GSTDTAP  > 气候变化
DOI10.1029/2019GL086185
Seismic Moment Evolution During Hydraulic Stimulations
Bentz, Stephan1; Kwiatek, Grzegorz1,2; Martinez-Garzon, Patricia1; Bohnhoff, Marco1,2; Dresen, Georg1,3
2020-03-16
发表期刊GEOPHYSICAL RESEARCH LETTERS
ISSN0094-8276
EISSN1944-8007
出版年2020
卷号47期号:5
文章类型Article
语种英语
国家Germany
英文摘要

Analysis of past and present stimulation projects reveals that the temporal evolution and growth of maximum observed moment magnitudes may be linked directly to the injected fluid volume and hydraulic energy. Overall evolution of seismic moment seems independent of the tectonic stress regime and is most likely governed by reservoir specific parameters, such as the preexisting structural inventory. Data suggest that magnitudes can grow either in a stable way, indicating the constant propagation of self-arrested ruptures, or unbound, for which the maximum magnitude is only limited by the size of tectonic faults and fault connectivity. Transition between the two states may occur at any time during injection or not at all. Monitoring and traffic light systems used during stimulations need to account for the possibility of unstable rupture propagation from the very beginning of injection by observing the entire seismicity evolution in near-real time and at high resolution for an immediate reaction in injection strategy.


Plain Language Summary Predicting and controlling the size of earthquakes caused by fluid injection is currently the major concern of many projects associated with geothermal energy production. Here, we analyze the magnitude and seismic moment evolution with injection parameters for prominent geothermal and scientific projects to date. Evolution of seismicity seems to be largely independent of the tectonic stress background and seemingly depends on reservoir specific characteristics. We find that the maximum observed magnitudes relate linearly to the injected volume or hydraulic energy. A linear relation suggests stable growth of induced ruptures, as predicted by current models, or rupture growth may no longer depend on the stimulated volume but on tectonics. A system may change between the two states during the course of fluid injection. Close-by and high-resolution monitoring of seismic and hydraulic parameters in near-real time may help identify these fundamental changes in ample time to change injection strategy and manage maximum magnitudes.


领域气候变化
收录类别SCI-E
WOS记录号WOS:000529112700037
WOS关键词GEOTHERMAL RESERVOIR STIMULATION ; FLUID-INJECTION ; INDUCED EARTHQUAKES ; MAXIMUM MAGNITUDE ; APPARENT STRESS ; COOPER BASIN ; SITE ; MECHANISMS ; REGIME ; DEPTH
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
引用统计
文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/279736
专题气候变化
作者单位1.German Res Ctr Geosci GFZ, Geomech & Sci Drilling, Helmholtz Ctr Potsdam, Potsdam, Germany;
2.Free Univ Berlin, Dept Earth Sci, Berlin, Germany;
3.Univ Potsdam, Inst Earth & Environm Sci, Potsdam, Germany
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GB/T 7714
Bentz, Stephan,Kwiatek, Grzegorz,Martinez-Garzon, Patricia,et al. Seismic Moment Evolution During Hydraulic Stimulations[J]. GEOPHYSICAL RESEARCH LETTERS,2020,47(5).
APA Bentz, Stephan,Kwiatek, Grzegorz,Martinez-Garzon, Patricia,Bohnhoff, Marco,&Dresen, Georg.(2020).Seismic Moment Evolution During Hydraulic Stimulations.GEOPHYSICAL RESEARCH LETTERS,47(5).
MLA Bentz, Stephan,et al."Seismic Moment Evolution During Hydraulic Stimulations".GEOPHYSICAL RESEARCH LETTERS 47.5(2020).
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