...
首页> 外文期刊>The Leading Edge >Hydraulic-fracturing-induced strain and microseismic using in situ distributed fiber-optic sensing
【24h】

Hydraulic-fracturing-induced strain and microseismic using in situ distributed fiber-optic sensing

机译:水力压裂引起的应变和微地震的原位分布光纤传感

获取原文
获取原文并翻译 | 示例
           

摘要

Hydraulic fracturing operations in unconventional reservoirs are monitored using distributed fiber-optic sensing through which physical effects such as temperature, strain, and microseismic activity can be measured. When combined with treatment curves and other reservoir information, these measurements give engineers more data to understand the effectiveness of a treatment program and make future reservoir management decisions. Distributed fiber-optic data are acquired within a borehole that is actively being fractured and is subsequently used as an observation well for treatments of a neighboring well. The large-aperture and finely sampled data acquisition provides a variety of measurements at different resolution scales as changes are induced in the reservoir. Distributed acoustic sensing microseismic events are observed with magnitudes above -2. The spatial distribution of events, up to 500 m from the observation well, allows us to estimate diffusivity and fracturing trends for nearby treatment wells. Microseismic events acquired using a standard three-component borehole tool provide insight into the type of events that can be observed only on one system or simultaneously on both systems. We correlate very low frequency (well below 1 Hz) strain-front behavior with the onset of microseismic events, as they are triggered by pore pressure and fracturing progress throughout the reservoir.
机译:非常规油藏中的水力压裂操作使用分布式光纤传感进行监控,通过该传感可以测量温度,应变和微地震活动等物理效应。当与处理曲线和其他储层信息结合使用时,这些测量值可为工程师提供更多数据,以了解处理程序的有效性并制定未来的储层管理决策。分布的光纤数据是在井眼中获取的,该井眼正在被积极压裂,随后被用作观测井,用于处理相邻井。由于在储层中引起变化,因此大口径和精细采样的数据采集可在不同的分辨率范围内提供各种测量结果。观察到的分布式声感测微震事件的幅度大于-2。事件的空间分布距观测井不超过500 m,这使我们能够估计附近处理井的扩散率和压裂趋势。使用标准的三分量钻孔工具获得的微震事件提供了对事件类型的洞察力,这些事件类型只能在一个系统上或在两个系统上同时观察到。我们将非常低频率(远低于1 Hz)的应变前行为与微地震事件的发生联系起来,因为它们是由孔隙压力和整个储层的压裂过程触发的。

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