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应用地球物理  2019, Vol. 16 Issue (1): 36-49    DOI: 10.1007/s11770-019-0748-3
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致密油岩石纵波频散及衰减特征研究:实验观测及理论模拟*
马汝鹏,巴晶,Carcione J. M. ,周欣,李帆
1. 河海大学地球科学与工程学院,地球探测研究所,南京211100;
2. Istituto Nazionale di Oceanografia e di Geofisica Sperimentale (OGS), Borgo Grotta Gigante 42c, Sgonico, Trieste 34010
Dispersion and attenuation of compressional waves in tight oil reservoirs: Experiments and simulations*
Ma Ru-Peng, Ba Jing, Carcione José Maria, Zhou Xin, and Li Fan
1 School of Earth Sciences and Engineering, Hohai University, Nanjing, 211100, China.
2 Istituto Nazionale di Oceanografia e di Geofisica Sperimentale (OGS), Borgo Grotta Gigante 42c, Sgonico, Trieste 34010, Italy
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摘要 非常规油气资源-致密油在中国有广泛分布,致密油储层孔隙类型多样、结构复杂。本文对12 块致密油岩石样本开展了超声波实验测量,根据记录的纵波波形,利用谱比法估算了岩石在饱和不同流体时的衰减,结果显示大部分致密油岩石样本在饱气状态下的纵波衰减强于饱水及饱油情况,并且,纵波衰减与岩石渗透率有较好的正相关性。基于扫描电镜分析结果,采用三重孔隙结构模型描述致密油岩石,正演模拟了致密油岩石的波传播特征。基于Biot 理论、Biot-Rayleigh 双重孔隙介质理论和三重孔隙模型对比讨论了致密油岩石的纵波速度频散和衰减规律,结果显示Biot 理论和Biot-Rayleigh 理论均无法解释该组致密油岩石样本的衰减特征规律,而采用三重孔隙结构模型的预测结果和实验结果能够达到很好的吻合。统计分析了致密油岩石的实验测量结果和模型参数,可推断在5–10%孔隙度范围内致密油岩石含更多的微裂隙,且在高孔隙度范围微裂隙尺寸更大。在不同孔隙度范围内,微裂隙和黏土包体体积比率相近,但微裂隙尺寸明显大于泥质尺寸,微裂隙体积模量低于泥质体积模量。
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关键词致密油岩石   结构非均质性   岩石物理实验   三重孔隙结构模型   纵波频散和衰减     
Abstract: We performed ultrasonic experiments in specimens from a tight oil reservoir. The P-wave attenuation of fluid-saturated specimens was estimated by the spectral ratio method. The results suggest that at ultrasonic frequencies, most specimens have stronger attenuation under gas-saturated conditions than at water- or oil-saturated conditions. The P-wave attenuation positively correlates with permeability. Scanning electron microscopy observations and the triple-porosity structure model were used to simulate the wave propagation. The P-wave velocity dispersion and attenuation are discussed on the basis of the Biot, Biot–Rayleigh double-porosity medium, and the triple-porosity structure models. The results suggest that the Biot and Biot–Rayleigh models cannot explain the attenuation, whereas the triple-porosity structure model is in agreement with the experimental data. Furthermore, we infer that microcracks are common in a porosity of 5%–10%, and the size of microcracks increases in samples with higher porosity. However, the volume ratios of microcracks and clay inclusions remain constant regardless of porosity variations. The size of microcracks is significantly larger than the clay inclusions, and the bulk modulus of microcracks is lower than the bulk modulus of clays.
Key wordsporosity   Biot   Rayleigh   wave   dispersion   attenuation   
收稿日期: 2018-11-07;
基金资助:

本研究由“江苏特聘教授”计划、国家自然科学基金项目(编号:41704109)和中央高校基本科研业务费项目(编号:2016B13114)资助。

通讯作者: 巴晶(Email: jba@hhu.edu.cn)     E-mail: Email: jba@hhu.edu.cn
作者简介: 马汝鹏,河海大学博士研究生。2016 年本科毕业于河海大学地质工程专业。2016年–至今,硕博连读于河海大学地球科学与工程学院地球探测与信息技术专业,主要研究方向为岩石物理、孔隙介质中波的衰减及频散特征等。
引用本文:   
. 致密油岩石纵波频散及衰减特征研究:实验观测及理论模拟*[J]. 应用地球物理, 2019, 16(1): 36-49.
. Dispersion and attenuation of compressional waves in tight oil reservoirs: Experiments and simulations*[J]. APPLIED GEOPHYSICS, 2019, 16(1): 36-49.
 
没有本文参考文献
[1] 付博烨,符力耘,魏伟,张艳. 超声岩石物理实验尾波观测中边界反射的影响分析[J]. 应用地球物理, 2016, 13(4): 667-682.
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