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Location of Microearthquakes Sources at Passive Seismic Monitoring of Hydraulic Fracturing

机译:水力压裂被动地震监测中微震源的定位

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The paper discusses microseismic monitoring during oil well stimulation by hydraulic fracturing, an emergent technology used for hydraulic fracturing layer control. The passive monitoring is a new widely developing technology of HFL control. The main factor affecting the results of passive seismic monitoring is the event location accuracy. The passive monitoring acquisition system utilizes one three components seismic probe deployed into the observation well. To evaluate the location accuracy of induced events for one observation well we applied traditional kinematic approach based on picking of earthquake P- and S-waves arrivals. The influence of geometric parameters of geophones location in a borehole, their quantity, picking errors of waves arrivals on the accuracy of microearthquakes location is studied.rnA new method based on dynamic event location using observations in one borehole is proposed and realized. Examples of realization of the new method of location on synthetic examples for isotropic and anisotropic media for P- and S-waves are given. The method was also tested on real data with the known earlier source location (perforation effect prior HFL). The method allows us to automate a process of microseismic data processing at the hydraulic fracturing and increase reliability of results of passive monitoring.
机译:本文讨论了在水力压裂增产油井过程中的微震监测技术,这是一种用于水力压裂层控制的新兴技术。被动监控是HFL控制的一项新兴的发展广泛的技术。影响被动地震监测结果的主要因素是事件定位精度。被动监测采集系统利用部署在观察井中的地震探头的三个组成部分。为了评估一口观测井的诱发事件的定位精度,我们采用了基于地震P波和S波到达选择的传统运动学方法。研究了地震检波器在井眼中位置的几何参数,其数量,波到达的拾取误差对微震定位精度的影响。提出并实现了一种基于动态事件定位并在一个井眼中进行观测的新方法。给出了在P波和S波各向同性和各向异性介质的合成示例上实现新定位方法的示例。还使用已知的较早源位置(HFL之前的射孔效应)对真实数据进行了测试。该方法使我们能够在水力压裂过程中自动化微地震数据处理过程,并提高被动监测结果的可靠性。

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