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    水中氢氧稳定同位素分析技术及其影响因素的研究进展

    Research Progress on Stable Isotope Analysis Techniques of Hydrogen and Oxygen in Water and Their Influencing Factors

    • 摘要: 水中氢氧稳定同位素分析在水文、地质、生态等领域的应用日趋广泛,然而不同介质样品的分析方法和效果存在明显差异。相较于传统的同位素比质谱法(IRMS),同位素比红外光谱法(IRIS)因分析快速、成本低、前处理简单等优势,已成为当前水中氢氧稳定同位素分析的首选方法。IRIS虽然在纯水或简单基质样品中可达到与IRMS相当的精度,但在分析油田废水、垃圾渗滤液、石油场地水、植物与土壤提取液等复杂样品时,挥发性有机质会导致分析精密度与准确度明显下降。系统综述了水中氢氧稳定同位素分析技术(IRMS和IRIS),比较了其优缺点,总结了记忆效应与基质效应对分析精度的影响,重点探讨了高矿化度与高有机质样品在采用IRIS技术分析时存在的问题以及解决对策,并对未来研究方向进行展望,以期为不同样品水中氢氧稳定同位素分析方法的选择与同位素应用效果评估提供参考(引用文献62篇)。

       

      Abstract: The application of hydrogen and oxygen stable isotope analysis of water in fields including hydrology, geology, and ecology was increasingly expanded. However, significant differences were observed in the analytical methods and effects of samples from different matrices. Compared with the traditional isotope ratio mass spectrometry (IRMS), isotope ratio infrared spectroscopy (IRIS) was recognized as the preferred method for current hydrogen and oxygen stable isotope analysis of water due to its advantages of rapid analysis, low cost, and simple pretreatment. IRIS achieves precision comparable to IRMS in pure water or simple matrix samples, but significant decreases in analytical precision and accuracy were caused by volatile organic matters when complex samples including oilfield wastewater, landfill leachate, petroleum-contaminated site water, and plant/soil extracts were analyzed. A systematic review of stable isotope analysis techniques of hydrogen and oxygen in water (IRMS and IRIS) was conducted. Their advantages and disadvantages were compared, and the impacts of memory effect and matrix effect on analytical precision were summarized. The problems and countermeasures of high-salinity and high-organic-matter samples analyzed by IRIS technique were focused on, and prospects for future research directions were put forward. This review was intended to provide references for the selection of analytical methods for hydrogen and oxygen stable isotopes in water from different samples and the evaluation of isotope application effects (62 ref. cited).

       

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