用户名: 密码: 验证码:
浅层高分辨率全程瞬变电磁系统中全程二次场提取技术研究
详细信息    本馆镜像全文|  推荐本文 |  |   获取CNKI官网全文
摘要
随着社会经济和城市建设的发展,对工程与环境地质问题的关注,需要对浅层近地表进行精细探测与评价。瞬变电磁法勘察是环境与工程探测的重要方法,主要用于地下水调查、地下固体废物与污染物探测、考古、土壤评价及城市管线探测等。
    近年来,高分辨率探测浅层的地下目标体已经成为瞬变电磁法发展的热门方向,消除实测全程瞬变信号中的一次场和线圈过渡过程的影响,是实现浅层高分辨率探测的关键技术。本论文以非磁性导电球体在斜阶跃激励下的全程瞬变电磁响应为基础,以消除实测全程瞬变信号中接收线圈的过渡过程影响、提取全程瞬变二次场为研究重点,结合中国地质大调查项目“轻便面积性时间域电法仪器完善与示范”、国家自然科学基金项目“浅层高分辨率全程瞬变电磁(ATTEM)系统与关键技术研究”、国家自然科学基金项目“近区磁源阵列瞬变电磁探测系统与实验研究”和国家科技十五攻关计划子专题“强场源瞬变电磁技术完善与升级”的科研工作,主要研究成果如下:
    1.研究了斜阶跃脉冲激励下的一次感应电压及其过渡过程,并以非磁性导电球体为模型研究了斜阶跃脉冲激励下的二次感应电压和全程瞬变响应特征,分析了接收线圈的过渡过程存在时,一次场和二次场同全程瞬变响应的关系。
    2.研究了一次感应电压及其过渡过程对全程瞬变电磁响应的影响,分析了接收线圈的各个电性参数对全程瞬变响应的影响,论证了剔除一次场的过渡过程可以获取全程瞬变二次场,可以缩小最早取样时间,使探测深度变小。
    3.以实际测量参数和理论计算相结合的方法,对浙江舟山市老虎山4测线和吉林长春地质宫327室内实测瞬变响应进行全程二次场提取的研究,证
    
    
    明了剔除一次场的过渡过程可以提高浅层探测的分辨率和精度,消除了视电阻率值在浅部出现高阻盖层现象,进一步验证了勘探深度变小。
    4.研究了提高瞬变电磁信号晚期信噪比的方法,提出三点指数逼近非线性平滑滤波和基于几何平均的近似对数等间隔取样处理方法,基于“烟圈”理论的一维快速反演和解释的方法,研制开发了一套ATTEM数据处理及解释软件。
    5.利用自行研制的ATTEM样机在长春蔡家活断层和浙江舟山连岛工程的勘察应用,进一步验证剔除一次场可以提高浅层的探测分辨率。
    全文的主要创新性工作:
    1.首次研究了在考虑接收线圈的过渡过程情况下对实测全程瞬变电磁响应剔除一次场的方法,实现全程二次场的提取,以提高近地表浅层勘探的分辨率和精度。
    2.针于自行研制的ATTEM系统的均匀密集采样方式,首次提出三点指数逼近非线性平滑滤波和近似对数等间隔取样处理的方法,以提高瞬变信号的晚期信噪比。
    3.从解释方法和测量系统上,突破了常规时间域电磁系统只测量衰减段瞬变响应及相应的解释方法,自行研制的ATTEM样机实现了全程瞬变响应的测量,并研制开发了可以剔除一次场影响的处理解释软件,在长春蔡家活断层和浙江舟山连岛工程勘察应用中,对提取全程二次场算法进行了验证。
    围绕“浅层高分辨率全程瞬变电磁系统中提取全程瞬变二次场的技术研究”有待进一步研究的工作:
    1.针对浅层高分辨率瞬变电磁探测问题,需要研究接收线圈的频率特性,缩短接收线圈的过渡过程,降低全程瞬变信号早期畸变。
    2.进一步研究在早期全程瞬变信号的超高速采样技术、高精度实时同步技术,提高记录数据的分辨率。
    3.结合时频分析、短时傅里叶变换、小波变换等技术,研究晚期瞬变信号的压制噪声技术,提高测量信号晚期信噪比,使数据可用范围加大。
    4.进一步研究多匝小线圈工作装置下的反演及解释工作。
    5.研究瞬变电磁信号偏移成像技术,目前国内研究的不够。
With the developing of social economic and city construction, and more attention for the engineering and environmental geology, shallow subsurface investigation and evaluation has become the key subject of current research. Transient electromagnetic exploration (TEM) is an important method for environment and engineering, mainly applied in ground water investigation, ground solid waste and poison detecting, archaeology, soil engineering studies and detecting city ground piping, etc.
    Recently, high resolution shallow subsurface sounding is a popular electromagnetic research orient. Removing primary field and transient process from the measured all-time TEM(ATTEM)signals is the key technology for high resolution shallow subsurface sounding. Based on all-time transient electromagnetic response of nonmagnetic conductive sphere under tilting step signal, this dissertation, which depends on China Geology Investigation Project ”Portable area TEM instrument advancement and demonstration” and National Natural Science Foundation ”Research on high resolution shallow subsurface all time TEM system and key technology” and “Research on near area magnetic source TEM system and experiment ” and National Science and Technology the tenth Five Plan ”Strong field source TEM technology perfecting and advancement”, mainly discusses on removing transient process from the
    
    
    measured all-time TEM signals and gaining the secondary field. The achievements are obtained as following:
    1. Research on primary induction voltage and its transient process under the tilting step impulse, and discuss all time transient response characterization of secondary induction voltage and its transient process based on nonmagnetic conductive sphere model. Analyze the all time transient response relation between the primary field and secondary field while the transient process exists in receiver coil.
    2.Research all time transient electromagnetic response affected by primary induction voltage and its transient process, and analyze all time transient response changing with the receive coil electrical parameters, also demonstrate to gain all time secondary field by removing primary field and reduce earliest sampling time in order to achieve smaller exploration depth.
    3. According to combine measured parameters and theoretical computation, research on all time secondary field extraction at line 4 Mountain Tiger Zhoushan Zhejiang Province and Changchun Geology Palace room 327, and prove further that removing the primary field can improve the resolution and precision of shallow subsurface sounding and it can eliminate high resistivity shallow layer during apparent resistivity reversion.
    4. It is put forward to adopt three-point exponential approximation nonlinear smooth filter and logarithm equal-interval based on geometry average approximation after researching on improving later signal noise ratio of transient electromagnetic signal. Develop a set of software for data process and inversion based on “smoke coil” theory one dimensional fast inversion method.
    5. The exploration results, using self-made ATTEM instrument Changchun Caijia alive faultage and zhoushan Liandao Engineering Zhejiang Province, prove further that removing primary field can improve resolution of shallow subsurface sounding.
    Main innovation in this dissertation:
    1.It is proposed firstly removing primary field from measured all time transient electromagnetic response while considering transient process of receiver coil and extract all time secondary field and improve resolution and precision of shallow subsurface exploration.
    2.To the end of equally compression sampling, it is put forward firstly to process data using three-point exponential approximation nonlinear smooth filter and logarithm equal-interval in order to enhance later signal noise ratio of
    
    
    transient electromagnetic signal.
    3. From the point of inversion method and measurement system, break through only measuring attenuation part of transient response in the routine time-domain electromagnetic
引文
[1] Коваленик.В.К., Электроразведка ,Изд, МГУ,1984
    [2] Сидоров.В.А., Импульсная индуктивнаяЭлектроразведка, Недра, Москва,1985
    [3] Kaufman, A.A and Keller,G.V., Inductive mining Prospecting Part: Theory, Elsevier, 1985,11-138
    [4] Nabighian, M.N., Quasi-Static transient response of a conducting half-space——An approximate representation , Geophysics , 1979,Vol, 44 No.10, 1700-1705
    [5] Nabighian, M.N edal., Electromagnetic methods in applied Geophysics- Theory VolumeⅠ,Socicty of Exploration Geophysicsts 1988,313-503
    [6] Aderson, W.L., Nonlinear Least-squares inversion of transient sounding for a central induction loop system , U.S.G.S Open-File Report 82-240
    [7] Ravenhurst, W R. Microcomputer modeling of fixed-loop time-domain EM systems, Canada Crone Geophysics Limited Technical Note,1987
    [8] McNeill, J.D., EM37 Ground transient electromagnetic system: Calculated depth of exploration, Geonics Limited Technical Note TN-10,1980
    [9] Eaton, P.A,Hohmann, G.W., A rapid inversion technique for transient electromagnetic sounding, physics of the Earth and Planetary Interiors,1989,53
    [10] McNeill, J.D, Bosnar, M.C., comparison of geoelectric section obtained acrossed a fault with EM39 borehole induction logger and TEM 47 time-Domain system in central loop sounding mode TN-23,1988
    [11] Pellerin , L., etal., VETEM-A very early time electromagnetic system, In the proceedings of the symposium on the application of geophysics to engineering and environmental problems. 1994, SAGEEP’94, USA, 795-802.
    
    [12] Pellerin, L., etal., VETEM-A very early time electromagnetic system—the first year, In the proceedings of the symposium on the application of geophysics to engineering and environmental problems. 1995,SAGEEP’95, USA, 727-731.
    [13] Pellerin, L., etal., VETEM-A very early time electromagnetic system—year 2, In the proceedings of the symposium on the application of geophysics to engineering and environmental problems. 1996,SAGEEP’96, USA, 91-100.
    [14] Pellerin , L., etal., The electromagnetic integrated demonstration at the Idaho National Engineering Laboratory Cold Test Pit, In the proceedings of the symposium on the application of geophysics to engineering and environmental problems. 1997,SAGEEP’97, USA, 725-734.
    [15] Pellerin, L., Electrical and electromagnetic methods for environmental and geotechnical investigations in the year 2000. 2000, Invited review papers, 15th Workshop on Electromagnetic induction in the earth, 151-177
    [16] Wright, D.L., etal., A VETEM survey of a former munitions foundry site at the Denver Federal Center: in Proceedings for SAGEEP’2000, 2000, Washington D.C., 459-468.
    [17] Lin Jun., 1997, Development of high-resolution Geophysical instrumentation for engineering and environmental investigation, International Workshop on high-resolution Geophysics, Tucson, USA
    [18] 何继善,电法勘探的发展和展望,地球物理学报,1997,40(增刊)
    [19] 林君, 电磁探测技术在工程与环境中的应用现状 物探与化探,2000,vol,24,No.3:166-177
    [20] 林君,甚早期时间域电磁法-VETEM,国外地质勘探技术,1997,6,20-21。
    [21] 静恩杰 李志鹏 瞬变电磁资料处理和解释 1995,7:83-87
    [22] 静恩杰 李志鹏 瞬变电磁基本原理 1995,7:99-101
    [23] 蒋邦远,实用近区磁源瞬变电磁法勘探,地质出版社,1998
    [24] 牛之琏,时间域电磁法原理,中南工业大学出版社,1992
    [25] 朴化荣,电磁测深原理,地质出版社,1990
    [26] 徐建华,.层状媒质中的电磁场与电磁波.北京:石油工业出版社,1997
    
    [27] West.G.F, Macnae,J.C., and Lamontagne, Y., A time-domain EM system measuring the step response of the ground 1984,Geophysics,49, 1010–1026.
    [28] Ravenhurst, W.R., Step and impulse calculations from pulse type time- domain electromagnetic data , 1998, 68th Ann. Internat.,Soc. Expl. Geophys., 814–816.
    [29] 李貅,瞬变电磁测深的理论与应用,陕西科学技术出版社,2002.9
    [30] 付良魁,电法勘探教程,地质出版社,1983
    [31] A.A.Kaufman, G.V.Keller.频率域和时间域电磁测深.王建谋译.地质出版社,1987
    [32] (澳) 布塞利G等人编著 将邦远译,瞬变场法野外工作方法和数据处理解释手册,北京:地质出版社,1992
    [33] Raiche, A.P., The effect of ramp function turn-off on the TEM response of layered earth Exploration. Geophys,vol,15:37-41
    [34] Raiche, A.P and Spies, B.R., Coincident loop transient electromagnetic master curves for interpretation of two-layer earths Geophysics ,vol.46, No.1 :53-64
    [35]Spies,B.R, Raiche, A.P., Calculation of apparent conductivity for
    the Transient electromagnetic(coincident loop) method using an HP-67 calculator Geophysics ,vol,45:1197-1204
    [36] Knight,J.H ,Raiche, A.P., Transient electromagnetic calculation using the Gaver-Stehfest inverse Laplace transform method Geophysics ,vol,47:47-60
    [37] McNeill, J.D ,Edwards, R.N and Thorborn,M., Approximate calculation of the transient electromagnetic response from buried conductive half-space Geophysics , 1984,vol,49,No.7
    [38] McNeill, J.D., Application of transient electromagnetic techniques Geonics Limited Technical Note TN-7,1980
    [39] MacNae, J.C, An atlas of primary fields due to fixed transmitter loop EM sources ,Crone Limited Technical Note ,1987
    [40] Gallagher, P.R,Ward, S.H and Hohmann,G.W., A model study of a thin plate in free space for the EM37 transient electromagnetic system, Geophysics 1985,Vol,50,No.6
    
    [41]米萨克N.纳比吉安,勘查地球物理电磁法,赵经祥译,地质出版社,1992
    [42] Guimin liu., Effect of transmitter current waveform on airborne TEM response Exploration Geophysics 1998, Vol,29: 35-41
    [43] Smith, R.S and Whitaker, S.A., Line Current filtering of fixed-loop transient electromagnetic date,Geophysical Prospeeting,1993,41
    [44] Kenneth Duckworth, Edward S. Krebes., Depth sounding by means of a coincident coil frequency-domain electromagnetic system. Geophysics, 1997, Vol,62,No.1 :49-55.
    [45] Kozhevnikov, N.O and Nikiforov.S.P., Early time TEM response of an ungrounded horizontal loop - a new look, 2000, 62nd Mtg.: Eur. Assn. Geosci. Eng., Session:D0011
    [46]Fitterman, D.V and Anderson, W.L Effect of transmitter turn off time on transient sounding. Geoexploration, 24,131-146
    [47]Levy,G.M., Correction of measured transient electromagnetic filed over a layered half-spece Geophysical Prospeeting,1969,vol,17,82-101
    [48] Cull, L.J , Asten, M.J.and Cull, J.P., Reflection models and ramp response for downhole TEM data: Explor. Geophys., 1998,29, 320–323.
    [49] Grant,F.S andWest,G.F., Interpretation Theory in applied Geophysics McGrow-Hiil book company , 1965
    [50] Misac, N.Nabighian., Electromagnetic Methods in Applied Geophysics Volume 2, Chapter 6, Time Domain Electromagnetic Prospecting Methods, 1994:427-458
    [51] McNeill, J.D., The galvanic of Current component in telectromagnetic surveys, Geonics Limited Technical Note TN-17,1985
    [52] Kamenetsky, F and Chr.Oelsner., Distortions of EM transients in coincident loops at short time–delays Geophysical Prospecting, 2000,Vol,48:983-993.
    [53]李实,李创社等 瞬变电磁仪早期信号测量的程控接收天线,仪器仪表学报,2002,vol,23,No.2:192-211
    [54] Smith, R.S and Balchz, S.J., Robust estimation of the band-limited inductive-limit response from impulse-response TEM measurements taken during the transmitter switch-off and the transmitter off-time 2001,Geophysics,vol 65,No 2 476-481
    
    [55] 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,2001.6,23(2)
    [56] Macnae, J.C., An atlas of primary fields due to fixed transmitter loop EM sources 1980,Res. in Applied Geophys. No. 13.
    [57] Smith,Richard.S and Annan,A.Peter., Using an induction coil sensor to indirectly measure the B-field response in the bandwidth of the transient electromagnetic method : Geophysics,vol 65,No 5: 1489–1494
    [58]白登海, Maxwell.A.Meju等 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年,vol,46,No.5:697-704.
    [59] 陈明生, 田小波.,电偶源瞬变电磁测深研究 (五 )——实测感应电压转换成垂直磁场 .煤田地质与勘探,1999,27(5):63-65
    [60] 戴远东等,在瞬变电磁法大地电磁测量中高TcSQUID探头与常规探头的比较,低温物理学报,1996.2,18(1)
    [61] 肖田元,张燕云等编著 系统仿真导论,清华大学出版社,2000年
    [62] Christensen, N.B., 1995, 1D imaging of central loop transient electromagnetic soundings, JEEG, vol ,2,No. 1, 53-66.
    [63] Eaton, P.A,Hohmann, G.W., A rapid inversion technique for transient electromagnetic sounding,physics of the Earth and Planetary Interiors,1989,53
    [64] Newman, G.A., Anderson, W. L., and Hohmann, G.W., Interpretation of transient electromagnetic soundings over three-dimensional structures for the central-loop configuration. Geophys. J. R. astr. Soc., 1987,89, 889-914.
    [65] Efferso.F., Auken.E. and Sorensen.K.I., Inversion of band-limited TEM responses: Geophys. 1999,Prosp., Eur. Assn. Geosci. Eng., 47, 551-564.
    [66] Isaev, I.O., Epov, M.I., Antonov, E.Y. and Plotnikov, A.E., 2001, Interpretation of TEM Small-Loop Data, 63rd Mtg.: Eur. Assn. of Expl. Geophys., Session: P145.
    [67] Jopie, I.Adhidjaja, Gerald.W.Hohmann, and Michael.L.oristaglio., Two-dimensional transient Electromagnetic responses Geophysics,vol 50 No.12 p2849-2861.
    
    [68] Eaton, P.A and Hohman, Q.W Aaeveluation of electromagnetic methods in the presence of geologic noise Geophysics,1987,vol,52, No.8,1106-1126
    [69] Macnae,James.C , Lamontagnet,Y and West,G.F., Noise processing technlques for time-domain EM systems Geophysics,vol 49 No.7 :934-948
    [70] 程德福 近区磁源瞬变电磁法信号检测技术研究,博士论文,2003,
    [71]Crone PEM System Operation Manual,Crone Geophysics Limited ,1986
    [72]Geoex SIROTEM-Ⅱ System Operation Manual , Geex Pty.Ltd.,1980 Geophysics Limited ,1986
    [73]Geonics EM-37 System Operation manual , Geonics Limited ,1986
    [74] 李创社,瞬变电磁勘探中早期信号的检测方法研究,煤田物探,1999.4
    [75] Spies, B.R and Dwight, E.Eggers., The use and misuse of apparent resistivity in electromagnetic methods Geophysics,1986,vol,51 No.7 :1462-1471.
    [76] Ward, S. H., and Hohmann, G. W., 1987, Electromagnetic theory for geophysical applications, in Electromagnetic methods in applied geophysics. Edited by Misac N. Nabighian, SEG, v1, theory, p221.
    [77] Macnae, J and Lamontagne,Y., 1984, Discussion on “Comparison of apparent resistivity functions for transient electromagnetic methods” by A. P. Raiche: Geophysics, Vol ,49, 312-313.
    [78] Bartel, L., 2001, Effects of surface conductors on the TEM late-time apparent resistivity, 71st Ann. Internat. Mtg: Soc. of Expl. Geophys., 1431-1434.
    [79] Ravenhurst, W.R., Microcomputer modeling of fixed-loop time-domain EM systems,Canada Crone Geophysics Limited Technical Note,1987
    [80] Smith, R.S,Edwards, R.N and Buseill, G., An automatic technique for presentation of coincident-loop impulse response, transient electromagnetic data,Geophysics,1994,Vol,59,No.10
    [81] 宋先旺等,瞬变电磁法全期视电阻率,矿产与地质,1997.4,11(2)
    [82] 严良俊等,瞬变电磁测深一维反演及结果分析,江汉石油学院学报,1994.12,16(增刊)15(2)
    [83] 张小路,瞬变电磁测深数据的近似分析,桂林工学院学报,1999.7,19(3)
    
    [84] 罗国平等,瞬变电磁法磁场及其视电阻率研究,中国煤田地质,2000.6,12(2)
    [85] 李金铭,罗延中,电法勘探新进展,地质出版社,1996
    [86] 杨长福 林长佑 等 三维瞬变电磁近似反演 地震学报 2000 vol.22 No 4:377-384。
    [87] 林长佑,瞬变电磁晚期场资料的一维反演,西北地质学报,1994.6,
    [88] 长谷川健 .水平电气双极子によろ层状大地のスチツア应答と见挂导电率について .物理探矿,1985,38(3):21-31
    [89]Borland/ Inprise公司.,C++Builder5开发人员指南 [M].北京,机械工业出版社,2000.
    [90]清宏计算机工作室.,C++Builder编程技巧 [M].北京,机械工业出版社,2001
    [91] 李大海等,瞬变电磁法资料处理及解释软件包的研制与应用,中国煤田地质,1997.3,9(1)
    [92] 北京飞天诚信公司 ROCKEY4使用手册4.0版,2003
    [93] 白登海 王立凤 等 城市活断层探测中电磁噪声和环境干扰对浅层电磁方法的影响.地震地质,2002,vol 24:549-555.
    [94] 阎述,陈明生等,瞬变电磁法探测地下洞体的有效性,COAL,GEOLOGY,&,EXPLORTION,1999,4.
    [95] 陈明生,闫述等,二维地质体的瞬变电磁场响应特征,地震地质,2001,vol,23,No.2:252~ 256

© 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