Modelling the Mixing Function to Constrain Coseismic
Hydrochemical Effects: An Example from the French Pyrénées |
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Authors: | Jean-Paul Toutain Margot Munoz Jean-Louis Pinaud Stéphanie Levet Matthieu Sylvander Alexis Rigo Jocelyne Escalier |
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Institution: | (1) Observatoire Midi-Pyrénées, LMTG, UMR 5563, 14 Avenue Edouard Belin, 31400 Toulouse, France;(2) BRGM, Orléans, France;(3) Observatoire Midi-Pyrénées, DTP, UMR 5562, 14 Avenue Edouard-Belin, 31400 Toulouse, France |
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Abstract: | Groundwater coseismic transient anomalies are evidenced and characterized by modelling the mixing function F characteristic
of the groundwater dynamics in the Ogeu (western French Pyrénées) seismic context. Investigations of water-rock interactions
at Ogeu indicate that these mineral waters from sedimentary environments result from the mixing of deep waters with evaporitic
signature with surficial karstic waters. A 3-year hydrochemical monitoring of Ogeu springwater evidences that using arbitrary
thresholds constituted by the mean ± 1 or 2σ, as often performed in such studies, is not a suitable approach to characterize transient anomalies. Instead, we have used
a mixing function F calculated with chemical elements, which display a conservative behavior not controlled by the precipitation of a mineral
phase. F is processed with seismic energy release (Es) and effective rainfalls (R). Linear impulse responses of F to Es and R have been calculated. Rapid responses (10 days) to rainwater inputs are evidenced, consisting in the recharge of the shallow
karstic reservoir by fresh water. Complex impulse response of F to microseismic activity is also evidenced. It consists in a 2-phase hydrologic signal, with an inflow of saline water in
the shallow reservoir with a response delay of 10 days, followed by an inflow of karstic water with a response delay of 70
days, the amount being higher than the saline inflow. Such a process probably results from changes in volumetric strain with
subsequent microfracturation transient episodes allowing short inflow of deep salted water in the aquifer. This study demonstrates
that groundwater systems in such environments are unstable systems that are highly sensitive to both rainfall inputs and microseismic
activity. Impulse responses calculation of F to Es is shown to be a powerful tool to identify transient anomalies. Similar processing is suggested to be potentially efficient
to detect precursors of earthquakes when long time-series (5 years at least) are available in areas with high seismicity. |
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Keywords: | Hydrochemical time-series mixing function transient anomalies volumetric strain |
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