首页> 外文期刊>Rapid Communications in Mass Spectrometry: RCM >Continuous analysis of δ ~(18)O and δD values of water by diffusion sampling cavity ring-down spectrometry: A novel sampling device for unattended field monitoring of precipitation, ground and surface waters
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Continuous analysis of δ ~(18)O and δD values of water by diffusion sampling cavity ring-down spectrometry: A novel sampling device for unattended field monitoring of precipitation, ground and surface waters

机译:扩散采样腔衰荡光谱法连续分析水的δ〜(18)O和δD值:一种用于无人值守现场监测降水,地下水和地表水的新型采样装置

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摘要

A novel sampling device suitable for continuous, unattended field monitoring of rapid isotopic changes in environmental waters is described. The device utilises diffusion through porous PTFE tubing to deliver water vapour continuously from a liquid water source for analysis of δ ~(18)O and δD values by Cavity Ring-Down Spectrometry (CRDS). Separation of the analysed water vapour from non-volatile dissolved and particulate contaminants in the liquid sample minimises spectral interferences associated with CRDS analyses of many aqueous samples. Comparison of isotopic data for a range of water samples analysed by Diffusion Sampling-CRDS (DS-CRDS) and Isotope Ratio Mass Spectrometry (IRMS) shows significant linear correlations between the two methods allowing for accurate standardisation of DS-CRDS data. The internal precision for an integration period of 3 min (standard deviation (SD) = 0.1 % and 0.3 % for δ ~(18)O and δD values, respectively) is similar to analysis of water by CRDS using an autosampler to inject and evaporate discrete water samples. The isotopic effects of variable air temperature, water vapour concentration, water pumping rate and dissolved organic content were found to be either negligible or correctable by analysis of water standards. The DS-CRDS system was used to analyse the O and H isotope composition in short-lived rain events. Other applications where finely time resolved water isotope data may be of benefit include recharge/discharge in groundwater/river systems and infiltration-related changes in cave drip water.
机译:描述了一种新颖的采样装置,其适合于连续,无人值守的现场监测环境水域中快速的同位素变化。该设备利用通过多孔PTFE管的扩散来连续不断地从液态水源输送水蒸气,以通过腔衰荡光谱分析(CRDS)分析δ〜(18)O和δD值。将分析后的水蒸气与液体样品中的非挥发性溶解污染物和颗粒污染物分离,可以将与许多水性样品的CRDS分析相关的光谱干扰降至最低。通过扩散采样-CRDS(DS-CRDS)和同位素比质谱(IRMS)分析的一系列水样品的同位素数据比较显示,两种方法之间存在显着的线性相关性,从而可以实现DS-CRDS数据的准确标准化。积分时间为3分钟的内部精度(对于δ〜(18)O和δD值,标准偏差(SD)分别为0.1%和0.3%)类似于使用自动进样器进样和蒸发的CRDS分析水离散水样。通过水标准分析,发现可变的气温,水蒸气浓度,水抽速和溶解的有机物含量的同位素影响可以忽略不计或可以校正。 DS-CRDS系统用于分析短期降雨事件中的O和H同位素组成。精细解析时间同位素数据可能会带来好处的其他应用包括地下水/河流系统中的补给/排放以及溶洞滴水中与渗透有关的变化。

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