for the analytical results are all less than 6.0%. The method detection limits are 2-40 g/g by the ICP-OES, and 6-80 ng/g by ICP-MS. The methods are used to determine the marine sediment reference materials (GBW07309, GBW07311, GBW07313), rock reference materials (GBW07103, GBW07104, GBW07105), and cobalt-rich crust reference materials (GBW07337, GBW07338, GBW07339), the obtained analytical results are in agreement with the certified values, and both of the relative standard deviation (RSD) and the relative error (RE) are less than 6.0%. The analytical method meets the requirements for determining 52 elements contents of bulk marine geological samples.
资助项目Special Basic Research Funds for Central Public Research Institutes for The First Institute of Oceanography, State Oceanic Administration of China[GY0213G06] ; Special Basic Research Funds for Central Public Research Institutes for The First Institute of Oceanography, State Oceanic Administration of China[GY02-2012G35]
WOS研究方向Oceanography
语种英语
出版者SPRINGER
WOS记录号WOS:000391778500013
内容类型期刊论文
源URL[http://ir.fio.com.cn/handle/2SI8HI0U/3268]  
专题业务部门_海洋地质与地球物理研究室
作者单位1.Ocean Univ China, Minist Educ, Key Lab Marine Chem Theory & Technol, Qingdao 266100, Peoples R China;
2.State Ocean Adm, Inst Oceanog 1, Key Lab Marine Sedimentary & Environm Geol, Qingdao 266061, Peoples R China;
3.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao 266061, Peoples R China
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GB/T 7714
Gao Jingjing,Liu Jihua,Li Xianguo,et al. The determination of 52 elements in marine geological samples by an inductively coupled plasma optical emission spectrometry and an inductively coupled plasma mass spectrometry with a high-pressure closed digestion method[J]. ACTA OCEANOLOGICA SINICA,2017,36(1):109-117.
APA Gao Jingjing,Liu Jihua,Li Xianguo,Yan Quanshu,Wang Xiaojing,&Wang Hongmin.(2017).The determination of 52 elements in marine geological samples by an inductively coupled plasma optical emission spectrometry and an inductively coupled plasma mass spectrometry with a high-pressure closed digestion method.ACTA OCEANOLOGICA SINICA,36(1),109-117.
MLA Gao Jingjing,et al."The determination of 52 elements in marine geological samples by an inductively coupled plasma optical emission spectrometry and an inductively coupled plasma mass spectrometry with a high-pressure closed digestion method".ACTA OCEANOLOGICA SINICA 36.1(2017):109-117.
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