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

被引:0
|
作者
Commer, Michael [1 ]
Pride, Steve R. [1 ]
Vasco, Donald W. [1 ]
Finsterle, Stefan [2 ]
Kowalsky, Michael B. [1 ]
机构
[1] Lawrence Berkeley Natl Lab, Earth & Environm Sci Area, Berkeley, CA 94720 USA
[2] Finsierle GeoConsulting, Kensington, CA USA
关键词
ELECTRICAL-RESISTIVITY TOMOGRAPHY; GROUND-PENETRATING RADAR; ENSEMBLE KALMAN FILTER; JOINT INVERSION; HYDRAULIC CONDUCTIVITY; PARAMETER-ESTIMATION; BOREHOLE RADAR; TRANSPORT; FLOW; SIMULATION;
D O I
10.1190/GEO2018-0787.1
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
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In many subsurface industrial applications, fluids are injected into or withdrawn from a geologic formation.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.
引用
收藏
页码:W1 / W16
页数:16
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