| Issue |
E3S Web Conf.
Volume 15, 2017
The 1st Scientific Practical Conference “International Innovative Mining Symposium (in memory of Prof. Vladimir Pronoza)”
|
|
|---|---|---|
| Article Number | 01002 | |
| Number of page(s) | 6 | |
| Section | Perspective Mining Technologies | |
| DOI | https://doi.org/10.1051/e3sconf/20171501002 | |
| Published online | 07 April 2017 | |
The influence of advancing speed of powered mining stope with single face on earth’s surface displacing in Kuzbass
1 T.F. Gorbachev Kuzbass State Technical University, Department of underground facilities and mines constructing and resource deposits mining, Vesennyaya St. 28, Kemerovo city, Russian Federation
2 LLC SIGI (Siberian Institute of Geotechnical Research), 653033, Prokopievsk, 11 Gagarina st., Russian Federation
* Corresponding author: raa@kuzstu.ru
The researches in the area of undermined rock massifs estimate the influence of advancing speed of mining stopes on earth’s surface shift-ing ambiguously. It reflects the lack of maturity of this trend. The aim of this paper is to establish the relationship between subsidence of individual points on the surface profile line along strike and the speed of stope’s advancing, taking into account other influencing factors. Dependencies of displacement of certain points of the earth’s surface undermined during mining operations can be identified by frequency instrumental observations on the profile lines. Further analysis is made by mathematical methods, in-cluding the random number theory. In the formation of the dynamic downfold of displacement the relationship between advancing speed and subsiding of individual points in the “behind the face” half-downfold can-not be traced. In the “front face” half-downfold the increase of mining stope advancing speed reduces dynamic subsidence. In the paper empirical relationships between subsidence of individual points on the surface and the position of the working face were shown.
© The Authors, published by EDP Sciences, 2017
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.
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