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我段管辖邯长线康城站,位于邯长线K21+200～K22+645处,20m深的路堑之中。地质条件不良,系泥质页岩夹砂岩组成,表层风化严重,地下水位高,终年不断,即便在严重干旱年份,也水流不止,以致自1973年交付运营以来翻浆冒泥长期得不到解决。为了摸清地下水的来源,我们曾作了大量调查,并于1981年3月聘请了邯郸矿务局水文地质专家前往康城站进行了调查。最后
I section under the jurisdiction of Han long-term station Cannes, is located in Han long line K21 +200 ~ K22 +645, 20m deep in the cutting. Poor geological conditions, composed of shale shale sandstone, serious surface weathering and high groundwater level, continue all year long. Even in the severe drought years, the water flow is more than normal. As a result, the mud and mud have not been solved since its delivery in 1973. In order to find out the source of groundwater, we conducted a large number of investigations. In March 1981, we employed a Handan Mining Bureau hydrogeology expert to conduct a survey at Cannes Station. At last