论文部分内容阅读
潘一矿区位于华北平原安徽省淮南市潘谢矿区,突水含水层较多,有灰岩水、砂岩水、煤系水以及四含水,其中主要为灰岩水、砂岩水。矿井突水是煤矿地区五大灾害之一(桂和荣,2005),判断突水含水层受到广泛的关注。利用水化学特征离子判别来判断主要突水含水层取得丰硕的成果,如阿克苏地区地下水化学特征及其形成原因分析运用TDS和各离子的相关性分
Panyi Mining Area is located in Pan Xie Mining Area, Huainan City, Huabei Plain, North China Plain. There are many inrush aquifers, including limestone, sandstone, coal series and four types of water, mainly limestone and sandstone. Water inrush from coal mines is one of the five major disasters in coal mines (Gui He-rong, 2005). Judging water inrush aquifers has received widespread attention. The use of water chemical characteristic ion discrimination to determine the main water inrush aquifer has achieved fruitful results, such as the chemical characteristics of groundwater in the Aksu area and the formation of reasons for the analysis of the use of TDS and ion correlation