首页 | 本学科首页   官方微博 | 高级检索  
     检索      

元素分析仪-同位素比值质谱仪测定海洋沉积物有机碳稳定同位素方法初探
引用本文:张媛媛,贺行良,孙书文,朱志刚.元素分析仪-同位素比值质谱仪测定海洋沉积物有机碳稳定同位素方法初探[J].岩矿测试,2012,31(4):627-631.
作者姓名:张媛媛  贺行良  孙书文  朱志刚
作者单位:1. 国土资源部海洋油气资源与环境地质重点实验室,山东青岛266071;青岛海洋地质研究所,山东青岛266071
2. 中国海洋大学海洋化学理论与工程技术教育部重点实验室,山东青岛,266100
基金项目:中国地质大调查项目(1212011120271)
摘    要:初步建立了利用元素分析仪-同位素比值质谱仪(EA-IRMS)联用技术测定海洋沉积物中有机碳稳定同位素的方法。标定了标准工作参考气CO2(δ13CvsPDB为-32.053‰);验证了仪器的稳定性,标准偏差为0.009‰;当离子流强度范围为0.4~8.7 V时,总体线性为0.0337‰/V,小于仪器线性指标0.06‰/V的要求;同时测定了国家标准物质GBW 04408、国际标准物质Urea和海洋沉积物样品M01的精密度和准确度,标准偏差在0.04‰~0.13‰范围内;并在三家实验室进行了测量比对实验,标准偏差小于0.20‰,满足地质样品再现性0.5‰的要求。所选样品区域δ13Corg范围为-25.29‰~-22.30‰,表明该海域总有机碳是陆源和海源两种来源的混合物。

关 键 词:海洋沉积物  有机碳稳定同位素  元素分析仪-同位素比值质谱法
收稿时间:2011/12/8 0:00:00

A Preliminary Study on the Determination of Organic Carbon Stable Isotope of Marine Sediment by Element Analyzer-Isotope Ratio Mass Spectrometer
ZHANG Yuan-yuan,HE Xing-liang,SUN Shu-wen and ZHU Zhi-gang.A Preliminary Study on the Determination of Organic Carbon Stable Isotope of Marine Sediment by Element Analyzer-Isotope Ratio Mass Spectrometer[J].Rock and Mineral Analysis,2012,31(4):627-631.
Authors:ZHANG Yuan-yuan  HE Xing-liang  SUN Shu-wen and ZHU Zhi-gang
Institution:Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology, Ministry of Land and Resources, Qingdao 266071, China;Qingdao Institute of Marine Geology, Qingdao 266071, China;Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology, Ministry of Land and Resources, Qingdao 266071, China;Qingdao Institute of Marine Geology, Qingdao 266071, China;Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao 266100, China;Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology, Ministry of Land and Resources, Qingdao 266071, China;Qingdao Institute of Marine Geology, Qingdao 266071, China
Abstract:Element Analyzer-Isotope Ratio Mass Spectrometer(EA-IRMS) technology was applied to determine organic carbon stable isotopes of marine sediment.Pure CO2 reference gas was calibrated via GBW 04408,and the δ13CvsPDB value of pure CO2 was determined to be-32.053‰.The stability and linearity of the EA-IRMS system were tested and verified through several experimental comparisons.The standard deviation of stability was 0.009‰.When ion intensities ranged from 0.4 to 8.7 V,the linearity of EA-IRMS system was 0.0337‰/V which was less than the requirement of linearity proxy of 0.06‰/V.Moreover,the precision and accuracy of the results for the national standard material of GBW 04408,international standard material of Urea and marine sediment sample of M01 were measured.The standard deviation was 0.13‰.The marine sediment samples were measured at three different labs.The standard deviation of the comparison results was less than 0.20‰ and met the need of reproducibility of 0.5‰.The TOC contents from marine sediment samples ranged from 0.13‰ to 1.11‰,with δ13Corg values ranging from-25.29‰ to-22.30‰,which indicate the derivation of organic matter from mixed terrestrial and marine organic materials.
Keywords:marine sediment  organic carbon stable isotope  Element Analyzer-Isotope Ratio Mass Spectrometry
本文献已被 CNKI 万方数据 等数据库收录!
点击此处可从《岩矿测试》浏览原始摘要信息
点击此处可从《岩矿测试》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号