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Imaging of a fluid injection process using geophysical data - A didactic example

机译:使用地球物理数据的流体注射过程的成像 - 一种教学例

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摘要

In many subsurface industrial applications, fluids are injected into or withdrawn from a geologic formation. It is of practical interest to quantify precisely where, when, and by how much the injected fluid alters the state of the subsurface. Routine geophysical monitoring of such processes attempts to image the way that geophysical properties, such as seismic velocities or electrical conductivity, change through time and space and to then make qualitative inferences as to where the injected fluid has migrated. The more rigorous formulation of the time-lapse geophysical inverse problem forecasts how the subsurface evolves during the course of a fluid-injection application. Using time-lapse geophysical signals as the data to be matched, the model unknowns to be estimated are the multiphysics forward-modeling parameters controlling the fluid-injection process. Properly reproducing the geo-physical signature of the flow process, subsequent simulations can predict the fluid migration and alteration in the subsurface. The dynamic nature of fluid-injection processes renders imaging problems more complex than conventional geophysical imaging for static targets. This work intents to clarify the related hydrogeophysical parameter estimation concepts.
机译:在许多地下工业应用中,流体注入或从地质形成中抽出或取出。精确地量化注入的流体改变了地下状态的地点,何时,何地,何时,何地,何时何地衡量。常规对这些过程的地球物理监测试图认为地球物理性质,例如地震速度或导电性,通过时间和空间改变以及对喷射流体已经迁移的位置进行定性推断的方式。延时地球物理逆问题的更严格的制定预测了地下在流体注射应用过程中的发展方式。使用时间流逝地球物理信号作为待匹配的数据,待估计的型号是控制流体喷射过程的多体态前进建模参数。适当地再现流程过程的地理物理签名,随后的模拟可以预测地下的流体迁移和改变。流体喷射过程的动态性质使成像问题比常规地球物理成像更复杂,用于静态目标。这种工作意图阐明了相关的水力学参数估计概念。

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