基于膜进样质谱仪测定海水溶解无机碳方法优化

Optimization of the Method for Determining Dissolved Inorganic Carbon in Seawater Based on Membrane Inlet Mass Spectrometry

  • 摘要: 海洋溶解无机碳(Dissolved Inorganic Carbon, DIC)的快速、准确测定对海洋碳酸盐体系研究至关重要。膜进样质谱仪(MIMS)因其能够高效测定溶解性气体,目前已成功用于海水中多种溶解性气体的测定,这一特点也为DIC分析提供了新的技术途径。本研究基于自组装MIMS发展了一种海水DIC测定方法,优化了海水DIC测定条件,并同步使用MIMS法和非色散红外法测定了南海水体样品中的DIC浓度。结果表明:当进样流速控制在0.85 mL∙min−1,进样时间为3 min,进样温度为20 ℃,酸化条件为添加20 μL 30% H2SO4时,MIMS测定海水DIC的精密度良好(变异系数可达0.2%);与非色散红外法测定结果吻合良好(回归斜率为1.018、R2=0.994),可满足海水DIC样品的测定要求。本研究发展了一种高效率的基于MIMS的海水DIC测定方法,该方法具有良好的实验室推广应用前景,可为膜进样质谱技术在海水碳循环研究领域的应用提供新的技术支撑。

     

    Abstract: The rapid and accurate determination of marine dissolved inorganic carbon (DIC) is crucial for the study of marine carbonate systems. Since membrane-introduction mass spectrometer (MIMS) can efficiently measure dissolved gases, it has been successfully applied to the determination of various dissolved gases in seawater. This feature also offers a new technical approach for DIC analysis. In this study, a method for the determination of seawater DIC was developed based on a self-assembled MIMS, and the determination conditions for seawater DIC were optimized. Meanwhile, MIMS and non-dispersive infrared methods were synchronously used to measure DIC concentrations in seawater samples collected from the South China Sea. The results indicate that when the sample flow rate is controlled at 0.85 mL∙min−1, the injection time is 3 min, the sample temperature is 20 ℃, and the acidification condition is the addition of 20 μL of 30% H2SO4, The precision of seawater DIC measurement by MIMS is satisfactory (the coefficient of variation can reach 0.2%); the results are in good agreement with those obtained by the non-dispersive infrared method (regression slope of 1.018, R2=0.994), which can meet the determination requirements for seawater DIC samples. This study develops an efficient MIMS-based method for seawater DIC determination. The method possesses promising prospects for laboratory popularization and application and can provide new technical support for the application of membrane-introduction mass spectrometry in the research field of seawater carbon cycle.

     

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