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Passive seismic velocity tomography and geostatistical simulation on longwall mining panel

Treść / Zawartość
Identyfikatory
Warianty tytułu
PL
Tomografia pasywna pola prędkości i symulacje geostatystyczne w obrębie pola ścianowego
Języki publikacji
EN
Abstrakty
EN
Generally, the accurate determination of the stress in surrounding rock mass of underground miting area has an important role in stability and ground control. In this paper stress redistribution around the longwall face has been studied using passive seismic velocity tomography based on Simultaneous Iterativa Reconstructive Technique (SIRT) and Sequential Gaussian Simulation (SGS). The mining-induced microseismic events are used as a passive source. Since such sources are used, the ray coverage is insufficient and in order to resolve this deficiency, the wave velocity is estimated in a denser network and by the SGS method. Consequently the three-dimensional images of wave velocity are created and sliced into the coal seam. To analyze the variations of stress around the panel during the study period, these images are interpreted. Results show that the state of stress redistribution around the longwall panel can be deduced from these velocity images. In addition, movements of the stressed zones, including front and side abutments and the goaf area, along the longwall face are evident. The applied approach illustrated in this paper can be used as a useful method to monitoring the stress changes around the longwall face continuously. His can have significant safety implications and contribute to improvements in operational productivity.
PL
Dokładne określenie naprężeń górotworu w warstwach otaczających wyrobiska podziemne ma podstawowe znaczenie dla stabilności i zabezpieczenia powierzchni. W artykule tym zbadano rozkłady naprężeń wokół przodka ścianowego przy wykorzystaniu tomografii pola prędkości, w oparciu o techniki rekonstrukcji przy równoczesnych iteracjach i sekwencyjnej symulacji Gaussa (SSG). Drobne wydarzenia mikrosejsmiczne wykorzystane zostały jako źródła bierne. Z uwagi na wykorzystanie takich źródeł, zasięg promieni jest niewystarczający, dlatego też prędkość fali określana jest przy użyciu gęstszej siatki i w oparciu o metody sekwencyjnej symulacji Gaussa. W rezultacie otrzymujemy trójwymiarowe obrazy prędkości fali, które następnie „narzucane” są warstwami na pokład węgla. Określenie naprężenia wokół pola w trakcie badania wymaga interpretacji tych obrazów. Wyniki wskazują, że rozkład stanu naprężenia wokół ściany można określić na podstawie obrazów prędkości. Ponadto, uwidaczniają się ruchy stref podlegających naprężeniom, w tym warstw sąsiadujących przednich i bocznych oraz obszaru samego wyrobiska wzdłuż przodka ściany. Zastosowane podejście może zostać wykorzystane jako skuteczna metoda bieżącego monitorowania zmian naprężeń w rejonie ściany. Ma to poważne znaczenie z punktu widzenia bezpieczeństwa pracy, a co za tym idzie przyczynia się do podniesienia wydobycia.
Rocznik
Strony
139--155
Opis fizyczny
Bibliogr. 67 poz., rys., wykr.
Twórcy
autor
  • Department of Mining Engineering, Science and Research Branch, Islamic Azad University, Tehran, Iran
autor
  • Stirling University, Stirling, Scotland, UK
autor
  • Department of Mining and Metallurgical Engineering, Amirkabir University of Technology, Tehran, Iran
autor
  • Department of Mining Engineering, Tarbiat Modares University, Tehran, Iran
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Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-8df0443e-c3f6-4fe0-835d-18df661aafda
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