Determination of Trace Elements in Thermomineral Waters of a High Altitude Area by Inductively Coupled Plasma-Mass Spectrometry

The mineralization extent of thermomineral water in Tibet is relatively high, together with high altitude and low air pressure, resulting in the differences in the working conditions of Inductively Coupled Plasma-Mass Spectrometry (ICP-MS) and Inductively Coupled Plasma-Optical Emission Spectrometry...

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Main Authors: JIANG Zhen-zhen, LIU Gao-ling, WANG Zhu, LI Ming-li, ZHUOMA QU-xi, SHAO Bei, DONG Rui, WANG Wei
Format: Article
Language:English
Published: Science Press, PR China 2016-09-01
Series:Yankuang ceshi
Subjects:
Online Access:http://www.ykcs.ac.cn/en/article/doi/10.15898/j.cnki.11-2131/td.2016.05.005
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author JIANG Zhen-zhen
LIU Gao-ling
WANG Zhu
LI Ming-li
ZHUOMA QU-xi
SHAO Bei
DONG Rui
WANG Wei
author_facet JIANG Zhen-zhen
LIU Gao-ling
WANG Zhu
LI Ming-li
ZHUOMA QU-xi
SHAO Bei
DONG Rui
WANG Wei
author_sort JIANG Zhen-zhen
collection DOAJ
description The mineralization extent of thermomineral water in Tibet is relatively high, together with high altitude and low air pressure, resulting in the differences in the working conditions of Inductively Coupled Plasma-Mass Spectrometry (ICP-MS) and Inductively Coupled Plasma-Optical Emission Spectrometry (ICP-OES) between Tibet and low altitude areas. Therefore, the measuring method in low altitude areas cannot be used in Tibet. By optimizing the working conditions of the instrument, adding internal standard, and establishing an interference correction equation, the influences of low pressure and hyper-salinity are eliminated. Simultaneous determination of 12 trace elements in thermomineral water by ICP-MS was developed in this study. At the same time, the radioactive element uranium in thermomineral water was also detected. Correlative factors of the calibration curve were all above 0.9995. The detection limits of this method were 0.012-0.128 μg/L, the relative standard deviations were 1.2%-6.8%, and the recoveries of spiked samples were 95.7%-106.5%. Combining with previous findings of this program, ICP-MS is more suitable for measuring trace elements in thermomineral water of hyper-salinity, while ICP-OES is suitable for the determination of major elements. The combination of these two methods can form a system of analytical techniques of thermomineral water in high altitude areas.
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spelling doaj.art-ddfa3f6372fa43c6a6182f9febf178a32023-02-09T01:25:48ZengScience Press, PR ChinaYankuang ceshi0254-53572016-09-0135547548010.15898/j.cnki.11-2131/td.2016.05.005ykcs-35-5-475Determination of Trace Elements in Thermomineral Waters of a High Altitude Area by Inductively Coupled Plasma-Mass SpectrometryJIANG Zhen-zhen0LIU Gao-ling1WANG Zhu2LI Ming-li3ZHUOMA QU-xi4SHAO Bei5DONG Rui6WANG Wei7Central Laboratory of Bureau of Geology and Exploration Tibet, Lhasa 850033, ChinaCentral Laboratory of Bureau of Geology and Exploration Tibet, Lhasa 850033, ChinaCentral Laboratory of Bureau of Geology and Exploration Tibet, Lhasa 850033, ChinaCentral Laboratory of Bureau of Geology and Exploration Tibet, Lhasa 850033, ChinaCentral Laboratory of Bureau of Geology and Exploration Tibet, Lhasa 850033, ChinaCentral Laboratory of Bureau of Geology and Exploration Tibet, Lhasa 850033, ChinaChaidamu Qingyuan Fan Mei Technology Co. Ltd, Chaidamu 817000, ChinaChaidamu Qingyuan Fan Mei Technology Co. Ltd, Chaidamu 817000, ChinaThe mineralization extent of thermomineral water in Tibet is relatively high, together with high altitude and low air pressure, resulting in the differences in the working conditions of Inductively Coupled Plasma-Mass Spectrometry (ICP-MS) and Inductively Coupled Plasma-Optical Emission Spectrometry (ICP-OES) between Tibet and low altitude areas. Therefore, the measuring method in low altitude areas cannot be used in Tibet. By optimizing the working conditions of the instrument, adding internal standard, and establishing an interference correction equation, the influences of low pressure and hyper-salinity are eliminated. Simultaneous determination of 12 trace elements in thermomineral water by ICP-MS was developed in this study. At the same time, the radioactive element uranium in thermomineral water was also detected. Correlative factors of the calibration curve were all above 0.9995. The detection limits of this method were 0.012-0.128 μg/L, the relative standard deviations were 1.2%-6.8%, and the recoveries of spiked samples were 95.7%-106.5%. Combining with previous findings of this program, ICP-MS is more suitable for measuring trace elements in thermomineral water of hyper-salinity, while ICP-OES is suitable for the determination of major elements. The combination of these two methods can form a system of analytical techniques of thermomineral water in high altitude areas.http://www.ykcs.ac.cn/en/article/doi/10.15898/j.cnki.11-2131/td.2016.05.005inductively coupled plasma-mass spectrometryhigh altitude areathermomineral waterhyper-salinitytrace elements
spellingShingle JIANG Zhen-zhen
LIU Gao-ling
WANG Zhu
LI Ming-li
ZHUOMA QU-xi
SHAO Bei
DONG Rui
WANG Wei
Determination of Trace Elements in Thermomineral Waters of a High Altitude Area by Inductively Coupled Plasma-Mass Spectrometry
Yankuang ceshi
inductively coupled plasma-mass spectrometry
high altitude area
thermomineral water
hyper-salinity
trace elements
title Determination of Trace Elements in Thermomineral Waters of a High Altitude Area by Inductively Coupled Plasma-Mass Spectrometry
title_full Determination of Trace Elements in Thermomineral Waters of a High Altitude Area by Inductively Coupled Plasma-Mass Spectrometry
title_fullStr Determination of Trace Elements in Thermomineral Waters of a High Altitude Area by Inductively Coupled Plasma-Mass Spectrometry
title_full_unstemmed Determination of Trace Elements in Thermomineral Waters of a High Altitude Area by Inductively Coupled Plasma-Mass Spectrometry
title_short Determination of Trace Elements in Thermomineral Waters of a High Altitude Area by Inductively Coupled Plasma-Mass Spectrometry
title_sort determination of trace elements in thermomineral waters of a high altitude area by inductively coupled plasma mass spectrometry
topic inductively coupled plasma-mass spectrometry
high altitude area
thermomineral water
hyper-salinity
trace elements
url http://www.ykcs.ac.cn/en/article/doi/10.15898/j.cnki.11-2131/td.2016.05.005
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