In-situ sampling for krypton-85 groundwater dating

• Published in: Journal of hydrology: X 2021-05, Vol.11, p.100075, Article 100075
• Main Authors: Musy, Stéphanie, Meyzonnat, Guillaume, Barbecot, Florent, Hunkeler, Daniel, Sültenfuss, Jürgen, Solomon, D. Kip, Purtschert, Roland
• Format: Article
• Language: English
• Subjects: Dating; Groundwater; Noble gases; Sampling Methodology; Tracers
• ISSN: 2589-9155; 2589-9155
• DOI: 10.1016/j.hydroa.2021.100075

•An innovative groundwater sampling method was developed for radio noble gases.•This method is an attractive alternative to conventional packer sampling.•In-situ sampling is a simple and inexpensive method for age stratigraphy assessment.•The method minimizes the disturbance of the natural groundwater flow field.•The age information from active and passive sampling is discussed in a pilot study. 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.