首页> 外文期刊>工程(英文)(1947-3931) >Maximum Magnitude of Seismicity Induced by a Hydraulic Fracturing Stage in a Shale Reservoir: Insights from Numerical Simulations
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Maximum Magnitude of Seismicity Induced by a Hydraulic Fracturing Stage in a Shale Reservoir: Insights from Numerical Simulations

机译:液压压裂阶段在页岩储层中诱导的最大幅度:数值模拟的见解

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摘要

A key unknown limiting assessment of risk posed by inducing anomalous seismicity during hydraulic fracturing is the potential maximum magnitude of an event. To provide insights into the variation in maximum magnitude that can be induced by a hydraulic fracturing stage, worst-case scenarios were simulated in 2D using coupled hydro-geomechanical models. The sensitivity of the magnitude to the hydro-geomechanical properties of the fault and matrix rock were quantitatively compared through parametric analysis. Our base model predicts a maximum event with moment magnitude (Mw) 4.31 and Mw values range from 3.97 to 4.56 for the series of simulations. The highest magnitude is predicted for the model with a longer fault and the lowest magnitude for the model with a smaller Young’s modulus. For our models, the magnitude is most sensitive to changes in the Young’s modulus and length of the fault and least sensitive to changes in the initial reservoir pressure (i.e. pore pressure) and the Poisson’s ratio.
机译:通过在液压压裂期间引起异常地震性构成的风险的关键未知评估是事件的潜在最大幅度。为了提供对可以通过液压压裂阶段引起的最大幅度的变化的见解,使用耦合的水力地理机械模型在2D中模拟最坏情况的情况。通过参数分析定量地比较了故障和矩阵岩石的大小与矩形地质力学性质的敏感性。我们的基础模型预测了一系列模拟的时刻幅度(MW)4.31和MW值的最大事件,范围为3.97至4.56。预测最高幅度,模型具有更长的故障和具有较小杨氏模量的模型的最低幅度。对于我们的模型,幅度对杨氏模量和故障长度的变化最敏感,并且对初始储层压力(即孔隙压力)和泊松比的变化最小敏感。

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