矿区寒武系灰岩地下水集中径流带展布及机理分析  

Study on distribution and mechanism of concentrated runoff zone in Cambrian limestone underground water of mining area

在线阅读下载全文

作  者:王心义[1,2] 曹冰琪 王麒[4] 赵彦琦[1] 陈国胜 张平卿[5] 刘小满[1] 

机构地区:[1]河南理工大学资源环境学院,河南焦作454000 [2]中国平煤神马能源化工集团有限责任公司能源化工研究院,河南平顶山467000 [3]开封市通达公路勘察设计有限公司,河南开封475003 [4]华北水利水电大学资源与环境学院,河南郑州450045 [5]平顶山天安煤业股份有限公司地测处,河南平顶山467000

出  处:《煤炭科学技术》2016年第8期35-38,115,共5页Coal Science and Technology

基  金:国家自然科学基金资助项目(41272250);河南省高校科技创新团队支持计划资助项目(15IRTSTHN027)

摘  要:为查明平顶山煤田二矿和吴寨矿寒武系灰岩地下水集中径流带赋存情况,在探明矿区地质断层发育特征的基础上,采用井下连通试验研究了地下水集中径流带的展布及成因和控水作用。研究结果表明:二矿和吴寨矿寒武系灰岩地下水流速达3 320.05 m/d,含水层渗透系数达36 911.11 m/d,证明了地下水集中径流带的存在;二矿逆断层及两侧断层破碎裂隙带的存在,是影响寒武系灰岩含水层集中径流带空间展布的关键因素;集中径流带总体上控制着寒武系灰岩地下水由西南向东北流动、自浅向深的运移。寒武系灰岩地下水集中径流带展布特征的确定,为类似条件煤层底板水害的防治奠定了基础。In order to ascertain the deposition condition of the concentrated runoff zone in the Cambrian limestone underground water in No.2 Mine and Wuzhai Mine of Pingdingshan Coalfield,based on the geological fault development features of the proved mining area,the underground connection test was applied to study the distribution and causes of the underground water concentrated runoff zone and the water control role. The study results showed that the flow velocity of Cambrian limestone underground water in No.2 Mine and Wuzhai Mine was3 320.05 m/d,the permeability coefficient of the aquifer was 36 911. 11 m/d and the occurrence of the underground water concentrated runoff zone was proved. The occurrences of the reverse fault and the broken crack zone in No.2 Mine would be the key factor affected to the space distribution of the concentrated runoff zone in the Cambrian limestone underground water. The concentrated runoff zone generally controlled the movement of the Cambrian limestone underground water from the south-west to north-east and from a shallow to deep. The determination on the distribution features of the concentrated runoff zone in Cambrian limestone underground water could set up the base to prevent and control the seam floor water disaster.

关 键 词:寒武系灰岩地下水 集中径流带 连通试验 渗透系数 

分 类 号:TD745[矿业工程—矿井通风与安全] TV213[水利工程—水文学及水资源]

 

参考文献:

正在载入数据...

 

二级参考文献:

正在载入数据...

 

耦合文献:

正在载入数据...

 

引证文献:

正在载入数据...

 

二级引证文献:

正在载入数据...

 

同被引文献:

正在载入数据...

 

相关期刊文献:

正在载入数据...

相关的主题
相关的作者对象
相关的机构对象