首页 | 本学科首页   官方微博 | 高级检索  
     

神府矿区活鸡兔矿井烧变岩水文地质特征
引用本文:牛建国. 神府矿区活鸡兔矿井烧变岩水文地质特征[J]. 煤田地质与勘探, 2001, 29(1): 37-39.
作者姓名:牛建国
作者单位:1.陕西煤田地质局 185队 陕西 榆林 719000
摘    要:烧变岩是活鸡兔矿井的顶板充水含水层,直接威胁着矿井的生产安全。烧变岩分布广泛,裂隙发育程度在垂向上规律明显:下剧—中强—上弱。其富水性除受构造、地形和地貌的控制外,还决定于是否接受其他含水层的补给。烧变岩水水质良好,符合国家饮用水标准,供排结合是矿井水综合利用的有效方法。

关 键 词:烧变岩  水文地质条件  活鸡兔矿井
文章编号:1001-1986(2001)01-0037-02
收稿时间:1999-12-17
修稿时间:1999-12-17

Hydrogeological characteristics of burnt rock in Huojitu Mine,Shenfu Mining Area
NIU Jian-guo. Hydrogeological characteristics of burnt rock in Huojitu Mine,Shenfu Mining Area[J]. COAL GEOLOGY & EXPLORATION, 2001, 29(1): 37-39.
Authors:NIU Jian-guo
Affiliation:1.No.185 Team, Shaanxi Bureau of Coal Geology, Yulin 719000, China
Abstract:The coal seam roof of Huojitu Mine is the burnt rock,which is the water impregnated aquifer,is dangerous to mine safety.The burnt rock distributed widely.The regularities of fracture development are vertically apparant,for example,the fractrues decrease upwards.The water abundance of the rock is controlled not only by structures,geographic and surface features,but also controlled by the recharge condition from other aquifer.The water quality of the rock can meet the drinking water standards of the state.Therefore,the water control combining dewatering and water supply is the effective way.
Keywords:burnt rock  hydrogeological conditions  Huojitu Mine  
本文献已被 CNKI 维普 万方数据 等数据库收录!
点击此处可从《煤田地质与勘探》浏览原始摘要信息
点击此处可从《煤田地质与勘探》下载全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号