Abstract

In this work, the analysis of TerraSAR-X satellite images combining both conventional and advanced Differential Synthetic Aperture Radar Interferometry (DInSAR) approaches has proven to be effective to detect and monitor fast evolving mining subsidence on urban areas in the Upper Silesian Coal Basin (Poland). This region accounts for almost three million inhabitants where mining subsidence has produced severe damage to urban structures and infrastructures in recent years. Conventional DInSAR approach was used to generate 28 differential interferograms between 5 July 2011 and 21 June 2012 identifying 31 subsidence troughs that account up to 245 mm of displacement in 54 days (equivalent to 1660 mm/year). SqueeSARTM processing yielded a very dense measurement point distribution, failing to detect faster displacements than 330 mm/year, which occur within the subsidence troughs detected with conventional DInSAR. Despite this limitation, this approach was useful to delimit stable areas where mining activities are not conducted and areas affected by residual subsidence surrounding the detected subsidence troughs. These residual subsidence mining areas are located approximately 1 km away from the 31 detected subsidence troughs and account for a subsidence rate greater than 17 mm/year on average. The validation of this methodology has been performed over Bytom City were underground mining activity produced severe damages in August 2011. Conventional DInSAR permitted to successfully map subsidence troughs between July and August 2011 that coincide spatially and temporally with the evolution of underground mining excavations, as well as with the demolition of 28 buildings of Karb district. Additionally, SqueeSARTM displacement estimates were useful to delimit an area of 8.3 km2 of Bytom city that is affected by a residual mining subsidence greater than 5 mm/year and could potentially suffer damages in the midterm. The comparison between geodetic data and SqueeSARTM for the common monitoring period yields and average absolute difference of 7 mm/year, which represents 14% of the average displacement rate measured by the geodetic benchmarks. These results demonstrate that the combined exploitation of high-resolution satellite SAR data through both conventional and advanced DInSAR techniques could be crucial to monitor fast evolving mining subsidence, which may severely impact highly populated mining areas such as the Upper Silesia Coal Basin (USCB).

Highlights

  • Subsidence is one of the most important hazards related to underground mining activities

  • Conventional Differential Synthetic Aperture Radar Interferometry (DInSAR) uses pairs of Synthetic Aperture Radar (SAR) images acquired over the same area at different times to generate maps of ground deformation, exploiting the fact that difference in the phase is eventually proportional to surface deformation [35,36]

  • The conventional DInSAR processing strategy has yielded 28 interferograms with 11 days interval (Table 2). Such maps, notwithstanding the fact that are affected by some atmospheric artifacts, are employed for a large-scale motion survey, determining the position, extent, contour, and approximate velocity of mining areas

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Summary

Introduction

Subsidence is one of the most important hazards related to underground mining activities. The impact of mining subsidence depends on many factors related to the type and the size of the mine, the type and the size of the structure, as well as the subsidence rate itself. Due to their complexity, values of critical ground movements have not been determined analytically. The surface area potentially affected by mining subsidence, subsidence trough, is greater than the area worked in the seam. The boundary of this surface is defined by the angle of draw or angle of influence, which extends upwards and outwards from the working face and varies from 8° to 45° depending on the coalfield [2,3]. In Poland mining subsidence phenomena has been studied by [4,5,6,7,8,9]

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