首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Estimates of Individual Fracture Compliances Along Boreholes From Full-Waveform Sonic Log Data
【24h】

Estimates of Individual Fracture Compliances Along Boreholes From Full-Waveform Sonic Log Data

机译:沿着全波形Sonic Log数据沿着钻孔均匀的个体骨折的估计

获取原文
获取原文并翻译 | 示例
           

摘要

An important seismic attenuation mechanism in fractured environments is related to energy conversion into reflected and transmitted waves at fracture interfaces. Using full-waveform sonic (FWS) log data, we show that it is possible to quantify transmission losses across a set of fractures from time delays and amplitude differences of the critically refracted P-wave as compared to intact sections along the borehole. In the presence of fractures, the transmission coefficient associated with a given fracture is obtained by combining information on transmission losses from multiple receivers and source positions into a linear system of equations for all fractures intersecting the borehole. Fracture compliance is computed from the inferred transmission coefficient based on a linear slip model. For validation, we use synthetic FWS log data obtained from numerical simulations of wave propagation in a water-filled borehole surrounded by low-permeability rocks with discrete fractures. The methodology is then applied to field data acquired along boreholes penetrating multiple fractures in a granodioritic host rock. We show that our estimations of mechanical compliance are consistent with previously reported values, which were estimated for individual fractures intersecting one of the boreholes with a related method valid only for isolated single fractures. Comparison between our estimates of fracture compliance and transmissivity profiles from previous hydraulic characterizations of the fractures suggests that the proposed method may also allow to locate the most permeable fractures along a borehole, which, in turn, opens the perspective of enhancing the design and effectiveness of subsequent hydraulic testing and fracturing experiments.
机译:裂缝环境中一种重要的地震衰减机制与裂缝界面处能量转换为反射波和透射波有关。利用全波形声波(FWS)测井数据,我们表明,与钻孔沿线的完整剖面相比,通过临界折射P波的时间延迟和振幅差异,可以量化穿过一组裂缝的传输损失。在存在裂缝的情况下,通过将来自多个接收器和震源位置的传输损耗信息组合成与钻孔相交的所有裂缝的线性方程组,可以获得与给定裂缝相关的传输系数。根据基于线性滑动模型的推断传输系数计算断裂柔度。为了验证这一点,我们使用了FWS合成测井数据,这些数据是通过对充满水的钻孔中的波传播进行数值模拟获得的,钻孔周围是具有离散裂缝的低渗透岩石。然后将该方法应用于沿穿过花岗闪长岩主岩中多条裂缝的钻孔获取的现场数据。我们表明,我们对机械顺应性的估计与之前报告的值一致,这些值是针对与其中一个钻孔相交的单个裂缝进行估计的,相关方法仅适用于孤立的单个裂缝。我们对裂缝柔度和透过率剖面的估计值与之前对裂缝的水力特征进行的比较表明,所提出的方法还可以定位钻孔沿线最具渗透性的裂缝,这反过来又为提高后续水力测试和压裂实验的设计和有效性开辟了前景。

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