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机构地区:[1]西安交通大学电子与信息工程学院,西安710049
出 处:《西安交通大学学报》2003年第2期215-218,共4页Journal of Xi'an Jiaotong University
基 金:教育部“教育振兴行动计划”资助项目.
摘 要:为提高瞬变电磁法的对地探测精度,从瞬变电磁场的传播特性和电磁响应特性两个角度考虑,提出了瞬变电磁成像方法:由野外实测磁场感应数据,经过反褶积和线性数字滤波求出波阻抗;用线性规划法求出每一微层走时所对应的反射系数序列,并以此为参数绘制成像结果图.对理论模型和实例资料的成像处理结果表明,采用瞬变电磁成像方法的成像处理结果比常规的瞬变电磁视电阻率处理剖面清晰、直观,大大增强了由瞬变电磁资料识别地下电性层状分界面的能力.In order to improve the prospecting precision to the earth of transient electromagnetic method (TEM), the idea of TEM imaging is proposed according to the characteristics of both electromagnetic wave propagation and response: the waveimpedance is calculated from observed data infield by the way of inversefaltung and linear digital filter; the sequence of reflection coefficients corresponding to every tinylever move time is calculated by the way of linear programming, and the imaging result section is drawn consequently. The imaging result obtained from theoretical model and real example indicates that the proposed method can improve greatly the ability to recognize the underground electric interface of TEM compared with the regular processed resistance section.
关 键 词:水平层状介质 瞬变电磁成像方法 瞬变电磁场 反射系数 电磁勘探 电磁响应
分 类 号:P631.325[天文地球—地质矿产勘探]
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