摘要
研究目的:在铁路勘探过程中,经常遇到采空区、软弱层等不良地质因素。对上述不良地质现象,地震映像法是一种有效的勘探方法。地下介质的复杂性决定了野外地震映像法采集波场资料的复杂性,资料解释和异常判别困难,有时甚至使方法失效。识别有效信号和干扰信号,可以提高资料的解释精度。研究结论:通过对实际模型的试算,有效地模拟了地震映像剖面。模拟剖面可以看到显著的物探异常,有效地反映了复杂结构中的波场形态和特征。研究表明,有限差分数值模拟不仅允许速度纵向变化,而且允许速度横向变化,更适用于实际模型,是一种行之有效的共偏移距剖面数值模拟方法。通过研究,可以更加准确地判定异常的空间位置和形态,提高探测精度,对实际的解释工作具有一定的指导意义。
Research purposes： In railway exploration process, we are often caught by bad geological factors such as goal, softlayer,etc. Under these unfavorable geological conditions, the seismic imaging method is an effective exploration method. The complexity of subsurface collection determines the complexity of the seismic wave field. The difficult of data interpretation and anomaly discrimination leads to the method fails sometimes. To differentiate effective signal and interference signals can improves the accuracy of data interpretation. Research conclusions：With the actual physical parameters, we effectively simulated the seismic imaging profile. On modeling profile ,we can see a significant geophysical anomaly, effectively reflecting the complex structure of the wave field in the shape and characteristics. The finite - difference numerical simulation method allows speed to change vertically and laterally, and better used on actual model. It＇ s effective for modeling common - offset profile. Through research, we can more accurately determine the anomaly location and shape, and improve the exploring precision. It has a certain significance to the interpretation of actual work.
出处
《铁道工程学报》
EI
北大核心
2012年第6期20-23,共4页
Journal of Railway Engineering Society
关键词
地震映像法
波动方程
数值模拟
提高精度
seismic imaging method
wave equation
numerical modeling
improving precision
