通过分布式声学传感器DAS的应变率测量来表征裂缝发育

Jin Tang, D. Zhu
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引用次数: 1

摘要

在多级水力压裂作业中,超大规模的泵注(高速率和体积)和地层的高非均质性(由于接触面积大)相结合,通常会导致复杂的裂缝生长,这是常规裂缝模型无法简单模拟的。由于缺乏对压裂机理的认识,使得水力压裂工艺的设计和优化变得困难。许多监测、测试和诊断技术已经应用于该领域,以描述水力裂缝的发展。分布式声传感器(DAS)测量应变率是复杂完井环境中裂缝监测的工具之一。DAS可以测量远场应变率,有助于裂缝表征、井间裂缝干扰识别和增产效果评估。许多现场应用表明,当附近的一口井被压裂时,DAS对观察井或周围的生产商有响应。建模和解释DAS应变率响应有助于定量绘制裂缝扩展图。在这项工作中,开发了一种方法来生成假设断裂系统的模拟应变率响应。物理区域包含一个因压裂而产生应变变化的处理井,以及一个沿其安装光纤传感器以测量裂缝扩展应变率响应的观测井。该工作不是使用复杂的裂缝模型来正演模拟裂缝扩展,而是从简单的二维裂缝扩展模型开始,为单条裂缝和多条裂缝提供相对合理和可接受范围内的假设裂缝几何形状。建立了位移不连续法(DDM)来模拟光纤传感器对岩石变形和应变速率的响应。在每个时间步,首先允许裂缝扩展,然后在裂缝接近观察井时估计应力、位移和应变场。然后,将应变速率计算为断裂扩展,生成断裂接近时的图形。扩展模拟监测了断裂扩展和应变速率响应。应变速率响应模式可用于识别裂缝发育。文中给出了不同压裂条件下的应变率响应实例。研究了注入速率分布与应变速率响应的关系,以展示利用DAS测量来诊断多级水力压裂的潜力。
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Characterize Fracture Development Through Strain Rate Measurements by Distributed Acoustic Sensor DAS
In multistage hydraulic fracturing treatments, the combination of extreme large-scale pumping (high rate and volume) and the high heterogeneity of the formation (because of large contact area) normally results in complex fracture growth that cannot be simply modeled with conventional fracture models. Lack of understanding of the fracturing mechanism makes it difficult to design and optimize hydraulic fracturing treatments. Many monitoring, testing and diagnosis technologies have been applied in the field to describe hydraulic fracture development. Strain rate measured by distributed acoustic sensor (DAS) is one of the tools for fracture monitoring in complex completion scenarios. DAS measures far-field strain rate that can be of assistance for fracture characterization, cross-well fracture interference identification, and well stimulation efficiency evaluation. Many field applications have shown DAS responses on observation wells or surrounding producers when a well in the vicinity is fractured. Modeling and interpreting DAS strain rate responses can help quantitatively map fracture propagation. In this work, a methodology is developed to generate the simulated strain-rate responds to assumed fracture systems. The physical domain contains a treated well that the generate strain variation in the domain because of fracturing, and an observation well that has fiber-optic sensor installed along it to measure the strain rate responses to the fracture propagation. Instead of using a complex fracture model to forward simulate fracture propagation, this work starts from a simple 2D fracture propagation model to provide hypothetical fracture geometries in a relatively reasonable and acceptable range for both single fracture case and multiple fracture case. Displacement discontinuity method (DDM) is formulated to simulate rock deformation and strain rate responds on fiber-optic sensors. At each time step, fracture propagation is first allowed, then stress, displacement and strain field are estimated as the fracture approaches to the observation well. Afterward, the strain rate is calculated as fracture growth to generate patterns as fracture approaching. Extended simulation is conducted to monitor fracture propagation and strain rate responses. The patterns of strain rate responses can be used to recognize fracture development. Examples of strain rate responses for different fracturing conditions are presented in this paper. The relationship of injection rate distribution and strain rate responses is investigated to show the potential of using DAS measurements to diagnose multistage hydraulic fracturing treatments.
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