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面向深部地热岩体的弹性波逆时偏移成像方法OACSTPCD

Elastic wave reverse time migration imaging method for deep geothermal rock mass

中文摘要英文摘要

地热能作为一种清洁能源正受到全世界的日益关注,因此对于深部地热岩体的高精度成像格外重要.传统的弹性波逆时偏移方法是利用耦合纵横波直接成像,从而得到耦合波场的成像结果;然而这种方法可能会出现串扰假象,导致成像结果不够清晰;为了解决这个问题,采用基于解耦的弹性波方程,实现纵横波场的分离;通过利用内积成像条件,对两个典型的干热岩模型进行数值测试.结果表明,相较于耦合波场成像结果,基于解耦方程分离得到的弹性波成像剖面具有更清晰的同相轴,深部能量更加均衡,该方法能够实现对深部地热岩体的高质量成像.

Geothermal energy is gaining global attention as a clean energy source,underscoring the significance of precise imaging of deep geothermal reservoirs.The conventional elastic reverse time migration(E-RTM)technique relies on direct imaging of coupled P-and S-waves,which often leads to imaging artifacts and unclear images.In this study,we propose an approach based on the decoupled elastic wave equation to independently handle P-and S-wavefields.We apply this approach to two typical hot dry rock models using inner product imaging conditions.The numerical simulations demonstrate that the de-coupled elastic wave imaging profiles provide clearer event representations and a more evenly distributed energy profile in the deeper regions compared to imaging results obtained from coupled wavefields.This method showcases the potential for achie-ving high-quality imaging of deep geothermal reservoirs.

黄建平;杨秀金;张鑫;王扬州;陈亮;高建明

中国石油大学(华东)地球科学与技术学院,山东青岛 266580山东能源集团南美有限公司,山东青岛 266000

地质学

深部地热岩体弹性波成像纵横波分离逆时偏移

deep geothermal rock masselastic wave imagingseparation of P-and S-wavesreverse time migration

《中国石油大学学报(自然科学版)》 2024 (001)

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山东能源集团深层高温地热重大科技项目(SNKJ2022A06-R23);山东省海洋科技基金青岛海洋科学与技术国家试点实验室(2021QNLM020001);创新研究群体项目(41821002);国家自然科学基金优秀青年项目(海外)(ZX20230152);中国石油重大科技专项(ZD2019-183-003)

10.3969/j.issn.1673-5005.2024.01.006

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