氪-85地下水测年的原位取样

IF 3.1 Q2 GEOSCIENCES, MULTIDISCIPLINARY Journal of Hydrology X Pub Date : 2021-05-01 DOI:10.1016/j.hydroa.2021.100075
Stéphanie Musy , Guillaume Meyzonnat , Florent Barbecot , Daniel Hunkeler , Jürgen Sültenfuss , D. Kip Solomon , Roland Purtschert
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引用次数: 2

摘要

氪-85和其他放射性惰性气体被广泛用于地下水测年。85Kr分析需要大量的水才能达到分析要求。通常,这些水被泵送到地面,通过气体抽取系统进行除气。大的抽油速率可能会扰乱自然流场,并且需要大量的现场物流。因此,我们提出了一种新的原位脱气方法,即用膜接触器直接在井中脱气地下水,并在地面收集气体。通过这种方式,可以方便现场工作,将地下水系统干扰降到最低,并在特定深度采集气体样品。我们证明了该系统对大气污染的密封性,收集时间为24小时,这足以用于85Kr的低水平计数和基于激光的计数方法。本研究中提出的原型的最小钻孔直径为7.5厘米,但可以很容易地减小到更小的直径。在一个案例研究中,我们将新被动方法获得的结果与传统封隔器设置采样的结果进行了比较。此外,还收集了两种取样方式下的3H/3He样品,并将测年结果与85Kr的测年结果进行了比较。示踪剂年龄之间有很好的一致性,年龄地层与多孔无承压含水层的预期年龄分布一致。此外,我们的研究强调了不同方法采样的年龄信息之间的差异。综上所述,在大多数情况下,新的原位准被动方法提供了更具代表性的年龄地层。
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In-situ sampling for krypton-85 groundwater dating

Krypton-85 and other radioactive noble gases are widely used for groundwater dating purposes. 85Kr analysis require large volumes of water to reach the analytical requirements. Conventionally, this water is pumped to the surface to be degassed with a gas extraction system. The large pumping rate may disturb the natural flow field and requires substantial field logistics. Hence, we propose a new in-situ degassing method, in which membrane contactors are used to degas the groundwater directly in the well and gas is collected at the surface. This way, field work is facilitated, groundwater system disturbance is minimized, and the gas sample is collected at a specific depth. We demonstrate the tightness of the system regarding atmospheric air contamination for a collection times of 24 h, which is sufficient for both low-level counting and laser-based counting methods for 85Kr. The minimal borehole diameter is 7.5 cm for the prototype presented in this research but can easily be reduced to smaller diameters. In a case study, we compare the results obtained with the new passive method with those from a conventional packer setup sampling. Additionally, 3H/3He samples were collected for both sampling regimes and the dating results were compared with those from 85Kr. A good agreement between tracer ages is demonstrated and the age stratigraphy is consistent with the expected age distribution for a porous unconfined aquifer. In addition, our study emphasizes the differences between the age information sampled with various methods. In conclusion, we demonstrate that the new in situ quasi-passive method provides a more representative age stratigraphy with depth in most cases.

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来源期刊
Journal of Hydrology X
Journal of Hydrology X Environmental Science-Water Science and Technology
CiteScore
7.00
自引率
2.50%
发文量
20
审稿时长
25 weeks
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