基岩裂隙水研究现状与展望
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摘要
针对基岩裂隙水既是宝贵资源但又对大型地下工程建设构成威胁,在综合分析国内外基岩裂隙研究成果的基础上,从概念、类型、基本特征、富集理论、运动机理和模型等方面论述了基岩裂隙水的研究现状和热点,针对生产应用实际列举了寻找、勘探基岩裂隙水的技术和方法,展望了拟深入研究的趋势,为基岩裂隙水运动理论的研究奠定了基础。
The bedrock fissure water is not only a kind of valuable resource but also a threat factor of large-scale underground construction projects.Based on comprehensive analysis on former researches of bedrock fissure water,the research status and hot lists of bedrock fissure water is discussed in the aspects of concept,types,basic features,enrichment theory,motion mechanism and motion model and so on.The techniques and methods of bedrock fissure water exploration and withdrawal is presented mainly to the actual application,and the trend of can be in-depth study also is proposed.They are all very important to the study of bedrock fissure water motion mechanism.
The bedrock fissure water is not only a kind of valuable resource but also a threat factor of large-scale underground construction projects.Based on comprehensive analysis on former researches of bedrock fissure water,the research status and hot lists of bedrock fissure water is discussed in the aspects of concept,types,basic features,enrichment theory,motion mechanism and motion model and so on.The techniques and methods of bedrock fissure water exploration and withdrawal is presented mainly to the actual application,and the trend of can be in-depth study also is proposed.They are all very important to the study of bedrock fissure water motion mechanism.
引文
[1]廖资生,束龙仓,林学钰.基岩裂隙水专家系统[M].西安:陕西科学技术出版社,1997.
[2]刘光亚.基岩地下水[M].北京:地质出版社,1979.
[3]胡海涛.论构造体系与地下水的网络[J].水文地质工程地质,1980,7(3):1-7.
[4]尹树人,肖有权.试论新构造断裂的水文地质意义[J].南京大学学报(自然科学版),1988,24(3):401-405.
[5]刘国昌.地质力学及其在水文地质工程地质方面的应用[M].北京:地质出版社,1979.
[6]肖楠森,林凤勋.山区基岩裂隙水资源的开发利用与新构造断裂特性的关系[J].工程勘察,1982(5):31-36.
[7]田开铭.偏流与裂隙水脉状径流[J].地质评论,1983,29(5):408-417.
[8]田开铭.裂隙水交叉流的水力特性[J].地质学报,1986(2):202-214.
[9]罗绍河,孙峰根.单一流径基岩裂隙水平均流速试验研究[J].河南地质,1996,14(4):277-281.
[10]孙峰根,罗绍河,王心义.单一流迳基岩水流平均流速方程[J].水文地质工程地质,1996(4):25-28.
[11]钱家忠,赵卫东,刘咏.小隙(b<3 mm)单一流径基岩水平均流速的实验研究[J].煤田地质与勘探,1999(4):35-38.
[12]钱家忠,刘咏,葛晓光.基岩裂隙流水位与流程关系的统计研究[J].煤田地质与勘探,2002,30(1):30-34.
[13]钱家忠,杨立华,李如忠,等.基岩裂隙系统中地下水运动物理模拟研究进展[J].合肥工业大学学报(自然科学版),2003,26(4):510-513.
[14]王媛,速宝玉,徐志英.裂隙岩体渗流模型综述[J].水科学进展,1996,7(3):276-282.
[15]钱家忠,赵卫东,潘国营.单一径流基岩裂隙水流态的实验研究[J].焦作工学院学报(自然科学版),2000,19(3):192-195.
[16]王珊林,史桂华,王德成.基岩裂隙水三维流数值模型研究及应用[J].东北水利水电,2000,18(4):36-38.
[17]Nordqvist A W,Tsang Y W,Tsang C F,et al.Effects of High Variance of Fracture Transmissivityon Transport and Sorption at Different Scales in aDiscrete Model for Fractured Rocks[J].Journal ofContaminant Hydrology,1996,22(1-2):39-66.
[18]Pruess K,Faybishenko B,Bodvarsson G S.Alter-native Concepts and Approaches for Modeling Flowand Transport in Thick Unsaturated Zones of Frac-tured Rocks[J].Journal of Contaminant Hydrology1999,38(1-3):281-322.
[19]Slough K J,Sudicky E A,Forsyth P A.NumericaSi mulation of Multiphase Flowand Phase Partitioningin Discretely Fractured Geologic Media[J].Journaof Contaminant Hydrology,1999(4):107-136.
[20]Liu H H,Bodvarsson G S.Constitutive Relationsfor Unsaturated Flow in a Fracture Network[J]Journal of Hydrology,2001,252:116-125.
[21]Wu Y S,Pan L,Pruess K.A Physically Based Ap-proach for Modeling Multiphase Fracture-matrix In-teractionin Fractured Porous Media[J].Advancesin Water Resources,2004,27:875-887.
[22]Tran N H,Ravoof A,Nguyen T,et al.Modelling ofType I Fracture Network:Objective Function For-mulation by Fuzzy Sensitivity Analysis[J].Mathe-matical and Computer Modelling,2009,49:1 283-1 287.
[23]Batte A G,Muwanga A,Sigrist P W,et al.VerticaElectrical Sounding as an Exploration Technique toI mprove on the Certainty of Groundwater Yield inthe Fractured Crystalline Basement Aquifers ofEastern Uganda[J].Hydrogeology Journal,200816:1 683-1 693.
[24]Revil A,Naudet V,Meunier J D.The Hydroelec-tric Problemof Porous Rocks:Inversion of the Po-sition of the Water Table from Self-potential Data[J].Geophysica Journal International,2004,159435-444.
[25]Yaramanci U,Lange G,Knodel K.Surface NMRwithin a Geophysical Study of an Aquifer at Halden-sleben(Germany)[J].Geophysical Prospecting1999,47:923-943.
[26]束龙仓,林学钰,廖资生.基岩裂隙水寻找与开发的专家系统建立[J].水文地质工程地质,1997(5):30-32.
[27]束龙仓,林学钰,廖资生.基岩裂隙水神经网络专家系统实例研究[J].水科学进展,1998,9(4):384-388.
[28]霍润科,刘汉东,李宁,等.基于模糊神经网络方法的新构造控水专家系统[J].系统理论工程与实践2003(11):135-139.
[29]陈建胜.专家系统在岩土工程中的应用综述[J].工程地质计算机应用,2007(2):29-31.
[30]崔建军,何继善,吴燕清,等.用神经网络技术进行地震波速反演[J].有色金属,2001,53(2):14-16.
[31]刘云祯.工程物探新技术[M].北京:地质出版社2006.
[2]刘光亚.基岩地下水[M].北京:地质出版社,1979.
[3]胡海涛.论构造体系与地下水的网络[J].水文地质工程地质,1980,7(3):1-7.
[4]尹树人,肖有权.试论新构造断裂的水文地质意义[J].南京大学学报(自然科学版),1988,24(3):401-405.
[5]刘国昌.地质力学及其在水文地质工程地质方面的应用[M].北京:地质出版社,1979.
[6]肖楠森,林凤勋.山区基岩裂隙水资源的开发利用与新构造断裂特性的关系[J].工程勘察,1982(5):31-36.
[7]田开铭.偏流与裂隙水脉状径流[J].地质评论,1983,29(5):408-417.
[8]田开铭.裂隙水交叉流的水力特性[J].地质学报,1986(2):202-214.
[9]罗绍河,孙峰根.单一流径基岩裂隙水平均流速试验研究[J].河南地质,1996,14(4):277-281.
[10]孙峰根,罗绍河,王心义.单一流迳基岩水流平均流速方程[J].水文地质工程地质,1996(4):25-28.
[11]钱家忠,赵卫东,刘咏.小隙(b<3 mm)单一流径基岩水平均流速的实验研究[J].煤田地质与勘探,1999(4):35-38.
[12]钱家忠,刘咏,葛晓光.基岩裂隙流水位与流程关系的统计研究[J].煤田地质与勘探,2002,30(1):30-34.
[13]钱家忠,杨立华,李如忠,等.基岩裂隙系统中地下水运动物理模拟研究进展[J].合肥工业大学学报(自然科学版),2003,26(4):510-513.
[14]王媛,速宝玉,徐志英.裂隙岩体渗流模型综述[J].水科学进展,1996,7(3):276-282.
[15]钱家忠,赵卫东,潘国营.单一径流基岩裂隙水流态的实验研究[J].焦作工学院学报(自然科学版),2000,19(3):192-195.
[16]王珊林,史桂华,王德成.基岩裂隙水三维流数值模型研究及应用[J].东北水利水电,2000,18(4):36-38.
[17]Nordqvist A W,Tsang Y W,Tsang C F,et al.Effects of High Variance of Fracture Transmissivityon Transport and Sorption at Different Scales in aDiscrete Model for Fractured Rocks[J].Journal ofContaminant Hydrology,1996,22(1-2):39-66.
[18]Pruess K,Faybishenko B,Bodvarsson G S.Alter-native Concepts and Approaches for Modeling Flowand Transport in Thick Unsaturated Zones of Frac-tured Rocks[J].Journal of Contaminant Hydrology1999,38(1-3):281-322.
[19]Slough K J,Sudicky E A,Forsyth P A.NumericaSi mulation of Multiphase Flowand Phase Partitioningin Discretely Fractured Geologic Media[J].Journaof Contaminant Hydrology,1999(4):107-136.
[20]Liu H H,Bodvarsson G S.Constitutive Relationsfor Unsaturated Flow in a Fracture Network[J]Journal of Hydrology,2001,252:116-125.
[21]Wu Y S,Pan L,Pruess K.A Physically Based Ap-proach for Modeling Multiphase Fracture-matrix In-teractionin Fractured Porous Media[J].Advancesin Water Resources,2004,27:875-887.
[22]Tran N H,Ravoof A,Nguyen T,et al.Modelling ofType I Fracture Network:Objective Function For-mulation by Fuzzy Sensitivity Analysis[J].Mathe-matical and Computer Modelling,2009,49:1 283-1 287.
[23]Batte A G,Muwanga A,Sigrist P W,et al.VerticaElectrical Sounding as an Exploration Technique toI mprove on the Certainty of Groundwater Yield inthe Fractured Crystalline Basement Aquifers ofEastern Uganda[J].Hydrogeology Journal,200816:1 683-1 693.
[24]Revil A,Naudet V,Meunier J D.The Hydroelec-tric Problemof Porous Rocks:Inversion of the Po-sition of the Water Table from Self-potential Data[J].Geophysica Journal International,2004,159435-444.
[25]Yaramanci U,Lange G,Knodel K.Surface NMRwithin a Geophysical Study of an Aquifer at Halden-sleben(Germany)[J].Geophysical Prospecting1999,47:923-943.
[26]束龙仓,林学钰,廖资生.基岩裂隙水寻找与开发的专家系统建立[J].水文地质工程地质,1997(5):30-32.
[27]束龙仓,林学钰,廖资生.基岩裂隙水神经网络专家系统实例研究[J].水科学进展,1998,9(4):384-388.
[28]霍润科,刘汉东,李宁,等.基于模糊神经网络方法的新构造控水专家系统[J].系统理论工程与实践2003(11):135-139.
[29]陈建胜.专家系统在岩土工程中的应用综述[J].工程地质计算机应用,2007(2):29-31.
[30]崔建军,何继善,吴燕清,等.用神经网络技术进行地震波速反演[J].有色金属,2001,53(2):14-16.
[31]刘云祯.工程物探新技术[M].北京:地质出版社2006.
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