首页> 外文期刊>Petroleum exploration and development >Hydraulic fracture propagation geometry and acoustic emission interpretation: A case study of Silurian Longmaxi Formation shale in Sichuan Basin, SW China
【24h】

Hydraulic fracture propagation geometry and acoustic emission interpretation: A case study of Silurian Longmaxi Formation shale in Sichuan Basin, SW China

机译:水力压裂扩展几何特征和声发射解释-以中国四川盆地志留系龙马溪组页岩为例

获取原文
           

摘要

A series of laboratory fracturing experiments was performed on samples mined from an outcrop of the Silurian Longmaxi Formation shale in the Sichuan Basin, using a true triaxial fracturing simulation system. To reveal the characteristics of acoustic emission (AE) response in hydraulic fracture (HF) propagation, the HF propagation geometry obtained by specimen splitting and CT scanning technology was compared with the interpretation results of AE monitoring. And the difference of hypocenter mechanism between hydraulically connected and unconnected regions was further discussed. Experimental results show that the AE events distribution indicates well the internal fractures geometry of the rock samples. Numerous AE events occur and concentrate around the wellbore where the HF initiated. Sparse AE events were presented nearby bedding planes (BPs) activated by the HF. AE events tended to be denser where HF geometry was more complex. The hydraulically connected region was obviously distinct with the spatial distribution of AE events, which resulted in the overestimation of stimulated reservoir volume (SRV) based on micro-seismic mapping result. Both tensile and shear events occurred in the zone connected by the HFs, while only shear events were observed around BPs which were not hydraulically connected. Thus, the hydraulically connected and unconnected region can be identified in accordance with the hypocenter mechanism, which is beneficial to improve the accuracy of SRV evaluation.
机译:使用真实的三轴压裂模拟系统,对四川盆地志留系龙马溪组页岩露头采出的样品进行了一系列的实验室压裂实验。为了揭示水力压裂(HF)传播中声发射(AE)响应的特征,将通过标本分裂和CT扫描技术获得的HF传播几何形状与AE监测的解释结果进行了比较。并进一步讨论了水力连通区域和非连通区域的震源机制的差异。实验结果表明,声发射事件的分布很好地表明了岩石样品的内部裂缝几何形状。发生大量的AE事件,并集中在HF开始的井眼周围。稀疏的AE事件出现在由HF激活的褥垫面(BP)附近。在HF几何更为复杂的地方,AE事件往往更密集。水力连通区域明显与声发射事件的空间分布明显不同,导致基于微地震测绘结果高估了受激储层体积(SRV)。拉伸事件和剪切事件都发生在由HF连接的区域中,而在没有水力连接的BP周围仅观察到剪切事件。因此,可以根据震源机制来识别液压连接区域和非连接区域,这有利于提高SRV评估的准确性。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号