用户名: 密码: 验证码:
矿井瞬变电磁场分布规律与应用研究
详细信息    本馆镜像全文|  推荐本文 |  |   获取CNKI官网全文
摘要
近几年,矿井瞬变电磁法在全国各个矿区逐渐得到了推广和应用,其应用效果和带来的经济和社会效益逐渐得到认可。但在矿井地质条件下,即巷道空间影响下瞬变电磁场在全空间内的分布规律没有得到系统的研究,研究巷道空间及空间内的金属体(工字钢、铁轨和金属锚网)对探测结果的影响规律是矿井瞬变电磁法资料解释及处理中的关键技术。本论文以均匀介质中瞬变电磁场响应理论为基础,编制了全空间瞬变电磁场正演模拟程序,结合数值计算和物理模型实验,总结了矿井地质条件下瞬变电磁场的分布规律。主要研究成果如下:
     1)研究了全空间条件下瞬变电磁场的传播规律。在早期阶段,感应电流集中分布于发射天线附近,电磁场主要反映地层浅部地质信息;在晚期阶段,高频成份被导电介质吸收,低频成份占主导地位,这时瞬变电磁场的传播主要是扩散过程,反映中深部的地质信息;
     2)研究了矿井瞬变电磁法最小及最大探测深度及其影响因素。由于采用多匝小回线天线,接收信号不仅包括探测目标体感应的有用地质信息同时还包括由于线圈产生的自感信号。在采样早期阶段线圈自感信号比目标体感应信号强,但其衰减速度较快。在线圈自感信号衰减时间范围内线圈自感信号与浅层地层介质感应信号很难分离,所以总存在一个无法分辨目标体感应信号的时间范围,这个范围则是矿井瞬变电磁法对应的探测盲区,即最小探测深度。线圈自感信号迅速衰减后,接收的信号主要为不同深度介质的感应信号。由于瞬变电磁场在介质中传播时能量不断地衰减,当能量衰减到一定程度时就不可分辨,无法识别更深地层介质的感应信息,所以对应一个最大探测深度;
     3)建立了全空间瞬变电磁场数学模型,并编写了三维有限元正演模拟程序。利用所编制的程序对不同模型及不同参数进行计算对比分析。在均匀全空间条件下分离回线装置与重叠回线装置所接收的感应信号衰减规律基本一致,但分离回线装置接收的响应值比重叠回线装置接收的响应值小,说明在相同条件下重叠回线装置的灵敏度较高;巷道空间的存在使瞬变电场响应值减小,但没有改变其整体上的衰减趋势。当巷道空间围岩介质中存在低阻异常体时,巷道空间对异常体响应曲线的影响主要集中在采样时间序列的早期阶段,而对采样时间序列的晚期阶段无影响,说明巷道空间的存在对浅层异常体的探测结果有影响,而且巷道空间越大,对探测结果影响越大;
     4)对巷道空间内金属体对感应场的干扰特征进行了物理模型实验:当天线位于巷道靠近探测目标体所在一侧时,接收到的响应值最高;当天线位于远离探测目标体一侧时,由于巷道空间的影响使探测结果的分辨能力降低。巷道内的金属体(工字钢、金属锚网和铁轨)使所接收到的信号值变大;
     5)根据数值模拟和物理模型实验结果,设计了矿井瞬变电磁探测方法与技术。如果探测目标体位于巷道顶板以上,同时巷道内有锚网支护底板上有铁轨时,发射接收天线置于巷道顶板;如果探测目标体位于工作面煤层,应将天线装置垂直巷道底板,并且靠近探测目标体所在巷道一侧,以获得探测目标体最大的感应信号;如果不能确定异常体的具体空间位置,应采用全方位探测技术。
     论文有图77幅,表4个,参考文献127篇。
Mine transient electromagnetic method has been gradually popularized and applied in many mining areas in recent years. The applied effect, economic performance and social benefits have been acknowledged, but the basic theory, construction technology, data processing and display technique of mine transient electromagnetic method, all that adopt the research production of transient electromagnetic method on the ground. In mining geological conditions, it is said that under the influence of the roadway space, the regularities of distribution of transient electromagnetic field in the full space has not been complete researched at the present time. It is very important that research the influence law of roadway space and metal bodies (double T-iron, rail and metal netting) to the detecting data for transient electromagnetic method data processing and data explanation. The paper made a procedure to simulate the full space transient electromagnetic field, which based on the theory of transient electromagnetic field in homogeneous medium. The main research findings as follow:
     1) The propagation characteristics of full-space induction field of transient electromagnetic method were researched. The results indicated that the induced current mainly distributed on the surface of the geologic body and the response of transient electromagnetic field mainly reflects the superficial information of the stratums during the early stage. But during the late stage, the high frequency component was absorbed by electrical medium, so low frequency sign was dominant. The mode of transmission of transient electromagnetic fields was mainly diffuse process which reflects the information of the deep stratums.
     2) The minimal and maximum detecting depth and its influence factors were researched. The results indicated that the acquisition data included not only the useful geologic signal about the aim body, but also the self-induced signal that because of the multi-turn little coils. During early stage, the self-induction signal is stronger than the useful geologic signal. It is difficult to separate the self-induction signal and the shallow stratum signal. Therefore, there is a time range, during which we cannot separate the useful signal, so before this time is the detecting blind zone for transient electromagnetic method, which is the minimal detecting depth. After the attenuation of self-induced signal, the signal is mainly induced signal for vary depths. Because of the energy attenuation, when we cannot distinguish the induced signal of deeper-stratum, which is the maximum detecting depth.
     3) The mathematical model of the full-space transient electromagnetic fields was established and the finite element numerical simulation method of three dimensions transient electromagnetic field was studied. The concept of area coordinates and cubage coordinates were introduced during the liner interpolation process, which made the design procedure of the mathematical model becomes easier. The memorize technology of ultra-large sparse matrix was studied, which saves the memory and the computation time. Contrasted and analysed the response characteristic of transient electromagnetic field for different models and different parameters. The results indicated that the induced signal of separate loops and overlap loops has the same attenuation laws in the homogeneous whole space, but the field value of former is smaller than the field value of later, which shows that overlap loops has a better sensitivity in the same conditions. The roadway space minished the response value of transient electromagnetic field, but did not change the attenuation trend. When there is a low resistivity body in the medium around the roadway space, the effects of the roadway space shows only in early period. This shows that the superficial layer is affected by the roadway space, and the roadway space is bigger, the effects is stronger.
     4) Through the physical model experiment, the paper concluded that, when transmission and reception are placed beside the aim body, the response is the strongest, and when transmission and reception are placed faraway from the aim body, the sensitivity will fall greatly. The response values become strong for the metal body (double T-iron, rail and metal netting) in roadway space, but the features keep the same for the abnormal body. The accepted induced signals mainly come from the response of terra medium near the roadway side during the survey, which is that the distance between antenna and aim body is smaller, the response is stronger.
     5) Base on the result of numerical simulation and physical model experiment, we designed the construction technology of mine transient electromagnetic method: If the detecting target locates in roof, and there are railway rail on the floor, the antenna should been placed near the roof. But for the target that locates under the floor, the antenna should been placed on the floor. When we cannot confirm the specific spatial location, the omni-bearing detecting technology should been applied.
引文
[1] 李貅.瞬变电磁测深的理论与应用.西安:陕西科学技术出版社.2002
    [2] 蒋邦远主编.实用近区磁源瞬变电磁法勘探.北京:地质出版社.1998
    [3] 何峰,蒋维庆.矿井音频电透视的应用. 中国煤炭学会第六届青年科技学术研讨会论文集.2000
    [4] 于景邨.矿井瞬变电磁法理论与应用技术研究.[博士学位论文]中国矿业大学.1999
    [5] 李金铭等.电法勘探新进展.北京.地质出版社.1996
    [6] 郑永祥,郗金栋.矿井无线电透视法试验研究.煤田地质与勘探.1978.03:22-31
    [7] 唐新功,胡文宝,严良俊.层状地层中三维薄板的瞬变电磁响应.石油地球物理勘探.2000.10,35(5):628-633.
    [8] 阎述,陈明生.线源频率电磁测深二维正演.煤田地质与勘探.1999.27(5,6):60-62,56-59.
    [9] 牛之琏.一维层状大地的瞬变电磁测深正演计算.煤田地质与勘探.1991,6
    [10] 殷长春,刘斌.瞬变电磁法三维问题正演及激电效应特征研究.地球物理学报.1994.8,37(增):486-49.
    [11] 阮百尧.Guptasarma算法在瞬变电磁正演计算中的应用.桂林工学院学报.1996,2
    [12] 刘继东.地面大回线源在地下形成的瞬变电磁场的反演研究.物探化探计算技术.1998,2
    [13] 卢健.瞬变电磁矩形线框一维正演及电磁信号去噪研究.[硕士论文]大连理工大学,2004.
    [14] 宛新林,席道瑛,高尔根.三维电阻率正演计算中的 Lanczos 迭代算法.岩土力学.2003.10,24(增):108-111.
    [15] 陈小斌,胡文宝.有限元直接迭代算法在 MT 二维正演计算中的应用.石油地球物理勘探.35(4)487-496.
    [16] 陈小斌,胡文宝.有限元直接迭代算法及其在线源频率域电磁响应计算中的应用.地球物理学报 45(1):119-130.
    [17] 吴小平,汪彤彤.利用共扼梯度算法的电阻率三维有限元正演.地球物理学报.2003.5,46(3):428-432.
    [18] 谢辉,钟燕辉,蔡迎春.电磁场有限元法在 GPR 正演模拟中的应用.河南科学.2003.6,21(3):295-298.
    [19] Wait J R. Transient EM propagation in a conducting medium. Geophysics, 1951, Vol.16:213-221.
    [20] Hjelt S E. Transient EM field of a two-layer sphere. Geoexploration, 1971, Vol.9:213-229.
    [21] Nabighian M N. Quasi-static transient response of a conducting half-space—An approximate represent -ation. Geophysics, 1979, Vol.44:1700-1705.
    [22] Jin-Fa Lee and Nicholas Buris. Solving Maxwell’s equations by edge element time domain methods. IEEE,1994, vol.3:1756-1759.
    [23] Raiche A P and Spies B R. Coincident loop transient electromagnetic master curves for interpretation of two-layer earth.Geophysics, 1981, Vol.46:53-64.
    [24] Knight J H and Raiche A P. Transient electromagnetic calculations using the Gaver-Stehfest inverse Laplace transform method. Geophysics, 1982, Vol.47(1):47-50.
    [25] Kaufman A A , Keller G V. Frequency and Transient Soundings. New York :Elsevier , 1983
    [26] Leppin M. Electromagnetic modeling of 3-D sources over 2-D inhomogenetices in the time domain. Geophysics, 1992, Vol.57:994-1003.
    [27] Newman G A and Hohmann G W. Time-domain EM response of a three-dimensional body in a layered earth. 54th Annual International SEG Meeting, 1986, 67-69.
    [28] Raiche A P et al. The joint use of coincient loop transient EM and schlunmberger sounding to relove layered structures. Geophysics, 1985, Vol.50:1618-1627.
    [29] Kuo J T and Cho D H. Transient time-domain electromagnetic. Geophysics, 1980, Vol.45:271-292.
    [30] Goldman M.M. and Stoyer C.H..Finite-difference caculations of the transient field of an axially symmetric earth for vertical magnetic dipole excitation.Geophsics,1983,48:953-962
    [31] M.M. Goldman. The integral-finite-difference method for calculating transient electromagnetic field in a horizontally stratified medium. Geophsical prospecting, 1983, 31: 664-686
    [32] Oristagtio M.L. and Hohmann G.W. Diffusion of electromagnetic field into a two-dimensional earth: A finite-difference approach. Geophsics, 1984, 49: 870-894
    [33] Adhidjaja J.I.et al. two-dimensional electromagnetic response. Geophsicis, 1985,50: 2849-2861
    [34] Goldman Y.A.. Finite-element solution for the transient electromagnetic response of arbitrary two-dimentional resistivity distribution. Geophsics, 1986, 51: 1450-1461
    [35] Leppin M., Electromagnetic modeling of 3-D sources over 2-D inhomogenetics in the time domain. Geophsics, 1992,57: 994-1003
    [36] L.A.Tabarovsky, M.M.Goldman, M.B.Rabinovich and K.M.Strck. 2.5-D Modeling in electromagnetic methods of geophsics. Journal of Applied Geophsics, 1996, 35: 261-284
    [37] Walter L.Aderson. Computation of Green’s tensor integrals for three-dimensional electromagnetic problems using fast Hankel transforms. Geophsics, 1984, 48(10): 1754-1759
    [38] Philip E. Wannamaker, Gerald W.Hohmann and William A.Sanfilipo. Electromagnetic modeling of three-dimensional bodies in layered earths using integral equations. Geophsics, 1984, 49(1): 60-74
    [39] San Filipo W.a.,Eaton P.A., Hohmann, G.W..The transient EM respose of a prism in aconductive half-space. 54th Annual International SEG Meeting, 1984,64-67
    [40] Newman G.A. and Homann G.W.. Time-domain EM response of a three-dimensional body in a layered earth. 54th Annual International SEG Meeting. 1986,67-69
    [41] Wang T and Hohmann G W. A finite-difference, time-domain solution for three-dimensional electromagnetic modeling. Geophysics, 1993, Vol.58:797-809.
    [42] Michaels S.Zhdanov, Sheng Fang. Quasi-linear approximation in 3-D electromagnetic modeling. Geophsics, 1996, 61(3):646-665
    [43] Tsili Wang and Alan C.Tripp. FDTD Simulation of EM wave propagation in 3-D media. Geophsics, 1996, 61(1):110-120
    [44] 方文藻,李予国.大回线法瞬变电磁测深正演计算.煤田地质与勘探.1991,2
    [45] 阎述,陈明生.线源频率电磁测深二维正演.煤田地质与勘探.1999.27(5,6):60-62,56-59.
    [46] 卢健.瞬变电磁矩形线框一维正演及电磁信号去噪研究.[硕士论文]大连理工大学,2004.
    [47] 黄俊革,阮百尧.三维电阻率测深有限元正演模拟中的边界影响.石油地球物理勘探. 2004.11,39(增):71-74.
    [48] 刘树才,岳建华,刘志新.煤矿水文物探技术与应用.徐州:中国矿业大学出版社.2005
    [49] 刘树才,岳建华. 瞬变电磁法在煤矿防治水中的应用. 第六届中国国际地球电磁学学术研讨会.北京,2003
    [50] 刘志新,于景村等. 矿井瞬变电磁法在水文钻孔探测中的应用. 物探与化探,2006,30(1):59-61
    [51] LIU Zhixin, YUE Jianhua, LIU Shucai.《Application of Synthetic Mine Geophysical Prospecting Technique in Detecting Collapse Columns》,International Conference “Waste Management, Environmental Geotechnology and Global Sustainable Development”, Ljubljana, SLOVENIA,28-30 August 2007.(国际会议论文)
    [52] 刘志新,岳建华,刘仰光。扇形探测技术在超前探测中的应用研究,中国矿业大学学报,2007,36(6):822-825.
    [53] 刘志新,于景邨,张华。小波变换在矿井瞬变电磁法中的应用,煤田地质与勘探,2007,35(4):70~72.
    [54] 刘志新,岳建华,刘仰光。矿井物探技术在突水预测中的应用,工程地球物理学报,2007,4(1):9~14.
    [55] 刘树才,刘志新,姜志海。瞬变电磁法在煤矿采区水文勘探中的应用,中国矿业大学学报,2005,34(4):414~417.
    [56] 于景邨,刘志新,汤金云。用瞬变电磁法探查综放工作面顶板水体的研究。中国矿业大学学报,2007,36(4):542-546.
    [57] 于景邨,刘志新,刘树才。深部采场突水构造矿井瞬变电磁法探查理论及应用,煤炭学报,2007,(8):818~821.
    [58] YU Jing-cun, LIU Zhi-xin, TANG Jin-yun. Research on Full Space Transient Electromagnetism Technique for Detecting Aqueous Structures in Coal Mines. Journal of china university of mining and technology, 2007 ,17(1):58-62.
    [59] 于景邨,刘志新,岳建华。煤矿深部开采中的地球物理技术现状及展望,地球物理学进展,2007,22(2)586~592.
    [60] 周仕新,岳建华.矿井中瞬变电磁场三维时域有限差分模拟.勘探地球物理进展,2005b,28(6).
    [61] 岳建华,甘会春. 矿井瞬变电磁法及其应用. 中国地球物理学会年会论文.南京:南京师范大学出版社,2003.
    [62] 白登海,何兆海,卢建等. 地下全空间瞬变电磁法及在煤矿水害预防中的应用。第六届中国国际地球电磁学学术研讨会.北京,2003.
    [63] 白登海. 时间域瞬变电磁法中心方式全程视电阻率的数值计算. 地球物理学报 2003,46(5) :697-704.
    [64] 陈明生,闫述石,显新,解海军.二维地质体的瞬变电磁场响应特征.地震地质,2001.06.
    [65] 闫述,陈明生,傅君眉.瞬变电磁场的直接时域数值分析.地球物理学报, 2002,45(2):275-284.
    [66] 闫述,石显新.井下全空间瞬变电磁法 FDTD 计算中薄层和细导线的模拟.煤田地质与勘探,2004,32(增刊) .
    [67] 白登海. 瞬变电磁法中两种关断电流对响应函数的影响及其应对策略.地震地质,2001,23(2):245-251.
    [68] 薛国强。论瞬变电磁测深法的探测深度。石油地球物理勘探,2004,39(5):575-578.
    [69] 乔松,周锰钰,白朗。勘探电磁场论。中国矿业大学出版社,1991.
    [70] 金建铭(美)著.王建国译.电磁场有限元方法.西安:西安电子科技大学出版社.1998.
    [71] 谢德馨等.三维涡流场的有限元分析.北京:机械工业出版社.2001.
    [72] 曹德欣,曹璎珞.计算方法.徐州:中国矿业大学出版社.2001.
    [73] 牛之链.时间域电磁法原理.长沙:中南工业大学出版社.1992.
    [74] 刘长学.超大规模稀疏矩阵计算方法.上海:上海科技出版社.1991.
    [75] 张光澄等.最优计算化方法.成都:成都科技大学出版社.1989.
    [76] 杨慧珠,张友生,陶果.井眼条件下弹性波传播问题的三维有限差分数值模拟.地球物理学进展. 2003,06.
    [77] 袁伟良,梁昌洪. 时域有限差分法的优化吸收边界条件. 西安电子科技大学学报. 1998,10.
    [78] 陈本池等.瞬变电磁场的波场变换研究.物探与化探,1999.06.
    [79] 吴小平,徐果明.利用ICCG迭代技术加快电阻率三维正演计算.煤田地质与勘探,1999.03.
    [80] 吴小平等.利用不完全 Cholesky 共轭梯度法求点源三维地电场.地球物理学报,1998.
    [81] 吕国印,张杰.瞬变电磁法感应探头自然频率与响应畸变,SEG2003,425~428.
    [82] 翁爱华,陆冬华.利用连分式定义瞬变电磁法全区视电阻率研究.煤田地质与勘探,2003,31(3):56~59.
    [83] 陈金方,于景村,李全,童宏树. 矿井TEM探测导水陷落柱及检测注浆效果. 江苏煤炭,2002,No.4: 7~8.
    [84] Kaufman A A , Keller G V. Frequency and Transient Soundings. New York :Elsevier , 1983.
    [85] Ward, S. H., and Hohmann G. W., 1988. Electromagnetic theory for geophysical applications, in M. N. Nabighian, Ed., Electromagnetic methods in applied geophysics, Vol.1,Theory : Society ofExploration Geophysicists, Chapter 4,130–311.
    [86] Anderson, W.L., 1981, Calculation of transient soundings for a central induction loop configuration(Program TCILOOP): USGS Open-file report 81-1309.
    [87] Anderson, W.L.,1989, A hybrid fast Hankel transform algorithm for electromagnetic modeling,Geophysics 54, 263–266.
    [88] Stefi Krivochieva, Michel Chouteau. Whole space modeling of a layered earth in time-domain electromagnetic measurements. Journal of Applied Geophysics, 2002,Vol.50:375-391.
    [89] 岳建华,何兵寿.超吸收边界条件在地质雷达剖面正演中的应用. 中国矿业大学学报 1999,28(5)
    [91] Wang Tsili, Hohmann G. W. ,1993,A finite-difference time-domain solution for three-dimensional electromagnetic modeling, Geophysics, Vol.58:797-817.
    [91] 阮百尧,徐世浙.线源二维时间域电磁响应的有限差分解.高校地质学报,1996,2(4).
    [92] 宋维琪.3D 瞬变电磁场有限差分正演计算.石油地球物理勘探,2000,35(6).
    [93] Commer M. , Newman G. A., 2004, A parallel finite-difference approach for three dimensional transient electromagnetic modeling with galvanic sources: Geophysics, VOL. 69, NO. 5,1192–1202.
    [94] 李竞生.华北型煤田水害防治技术进展[J]. 论文集//世纪之交的煤炭科学技术.煤炭学报,1997,22(增刊):98-99.
    [95] 靳德武. 我国煤层底板突水问题的研究现状及展望[J]. 煤炭科学技术,2002,30(6):1-4.
    [96] 王 军. 矿山地下水害防治技术新进展[J]. 采矿技术,2002,2(3):55-58.
    [97] 杨善安.采场底板断层突水及其防治方法[J]. 煤炭学报,1994,19(6):620-625.
    [98] 罗润林. 一种层状大地瞬变电磁响应正演计算的改进方法. 物探化探计算技术,2005,27(1).
    [99] 张运霞. PROTEM67D 瞬变电磁仪器在矿井水文地质勘探中的应用效果. 工程地球物理学报,2005,3(2)12-15.
    [100] 王兴泰,万明浩等. 工程与环境物探新方法新技术. 北京:地质出版社, 1996.
    [101] 崔霖沛,吴其斌. 环境地球物理方法及其应用. 北京:地质出版社, 1997.
    [102] 霍全明,王玉海,罗国平等.瞬变电磁法在煤矿水害预测防治中的应用. 西安:西北工业大学出版社,1994.
    [103] 于景村. 矿井瞬变电磁法理论与应用技术研究.中国矿业大学博士学位论文,2001.
    [104] 时晗.瞬变电磁法在巨厚覆盖层地区勘查地下水源的应用.中国煤田地质,2005,(3).
    [105] 牛向东,张运霞,韩自豪,周建雄.瞬变电磁法在探测导水通道中的应用.山东科技大学学报(自然科学版),2005,(2).
    [106] 张晓永.瞬变电磁法的中深部铝土矿预测研究.工程地球物理学报,2005,(2).
    [107] 郝威,周学军.采用瞬变电磁法的海底光缆定位.光纤与电缆及其应用技术,2005,(1).
    [108] 唐新功,胡文宝,严良俊.瞬变电磁法找水研究.工程地球物理学报,2005,(3).
    [109] 高永才,李永年,王绪本,徐雯琪.瞬变电磁法金属管道腐蚀检测理论初探.物探化探计算技术,2005,(1) .
    [110] 何展翔,罗延钟.西方地面瞬变电磁法理论的发展现状.国外地质勘探技术,1989. [111 丁世荣,方文藻.球形地质体在阶跃磁偶极源激励下的瞬变电磁响应.辽宁师范大学学报(自然科学版),1997,20(3):218~223.
    [112] 唐新功,胡良俊等.层状地层中三维薄板的瞬变电磁响应.石油地球物理勘探,2000,35(5):628~633.
    [113] 宋维琪.3D 瞬变电磁场有限差分正演计算.石油地球物理勘探,2000,35(6):751~756.
    [114] 王华军,罗延钟.中心回线瞬变电磁法 2.5 维有限单元算法.地球物理学报,2003,46(6):855~862.
    [115] 罗延钟,张胜业等.时间域航空电磁法一维正演研究.地球物理学报,2003,46(5):719~724.
    [116] 殷长春,刘斌.瞬变电磁法三维问题正演及激电效应特征研究.地球物理学报,1994,37(增Ⅰ):486~492.
    [117] 蒋邦远,磁源瞬变电磁法测深一维反演经验式及应用效果,物探与化探,2000,24(4):99~104.
    [118] 严良俊,徐世浙等.中心回线瞬变电磁测深法快速电阻率成像方法及应用.煤田地质与勘探,2002,30(6):58~61.
    [119] 苏朱刘,胡文宝.中心回线方式瞬变电磁测深虚拟全区视电阻率和一维反演方法.石油物探,2002,41(2):116~221.
    [120] 宋先旺,姜胜华.瞬变电磁法全期视电阻率、视深度求解方法与应用.矿产与地质,1997,41(2):129~136.
    [121] Brian R.Spies,Swight E.Eggers.The use and misuse of apparent resistivity in electromagnetic methods.Geophysics,1986,51(7):1462~1471.
    [122] Morrison H F,Phillips R J,O’bien D P.Quantitative interpretation of transient electromagnetic fields over a layered half space.Geophys.Prosp.1969,17:82~101.
    [123] Kaufman A A,Keller GV.Frequency and Transient Soundings.New York :Elsevier,1983.
    [124] Lee T , Thomas L.The transient electromagnetic response of a polarizable sphere in a conducting half space.Geophys .Prosp.1992 , 40 :541~563.
    [125] Willian A S,Perry A E,Hohmann GW.The effect of a conductive half space on the transient electromagnetic response of a three dimensional body.Geophysics,1985,50(7):1144~1162.
    [126] 王作宇,刘鸿泉.承压水上采煤[M].北京:煤炭工业出版社,1993.
    [127] 刘志新,岳建华,刘仰光。《矿井物探技术在突水预测中的应用》,工程地球物理学报,2007,4(1):9~14.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700