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Large magnitude events during injections in geothermal reservoirs and hydraulic energy: A heuristic approach

机译:地热储层和水力能注入过程中的大事件:一种启发式方法

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The occurrence of induced seismicity during reservoir stimulation requires robust real-time monitoring and forecasting methods for risk mitigation. We propose to derive an estimation of M-max (here defined as the largest single seismic event occurring during or after reservoir stimulation) using hydraulic energy as a proxy to forecast the total induced seismic moment and to model the transient evolution of the seismic moment distribution (based on the Gutenberg-Richter relation). The study is applied to the vast dataset assembled at the European pilot research project at Soultz-sous-Forets (Alsace, France), where four major hydraulic stimulations were conducted at 5 km depth. Although the model could reproduce the transient evolution trend of M-max for every dataset, detailed results show different agreement with the observations from well to well. This might reveal the importance of mechanical and geological conditions that may show strong local variations in the same EGS. (C) 2014 Elsevier Ltd. All rights reserved.
机译:在储层增产过程中诱发地震活动的发生,需要鲁棒的实时监测和预测方法来减轻风险。我们建议使用水力能量作为代理来推导M-max(此处定义为在储层增产期间或之后发生的最大单个地震事件)的估计,以预测总诱发地震矩并为地震矩分布的瞬态演化建模(基于古腾堡-里希特关系)。该研究适用于在Soultz-sous-Forets(法国阿尔萨斯)的欧洲试点研究项目中组装的庞大数据集,该项目在5 km的深度进行了四次主要的水力增产。尽管该模型可以再现每个数据集的M-max的瞬态演化趋势,但详细的结果表明,不同井之间的观测结果存在不同的一致性。这可能揭示了机械和地质条件的重要性,这些条件可能在同一EGS中显示出强烈的局部变化。 (C)2014 Elsevier Ltd.保留所有权利。

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