The Potential of Isotopic Tracers for Precise and Environmentally Clean Stream Discharge Measurements

Author:

Picard Antoine1ORCID,Barbecot Florent1ORCID,Bardoux Gérard2,Agrinier Pierre2,Gillon Marina3,Corcho Alvarado José A.4,Schneider Vincent5ORCID,Hélie Jean-François1ORCID,de Oliveira Frédérick1

Affiliation:

1. Geotop-UQAM, Hydro Sciences, Université du Québec à Montréal, CP8888 succ. Centre-Ville, Montreal, QC H3C 3P8, Canada

2. Institut de Physique du Globe de Paris, 1 rue Jussieu, 75005 Paris, France

3. UMR 1114 EMMAH, Avignon Université, 301 rue Baruch de Spinoza, 84916 Avignon, France

4. Spiez Laboratory, Federal Office for Civil Protection, Austrasse, 3700 Spiez, Switzerland

5. Andra, DI/CA/QSE, Service «Qualité Sûreté et Environnement», Centre de l’Aube BP 7, 10200 Soulaines-Dhuys, France

Abstract

Accurate discharge measurement is mandatory for any hydrological study. While the “velocity” measurement method is adapted to laminar flows, the “dilution” method is more appropriate for turbulent streams. As most low-gradient streams worldwide are neither laminar nor turbulent, a methodological gap appears. In this study, we demonstrate that the application of the “dilution” method to a low-gradient small stream gives very satisfactory results in addition to revealing surface/subsurface processes. A variety of chemical and isotopic tracers were injected into the stream (anions, fluorescent dyes, and chloride and hydrogen isotopes). We report the first use of 37Cl for stream discharge measurement and show that 37Cl and 2H can be reliably used as quantitative tracers. Discharge uncertainty calculations show that deuterium is the most accurate tracer method used. We also compare the differences in the tailing part of the restitution curves of tracers and investigate the role of transient surface and hyporheic zones in solute transport in light of a simple transport modelling approach. We conclude that isotopic tracers can be used as “environmentally friendly” tracers for discrete stream discharge measurements and that the application of multi-tracers tests in rivers opens the path to a better understanding of surface–subsurface interaction processes.

Funder

NSERC discovery grant of Florent Barbecot

Publisher

MDPI AG

Subject

Earth-Surface Processes,Waste Management and Disposal,Water Science and Technology,Oceanography

Reference37 articles.

1. Francis, T. (2008). Streamflow Measuremen, CRC Press.

2. WMO (2008). Guide to Hydrological Practice Volume I—From Measurement to Hydrological Information, WMO.

3. Estimating groundwater mean transit time from SF6 in stream water: Field example and planning metrics for a reach mass-balance approach;Jensen;Hydrogeol. J.,2022

4. Quantifying groundwater discharge to Cockburn River, southeastern Australia, using dissolved gas tracers 222Rn and SF6;Cook;Water Resour. Res.,2006

5. Le Coz, J., Camenen, B., Dramais, G., Ribot-Bruno, J., Ferry, M., and Rosique, J.L. (2011). Guide Technique Pour le Contrôle des Débits Réglementaires, ONEMA, Cemagref.

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