Citation: LI Tie-Jun, LI Hong-Wei, LIU Xiu-Jin, FENG Lian-Jun. Stepwise Fluorination Method for Determination of Oxygen Isotopic Ratio of Diatoms[J]. Chinese Journal of Analytical Chemistry, ;2012, 40(12): 1897-1901. doi: 10.3724/SP.J.1096.2012.20497 shu

Stepwise Fluorination Method for Determination of Oxygen Isotopic Ratio of Diatoms

  • Corresponding author: LI Tie-Jun, 
  • Received Date: 10 May 2012
    Available Online: 6 August 2012

    Fund Project: 本文系中国科学院仪器设备功能开发技术创新项目(No.yg2011001)资助 (No.yg2011001)

  • Determination of the δ18O value of diatom can obtain the initial information of its oxygen isotopic composition, and also has favorable application prospects in paleoenvironment, paleontology, petroleum exploration and environmental prediction. We carried out eight-step fluorination experiments with BrF5 reagent on diatom samples and quartz standard to reveal variation of oxygen isotopic composition in different steps. The eight-step fluorination determined the proportion of surface oxygen to be 25%-28%. The δ18O values obtained from the above processes were all around (35.34±0.15)‰. Then we simplified the eight-step fluorination to two-step fluorination. First, we removed the surface oxygen of specific sedimentary diatoms, and then totally fluoridated the samples. The difference of δ18O values from eight-step and two-step fluorination experiments on the same samples was only 0.3‰. The accuracy of measurement has reached or preceded the repeated measurement error of ±0.5‰ in the international studies. On the basis of many conditional experiments, the stepwise fluorination methods on the diatoms were established. For diatom samples with weight of a mg, the 0.392 aK mL (K=0.18) BrF5 were loaded in the first step, and heated to 550℃ for 1 h; and then five times of theoretical quantity of BrF5 were loaded in the second step after the system regain vacuum, and heated to 550℃ for 3 h. The released oxygen were converted to CO2, and then analysed by MAT-252 to obtain δ18O value of diatom samples.
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