首页> 外文期刊>Analytical chemistry >Measurement of δ~(18)O, δ~(17)O, and ~(17)O-excess in Water by Off-Axis Integrated Cavity Output Spectroscopy and Isotope Ratio Mass Spectrometry
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Measurement of δ~(18)O, δ~(17)O, and ~(17)O-excess in Water by Off-Axis Integrated Cavity Output Spectroscopy and Isotope Ratio Mass Spectrometry

机译:偏轴积分腔输出光谱法和同位素比质谱法测量水中的δ〜(18)O,δ〜(17)O和〜(17)O含量

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Stable isotopes of water have long been used to improve understanding of the hydrological cycle, catchment hydrology, and polar climate. Recently, there has been increasing interest in measurement and use of the less-abundant ~(17)O isotope in addition to ~2H and ~(18)O. Off-axis integrated cavity output spectroscopy (OA-ICOS) is demonstrated for accurate and precise measurements δ~(18)O, δ~(17)O, and ~(17)O-excess in liquid water. OA-ICOS involves no sample conversion and has a small footprint, allowing measurements to be made by researchers collecting the samples. Repeated (514) high-throughput measurements of the international isotopic reference water standard Greenland Ice Sheet Precipitation (GISP) demonstrate the precision and accuracy of OA-ICOS: δ~(18)O_(VSMOW-SLAP) = -24.74 ± 0.07‰ (1σ) and δ~(17)O_(VSMOW-SLAP) = -13.12 ± 0.05‰ (1σ). For comparison, the International Atomic Energy Agency (IAEA) value for δ~(18)O_(VSMOW-SLAP) is -24.76 ± 0.09‰ (1σ) and an average of previously reported values for δ~(17)O_(VSMOW-SLAP) is -13.12 ± 0.06‰ (1σ). Multiple (26) high-precision measurements of GISP provide a ~(17)O-excess_(VSMOW-SLAP) of 23 ± 10 per meg (1σ); an average of previously reported values for ~(17)O-excess_(VSMOW-SLAP) is 22 ± 11 per meg (1σ). For all these OA-ICOS measurements, precision can be further enhanced by additional averaging. OA-ICOS measurements were compared with two independent isotope ratio mass spectrometry (IRMS) laboratories and shown to have comparable accuracy and precision as the current fluorination-IRMS techniques in δ~(18)O, δ~(17)O, and ~(17)O-excess. The ability to measure accurately δ~(18)O, δ~(17)O, and ~(17)O-excess in liquid water inexpensively and without sample conversion is expected to increase vastly the application of δ~(17)O and ~(17)O-excess measurements for scientific understanding of the water cycle, atmospheric convection, and climate modeling among others.
机译:长期以来,稳定的水同位素已被用来增进对水文循环,集水区水文和极地气候的了解。近年来,除了〜2H和〜(18)O外,人们对测量和使用含量较低的〜(17)O同位素的兴趣也越来越高。离轴集成腔输出光谱(OA-ICOS)被证明可以准确和精确地测量液态水中δ〜(18)O,δ〜(17)O和〜(17)O-过量。 OA-ICOS不涉及样品转换,而且占地面积小,允许研究人员收集样品进行测量。对国际同位素参考水标准格陵兰冰盖降水(GISP)进行的重复(514)高通量测量证明了OA-ICOS的精度和准确性:δ〜(18)O_(VSMOW-SLAP)= -24.74±0.07‰( 1σ)和δ〜(17)O_(VSMOW-SLAP)= -13.12±0.05‰(1σ)。为了进行比较,国际原子能机构(IAEA)的δ〜(18)O_(VSMOW-SLAP)值为-24.76±0.09‰(1σ),是先前报道的δ〜(17)O_(VSMOW-SLAP)的平均值。 SLAP)为-13.12±0.06‰(1σ)。 GISP的多个(26)高精度测量结果提供的〜(17)O-excess_(VSMOW-SLAP)为23±10 / mcg(1σ); 〜(17)O-excess_(VSMOW-SLAP)的先前报告值的平均值为每兆(1σ)22±11。对于所有这些OA-ICOS测量,可以通过附加平均来进一步提高精度。将OA-ICOS测量值与两个独立的同位素比率质谱(IRMS)实验室进行了比较,结果表明,在δ〜(18)O,δ〜(17)O和〜( 17)O过量。廉价且无需样品转换即可准确测量液态水中δ〜(18)O,δ〜(17)O和〜(17)O-过量的能力有望大大提高δ〜(17)O和〜(17)O过量测量,用于科学地了解水循环,大气对流和气候模拟等。

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