典型华北型煤矿区主要充水含水层水文地球化学特征及控制因素Hydrogeochemical Characteristics and Controlling Factors of Main Water Filled Aquifers in the Typical North China Coalfield
武亚遵;潘春芳;林云;曹飞龙;王子杰;
摘要(Abstract):
地下水形成、演化过程中控制因素不同所造成的水化学组分的差异性是矿井涌水水源识别的基础,为揭示矿井主要充水含水层水化学作用及控制因素,以位于太行山东麓的典型华北型煤矿区——鹤壁矿区为研究对象,采用统计分析、Piper三线图、Gibbs图、离子相关性分析与主成分分析法对矿区122个地下水水化学资料进行了分析研究。结果表明鹤壁矿区主要充水含水层中地下水的化学组分主要受岩石的风化作用控制。奥灰水主要水化学类型为HCO_3-Ca·Mg型,水中Ca~(2+)、Mg~(2+)主要来自碳酸盐岩(方解石和白云石)的溶解。二灰水主要水化学类型为HCO_3·SO_4-Ca·Mg型或SO_4·HCO_3-Ca·Mg型,其中Ca~(2+)、Mg~(2+)、HCO_3~-的主要来源于碳酸盐岩的溶解,SO_4~(2-)来自硫酸盐岩的溶解作用和黄铁矿的氧化作用。砂岩水主要水化学类型为HCO_3-Na型,Na~+、Cl~-与HCO_3~-主要来自盐岩的溶解和硅酸盐矿物的风化作用。八灰水既有HCO_3-Ca·Mg型和HCO_3·SO_4-Ca·Mg型,也有HCO_3-Na型,Ca~(2+)、Mg~(2+)、HCO_~3-和SO_4~(2-)的来源与二灰水一致,Na~+和Cl~-可能来自盐岩的溶解作用以及砂岩水与八灰水的混合作用。
关键词(KeyWords): Piper三线图;离子相关分析;主成分分析;华北型煤矿区
基金项目(Foundation): 国家自然科学基金项目(41602265;41502224);; 河南省高等学校重点科研项目(16A170012)
作者(Author): 武亚遵;潘春芳;林云;曹飞龙;王子杰;
Email:
DOI: 10.19509/j.cnki.dzkq.2018.0526
参考文献(References):
- [1]赵铁锤.华北地区奥灰水综合防治技术[M].北京:煤炭工业出版社,2006.
- [2]邓云辉,薛小奇,于计华,等.平禹一矿特大突水灾害治理及快速复矿技术研究[J].现代矿业,2010,26(2):136-138.
- [3]李松营,武强,滕吉文,等.新安矿13151工作面煤壁侧底板突水分析[J].中国煤炭,2015,41(6):40-43.
- [4]刘存玉,关永强.峰峰集团九龙矿15423N工作面特大突水原因剖析[J].煤矿安全,2013,44(8):187-190.
- [5]Panda U C,Sundaray S K,Rath P,et al.Application of factor and cluster analysis for characterization of river and estuarine water systems:a case study from Mahanadi River(India)[J].Journal of Hydrology,2006,331(3):434-445.
- [6]Panagopoulos G P,Angelopoulou D,Tzirtzilakis E E,et al.The contribution of cluster and discriminant analysis to the classification of complex aquifer systems[J].Environmental Monitoring and Assessment,2016,188(10):591.
- [7]钱家忠,潘婧,赵卫东,等.基于SVM的潘三矿B8组与C13组煤开采中突水水源判别模型[J].系统工程理论与实践,2011,31(12):2425-2430.
- [8]Li Jianlin,Zhang Hongyun.Application of BP neural network to determine of mine water inrush sources based on Matlab[C]//International Conference on Artificial Intelligence.Management Science and Electronic Commerce.IEEE,2011:179-182.
- [9]黄平华,陈建生.基于多元统计分析的矿井突水水源Fisher识别及混合模型[J].煤炭学报,2011,36(增刊1):131-136.
- [10]张瑞钢,钱家忠,马雷,等.可拓识别方法在矿井突水水源判别中的应用[J].煤炭学报,2009,34(1):33-38.
- [11]Sun Linhua.Statistical analysis of hydrochemistry of groundwater and its implications for water source identification:A case study[J].Arabian Journal of Geosciences,2014,7(9):3417-3425.
- [12]Gibbs R J.Mechanisms controlling world water chemistry[J].Science,1970,170:1088-1090.
- [13]Miretzky P,Conzonno V,Cirelli A F.Geochemical mechanism controlling pampasic ponds hydrochemistry:Salado River Drainage Basin,Argentina[J].Revista Brasileira de Recursos Hídricos 2001,6(4)29-39.
- [14]Li Peiyue,Qian Hui,Wu Jianhua,et al.Major ion chemistry of shallow groundwater in the Dongsheng Coalfield,Ordos Basin,China[J].Mine Water and the Environment,2013,32(3):195-206.
- [15]孙一博,王文科,段磊,等.关中盆地浅层地下水地球化学的形成演化机制[J].水文地质工程地质,2014,41(3):29-35.
- [16]张未,程东会,齐丽军.吉林省长岭县浅层地下水水文地球化学演化规律分析[J].水资源与水工程学报,2016,27(5):59-63.
- [17]刘永林.不同构造单元水体水化学特征及硒区域分异机制[D].北京:中国科学院大学,2013.
- [18]肖长来,梁秀娟,王彪.水文地质学[M].北京:清华大学出版社,2010.
- [19]Sun Linhua,Gui Herong.Groundwater quality and evolution in a deep limestone aquifer,northern Anhui Province,China:Evidence from hydrochemistry[J].Fresenius Environmental Bulletin,2013,22(4):1126-1131.
- [20]Karro E,Marandi A,Vaikm?e R.The origin of increased salinity in the Cambrian-Vendian aquifer system on the Kopli Peninsula,northern Estonia[J].Hydrogeology Journal,2004,12(4):424-435.
- [21]Sami K.Recharge mechanisms and geochemical processes in a semi-arid sedimentary basin,Eastern Cape,South Africa[J].Journal of Hydrology,1992,139(1/4):27-48.
- [22]Ravikumar P,Somashekar R K.Principal component analysis and hydrochemical facies characterization to evaluate groundwater quality in Varahi River Basin,Karnataka State,India[J].Applied Water Science,2015,7(2):745-755.
- [23]Reddy K S,Kumar M S.Principal component analysis:Deeper aquifer groundwater quality of Bhaskar Rao Kunta watershed,Nalgonda district,Andhra Pradesh,India[J].Nature Environment&Pollution Technology,2012,11(3):425-429.
- [24]Yidana S M,Banoeng-Yakubo B.Analysis of groundwater quality using multivariate and spatial analyses in the Keta Basin,Ghana[J].Journal of African Earth Sciences,2010,58(2):220-234.
- [25]李俊霞,苏春利,谢先军,等.多元统计方法在地下水环境研究中的应用:以山西大同盆地为例[J].地质科技情报,2010,29(6):94-100.
- [26]Chen Luwang,Xie Wenping,Feng Xiaoqing,et al.Formation of hydrochemical composition and spatio-temporal evolution mechanism under mining-induced disturbance in the Linhuan coal-mining district[J].Arabian Journal of Geosciences,2017,10(3):57.
- [27]Cloutier V,Lefebvre R,Therrien R,et al.Multivariate statistical analysis of geochemical data as indicative of the hydrogeochemical evolution of groundwater in a sedimentary rock aquifer system[J].Journal of Hydrology,2008,353(3):294-313.
- [28]李小牛.煤矿开采排水对岩溶水水质的影响研究:以山西省为例[C]//2010地下水资源配置与优化调度及污染防治技术研讨会.2012.
- [29]李义连,王焰新.娘子关泉域岩溶地下水SO2-4,Ca2+,Mg2+污染分析[J].地质科技情报,1998,17(增刊2):111-114.