Risk assessment method of coal seam floor water inrush based on the combination of gray correlation and fdahp
A coal seam floor water inrush, gray correlation technology, applied in the direction of instruments, data processing applications, calculations, etc., can solve problems such as lack of scientific analysis and separation from objective reality
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Embodiment 1
[0097] figure 1 It is a flow chart of a method for evaluating the risk of water inrush from a coal seam floor provided by the present invention. figure 1 In, the inventive method comprises the steps:
[0098] (1) Determine the main controlling factors of water inrush from the coal seam floor;
[0099] Controlling factors, including:
[0100] ① geological structure;
[0101] ②Thickness of effective waterproof layer;
[0102] ③Thickness percentage of brittle rock under mine pressure failure zone;
[0103] ④Water inflow from borehole;
[0104] ⑤Aquifer thickness;
[0105] ⑥Aquifer water pressure.
[0106] Further, the geological structure is a fault strength index.
[0107] Further, the geological structure is the density of fault intersections and pinch-out points.
[0108] Further, the geological structure is the fractal value of the fold axis.
[0109] (2) Data collection and standardization processing, and the establishment of thematic maps of the main controlling f...
Embodiment 2
[0169] The 13th coal seam is currently being mined in a certain mining area, and the Ordovician aquifer is relatively close to the 13th coal seam, which constitutes the main water-filled aquifer for the mining of the 13th coal seam. The Benxi Formation and Taiyuan Formation strata between the Ordovician and the 13th coal seam constitute the aquitard formation. The total thickness of the Ordovician limestone aquifer in this area is more than 800 m. There are a total of 30 downhole hydrological drilling holes in the well field to expose Austrian ash, and the water inflow from the drilling holes is 0-110m 3 / h, it can be seen that Austrian ash is extremely water-rich but the distribution is extremely uneven. Due to the existence of fractures and fissures, as well as the fissures produced by mining activities on the floor damage the integrity of the water-resisting layer group, the Austrian ash confined water may flow into the mining face along these channels under pressure. Dur...
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