Issue |
E3S Web Conf.
Volume 35, 2018
Scientific-Research Cooperation between Vietnam and Poland (POL-VIET 2017)
|
|
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Article Number | 04003 | |
Number of page(s) | 8 | |
Section | Geodesy and mining surveying | |
DOI | https://doi.org/10.1051/e3sconf/20183504003 | |
Published online | 23 March 2018 |
Vertical Displacement of the Surface Area over the Leakage to the Transverse salt Mine in 1992–2012
AGH University Science and Technology, Faculty of Mining Surveying and Environmental Engineering, A. Mickiewicza Av. 30, 30-059 Krakow, Poland
* Corresponding author: lipecki@agh.edu.pl
The leakage of water in the salt mine caused considerable deformation of the surface. This article shows the vertical displacement in the area of leakage to the mine excavation, measured by precision leveling, carried out from the first days of leakage in 1992 until 2012. The geological and hydrogeological conditions of the mine, as well as the associated water hazards were described, which in conjunction with the inconvenient location of the excavation site in the northern frontage of the Carpathians and also inadequately conducted mining operations, contributed to the risk of flooding mine. The analysis of the vertical movements of the surface – subsidence and uplift – were present as well as the process of formation of the depression trough in the form of maps and graphs. The analyzes were based on 49 measurement series, starting from the first days of the disaster within the next 20 years. The course of development of the depression trough and the condition of the surface after stopping the water from the rock mass has been shown, which caused the surface to uplift.
Key words: salt mining / surveying / subsidence monitoring
© The Authors, published by EDP Sciences, 2018
This is an Open Access article distributed under the terms of the Creative Commons Attribution License 4.0, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. (http://creativecommons.org/licenses/by/4.0/).
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