Abstract :
[en] This study assesses hydrogeological hazards in the Saint-Vaast region, Belgium, impacted by three decades of deformation post-coal mine closure. Using Persistent Scatterer Interferometric Synthetic Aperture Radar (PS-InSAR) applied to 30 years of Synthetic Aperture Radar (SAR) data along with geological investigations and 13 years of piezometric well data, we analysed subsurface dynamics leading to environmental hazards in the region. We focused on identifying key periods of significant deformation pattern changes. The soft Wealden terrains (Lower Cretaceous) are characterized by alternating sandstones, clay, and sand facies, composing the sedimentary roof of an old mine drainage adit dug at 30 m depth. The presence of this mined adit structure is contributing to the current vulnerability of the region. Especially, when the abandoned mine drainage adit was filled with water following the cessation of pumping. Due to an increase in the water level in the Wealden aquifer below the gallery, natural groundwater flow paths and pressures have increased over time. At least two significant mudflow outbursts, in 2009 and 2018, occurred. This study shows that both events were correlated with changes in water level and deformation. Moreover, results suggest a new phase of rising water levels and ground uplift due to increased pressure in the Wealden aquifer. A crucial outcome of this research is the assessment of the potential for another similar incident soon, informed by the correlation analysis of water level and ground displacement time series.
Funding text :
We extend our profound appreciation to the European Space Agency (ESA) for the provision of ERS1/2, Envisat ASAR, and Sentinel-1 A radar data, which were instrumental in our research. Our heartfelt thanks also go to the Scientific Institute of Public Service (ISSeP) for their invaluable contribution to piezometric data and hydrogeologic reports. Additionally, we are grateful for the support from the BELSPO Brain-funded LASUGEO project (monitoring LAnd SUbsidence caused by Groundwater exploitation through gEOdetic measurements), which underpinned this study.
Scopus citations®
without self-citations
1