單侯礦區(qū)地下徑流賦存規(guī)律分析及煤層開采危險(xiǎn)性評(píng)價(jià)
[Abstract]:The limestone aquifer of the bottom plate of the single weatherfield is developed and the thickness of the bottom layer is unevenly distributed. Under the combined action of limestone water pressure and mining failure, the water inrush accident of bismuth production is carried out. In this paper, the characteristics of water-bearing rock in main mining seam floor and Ordovician limestone in the mine field are studied. Firstly, the geological and hydrogeological characteristics of limestone in the floor of the mining area are analyzed. The results show that the Ordovician aquifer, which has a major influence on coal seam mining, has potential threat to coal seam No. 1 and No. 5. Strong runoff, uneven water rich. By means of water exploration and geophysical analysis, the karst development areas of Ordovician limestone in different mining areas are obtained through detailed exploration of the Ordovician strata. Secondly, the three-dimensional modeling software 3Dmine is used to model and analyze the hydrological behavior of the Ordovician aquifer in the mining area, which provides a convenient condition for more accurate calculation of the area and volume of the flow field in the area. At the same time, according to the spatial relationship between aquifer and coal seam roof and floor, the contour map of water inrush coefficient is established. Finally, a numerical simulation model of water inrush from bottom plate and fault is established according to the relevant parameters. In order to make the model more suitable, the meridian calculation under multiple working conditions is adopted. The calculated results are of great significance to the safety production under the existing mining technology.
【學(xué)位授予單位】:遼寧工程技術(shù)大學(xué)
【學(xué)位級(jí)別】:碩士
【學(xué)位授予年份】:2014
【分類號(hào)】:TD745
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