震电效应研究在资源勘探中的应用前景
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摘要
石油、天然气和水的储层主要为含流体多孔介质 .由于油气和水资源勘探的日益增长的需要 ,与含流体多孔介质密切相关的震电效应研究在我国得到了迅速发展 .针对声电测井探测渗透率、地震波传播的损耗及其控制、天然电磁波与电磁场的产生机制及其利用等问题 ,已对第一类震电效应 (震阻效应或I效应 )、第二类震电效应 (流动电势效应或E效应 )以及充放电 (激发极化 )效应 ,开展了理论和实验研究 ,取得了相当大的进展 .随着油气勘探二次创业的到来 ,将为震电效应在资源勘探中的应用带来巨大的机遇和挑战
The reservoir of oil, gas and underground water are saturate porous medium. As increasing requirement for oil, gas and underground water, research on seismo electric effect that is closely related to the saturate porous medium rapidly developed in our country. The theoretical and experiment studies are carried out on the E effect, I effect and the charge and discharge effect about the permeability detection in acoustic wave well logging, attenuation of seismic wave propagation and its control, and the mechanism of natural EM radiation and its application. As long as the secondary pioneer of oil exploration, the application of seismo electric effect will meet great chance and challenges.
The reservoir of oil, gas and underground water are saturate porous medium. As increasing requirement for oil, gas and underground water, research on seismo electric effect that is closely related to the saturate porous medium rapidly developed in our country. The theoretical and experiment studies are carried out on the E effect, I effect and the charge and discharge effect about the permeability detection in acoustic wave well logging, attenuation of seismic wave propagation and its control, and the mechanism of natural EM radiation and its application. As long as the secondary pioneer of oil exploration, the application of seismo electric effect will meet great chance and challenges.
引文
[1] Thompson,R .R .Theseismoelectriceffect[J].Geophysics,1936,1:327.
[2] Ivannov,A .G .Effectofelectriczationofearthlayersbye lasticwavespassingthroughthem(inRussian)[J].DokladyAkademiiNauk,SSSR ,1939,24:41～43.
[3] Frenkel,J .OnthetheoryofSeismicandSeismoelectricPhenomenainamoistsoil[J].J.Physics,(Soviet),1944,8(4):230～241.
[4] 傅承义.地表层的本质对于地震勘测的几种影响[J].中国科学,1951,2(3):271～281.
[5] BiotMA .Theoryofpropagationofelasticwaveinafluid saturatedporoussolid,I low frequencyrange[J].J .A coust.Soc.Am.,1956,28:168～178.
[6] Dmowska,Electromechnicalphenomenaassociatedwithearthquakes[J].GeophysicalSurveys,1977,3:157～174.
[7] R .C .Rogers,S .S .Antman.Steady stateproblemsofnon linearelectro magneto thermo elasticity[J].ArchRation.Mech.&Anal,1986,95(4):279～323.
[8] Potapof.O .A ,etal1995,Principleofseismo electricprospecting,Ned’la,Moskow.波达波夫,中译本(译者:裘慰庭)震电勘探方法,北京:石油出版社,1997.
[9] D ,MarshallandT ,R ,Madden.Inducedpolarizationastudyofitscause[J].Geophysics,1959,24(4):796～816.
[10] Morgan,F .D .E .R .Madden,andT .R .Madden.Streamingpotentialpropertiesofwesterlygranitewithap plication[J].J.Geophys.Res.,1989,12449～12461.
[11] G .Pantelis.Saturated unsaturatedflowinunconfinedaquifers[J].Z .Angew.Math.&Phys.(Switzerland),1985,36(5):648～657.
[12] 蒋洪堪,蒋承菘.访苏见闻-介绍苏联的几种电法[J].物探与化探,1984(1):12～19.
[13] 高章伟.苏联物探技术点滴[J].国外油气勘探,1990,98.
[14] 波利亚科娃.(楚泽涵译).电声测井一种新的测井方法[J].地质与勘探,1990,4.
[15] 巴莲科娃,切勒尼克.(王勋弟译).脉冲谐波激励的电声测井,1991,6(1):11～15.
[16] Neev,J.andF .R .Yeatts.Electrokineticeffectsinfluidsaturatedporoelasticmedia[J].Phys.Rev.B ,1989,40:9135～9142.
[17] Thompson,A .H .,Gist,G .A .Geophysicalapplicationsofelectrokineticconversion[J].TheLeadingEdge,1993,1169～1173.
[18] Zhu,Z .,C .Cheng,andM .Toksoz.Experimentalstudyofflexuralwavesinafracturedorcasedboreholemodel[A].In:soc.,pxplgeophys.64thann,internat.mtg,Abstract[C],1994,70～73.
[19] Haartsen,MW .CoupledElectromagneticandAcousticWavefieldModelinginPoro elasticMediaanditsApplica tionsinGeophysicalExploration[D ].Ph.DThesisofMIT ,1995.
[20] V .Mikhailov,M .W .Haartsen,andM .N .Toksoz.Elec troseismicinvestigationoftheShallowsubsurface,Fieldmeasurementandnumericalmodeling[J].Geophysics,1997,62(1):97～105.
[21] ButlerKE ,RusselRD ,KepicAW ,etal.Measurementoftheseismoelectricresponsefromashallowboundary[J].Geophysics,1996,61:1769～1778.
[22] Pride,SR ,MorganFD .Electrokineticdissipationin ducedbyseismicwave[J].Geophysics,1991,56:914～925.
[23] Pride,S .Governingequationsforthecoupledelectromag neticsandacousticsofporousmedia[J].Phys.Rev.B ,1994,50:15678～15696.
[24] PrideSR ,HaartsenMW ,ToksozMN .Electroseismicwaveproperties[J].J .AcousticalSoc.Am.100(3):1301～1315.
[25] V .Mikhailov,QueenJ ,andM .N .Toksoz.UsingBore holeelectroseismicmeasurementtodetectandcharacterizefractured(permeable)zones[J].Geophysics,2000,65:1098～1112.
[26] 裘慰庭.震电效应在油气勘探中的应用前景[A].见:牛毓荃主编石油物探新技术系列调研成果[C].北京:石油工业出版社,1996,640～651.
[27] 周成当,尉中良,管志宁,等.双相孔隙介质中低频声激发极化电场模拟[J].现代地质,1999,13(增刊):118～124.
[28] 胡恒山,刘家琦.对波达波夫震电波方程组的几点注解[J].地球物理学报(待发表).
[29] 戴世坤.双相介质中的震电效应和震电波场传播理论[D].博士后研究工作报告,北京:石油大学,1996.
[30] 胡恒山,王克协.井孔周围周对称声电耦合波:(1)理论[J].测井技术[J].1999,23(6):427～423.
[31] 胡恒山,王克协.井孔周围周对称声电耦合波:(2)声电效应测井数值模拟[J].测井技术,2000,24(1):3～13.
[32] 胡恒山,刘家琦,王洪滨,等.声电效应测井响应的似稳场近似模拟[J].地球物理学报(待发表).
[33] Mavko,G .M ,Nur,A .Waveattenuationinpartiallysatu ratedrocks[J].Geophysics,1979,44:161～178.
[34] Toksoz,MN ,Johnston,D .H .andTimur,A .T .Atten uationofseismicwavesindryandsaturatedrocksⅠlabo ratorymeasurements[J].Geophysics,1979,44:681～690.
[35] Toksoz,MN ,Johnston,D .H ,Timur,A .T .Attenua tionofseismicwavesindryandsaturatedrocksⅡmecha nisms[J].Geophysics,1979,44:691～711.
[36] PointerT ,LiuE ,andHudson.Seismicwavepropagationincrackedporousmedia[J].GeophysJ .Int.2000,142:199～231.
[37] 赵玉林,钱复业,张德倍,等.地电台的最佳台址条件———岩石电阻率对应变的高放大系数及低的干扰幅度[A].见:地磁地电分册[C].北京:地震出版社,1988:170～179.
[38] 毛桐恩,席继楼,王燕琼,等.地震过程中的大地电场变化特征[J].地球物理学报,1999,42(4):520～528.
[39] 王玲,何继善.描述激电效应的非线性扩散方程[J].地球物理学报,1999,42(6):849～857.
[40] 刘洪,严洪瑞,等.电场地震资料的特征[A].见:寸丹集(庆祝刘光鼎院士工作50周年学术论文集)[C],北京:科学出版社,1998,145～153.
[41] YanHongrui.Seismicsurveyinelectricfield:Anewseis mo electricprospectingmethod[A].SEG98AnnualMeet ingAbstract(ISSN 1052-3812)[C].1998,984～987.
[42] 严洪瑞,刘洪,等.震电勘探方法在大庆油田的现场实验[J].地球物理学报,1999,42(2):257～267.
[43] 李建勇,刘洪,李幼铭,等.大庆电场地震实验资料的面波特征[J].地球物理学进展,2001,16(4):29～34.
[44] 杨进,谭捍东,傅良魁.被动源激发极化法的数值模拟结果[J].现代地质,1999,13(增刊):132～133.
[45] 孙卫斌.振动激励场效应及实测技术研究[D].[硕士学位论文],北京:中国地质大学,1999.
[46] 石昆法.震电效应原理和初步实验结果[J].地球物理学报,2001,44(5):720～728.
[47] 煤炭科技动态编辑部编.一种最新的地球物理探测技术[M].北京:煤炭科技出版社,1985.
[48] GeophysicalInternationalCompany.岩性电测深法[A].见:电法勘探译文集[C].北京:地质出版社,1987,172～179.
[49] 张立敏.岩性探测技术研讨会会讯[J].地球物理学报,1987,30(1):17.
[50] 地球物理学报编辑部.第二次岩性探测技术研讨会及学习班[J].地球物理学报,1989,32(4):21.
[51] Elam,J .G .,(戈盾译).新方法有助于改善地下解释[A].见:石油地球物理勘探参考资料[C].北京:石油工业出版社,1990.
[52] 关士聪.“空间源直接探矿仪”找油应用及研究新进展[J].石油与天然气地质,1991,12:35.
[53] 刘洪.利用动电效应进行地下油气水勘探的方法[J].石油物探信息,1993,1.
[54] 刘洪,李幼铭.关于震电勘探油气水的几点看法[J].石油物探,1994,33(2):94～101.
[55] 刘洪.利用天然电磁场高分辨探测地下油气水的可能性[J].地球物理学报,1994,37(6):828～835.
[56] 刘光鼎.中国油气资源企盼二次创业[J].地球物理学进展,2001,16(4):1～3.
[2] Ivannov,A .G .Effectofelectriczationofearthlayersbye lasticwavespassingthroughthem(inRussian)[J].DokladyAkademiiNauk,SSSR ,1939,24:41～43.
[3] Frenkel,J .OnthetheoryofSeismicandSeismoelectricPhenomenainamoistsoil[J].J.Physics,(Soviet),1944,8(4):230～241.
[4] 傅承义.地表层的本质对于地震勘测的几种影响[J].中国科学,1951,2(3):271～281.
[5] BiotMA .Theoryofpropagationofelasticwaveinafluid saturatedporoussolid,I low frequencyrange[J].J .A coust.Soc.Am.,1956,28:168～178.
[6] Dmowska,Electromechnicalphenomenaassociatedwithearthquakes[J].GeophysicalSurveys,1977,3:157～174.
[7] R .C .Rogers,S .S .Antman.Steady stateproblemsofnon linearelectro magneto thermo elasticity[J].ArchRation.Mech.&Anal,1986,95(4):279～323.
[8] Potapof.O .A ,etal1995,Principleofseismo electricprospecting,Ned’la,Moskow.波达波夫,中译本(译者:裘慰庭)震电勘探方法,北京:石油出版社,1997.
[9] D ,MarshallandT ,R ,Madden.Inducedpolarizationastudyofitscause[J].Geophysics,1959,24(4):796～816.
[10] Morgan,F .D .E .R .Madden,andT .R .Madden.Streamingpotentialpropertiesofwesterlygranitewithap plication[J].J.Geophys.Res.,1989,12449～12461.
[11] G .Pantelis.Saturated unsaturatedflowinunconfinedaquifers[J].Z .Angew.Math.&Phys.(Switzerland),1985,36(5):648～657.
[12] 蒋洪堪,蒋承菘.访苏见闻-介绍苏联的几种电法[J].物探与化探,1984(1):12～19.
[13] 高章伟.苏联物探技术点滴[J].国外油气勘探,1990,98.
[14] 波利亚科娃.(楚泽涵译).电声测井一种新的测井方法[J].地质与勘探,1990,4.
[15] 巴莲科娃,切勒尼克.(王勋弟译).脉冲谐波激励的电声测井,1991,6(1):11～15.
[16] Neev,J.andF .R .Yeatts.Electrokineticeffectsinfluidsaturatedporoelasticmedia[J].Phys.Rev.B ,1989,40:9135～9142.
[17] Thompson,A .H .,Gist,G .A .Geophysicalapplicationsofelectrokineticconversion[J].TheLeadingEdge,1993,1169～1173.
[18] Zhu,Z .,C .Cheng,andM .Toksoz.Experimentalstudyofflexuralwavesinafracturedorcasedboreholemodel[A].In:soc.,pxplgeophys.64thann,internat.mtg,Abstract[C],1994,70～73.
[19] Haartsen,MW .CoupledElectromagneticandAcousticWavefieldModelinginPoro elasticMediaanditsApplica tionsinGeophysicalExploration[D ].Ph.DThesisofMIT ,1995.
[20] V .Mikhailov,M .W .Haartsen,andM .N .Toksoz.Elec troseismicinvestigationoftheShallowsubsurface,Fieldmeasurementandnumericalmodeling[J].Geophysics,1997,62(1):97～105.
[21] ButlerKE ,RusselRD ,KepicAW ,etal.Measurementoftheseismoelectricresponsefromashallowboundary[J].Geophysics,1996,61:1769～1778.
[22] Pride,SR ,MorganFD .Electrokineticdissipationin ducedbyseismicwave[J].Geophysics,1991,56:914～925.
[23] Pride,S .Governingequationsforthecoupledelectromag neticsandacousticsofporousmedia[J].Phys.Rev.B ,1994,50:15678～15696.
[24] PrideSR ,HaartsenMW ,ToksozMN .Electroseismicwaveproperties[J].J .AcousticalSoc.Am.100(3):1301～1315.
[25] V .Mikhailov,QueenJ ,andM .N .Toksoz.UsingBore holeelectroseismicmeasurementtodetectandcharacterizefractured(permeable)zones[J].Geophysics,2000,65:1098～1112.
[26] 裘慰庭.震电效应在油气勘探中的应用前景[A].见:牛毓荃主编石油物探新技术系列调研成果[C].北京:石油工业出版社,1996,640～651.
[27] 周成当,尉中良,管志宁,等.双相孔隙介质中低频声激发极化电场模拟[J].现代地质,1999,13(增刊):118～124.
[28] 胡恒山,刘家琦.对波达波夫震电波方程组的几点注解[J].地球物理学报(待发表).
[29] 戴世坤.双相介质中的震电效应和震电波场传播理论[D].博士后研究工作报告,北京:石油大学,1996.
[30] 胡恒山,王克协.井孔周围周对称声电耦合波:(1)理论[J].测井技术[J].1999,23(6):427～423.
[31] 胡恒山,王克协.井孔周围周对称声电耦合波:(2)声电效应测井数值模拟[J].测井技术,2000,24(1):3～13.
[32] 胡恒山,刘家琦,王洪滨,等.声电效应测井响应的似稳场近似模拟[J].地球物理学报(待发表).
[33] Mavko,G .M ,Nur,A .Waveattenuationinpartiallysatu ratedrocks[J].Geophysics,1979,44:161～178.
[34] Toksoz,MN ,Johnston,D .H .andTimur,A .T .Atten uationofseismicwavesindryandsaturatedrocksⅠlabo ratorymeasurements[J].Geophysics,1979,44:681～690.
[35] Toksoz,MN ,Johnston,D .H ,Timur,A .T .Attenua tionofseismicwavesindryandsaturatedrocksⅡmecha nisms[J].Geophysics,1979,44:691～711.
[36] PointerT ,LiuE ,andHudson.Seismicwavepropagationincrackedporousmedia[J].GeophysJ .Int.2000,142:199～231.
[37] 赵玉林,钱复业,张德倍,等.地电台的最佳台址条件———岩石电阻率对应变的高放大系数及低的干扰幅度[A].见:地磁地电分册[C].北京:地震出版社,1988:170～179.
[38] 毛桐恩,席继楼,王燕琼,等.地震过程中的大地电场变化特征[J].地球物理学报,1999,42(4):520～528.
[39] 王玲,何继善.描述激电效应的非线性扩散方程[J].地球物理学报,1999,42(6):849～857.
[40] 刘洪,严洪瑞,等.电场地震资料的特征[A].见:寸丹集(庆祝刘光鼎院士工作50周年学术论文集)[C],北京:科学出版社,1998,145～153.
[41] YanHongrui.Seismicsurveyinelectricfield:Anewseis mo electricprospectingmethod[A].SEG98AnnualMeet ingAbstract(ISSN 1052-3812)[C].1998,984～987.
[42] 严洪瑞,刘洪,等.震电勘探方法在大庆油田的现场实验[J].地球物理学报,1999,42(2):257～267.
[43] 李建勇,刘洪,李幼铭,等.大庆电场地震实验资料的面波特征[J].地球物理学进展,2001,16(4):29～34.
[44] 杨进,谭捍东,傅良魁.被动源激发极化法的数值模拟结果[J].现代地质,1999,13(增刊):132～133.
[45] 孙卫斌.振动激励场效应及实测技术研究[D].[硕士学位论文],北京:中国地质大学,1999.
[46] 石昆法.震电效应原理和初步实验结果[J].地球物理学报,2001,44(5):720～728.
[47] 煤炭科技动态编辑部编.一种最新的地球物理探测技术[M].北京:煤炭科技出版社,1985.
[48] GeophysicalInternationalCompany.岩性电测深法[A].见:电法勘探译文集[C].北京:地质出版社,1987,172～179.
[49] 张立敏.岩性探测技术研讨会会讯[J].地球物理学报,1987,30(1):17.
[50] 地球物理学报编辑部.第二次岩性探测技术研讨会及学习班[J].地球物理学报,1989,32(4):21.
[51] Elam,J .G .,(戈盾译).新方法有助于改善地下解释[A].见:石油地球物理勘探参考资料[C].北京:石油工业出版社,1990.
[52] 关士聪.“空间源直接探矿仪”找油应用及研究新进展[J].石油与天然气地质,1991,12:35.
[53] 刘洪.利用动电效应进行地下油气水勘探的方法[J].石油物探信息,1993,1.
[54] 刘洪,李幼铭.关于震电勘探油气水的几点看法[J].石油物探,1994,33(2):94～101.
[55] 刘洪.利用天然电磁场高分辨探测地下油气水的可能性[J].地球物理学报,1994,37(6):828～835.
[56] 刘光鼎.中国油气资源企盼二次创业[J].地球物理学进展,2001,16(4):1～3.
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