首页 | 本学科首页   官方微博 | 高级检索  
     检索      

基于离散余弦变换的磁位谱分析及磁异常导数计算方法
引用本文:张凤旭,张凤琴,孟令顺,刘财.基于离散余弦变换的磁位谱分析及磁异常导数计算方法[J].地球物理学报,2007,50(1):297-304.
作者姓名:张凤旭  张凤琴  孟令顺  刘财
作者单位:1.吉林大学地球探测科学与技术学院,长春130026 2 吉林大学物理学院,长春130023
基金项目:大庆探区外围中新生代断陷盆地群演化与油气远景项目,面向21世纪教育振兴行动计划(985计划)
摘    要:针对提高磁异常导数的计算精度,提出磁位离散余弦变换谱的分析方法. 根据重磁位场的泊松公式,利用余弦变换给出磁位与磁场分量间的余弦变换谱关系,推导出磁异常n阶导数的余弦变换谱公式. 利用余弦变换法计算的无限长水平圆柱体磁异常水平和垂向一阶导数的最大误差分别为-028 nT/m、047 nT/m;水平一阶导数的误差一般在-357%~327%之间,垂向一阶导数的误差一般在-194%~188%之间;计算的磁异常一阶导数值与理论值大致重合,而且不受有效磁化倾角的影响. 而Fourier变换法计算的水平和垂向一阶导数最大误差分别为-1062 nT/m、1442 nT/m,计算曲线与理论曲线偏离大,受磁化倾角的影响也较大. 这说明与Fourier变换法相比,余弦变换法计算的异常导数精度高,而且具有良好的稳定性.

关 键 词:离散余弦变换  磁位  磁异常导数  计算精度  
文章编号:0001-5733(2007)01-0297-08
收稿时间:2005-12-29
修稿时间:2005-12-29

Magnetic potential spectrum analysis and calculating method of magnetic anomalyderivatives based on discrete cosine transform
ZHANG Feng-Xu,ZHANG Feng-Qin,MENG Ling-Shun,LIU Cai.Magnetic potential spectrum analysis and calculating method of magnetic anomalyderivatives based on discrete cosine transform[J].Chinese Journal of Geophysics,2007,50(1):297-304.
Authors:ZHANG Feng-Xu  ZHANG Feng-Qin  MENG Ling-Shun  LIU Cai
Institution:1.College of Geo_Exploration Science and Technology, Jilin University, Changchun 130026, China 2 College of Physics, Jilin University, Changchun 130023, China
Abstract:A method of magnetic potential spectrum based on the cosine transform is proposed in order to improve the calculating accuracy of magnetic anomaly derivatives. According to the Poisson equation of gravitymagnetic potential, we derive the relation of cosine transform spectrum between magnetic potential and magnetic field constituent and deduce the cosine transform spectrum formula of n degree derivatives using the cosine transform. The horizontal and vertical first derivatives of magnetic anomalies of an infinite cylinder are calculated by the cosine transform method, in which the maximum errors are - 0.28 nT/m and 0.47nT/m, respectively and the percent errors are generally within - 3.57 % - 3.27 % and - 1.94 % - 1.88 %, respectively except several data of the boundary and part are bigger because of remains of Gibbus effect. The calculating curve and theoretical curve are approximately coincident, and there is no influence by effective magnetic dip angle in computing. But the errors with the Fourier transform method are - 10.62nT/m and 14.42nT/m, there is large departure between the calculating curve and theoretical curve and evident influence by effective magnetic dip angle in computing. It indicates that the calculating accuracy of magnetic anomaly derivatives calculated by cosine transform is higher than Fourier transform, and the computing stability is excellent.
Keywords:Discrete cosine transform  Magnetic potential  Magnetic anomaly derivative  Calculating accuracy
本文献已被 CNKI 维普 万方数据 等数据库收录!
点击此处可从《地球物理学报》浏览原始摘要信息
点击此处可从《地球物理学报》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号