Identyfikatory
Warianty tytułu
Języki publikacji
Abstrakty
The rock mass disturbed by mining activities in a copper ore mine has a structure consisting of thick layers of predominantly high mechanical parameters. The layers, due to their strength properties and dimensions, have low deformability which influences a vast area in the form of increased stresses. This area is a part of a rock massif where dynamic destruction periodically occurs in particular fragments as the post-mining cavity expands. The size of such an identified fragment of the rock mass depends on the extent of goafs and the distance between them and mining operations as well as inhomogeneities and confinement in the rock massif. The specific structure of the overlying layers, especially their mechanical properties, determine, to a vast extent, the cracks of anthropogenic influence in the rock massif, which result in foci of seismic tremors often recorded far from the areas of conducted mining activities. A selection of seismic tremors for their spatial location, related to the conducted mining operations and the time of their occurrence, can be useful for forecasting areas which determine seismic hazards in the area of mining operations. The aspect of the analysis of seismic tremors recorded in Division G-23 may indicate the location of the areas of the rock mass which remains in a state of boundary energy balance until another portion of seismic energy is released ‘stabilizing’ the area containing this rock mass. The article presents results of the analysis of a set of tremors between 2013 and 2015, induced by mining activities in Division G-23, in order to forecast areas of seismic activity in the rock mass disturbed by mining operations.
Wydawca
Czasopismo
Rocznik
Tom
Strony
31--37
Opis fizyczny
Bibliogr. 13 poz.
Twórcy
autor
- Department of Rockburst and Rock Mechanics, Central Mining Institute, 40-166 Katowice, Plac Gwarkow 1, Poland
Bibliografia
- 1. Burtan, Z. (2012). Wpływ eksploatacji w rejonach zaburzeń tektonicznych o dużych zrzutach na kształtowanie się zagrożenia sejsmicznego w kopalniach Legnicko-Głogowskiego Okręgu Miedziowego [Impacts of mining operations in the tectonically disturbed regions with dislocations of considerable thrust on seismic hazard levels in copper mines in the Legnica-Głogów Copper Fields (LGOM region)]. Kraków: Wydawnictwo AGH.
- 2. Butra, J. (2010). Eksploatacja złoża rud miedzi w warunkach zagrożenia tąpaniami i zawałami [Mining copper ore deposits under rockburst and caving hazard]. Wrocław: Cuprum Centrum Badawczo-Rozwojowe.
- 3. Drzewiecki, J. (2013). Próba zdefiniowania obszarów akumulacji energii w górotworze na podstawie lokalizacji ognisk wstrząsów sejsmicznych [An attempt to define the areas of energy storage in the subsurface on the basis of seismic outbreaks location]. CUPRUM. Czasopismo Naukowo-Techniczne Górnictwa Rud, (1), 5-15.
- 4. Drzewiecki, J. (2015). Zmienność obszaru aktywności sejsmicznej indukowanej eksploatacją oddziału wydobywczego KGHM Polska Miedź SA [The variability of the seismic activity area induced by the exploitation of the mining division of KGHM Polska Miedz SA]. CUPRUM. Czasopismo Naukowo-Techniczne Górnictwa Rud, (4), 77-88.
- 5. Dubiński, J. (1997). Effectiveness of geophysical methods for assessment of rock mass state. In Z. Rakowski (Ed.), Proceedings of the International Conference Geomechanics 96, Roznov P.R. (Czech Republic), 3-6 September 1996 (pp. 19-26). Rotterdam: Balkema.
- 6. Dubiński, J., Drzewiecki, J. (2013). The model of rock mass destruction in conditions of exploitation of copper ore deposit. Paper presented at the World Mining Congress, 11-15 August, Montreal, Canada.
- 7. Dubiński, J., Lurka, A., & Mutke, G. (2013). Seismic hazard assessment using bendray and rectilinear passive tomography in the Polkowice-Sieroszowice cooper mine. In Proceedings of 8th International Symposium on Rockburst and Seismicity in Mines, 1-7 September 2013, St. Petersburgh (pp. 137-144). Perm, Russia: Inter-YES Ltd.
- 8. Gibowicz, S. J., & Kijko, A. (1994). Introduction to mining seismology. San Diego: Academic Press.
- 9. Gogolewska, A., & Bartlewska, M. (2004). Profilaktyka tąpaniowa w wybranych oddziałach eksploatacyjnych O/ZG „Polkowice-Sieroszowice” KGHM „Polska Miedź” SAw latach 2001-2003 [Rockburst prevention in selected mining panels of “Polkowice-Sieroszowice” copper mine in 2001-2003]. Prace Naukowe Instytutu Górnictwa Politechniki Wrocławskiej. Studia i Materiały, 106(30), 55-71.
- 10. Lurka, A., & Mutke, G. (2008). Poprawa dokładności lokalizacji składowej pionowej hipocentrów wstrząsów górniczych [Improvement of vertical component location of seismic events in underground mines]. Gospodarka Surowcami Mineralnymi, 24(2/3), 261-270.
- 11. Machoń, T. (2013). Aktywność sejsmiczna w kopalniach rud miedzi KGHM Polska Miedź SA w latach 1970-2011 [Seismic activity in copper mines of KGHM Polska Miedz SA between 1970 and 2011]. Przegląd Górniczy, 69(12), 81-88.
- 12. Regulation of the Minister of Internal Affairs and Administration (2002). Rozporządzenie Ministra Spraw Wewnętrznych i Administracji z dnia 14 czerwca 2002 r. w sprawie zagrożeń naturalnych w zakładach górniczych [Regulation of the Minister of Internal Affairs and Administration of June, 14, 2002 on natural hazards in mining plants. Journal of Laws no. 94, item 841].
- 13. Stec, K. (2009). Characteristics of the processes taking place at the sources of high energy tremors occurring in the Upper Silesian coal Basin in Poland e regional character of the phenomenon. In C. Tang (Ed.), Controlling seismic hazard and sustainable development of deep mines. Proceedings of 7th International Symposium on Rockburst and Seismicity in Mines, 21-23 August 2009 (Vol. 1, pp. 415-426). New York: Rinton Press.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-2bf868b1-701e-41c4-b4e5-484aa5c98d29