煤储层各向异性地震波场模拟
李东会1 ,董守华1 ,赵小翠1 ,鲁磊2 ,张聪3 ,李淑杰4
1.中国矿业大学 资源与地球科学学院,江苏 徐州221008;2.中国矿业大学 安全工程学院,江苏 徐州221008;3.华北油田煤层气分公司,山西 晋城048000;4.长春理工大学 经济管理学院,吉林 长春130022
SEISMIC WAVE SIMULATION OF ANISOTROPY IN COALBED MEDIA
LI Dong-hui 1 , DONG Shou-hua 1 , ZHAO Xiao-cui 1 , LU Lei 2 , ZHANG Cong 3 , LI Shu-jie 4
1.School of Resources and Geoscience, CUMT, Xuzhou221008, China; 2.Faculty of Safety Engineering, CUMT, Xuzhou221008, China;3.CBM Branch Company of North China Oilfield, Jincheng048000, China;4.School of Economics and Management, Changchun University of Science and Technology, Changchun130022, China
摘要 对中国煤层的裂隙系统进行了系统分类;阐述了各类裂隙的主要成因。基于二维二分量各向异
性弹性波方程交错网格高阶有限差分法数值模拟,对各向同性介质模型和高裂隙密度(含干裂隙和饱和
水裂隙)煤层的二维层状模型进行了弹性波场数值模拟。结果表明:煤层含裂隙后与不含裂隙时相比,反
射时差的变化已不足以识别,但由于波速的改变会使煤层顶底、界面的波阻抗发生变化,从而引起波的
动力学特征的改变,AVO 现象尤其明显。含气和含水裂隙煤层中在x分量和z分量表现为极性相反
,而且含水裂隙煤层中的波速比含气裂隙煤层的波速要快。因此,应用各向异性理论研究煤层裂隙的
特征是可能的。
Abstract :In this paper, systematic classification was conducted for the fissure systems of China's coal
seams, and the main causes for the different types of fissures were described. Based on 2D, 2C
anisotropic elastic waveequation staggering grid highorder finitedifference numerical
simulation, the authors carried out the numerical simulation of elastic wave field for the isotropy model
and the water-saturated and dry media 2D layered model with fracturebearing coal seams of high
fracturing density. The results show that, in comparison with the fracturesfree coalseam, the
fracturesbearing coalseam has the following characteristics: the surge impedance of the boundary
plane at the top and the bottom is changed due to the change of wave velocity, causing the change of
dynamic characteristics of the wave. The AVO phenomenon is especially obvious. The characteristics of
x component and z omponent are opposite in dry fractural media and in watersaturated
fractural media, and the velocity of wave is faster in watersaturated fractural media than in dry
fractural media. It is thus thought that coalseam fractures are detectable by using anisotropy theory.
出版日期: 2010-10-15
基金资助: "973"国家重点基础研究发展计划项目(2009CB219603);国家科技重大专项项目
(2008ZX05035-005-003)
通讯作者:
李东会(1981-),男,河南省辉县人,现在为中国矿业大学博士研究生。研究方向为地震
勘探理论与方法和数值模拟,公开发表学术论文数篇。
引用本文:
李东会, 董守华, 赵小翠, 鲁磊, 张聪, 李淑杰. 煤储层各向异性地震波场模拟[J]. 物探与化探, 2010, 34(5): 604-609.
LI Dong-Hui, DONG Shou-Hua, DIAO Xiao-Cui, LU Lei, ZHANG Cong, LI Chu-Jie. SEISMIC WAVE SIMULATION OF ANISOTROPY IN COALBED MEDIA. Geophysical and Geochemical Exploration, 2010, 34(5): 604-609.
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