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Changes of hydrogeological conditions in the area of liquidated hard coal mines in the north-eastern part of Upper Silesia Coal Basin (southern Poland)

机译:上硅煤盆地东北部清盘煤矿地区水文地质条件的变化(南波兰)

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Restructuring program that has been introduced since early 90's of the 20th century in the Polish hard coal mining, intensified the process of liquidating hard coal mines mainly in the northern part of the Upper Silesian Coal Basin. Eleven of hard coal, in which exploitation had been terminated in the years 1995-2000, were analysed in detail. Their total mining area was 252,7 km~2. Drainage of the workings in the closed hard coal mines is developed by means of one out of four methods: stationary, deep-well, mixed stationary - deep-well and gravitational. In flooded hard coal mines the rate of rising water table range from 0,04 to 1,28 m/d. The groundwater inflow into the analyzed area was reduced from 258,9 m~3/min (in 1988) to 112,2 m~3/min (in 2004), i.e. by ca. 43,3 percent. The amount of water collected in mine workings flooded till is 48,6 mill m~3 totally.
机译:自20世纪90年代初期以来在波兰硬煤采矿以来,重组计划加剧了主要在煤炭盆地北部的北部灭火煤矿的过程。详细分析了1995 - 2000年临近终止的硬煤11次。他们的矿区总矿区为252,7 km〜2。通过四种方法中的一项制定了封闭式硬煤矿井的工作排水:固定,深井,混合静止 - 深井和引力。在洪水硬煤矿井中,水位的速度范围为0.04至1,28 m / d。进入分析区域的地下水流入从258,9m〜3 / min(1988年)降低至112,2m〜3 / min(2004年),即通过CA。 43,3%。在矿井工作中收集的水量淹没,直到完全达到48,6米米米〜3。

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