scholarly journals Effects of torpedo blasting on rockburst prevention during deep coal seam mining in the Upper Silesian Coal Basin

2017 ◽  
Vol 9 (4) ◽  
pp. 694-701 ◽  
Author(s):  
Ł. Wojtecki ◽  
P. Konicek ◽  
J. Schreiber
2013 ◽  
Vol 58 (4) ◽  
pp. 1163-1176 ◽  
Author(s):  
Mirosław Wierzbicki

Abstract This paper presents the results of studies on gas sorption performed by means of the gravimetric method. The tests were performed on two coal samples of different metamorphism degrees, came from two regions of Upper Silesian Coal Basin, Poland. The changes in sorption capacity of coals were measured in the pressure range from 0.1 MPa to 17 MPa and in temperatures ranging from 291K to 333K. Coal of a lower coalification degree was a better methane sorbent. Changes in sorption capacity of tested coals were linearly dependent on the temperature. The increase in temperature of 10K reduces the Langmuir sorption of about 0.7-0.8 [cm3/g]. Such increase of temperature causes a nonlinear increase of the Langmuir pressure (b-1). These results showed that the rise of rock temperature, caused by geothermal gradient, can induce a significant increase of equilibrium pressure of methane in coal seam. An increase of coal seam temperature may cause an increase of gas and coal outburst risk in a coal mine.


Author(s):  
Łukasz Wojtecki ◽  
Iwona Gołda ◽  
Maciej J. Mendecki

Abstract Underground coal seam mining has been carried out in the Upper Silesian Coal Basin, Poland, for many years and with a simultaneous increase in exploitation depth. Frequently, coal seams are not fully extracted due to numerous reasons which lead to their edges and remnants remaining in the rock mass. Even in the case of the full extraction of a coal seam, mining usually ends at the border of a protecting pillar to protect underground or surface objects, sometimes at the border of the mining area, or some distance from the old goaf or high throw fault. Extraction of subsequent coal seams in an analogous range results in a cluster of coal seam edges remaining. In the vicinity of the mentioned remainders, the disrupted stress distribution is expected. The infraction of the aforementioned equilibrium repeatedly results in the occurrence of strong mining tremors. The observations from the studied coal seam no. 408’s longwall panel indicated that mining works are able to disturb the present stress-strain equilibrium in the area of the edges of other coal seams, even if they are located at a greater vertical distance away. The seismological parameters and distributions have been applied for this purpose.


Terra Nova ◽  
2022 ◽  
Author(s):  
Jerzy Nawrocki ◽  
Justyna Ciesielczuk ◽  
Dominik Jura ◽  
Monika J. Fabiańska ◽  
Magdalena Misz‐Kennan

Author(s):  
S. K. Baymukhametov ◽  
A. Zh. Imashev ◽  
F. A. Mullagaliev ◽  
L. F. Mullagalieva ◽  
K. S. Kolikov

2020 ◽  
Author(s):  
Justyna Ciesielczuk ◽  
Jerzy Nawrocki ◽  
Dominik Jura ◽  
Monika J. Fabiańska ◽  
Magdalena Misz-Kennan ◽  
...  

Sign in / Sign up

Export Citation Format

Share Document