山东大学学报(工学版) ›› 2015, Vol. 45 ›› Issue (3): 48-57.doi: 10.6040/j.issn.1672-3961.0.2014.096
戚志鹏, 李貅, 赵威, 智庆全, 刘磊
QI Zhipeng, LI Xiu, ZHAO Wei, ZHI Qingquan, LIU Lei
摘要: 为避免地层导电性对核磁共振解释的影响,实现了考虑层状导电介质影响下的核磁共振一维正反演。利用层状导电介质的频域磁场响应对核磁共振激发磁场进行计算,求解过程中对核函数进行了改造,降低了其震荡性,使积分更容易实现,在此基础上实现了考虑电性影响的核磁共振一维正演。在反演解释方面,借助瞬变电磁法给出地电断面,利用超平面拟合算法实现了含水层含水率参数反演。将反演结果与商用软件反演结果进行对比,计算结果基本一致,且本研究算法具有更好的分层效果。
中图分类号:
[1] 林君,段清明,王应吉,等.核磁共振找水仪原理与应用[M].北京:科学出版社,2010. [2] 王鹏.均匀地电条件下地面核磁共振三维正演[D].武汉:中国地质大学, 2008. WANG Peng. Three dimensional forward modeling of surface nuclear magnetic resonance in uniformity medium[D]. Wuhan:China University of Geosciences, 2008. [3] 孙淑琴,林君,张世雄.导电性对地面核磁共振信号的影响研究[J].物探化探计算技术,2005,27(2):127-130. SUN Shuqin, LIN Jun, ZHANG Shixiong. Influence investigation of earth electrical conductivity on surface NMR signals[J]. Computing techniques for geophysical and geochemical exploration, 2005, 27(2):127-130. [4] 翁爱华,李舟波,王雪秋.层状导电介质中地面核磁共振响应特征理论研究[J].地球物理学报,2004,47(1):156-63. WENG Aihua,LI Zhoubo,WANG Xueqiu.A study on surface nuclear magnetic resonance over layered conductive earth[J]. Chinese J Geophys, 2004, 47(1):156-163. [5] HERTRICH M, YARAMANCI U. Joint inversion of surface nuclear magnetic resonance and vertical electrical sounding[J]. Journal of applied geophysics, 2002, 50(1-2):179-191. [6] BRAUN M, YARAMANCI U. Inversion of surface-NMR signals using complex kernel[C]//Proceedings of the 9th EEGS conference. Prague, Czech Repulic: EEGS, 2003:9. [7] 翁爱华,李舟波,王雪秋.地面核磁共振响应数值模拟研究[J].物探化探计算技术,2002,24(2):97-98. WENG Aihua, LI Zhoubo, WANG Xueqiu. Numerical simulation of surface NMR[J]. Computing Techniques for Giophysical and Geochenical Exploration, 2002, 24(2):97-98. [8] 翁爱华,王雪秋,刘国兴,等.导电性影响的地面核磁共振反演[J]. 地球物理学报,2007,50(3):890-896. WENG Aihua, WANG Xueqiu, LIU Guoxing, et al. Nonlinear inversion of surface nuclear magnetic resonance over electrically conductive medium[J]. Chinese J Geophys, 2007, 50(3):890-896. [9] 戴苗, 胡祥云,吴海波,等.地面核磁共振找水反演[J]. 地球物理学报, 2009, 52(10):2676-2682. DAI Miao, HU Xiangyun, WU Haibo, et al. Inversion of surface nuclear magnetic resonance[J]. Progress in geophysics, 2009, 52(10):2676-2682. [10] 林婷婷,慧芳,蒋川东,等.分层多指数磁共振弛豫信号反演方法研究[J].地球物理学报, 2013,56(8):2849-2861. LIN Tingting, HUI Fang, JIANG Chuandong, et al. Layered multi-exponintial inversion method on surface magnetic resonance sounding dataset[J]. Chinese J Geophys, 2013, 56(8):2849-2861. [11] 万玲, 林婷婷, 林君,等.基于自适应遗传算法的MRS-TEM联合反演方法研究[J]. 地球物理学报, 2013, 56(11): 3728-3740. WAN Ling, LIN Tingting, LIN Jun, et al. Joint inversion of MRD and TEM data based on adaptive genetical algorithm[J]. Chinese J Geophys, 2013, 56(11):3728-3740. [12] 翁爱华,王雪秋.利用数值积分提高一维模型电偶源电磁测深响应计算精度[J].西北地震学报, 2003, 25(3):193-197. WENG Aihua, WANG Xueqiu. Utilizing direct integration to enhance calculation accuracy of 1d electromagnetic response for current dipole source[J]. Northwestern Seismological Journal, 2003, 25(3):193-197. [13] 华军,蒋延生,汪文秉. 双重贝塞尔函数积分的值计算[J]. 煤田地质与勘探, 2001, 29(3):58-61. HUA Jun, JIANG Yansheng, WANG Wenbing. The numerical integration of dual hankel transformation[J]. Coal Geology & Exploration, 2001, 29(3):58-61. [14] 张伟,王绪本,覃庆炎.汉克尔变换的数值计算与精度对比[J].物探与化探,2010,34(6):753-755. ZHANG W, WANG X B, QIN Q Y. Research and application on numerical integration of Henkel transforms by digital filtering[J]. Geophysical & Geochemical Exploration, 2010, 34(6):753-755. [15] 戚志鹏,李貅,朱宏伟,等.大定源装置下瞬变电磁法视电阻率定义[J]. 地球物理学进展, 2011, 26(4):1350-1358. QI Zhipeng, LI Xiu, ZHU Hongwei, et al. Definition of apparent receptivity for center vertical component of large loop TEM configuration[J]. Progress in Geophysics, 2011, 26(4):1350-1358. [16] SUN Huaifeng, LI Xiu, LI Shucai, et al. Multi-component and multi-array TEM detection in karst tunnels[J]. J Geophys Eng, 2012(9):359-373. [17] WEICHMAN P B, Dong Rong Lun, RITZWOLLER M H, et al. A study of surface nuclear magnetic resonance inverse problem[J]. Journal of Applied Geophysics, 2002, 50(2):129-147. [18] GUILLEN A, LEGCHENKO A. Inversion of surface nuclear magnetic resonance data by an adapted Monte Carlo method applied to waterresource characterization[J]. Journal of Applied Geophysics, 2002, 50(2):193-205. [19] MOHNKE O, YARAMANCI U. A new inversion scheme for surface NMR amplitudes using simulated annealing[C]//Proceedings of the 61st EAGE Conference.[s.n.]:EAGE, 1999:262-280. [20] MOHNKE O, YARAMANCI U. Smooth and block inversion of surface NMR amplitudes and decay times using simulated annealing[J]. Journal of Applied Geophysics, 2002, 50(2):163-177. [21] LEGCHENKO A, EZERSKY M, GIRARD J-F, et al.Interpretation of magnetic resonance sounding in rocks with high electrical conductivity[J].Journal of Applied Geophysics, 2008(66):118-127. [22] BRAY C L, SCHALLER N C, IANNOPOLLO S L, et al. A study of 1H NMR signal from hydrated synthetic sands[J]. Journal of Environmental and Engineering Geophysics, 2006, 11(1):1-8. [23] GUILLEN A, LEGCHENKO A. Application of linear programming techniques to the inversion of proton magnetic resonance measurements for water prospecting from the surface[J]. Journal of Applied Geophysics, 2002, 50:149-162. [24] 李貅.瞬变电磁测深的理论与应用[M].西安:陕西科学技术出版社,2002. [25] 朴化荣.电磁测深法原理[M].北京:地质出版社,1990:1-10. |
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