韩复兴^1,,
孙建国^1,,,
王坤²
1. 吉林大学地探学院波动理论与成像技术实验室, 长春 130026
2. 吉林交通职业技术学院, 长春 130012

基金项目: 国家自然科学基金项目（41504084，41274120）资助


详细信息

作者简介: 韩复兴, 男, 1981年8月生, 陕西省西安市人, 2009年吉林大学地球探测科学与技术学院应用地球物理系博士毕业, 副教授, 主要从事地震波传播与成像方面的学习与研究.E-mail:hanfx@jlu.edu.cn

通讯作者: 孙建国, 男, 1956年生, 辽宁省丹东市人, 教授, 博士生导师, 主要从事地下波动理论与成像技术、钻孔电磁波法、地球物理中的天线问题及岩石物理学等方面的研究.E-mail:sun_jg@jlu.edu.cn

中图分类号: P631

收稿日期:2018-08-02
修回日期:2018-08-30
上线日期:2018-11-05

The applications of model smoothing based on partial differential equation in migration imaging

HAN FuXing^1,,
SUN JianGuo^1,,,
WANG Kun²
1. Theory of Ministry for Land and Resources, College for Geoexploration Science Technology, Jilin University, Changchun 130026, China
2. Jilin Communications Polytechnic, Changchun 130012, China


More Information

Corresponding author: SUN JianGuo,E-mail:sun_jg@jlu.edu.cn

MSC: P631

--> Received Date: 02 August 2018
Revised Date: 30 August 2018
Available Online: 05 November 2018


摘要
摘要:本文针对射线类偏移成像当中的速度模型光滑处理问题，借鉴数字图像处理当中的偏微分方程法，基于能量泛函，应用变分方法导出基于速度模型的偏微分方程实现射线类偏移成像当中的速度模型的光滑处理.由于偏微分方程法具有线性叠加特性、模型解的唯一性和局部特征保持性，因此，应用该算法可以实现基于原始速度模型空间结构的模型光滑处理.通过在原始速度模型以及光滑处理后的速度模型上计算速度的空间分布以及地震波走时、射线路径可以得出，偏微分方程法对速度模型的光滑处理能够很好地保持原始模型的空间结构，偏移成像结果也证明了该方法的实用性.
关键词: 偏微分方程/
模型光滑/
卷积算子/
偏移成像

Abstract:In view of the problem of velocity model smoothing in ray type migration imaging, by reference to partial differential equation method in digital image processing, and based on the energy functional, we derived the partial differential equations based on velocity model, using the variational method to achieve velocity model smoothing in ray type migration imaging. Because the partial differential equations have the characteristics of linear superposition, model solution uniqueness and local features retention, therefore, the application of the algorithm can be very good to keep edge characteristics and the characteristics smoothing of velocity model, without breaking the spatial structure of the original velocity model. By calculating the spatial distribution of velocity, the travel time, and the ray paths of the seismic waves on the original and smoothed velocity model, it can be concluded that the smoothing of the velocity model using PDE method is good for keeping the spatial structure of the original model, the results of migration imaging also prove the practicability of this method.
Key words:Partial differential equation/
Model smoothing/
Convolution operator/
Migration imaging



PDF全文下载地址:

http://www.geophy.cn/data/article/export-pdf?id=dqwlxb_14762