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海洋沉积物中孔隙水的氯同位素测量方法研究
引用本文:李艳平,蒋少涌,杨涛,濮巍.海洋沉积物中孔隙水的氯同位素测量方法研究[J].高校地质学报,2006,12(3):388-391.
作者姓名:李艳平  蒋少涌  杨涛  濮巍
作者单位:1.南京大学地球科学系内生金属矿床成矿机制研究国家重点实验室,南京210093;2.南京大学海洋地球化学研究中心,南京210093
基金项目:国家高技术研究发展计划(863计划) , 天然气水合物探测技术项目 , 国家自然科学基金
摘    要:采用Ba型、H型和Cs型三步阳离子交换树脂法,对海洋沉积物中孔隙水的氯进行了分离和提纯。氯的回收率达99.6%,能满足氯同位素质谱测定的需要。氯同位素的测量采用基于Cs2Cl^+离子的高精度正热电离质谱法,对ISL354NaCI标准物质的多次测量结果为”CI/”CI=0.319130±0.000029,对一个南海海底沉积物中孔隙水的多次测量结果为^37CI/^35CI=0.319144±0.000043,表明此方法的稳定性好,测量精度高,可用于海洋沉积物中孔隙水的氯同位素示踪研究

关 键 词:  同位素测定  正热电离质谱法  海洋沉积物孔隙水
文章编号:1006-7493(2006)03-0388-04
收稿时间:2006-06-22
修稿时间:2006-06-26

Analytical Method of Chlorine Isotopic Composition in the Marine Sediment Porewaters
LI Yan-ping,JIANG Shao-yong,YANG Tao,PU Wei.Analytical Method of Chlorine Isotopic Composition in the Marine Sediment Porewaters[J].Geological Journal of China Universities,2006,12(3):388-391.
Authors:LI Yan-ping  JIANG Shao-yong  YANG Tao  PU Wei
Institution:1. State Key Laboratory for Mineral Deposits Research, Department of Earth Sciences, Nanjing University, Nanjing 210093, China; 2. Center for Marine Geochemistry Research, Nanjing University, Nanjing 210093, China
Abstract:A simple technique using three step cation-exchanges (Ba-type, H-type, and Cs-type)was used to enrich and purify CI from the sediment porewater samples. The recovery of CI is better than 99.6%. After purification, the ^37CI/^35CI ratios of porewater samples were measured using positive ion thermal ionization mass spectrometry based on the measurement of Cs2Cl^+ ion with graphite load. The measured results for both the NaCI standard and one porewater sample show that the method has high stability and high precision (0.09 -0.13‰). Initial results for porewater sampled from the South China Sea reveal significant -δ^37 Cl variation, and it may have great implications for further gas hydrate exploration in the area
Keywords:chlorine  isotope ratio measurement  positive ion thermal ionization mass spectrometry  marine sediment porewater
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