李粮店煤矿水文地质特征研究
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摘要
本文通过资料收集、抽水试验、水化学分析和室内资料整理等方法,研究了李粮店煤矿地质、水文地质特征,查明了区域地下水的补给、径流和排泄规律。研究认为,区域地下水的主要补给来源为大气降水,其次为岩溶裂隙水;区域地下水由北西向南东径流为主,主要径流带为断裂破碎带;岩溶裂隙水主要以泉的形式排泄,新生界孔隙水以农灌抽水和蒸发排泄为主。煤层底板为太原组上段灰岩岩溶裂隙承压含水层和寒武—奥陶系灰岩岩溶裂隙承压含水层,岩溶裂隙发育,含、富水性极不均一,水文地质条件相对比较复杂。威胁煤矿安全生产的含水层是太原组灰岩岩溶裂隙承压含水层,该含水层为二1煤层底板直接充水含水层。
在综合分析了李粮店煤矿地质、水文地质特征的基础上,研究了矿井充水水源、充水因素、充水通道等;利用水文地质比拟法和稳定流解析法预测了矿井涌水量,即正常涌水量为1400m3/h,最大涌水量为2000m3/h;制定了合理的防治水措施,为以后矿井的正常生产和水害防治提供了科学依据。
In this paper, the characteristics of regional groundwater recharge, runoff and discharge have been researched through data collection, pumping tests, water chemistry analysis and data analysis. The main recharge of regional groundwater is precipitation, followed by the karst crevice water; Regional groundwater flow from the northwest to southeast. The main runoff zone is fracture zone. Karst crevice water is mainly discharged in form of spring. Mesozoic and Cenozoic porous water is mainly discharged in agricultural irrigation and evaporation. Coal floor is composed of Taiyuan coal for the upper limestone karst fractured confined aquifer and the Cambrian-Ordovician limestone karst-fractured confined aquifer. Karst fissure is developed and water-bearing are heterogeneous. Hydrogeological conditions are relatively more complicated. Threat to mine safety and production of aquifer is a limestone karst fractured Taiyuan confined aquifer, the aquifer for the two coal floor directly to a water-filling aquifer.
Based on the comprehensive analysis of the Liliangdian coal geology and hydrogeological conditions, the water-filling sources and factors and channels have been researched. The mine water is prevented by hydrogeology analogue method and steady flow analysis, the normal water yield 1400m3/h, the largest water yield 2000m3/h. The reasonable prevented measures are formulated, which provide scientific basis for the mine production and flood prevention in the future.
在综合分析了李粮店煤矿地质、水文地质特征的基础上,研究了矿井充水水源、充水因素、充水通道等;利用水文地质比拟法和稳定流解析法预测了矿井涌水量,即正常涌水量为1400m3/h,最大涌水量为2000m3/h;制定了合理的防治水措施,为以后矿井的正常生产和水害防治提供了科学依据。
In this paper, the characteristics of regional groundwater recharge, runoff and discharge have been researched through data collection, pumping tests, water chemistry analysis and data analysis. The main recharge of regional groundwater is precipitation, followed by the karst crevice water; Regional groundwater flow from the northwest to southeast. The main runoff zone is fracture zone. Karst crevice water is mainly discharged in form of spring. Mesozoic and Cenozoic porous water is mainly discharged in agricultural irrigation and evaporation. Coal floor is composed of Taiyuan coal for the upper limestone karst fractured confined aquifer and the Cambrian-Ordovician limestone karst-fractured confined aquifer. Karst fissure is developed and water-bearing are heterogeneous. Hydrogeological conditions are relatively more complicated. Threat to mine safety and production of aquifer is a limestone karst fractured Taiyuan confined aquifer, the aquifer for the two coal floor directly to a water-filling aquifer.
Based on the comprehensive analysis of the Liliangdian coal geology and hydrogeological conditions, the water-filling sources and factors and channels have been researched. The mine water is prevented by hydrogeology analogue method and steady flow analysis, the normal water yield 1400m3/h, the largest water yield 2000m3/h. The reasonable prevented measures are formulated, which provide scientific basis for the mine production and flood prevention in the future.
引文
[1]靳德武,董书宁,刘其声.带(水)压开采安全评价技术及其发展方向.煤田地质与勘探,2005,33(2):21-25
[2]庞渭舟,刘维周.煤炭水文地质学.北京:煤炭工业出版社,1980
[3]中国煤炭工业劳动保护科学技术汇编委员会.矿井水害防治技术.北京:煤炭工业出版社,2007.96-98
[4]武强,金玉洁.华北型煤田矿井防治水决策系统.北京:煤炭工业出版社,1995
[5]李正根.水文地质学.北京:地质出版社,1980
[6] Amezketa, E. Aragues, R.; Gazol, R. Efficiency of sulfuric acid, mined gypsum, and two gypsum by-products in soil crusting prevention and sodic soil reclamation Agronomy Journal, v 97, n 3, 2005, p 983-989
[7]王永红,沈文.中国煤矿水害预防及治理[M] .北京:煤炭工业出版社,1996.24-28
[8]武强,李周尧.矿井水灾防治[M] ..北京:中国矿业大学出版,2002.110-116
[9]虎维岳.矿山水害防治理论[M] .北京:煤炭工业出版社,2005
[10]管恩太.河南省煤矿开采水害综合控制技术研究[M].北京:地质出版社,2006
[11] ArcherGC,FenvesG,ThewaltC. A new object-oriented finite element analysis program architecture. Computers & Structures,1999,70(1): 63-75
[12] DavidBanks,PaulLYounger. Mine-water chemistry: the good,the bad and the ugly. Environmental Geology,1997,32(3):157-174
[13] Georg Kaufmann Modelling unsaturated flow in an evolving karst aquifer Journal of Hydrology 276 (2003)53-70
[14] To, Tanya Bangthanh Nordstrom, D. Kirk; Cunningham, Kirkwood M.; Ball, James W.; McCleskey, R. Blaine New method for the direct determination of dissolved Fe(III) concentration in acid mine waters Environmental Science and Technology, v 33, n 5, Mar 1, 1999, p 807-813
[15] Amos Frunkin Hydrology and denudation rates of halite karst Journal of Hydrology 162 (1994) 171-189
[16]章至洁,韩宝平,张月华.水文地质学基础[M].徐州:中国矿业大学出版社,1995
[17]王大纯,等.水文地质学基础(水文地质及工程地质专用)[M].北京:地质出版社,1980
[18]卜昌森,张希诚,尹万才.“华北型”煤田水害及防治现状[J].地质评论,2001,47(7):405-408
[19]张金才,刘天泉.采煤工作面地板应力及位移的模拟实验研究.煤炭科研参考资料,1991.(2)
[20]中国科学院地质所.中国煤矿岩溶水突水机理的研究.北京:科学出版社,1992
[21] B.H.G,布雷斯,E.T.布朗.地下采矿岩石力学,冯树仁等译.北京:煤炭工业出版社,1990.6
[22]王金安.承压水体上采煤相似模拟实验.矿山压力与顶板管理,1990,(3):56-58
[23]蒋金泉,宋振骐.回采工作面地板活动及其对突水的影响的研究.山东矿业学院学报,1987,12(4)
[24]黎良杰.采场底板突水机理的研究:[博士学位论文].北京:中国矿业大学,1995
[25]黎良杰,钱鸣高.底板岩体结构稳定性与底板突水关系的研究.中国矿业大学学报,1995,(4)
[26]中国统配煤矿总公司技术发展局,华北型煤田奥灰岩溶水综合防治工业性实验.1989
[27]王左与,刘鸿泉.承压水上采煤[M].北京:煤炭工业出版社,1997,4(1):22-24
[28] Viqneault Bernard Geochemical changes in sulfidic mine tailing stored under a shallow wanter cover Water Research v35,n4,Mar 2001,p1066-1076
[29] Waybrant, K.R. Treatment of mine drainage using permeable reactive barriers: Column experiments Environmental Science and Technology, v 36, n 6, Mar 15, 2002, p 1349-1356
[30]李白英,沈光寒,荆自刚等.预防采掘工作面底板突水的理论与实践,第十二届国际采矿安全会议论文集[M].北京:煤炭工业出版社
[31]李白英等.采动矿压与底板突水的研究.煤田地质与勘探,1986,2
[32] Jacob, Donna L.; Otte, Marinus L. Influence of Typha latifolia and fertilization on metal mobility in two different Pb-Zn mine tailings types Science of the Total Environment, v 333, n 1-3, Oct 15, 2004, p 9-24
[33] Wu, Qiang Preliminary study on water disaster emergency rescue counterplan in coal mine Meitan Xuebao/Journal of the China Coal Society, v 31, n 4, August, 2006, p 409-413 Language: Chinese
[34]陈昭炎,苏问智.煤田水文地质学[M].北京:煤炭工业出版社
[35]高航,孙振鹏.煤层底板采动影响的研究.山东矿业学院学报,1987,1
[36]张金才.煤层底板采动影响特征.岩土力学进展,1990
[37]杨成田.专门水文地质学[M] .北京:地质出版社, 1981 (7)
[38]张银海.浅析李粮店矿区水文地质条件与矿井水综合利用[J].中州煤炭,2006,6
[39]张银海.浅谈李粮店井田瓦斯赋存规律[J].中州煤炭,2007,3
[40]李桂玲.天津海岸带松散岩类地下水地球化学特征调查与评价[D].中国地质大学(北京) , 20
[41]柴登榜.主编矿井地质手册[M] .北京:煤炭工业出版社, 1984
[42]胡宏清.喀斯特煤矿山矿井突水预测及水害防治研究[D].贵州大学, 2007
[43]张淼,郭启文,刘松.李粮店第四系井筒涌水量预测[J].中州煤炭,2007,1.
[44]肖有才,张孔敏.北方岩溶矿井突水淹井分析与最大涌水量计算.煤炭学报, 2004(增)
[45]刘照邦,岳崇利,贺宝峰.平禹煤电公司新峰一矿防治水方案浅析.中州煤炭2007, 6
[46]陈昭炎,苏问智.煤田水文地质学[M].北京:煤炭工业出版社
[47]王瑞华,符勇,王宏宇.李粮店矿区涌水量预算.中州煤炭,2009,10.
[48]陈葆仁.地下水动态及其预测[M].科学出版社,1998
[49]王胜虎,张华民,韩爱斌.王庄井田水文地质条件分析[J].中州煤炭,2004,6
[50]牛森营.郑州矿区一1煤开采水害防治研究.煤炭工程,2007,4
[2]庞渭舟,刘维周.煤炭水文地质学.北京:煤炭工业出版社,1980
[3]中国煤炭工业劳动保护科学技术汇编委员会.矿井水害防治技术.北京:煤炭工业出版社,2007.96-98
[4]武强,金玉洁.华北型煤田矿井防治水决策系统.北京:煤炭工业出版社,1995
[5]李正根.水文地质学.北京:地质出版社,1980
[6] Amezketa, E. Aragues, R.; Gazol, R. Efficiency of sulfuric acid, mined gypsum, and two gypsum by-products in soil crusting prevention and sodic soil reclamation Agronomy Journal, v 97, n 3, 2005, p 983-989
[7]王永红,沈文.中国煤矿水害预防及治理[M] .北京:煤炭工业出版社,1996.24-28
[8]武强,李周尧.矿井水灾防治[M] ..北京:中国矿业大学出版,2002.110-116
[9]虎维岳.矿山水害防治理论[M] .北京:煤炭工业出版社,2005
[10]管恩太.河南省煤矿开采水害综合控制技术研究[M].北京:地质出版社,2006
[11] ArcherGC,FenvesG,ThewaltC. A new object-oriented finite element analysis program architecture. Computers & Structures,1999,70(1): 63-75
[12] DavidBanks,PaulLYounger. Mine-water chemistry: the good,the bad and the ugly. Environmental Geology,1997,32(3):157-174
[13] Georg Kaufmann Modelling unsaturated flow in an evolving karst aquifer Journal of Hydrology 276 (2003)53-70
[14] To, Tanya Bangthanh Nordstrom, D. Kirk; Cunningham, Kirkwood M.; Ball, James W.; McCleskey, R. Blaine New method for the direct determination of dissolved Fe(III) concentration in acid mine waters Environmental Science and Technology, v 33, n 5, Mar 1, 1999, p 807-813
[15] Amos Frunkin Hydrology and denudation rates of halite karst Journal of Hydrology 162 (1994) 171-189
[16]章至洁,韩宝平,张月华.水文地质学基础[M].徐州:中国矿业大学出版社,1995
[17]王大纯,等.水文地质学基础(水文地质及工程地质专用)[M].北京:地质出版社,1980
[18]卜昌森,张希诚,尹万才.“华北型”煤田水害及防治现状[J].地质评论,2001,47(7):405-408
[19]张金才,刘天泉.采煤工作面地板应力及位移的模拟实验研究.煤炭科研参考资料,1991.(2)
[20]中国科学院地质所.中国煤矿岩溶水突水机理的研究.北京:科学出版社,1992
[21] B.H.G,布雷斯,E.T.布朗.地下采矿岩石力学,冯树仁等译.北京:煤炭工业出版社,1990.6
[22]王金安.承压水体上采煤相似模拟实验.矿山压力与顶板管理,1990,(3):56-58
[23]蒋金泉,宋振骐.回采工作面地板活动及其对突水的影响的研究.山东矿业学院学报,1987,12(4)
[24]黎良杰.采场底板突水机理的研究:[博士学位论文].北京:中国矿业大学,1995
[25]黎良杰,钱鸣高.底板岩体结构稳定性与底板突水关系的研究.中国矿业大学学报,1995,(4)
[26]中国统配煤矿总公司技术发展局,华北型煤田奥灰岩溶水综合防治工业性实验.1989
[27]王左与,刘鸿泉.承压水上采煤[M].北京:煤炭工业出版社,1997,4(1):22-24
[28] Viqneault Bernard Geochemical changes in sulfidic mine tailing stored under a shallow wanter cover Water Research v35,n4,Mar 2001,p1066-1076
[29] Waybrant, K.R. Treatment of mine drainage using permeable reactive barriers: Column experiments Environmental Science and Technology, v 36, n 6, Mar 15, 2002, p 1349-1356
[30]李白英,沈光寒,荆自刚等.预防采掘工作面底板突水的理论与实践,第十二届国际采矿安全会议论文集[M].北京:煤炭工业出版社
[31]李白英等.采动矿压与底板突水的研究.煤田地质与勘探,1986,2
[32] Jacob, Donna L.; Otte, Marinus L. Influence of Typha latifolia and fertilization on metal mobility in two different Pb-Zn mine tailings types Science of the Total Environment, v 333, n 1-3, Oct 15, 2004, p 9-24
[33] Wu, Qiang Preliminary study on water disaster emergency rescue counterplan in coal mine Meitan Xuebao/Journal of the China Coal Society, v 31, n 4, August, 2006, p 409-413 Language: Chinese
[34]陈昭炎,苏问智.煤田水文地质学[M].北京:煤炭工业出版社
[35]高航,孙振鹏.煤层底板采动影响的研究.山东矿业学院学报,1987,1
[36]张金才.煤层底板采动影响特征.岩土力学进展,1990
[37]杨成田.专门水文地质学[M] .北京:地质出版社, 1981 (7)
[38]张银海.浅析李粮店矿区水文地质条件与矿井水综合利用[J].中州煤炭,2006,6
[39]张银海.浅谈李粮店井田瓦斯赋存规律[J].中州煤炭,2007,3
[40]李桂玲.天津海岸带松散岩类地下水地球化学特征调查与评价[D].中国地质大学(北京) , 20
[41]柴登榜.主编矿井地质手册[M] .北京:煤炭工业出版社, 1984
[42]胡宏清.喀斯特煤矿山矿井突水预测及水害防治研究[D].贵州大学, 2007
[43]张淼,郭启文,刘松.李粮店第四系井筒涌水量预测[J].中州煤炭,2007,1.
[44]肖有才,张孔敏.北方岩溶矿井突水淹井分析与最大涌水量计算.煤炭学报, 2004(增)
[45]刘照邦,岳崇利,贺宝峰.平禹煤电公司新峰一矿防治水方案浅析.中州煤炭2007, 6
[46]陈昭炎,苏问智.煤田水文地质学[M].北京:煤炭工业出版社
[47]王瑞华,符勇,王宏宇.李粮店矿区涌水量预算.中州煤炭,2009,10.
[48]陈葆仁.地下水动态及其预测[M].科学出版社,1998
[49]王胜虎,张华民,韩爱斌.王庄井田水文地质条件分析[J].中州煤炭,2004,6
[50]牛森营.郑州矿区一1煤开采水害防治研究.煤炭工程,2007,4