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Degassing behavior of noble gases from groundwater during groundwater sampling

机译:地下水采样期间地下水中高贵气体的脱气行为

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摘要

Noble gases dissolved in groundwater have been used to evaluate characteristics such as origin, residence time and recharge temperature. Although obtaining samples without degassing is highly desired, in certain cases, degassing during sampling is unavoidable. This study investigated the degassing behavior of noble gases during sampling and evaluated the correction methods that can be applied. Groundwater samples were obtained from an underground laboratory and a deep borehole. The amount of exsolved gas was estimated by comparing pressurized and non-pressurized samples. Henry's model, which assumes equilibrium between gas and water, and a diffusion model were applied to the results. In addition, the compositions of gases extracted into an evacuated vessel or hollow fiber contactor were also compared with those of pressurized groundwater samples. The results indicated that significant degassing occurred in unpressurized samples, but equilibrium was achieved between gas and water when the total dissolved gas pressure (TDGP) was relatively small (up to 4.2 atm). Therefore, the d'(Ne) value, defined as the difference between the Ne concentration of air-saturated water and a sample normalized by the Ne concentration of air-saturated water, could be used in Henry's model to correct exsolution. However, inclusion of the effects of excess air and contamination is problematic. However, when TDGP was high (32 atm in this study), the degassing behavior completely changed and could not be predicted by Henry's model. During extraction of noble gases using an evacuated vessel and hollow fiber contactor, degassing was observed to take place following the diffusion model. As a result, fractionation between Ne vs. Kr and Xe was significant. Thus, although we could extract dissolved Ne with a high recovery ratio (over 0.85), the ratios of Kr/Ne and Xe/Ne were found to be significantly smaller than those in groundwater. The gases extracted by an evacuated vessel or hollow fiber conta
机译:溶解在地下水中的惰性气体已用于评估起源,停留时间和充电温度等特性。尽管在某些情况下,非常需要在不脱气的情况下获得样品,但在某些情况下,取样过程中脱气是不可避免的。本研究研究了在取样过程中惰性气体的脱气行为,并评估了可以应用的校正方法。地下水样品是从地下实验室和深层钻孔中获得的。通过比较加压和非加压样品来估计exsolved气体的量。亨利的模型,假设气体和水之间的平衡和扩散模型应用于结果。此外,还与加压地下水样品的含量提取到抽空容器或中空纤维接触器中的气体组合物。结果表明,在整个溶解气体压力(TDGP)相对较小的(高达4.2atm)时,在气体和水之间实现显着脱气,但在气体和水之间实现平衡。因此,D'(NE)值定义为呼吸饱和水的NE浓度与通过饱和水的NE浓度标准化的样品之间的差异,可用于Henry模型以纠正exolution。然而,包含过量空气和污染的影响是有问题的。然而,当TDGP高(本研究中的32个ATM)时,脱气行为完全改变,无法通过亨利模型预测。在使用抽空的容器和中空纤维接触器提取惰性气体期间,观察到在扩散模型之后进行脱气。结果,Ne与KR和XE之间的分馏是显着的。因此,尽管我们可以用高回收率(超过0.85)提取溶解的NE,但发现KR / NE和XE / NE的比率明显小于地下水中的比率。通过抽空的容器或中空纤维CONTA提取的气体

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  • 作者单位

    Cent Res Inst Elect Power Ind Civil Engn Res Lab 1646 Abiko Abiko Chiba 2701194 Japan;

    Cent Res Inst Elect Power Ind Civil Engn Res Lab 1646 Abiko Abiko Chiba 2701194 Japan;

    Univ Utah Dept Geol &

    Geophys 115 S 1460 E RM 205 Salt Lake City UT 84112 USA;

    Japan Atom Energy Agcy Horonobe Underground Res Ctr 432-2 Hokushin Horonobe Chou Hokkaido 0983224 Japan;

    Cent Res Inst Elect Power Ind Civil Engn Res Lab 1646 Abiko Abiko Chiba 2701194 Japan;

    Cent Res Inst Elect Power Ind Civil Engn Res Lab 1646 Abiko Abiko Chiba 2701194 Japan;

    IAEA Isotope Hydrol Lab Vienna Int Ctr A-1400 Vienna Austria;

    Japan Atom Energy Agcy Tono Geosci Ctr 1-64 Yamanouchi Akiyo Cho Mizunami City Gifu 5096132 Japan;

    Japan Atom Energy Agcy Tono Geosci Ctr 1-64 Yamanouchi Akiyo Cho Mizunami City Gifu 5096132 Japan;

    Geol Survey Japan Groundwater Res Grp Inst Georesources &

    Environm Natl Inst Adv Ind Sci &

    Technol AIST AIST Tsukuba Cent 7 1-1-1 Higashi Tsukuba Ibaraki 3058567 Japan;

    Geol Survey Japan Groundwater Res Grp Inst Georesources &

    Environm Natl Inst Adv Ind Sci &

    Technol AIST AIST Tsukuba Cent 7 1-1-1 Higashi Tsukuba Ibaraki 3058567 Japan;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地球化学;
  • 关键词

    Groundwater; Noble gases; Degassing; Henry's model; Diffusion model;

    机译:地下水;惰性气体;脱气;亨利的模型;扩散模型;

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