Szczegóły publikacji
Opis bibliograficzny
Monitoring post-mining surface uplift induced by mine flooding using EGMS and PSInSAR: a case study from the Upper Silesian Coal Basin (Poland) / Violetta Sokoła-Szewioła, Paweł SOPATA, Dawid Mrocheń // Remote Sensing [Dokument elektroniczny]. — Czasopismo elektroniczne ; ISSN 2072-4292 . — 2026 — vol. 18 iss. 10 art. no. 1548, s. 1–23. — Wymagania systemowe: Adobe Reader. — Bibliogr. s. 22–23, Abstr. — Publikacja dostępna online od: 2026-05-13. — D. Mrocheń - afiliacja: Strata Mechanics Research Institute, Polish Academy of Sciences, Kraków
Autorzy (3)
- Sokoła-Szewioła Violetta
- AGHSopata Paweł
- Mrocheń Dawid
Słowa kluczowe
Dane bibliometryczne
| ID BaDAP | 168088 |
|---|---|
| Data dodania do BaDAP | 2026-06-03 |
| Tekst źródłowy | URL |
| DOI | 10.3390/rs18101548 |
| Rok publikacji | 2026 |
| Typ publikacji | artykuł w czasopiśmie |
| Otwarty dostęp |  |
| Creative Commons | |
| Czasopismo/seria | Remote Sensing |
Abstract
This study investigates vertical surface displacements in an area previously impacted by extensive underground hard coal extraction, specifically focusing on the closed “Kazimierz-Juliusz” mine in the Upper Silesian Coal Basin (Poland). The cessation of mining operations and formal decommissioning do not necessarily signify the termination of ground instability; rather, the discontinuation of mine water pumping triggers a progressive groundwater rebound within the rock mass. This hydrogeological shift leads to a redistribution of stresses in the geological structure, inducing deformation processes that manifest as surface uplift. This research aims to characterize the temporal evolution and magnitude of post-closure surface elevation changes by integrating satellite radar interferometry with conventional geodetic surveys. The analysis, spanning a 28-month observation period, utilizes both Persistent Scatterer Interferometry (PSInSAR) and European Ground Motion Service (EGMS) data, complemented by precise geometric leveling. The results reveal a low-magnitude deformation process, with detected uplift rates reaching approximately 1 cm/year. The synergistic integration of InSAR-based monitoring and classical geodesy allowed for robust cross-validation, significantly enhancing the reliability of the findings both qualitatively and quantitatively.
