Abstract

Abstract. The salt mining industrial exploitation located in Vauvert (France) has been injecting water at high pressure into wells to dissolve salt layers at depth. The extracted brine has been used in the chemical industry for more than 30 years, inducing a subsidence of the surface. Yearly leveling surveys have monitored the deformation since 1996. This dataset is supplemented by synthetic aperture radar (SAR) images, and since 2015, global navigation satellite system (GNSS) data have also continuously measured the deformation. New wells are regularly drilled to carry on with the exploitation of the salt layer, maintaining the subsidence. We make use of this careful monitoring by inverting the geodetic data to constrain a model of deformation. As InSAR and leveling are characterized by different strengths (spatial and temporal coverage for InSAR, accuracy for leveling) and weaknesses (various biases for InSAR, notably atmospheric, very limited spatial and temporal coverage for leveling), we choose to combine SAR images with leveling data, to produce a 3-D velocity field of the deformation. To do so, we develop a two-step methodology which consists first of estimating the 3-D velocity from images in ascending and descending acquisition of Sentinel 1 between 2015 and 2017 and second of applying a weighted regression kriging to improve the vertical component of the velocity in the areas where leveling data are available. GNSS data are used to control the resulting velocity field. We design four analytical models of increasing complexity. We invert the combined geodetic dataset to estimate the parameters of each model. The optimal model is made of 21 planes of dislocation with fixed position and geometry. The results of the inversion highlight two behaviors of the salt layer: a major collapse of the salt layer beneath the extracting wells and a salt flow from the deepest and most external zones towards the center of the exploitation.

Highlights

  • Rock salt is a sedimentary rock formed by the evaporation of seawater under specific conditions at different geological times

  • We propose a methodology to combine InSAR and leveling data to produce a 3-D velocity field associated with the salt extraction of Vauvert (Doucet, 2018)

  • We can compute the weighted rms (WRMS) from McCaffrey (2005), which gives an estimation of the a posteriori weighted scatter in the fit

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Summary

Introduction

Rock salt (halite) is a sedimentary rock formed by the evaporation of seawater under specific conditions at different geological times. Halite deposits are located underground or inside mountains, though some can be found on the surface in arid regions. They mainly contain crystals of sodium chlorite (NaCl) but can include impurities such as clay, anhydrite, or calcite. The buried layers of rock salt can be dissolved by injecting water during the so-called solution mining process. This process is used to extract salt in the form of brine (for the chemical industry). Solution mining aims at creating salt caverns for the storage of fossil fuels such as natural gas, oil, and petroleum products (refined fuels, liquefied gas) and for the storage of hydrogen and compressed air (Donadei and Schneider, 2016)

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