Szczegóły publikacji
Opis bibliograficzny
Application of geotechnical monitoring tools for deformation analysis in the vicinity of the Dębina salt dome (Bełchatów mine, Poland) : technical note / Marek CAŁA, Joanna JAKÓBCZYK, Katarzyna CYRAN // Engineering Geology ; ISSN 0013-7952. — 2017 — vol. 230, s. 130–141. — Bibliogr. s. 141, Abstr. — Publikacja dostępna online od: 2017-10-07
Autorzy (3)
Słowa kluczowe
Dane bibliometryczne
| ID BaDAP | 110067 |
|---|---|
| Data dodania do BaDAP | 2017-12-05 |
| Tekst źródłowy | URL |
| DOI | 10.1016/j.enggeo.2017.09.027 |
| Rok publikacji | 2017 |
| Typ publikacji | artykuł w czasopiśmie |
| Otwarty dostęp |  |
| Czasopismo/seria | Engineering Geology |
Abstract
The presence of the Dębina salt dome (DSD) entails new challenges for the exploitation of the Bełchatów lignite (brown coal) deposit. Poland is the 5th largest world lignite producer (63.1 Mt). The Bełchatów open-pit mine provides more than a half of the brown coal production capacity in Poland. The geological structure of the Bełchatów area is complex due to tectonic and sedimentation processes, as well as to the presence of the DSD, which determines rather unique geological conditions in comparison to other brown coal mines. Halokinetic processes connected with rising of the DSD contributed to shaping the present lignite seams form. Brown coal extraction in such a complex environment endangers stability of pit wall slopes. The long-term mining of the Bełchatów coal field and relaxation processes are factors that influence the development of both vertical and horizontal displacements. Of particular concern is the stability of the Bełchatów western pit wall slope, outlining the necessity of a comprehensive geotechnical monitoring effort. A geodetic network aimed at measuring vertical displacements was installed above the salt dome. In order to measure horizontal displacements, borehole inclinometers were also installed on several mine benches. The analysis of vertical displacements revealed that the eastern part of the dome has been uplifted, while the southern, south-eastern and northern parts have undergone subsidence. Our study of horizontal displacements indicated zones of potential shear movements. The deformations were primarily connected with changes in geometry and steepening of the Bełchatów western pit slope. However, relaxation processes caused a change in the primary stress conditions of the DSD and may have triggered the halokinetic salt movement.
