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渭北东部奥陶灰岩地下水硫酸盐起源的化学同位素研究 被引量:2
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作者 范基姣 马致远 +1 位作者 何锦 刘瑞平 《地下水》 2005年第5期344-346,共3页
通过对渭北东部奥陶灰岩地下水中SO42-、δD、δ34S、1δ8O的分析研究,认为奥陶灰岩地下水中硫酸盐起源主要为海相硫酸盐的溶解,其次为南部古沉积咸水混入。
关键词 奥陶灰岩地下水 硫同位素 盐化机制
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矿区寒武系灰岩地下水集中径流带展布及机理分析
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作者 王心义 曹冰琪 +4 位作者 王麒 赵彦琦 陈国胜 张平卿 刘小满 《煤炭科学技术》 CAS 北大核心 2016年第8期35-38,115,共5页
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... 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。 展开更多
关键词 寒武系灰岩地下水 集中径流带 连通试验 渗透系数
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灰岩岩溶裂隙水赋存特征及其对矿井充水影响 被引量:9
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作者 牛俊伟 申江 《中州煤炭》 2013年第10期114-117,共4页
针对伯方煤矿开采的山西组下部3号煤层受底板承压水威胁实际,通过分析研究灰岩岩溶裂隙含水层富水性、隔水层岩性组合特征及隔水性,断裂构造发育程度及导水性,采用定量、定性相结合的方法,评价了灰岩地下水突水危险性及危害程度,并提出... 针对伯方煤矿开采的山西组下部3号煤层受底板承压水威胁实际,通过分析研究灰岩岩溶裂隙含水层富水性、隔水层岩性组合特征及隔水性,断裂构造发育程度及导水性,采用定量、定性相结合的方法,评价了灰岩地下水突水危险性及危害程度,并提出了相应的防治技术措施,为实现矿井安全生产提供了科学依据。 展开更多
关键词 灰岩地下水 富水性 突水危险性 防治水
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桌子山煤田奥灰水水化学特征及成因分析 被引量:4
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作者 王世东 《煤炭科学技术》 CAS CSCD 北大核心 2022年第8期180-188,共9页
桌子山煤田奥陶系灰岩地下水是区域煤层开采的主要充水水源,同时也是乌海市重要的地下水水源,研究该区域水文地球化学特征及成因,对矿井水害防治及地下水资源开发利用均具有重要意义。以奥陶系灰岩水为研究对象,采集煤田奥陶系灰岩地下... 桌子山煤田奥陶系灰岩地下水是区域煤层开采的主要充水水源,同时也是乌海市重要的地下水水源,研究该区域水文地球化学特征及成因,对矿井水害防治及地下水资源开发利用均具有重要意义。以奥陶系灰岩水为研究对象,采集煤田奥陶系灰岩地下水样37组,综合利用piper三线图、Gibbs图及离子比例关系分析了奥陶系灰岩地下水化学特征及其形成作用。研究结果表明:桌子山煤田奥陶系灰水水化学组分的分布特征与地下水径流方向密切相关,Na^(+)+K^(+)、HCO^(-)_(3)、Cl^(-)和SO^(2-)_(4)的离子浓度及理化指标TDS、pH值由补给区向排泄区呈现增大的趋势,Ca^(2+)和Mg^(2+)浓度呈现减小的趋势,并且以上指标在煤田北部和南部地区变化较大;由桌子山补给区向甘德尔山再转南北向径流的水化学类型变化较为明显,主要为“水迟缓交替作用带”,经历正向离子交换作用,而由桌子山补给区向南径流的水化学类型始终为SO_(4)·Cl-Ca·Na型,控制作用由“水迟缓交替作用带”转为“水消极交替作用带”,反向离子交换作用强烈;整个桌子山煤田可划分为北、中、南3个水化学特征区,煤田北部因地质构造的缘故使地下水形成滞留区,径流过程紊乱且形成过程较复杂,中部未受到地质构造阻挡,径流方向不变,地下水化学形成过程简单,而南部因地层加深和断层阻隔的缘故形成滞留带,使地下水水化学形成过程较复杂。 展开更多
关键词 桌子山煤田 水化学特征 水化学形成作用 奥陶系灰岩地下水 地下水水源地
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综合物探技术在焦作矿区防治水中的应用 被引量:1
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作者 杨建增 《中州煤炭》 2013年第9期66-68,共3页
焦作矿区位于华北型煤田的中部,是著名的大水矿区,主要受煤系地层下的巨厚奥陶系灰岩地下水威胁,水文地质条件复杂、含水层多、裂隙较发育。为了减少突水事故的发生,在焦作矿区采煤工作面分别应用了瞬变电磁、直流电法、无线电波坑透仪... 焦作矿区位于华北型煤田的中部,是著名的大水矿区,主要受煤系地层下的巨厚奥陶系灰岩地下水威胁,水文地质条件复杂、含水层多、裂隙较发育。为了减少突水事故的发生,在焦作矿区采煤工作面分别应用了瞬变电磁、直流电法、无线电波坑透仪等物探手段进行探测,预测结果有效遏制了突水事故的发生。 展开更多
关键词 焦作矿区 奥陶系灰岩地下水 综合物探技术 突水事故
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Geochemistry of rare earth elements in groundwater from deep seated limestone aquifer in Renlou Coal Mine,Anhui Province,China 被引量:6
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作者 孙林华 桂和荣 +1 位作者 陈陆望 陈松 《Journal of Central South University》 SCIE EI CAS 2011年第5期1646-1653,共8页
Rare earth element (REE) concentrations were measured by ICP-MS for groundwater collected from deep seated Taiyuan Fm limestone aquifer (from -400 to -530 m) in Renlou Coal Mine, northern Anhui Province, China. It... Rare earth element (REE) concentrations were measured by ICP-MS for groundwater collected from deep seated Taiyuan Fm limestone aquifer (from -400 to -530 m) in Renlou Coal Mine, northern Anhui Province, China. It can be concluded that the groundwater is warm (34.0-37.2 ℃) C1-Ca, Na type water with circum-neutral pH (7.35-8.28) and high total dissolved solids (TDS, 1 746-2 849 mg/L). The groundwater exhibits heavy REEs enrichment relative to light REEs compared with Post Archean Average Shale (PAAS), as well as their aquifer rocks (limestone). The enrichment of REEs is considered to be controlled by terrigeneous materials (e.g. zircon) in aquifer rocks, whereas the fractionation of REEs is controlled by marine derived materials (e.g. calcite), to a less extent, terrigeneous materials and inorganic complexation. The Ce anomalies normalized to PAAS and aquifer rocks are weak, which probably reflects the signature of the aquifer rock rather than redox conditions or pH. The similarities of REE patterns between groundwater and aquifer rocks imply that aquifer rocks play important roles in controlling the REE characteristics of groundwater, and then provide a probability for discrimination of groundwater sources by using REEs. 展开更多
关键词 rare earth elements GEOCHEMISTRY water-rock interaction limestone aquifer GROUNDWATER
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Detection and treatment of water inflow in karst tunnel:A case study in Daba tunnel 被引量:7
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作者 LI Xiang-hui ZHANG Qing-song +3 位作者 ZHANG Xiao LAN Xiong-dong DUAN Chong-hao LIU Jian-guo 《Journal of Mountain Science》 SCIE CSCD 2018年第7期1585-1596,共12页
In a karst tunnel, fissures or cracks that are filled with weathered materials are a type of potential water outlet as they are easily triggered and converted into groundwater outlets under the influence of high groun... In a karst tunnel, fissures or cracks that are filled with weathered materials are a type of potential water outlet as they are easily triggered and converted into groundwater outlets under the influence of high groundwater pressure. A terrible water inrush caused by potential water outlets can seriously hinder the project construction. Potential water outlets and water sources that surrounding the tunnel must be detected before water inflow can be treated. This paper provides a successful case of the detection and treatment of water inflow in a karst tunnel and proposes a potential water outlet detection(PWOD) method in which heavy rainfall(>50 mm/d) is considered a trigger for a potential water outlet. The Daba tunnel located in Hunan province, China, has been constructed in a karst stratum where the rock mass has been weathered intensely by the influence of two faults. Heavy rain triggered some potential water outlets, causing a serious water inrush. The PWOD method was applied in this project for the treatment of water inflow, and six potential water outlets in total were identified through three heavy rains. Meanwhile, a geophysical prospecting technique was also used to detect water sources. The connections between water outlets and water sources were identified with a 3-D graphic that included all of them. According to the distribution of water outlets and water sources, the detection area was divided into three sections and separately treated by curtain grouting. 展开更多
关键词 Karst tunnel Water inrush Potential water outlet detection Geophysical prospecting technique Water inflow GROUTING
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